U. S. DEPARTMENT OF THE INTERIOR PROTOTYPE OIL SHALE LEASING PROGRAM OIL SHALE TRACT C-b INTERIM MONITORING REPORT SUPPLEMENT (November 1976 Through August 1977) Submitted to: Mr. Peter A. Rutledge Area Oil Shale Supervisor Conservation Division U. S. Geological Survey Grand Junction, Colorado Bye: C-b Shale 0il Venture Occidental Oil Shale, Inc., Operator Ashland Colorado December 16, 1977 BLM Library D-S5E%A, Building 50 Dei... *: Federal Center P. 0. Box 25047 4 Denver, CO 80225-0047 (O83 nathLius APSas oa a P tsta90 Sarwbe% i gags. : pa son Gs i; ~ES208, i ape . _ » 4 aS eS © echespiaas” som 2 sata usr MaRTT . ; over Jauquh., beat gveL -pacdmevo) Rie are oer vis at Bae ; A . a7 a roan | e mG “PR ad, ’ 7 7 ls : Sa ar: Y eee £ Per qr: rae a = Mal hh he = Mest i 7 . :03 best inidud epbefiud .A rot]! 1M Toetvisquce siste [10 sath moiervid noktevisenta - yeviue isotgotoso -.f , abstolo) . norton obsroloq? Bris | ~ 2) sb 40] ms D | o~ ty to . i. = xs Sell ; 7 7 at 7 @ INTRODUCTION The Environmental Baseline Period for Oil Tract C-b covered the period from November 1, 1974 to October 31, 1976. Results have been reported in 9 Quarterly Data Reports, 8 Quarterly Summary Reports, Annual Summary and Trends Report and a 5-volume Final Baseline Report, all submitted to the Area Oil Shale Supervisor. From November 1, 1976 through August 31, 1977 the C-b Tract has been under a period of suspension of the Federal Oil Shale Lease. The results from this period, known as the Interim Monitoring Phase, were reported in a data report submitted to the Area Oil Shale Supervisor on October 14, 1977. This report is a supplement to the Interim Monitoring Report and includes additional data and corrections not found in the previous report, due to data lag. For consistency with all previous quarterly reports an identical outline and tabbing have been followed in this report. Tabs are sub- divided as required for corrections or additions to the Interim Monitor- ing Report or the Final Environmental Baseline Report. All corrections will bear the same table and page numbers that were assigned to them in the text in which they previously appeared. Xe ~ as i & eb OF sib 9 suakyore ‘Ts. Anes on ASE: is tawofiot nved evet Qaiddet bye ent be a - hens nn. exwoqet xisooaw -due ete 2deT tor ine mitetal ef% of amok Fi bs enoisoeT102° LTA mont od beng tee " enn ee Qt BA 2 par ar 1 Soto ey. Sige R ie es 2% oe Eevivue ot we fea pore lait «it 10 PORRA 4 : egen tem oldaf. chor oft -yasd Fine t yi? foifa iz reat wit at - TABLE OF CONTENTS BY VOLUME NUMBER Volume Number Table of Contents II. ENVIRONMENTAL BASELINE MONITORING PROGRAMS B. Air Quality 1. Air Quality and Surface Meteorology 2. Low Altitude Meteorology References Final Baseline Report I C. Biology 1. Terrestrial Wildlife Studies 2. Aquatic Studies Tit. OfHER STUDIES B. Revegetation Program C. Microenvironmental Program ~ a duré sae en “m f f mergovs nod 143 spavell 7 ‘ rsh ord J 6In@ uN, { vv es ai w ‘ AIR QUALITY & SURFACE METEOROLOGY CORRECTIONS TO INTERIM MONITORING REPORT VOLUME I1 II B-1_ _Air Quality and Surface Meteorology Table/Figure No. Table II B-4a Table Table Table Table Table Table Table Table Table Table Table Table Table II ek ED sa Tt ig! II Tek ip ie. 1} If Tt B-5 B-6 27 B-8 B-9 B-10 Bat B-12 B-13 B-14 B-15 B-16 B-18 Figure. fi B-2 Table Il B-21 Taple ii B-Z 72 Description fexe Air Quality Summary, Trailer 023. This table summarizes air quality data maxima for the quarter June-August 1977. 1-, 3-, and 24-hour Max. Concentrations, SO, l-hour Max. Concentrations, SO, (second instrument) l-hour Max. Concentrations, H,S 24-hour Max. Concentrations, Particulates 3-hour Max. Concentrations, Total HC 3-hour Max. Concentrations, Non-Methane HC 3-hour Max. Concentrations, CHy l-hour and 8-hour Max. Concentrations, CO l-hour Max. Concentrations, NO l-hour Max. Concentrations, NO, l-hour Max. Concentrations, Oz Monthly Average Concentrations of All Gaseous Constituents Meteorological Summary: Wind Speed and Direction, Station 023 Wind Roses at 30' Elevation, Station 023 Solar Radiation Temperature and Relative Humidity for Station 023 11 B=a Page TH Ee IT Tt II ET II B-5 B-9a B-10 Bu B12 Bois B-14 B=i5 B-16 Bally B-18 B-19 B- 20 B-21 B-23 B=-25 B-27 B-28 THIS PAGE LEFT BLANK INTENTIONALLY II B-1 Air Quality and Surface Meteorology Air Quality Station 023, the precipitation gauges at Stations 020 and 023 and the MRI Mechanical Weather Station were utilized to provide air quality and surface meteorological data. References 1-10 containing basic data are included at the end of the air quality section. Table/Figure No. Description Page Table II B-2 Air Quality Summary, Trailer 023. II B-7 This table summarizes air quality data maxima for the quarter September-November 1976. fabilie «it B=5 Trailer 023 December 1976-February 1977 II B-8 Table II B-4 Trailer 023 March-May 1977 It B=9 Table II B-4a Trailer 023 June-August 1977 It B-9a Maximum Concentrations Table II B-5 1-, 3- and 24-hour Max. Concentrations, SO, II B-10 Table II B-6 1-hour Max. Concentrations , SO, (second instrument) II B-1l Table II B-7 l-hour Max. Concentrations, HS II B-12 Table II B-8 24-hour Max. Concentrations, Particulates II B-13 Table II B-9 3-hour Max. Concentrations, Total HC II B-14 Table II B-10 3-hour Max. Concentrations, Non-Methane HC II B-15 Table II B-11 3-hour Max. Concentrations, CHy II B-16 Table II B-12 l1-hour and 8-hour Max. Concentrations, CO PL B-17 Table II B-13 l-hour Max. Concentrations, NO II B-18 Table II B-14 l-hour Max. Concentrations, NO, II B-19 Table II B-15 l-hour Max. Concentrations, Oz II B-20 These tables summarize the maximum concentrations for each month to date. IP B-$ Table/Figure No. Table 11 B-16": Table {I B-17 Table II B-18 Table II B-19 Figure II B-2 Table II B-20 Table IT 5-21 Table II B-22 Table {I B-23 Table II B-24 thru 63 Table TI B-64 thru 81 Description Monthly Average Concentrations All gaseous constituents Meteorological Summary Monthly Vector Averages for Winds Wind Speed and Direction a. Station 023 b. Station 044 Wind Roses at Station 023 Precipitation Solar Radiation Temperature and Relative Humidity for Station 023 Temperature for Station 044 Wind Speed, Wind Direction, Temperature as hourly diurnal values for MRI station. data are obtained at 7-foct height. speed is also presented at 30-feet by utilizing the logarithmic profile as presented in the 4th and 5th Quarterly Summary Reports. 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LL/S/8 bye £L/92/8 i a 00:6T LL/S/8 gf" 00:20 LL/S7/8 72° LL/61/L 69° “LL-L2-9 PUB *LL-b2-9 “L2-O1-9 ‘L2-8-9 :SouTa y paaanod0 ¢729 UOTIwIS IB ounf 1OF XvW ANOY-yZ OU, ; { *00:£0 0 2£2-92-£ pur “00:10 O ££-2-£ ‘O0!P2 LL-T-£ ‘O0:E2 a LL-T-£ :sowTa y anol-T DULL ££-9T-T PUB *O0:02 @ LL-£-T ‘00:8T a L--£-T :SsoUT3 ¢ pasanodo ¢7¢9 snout ot) ie. , “00:TO 8 2é-£2-T PUB “OO: ¥2 OB Lé-22-T ‘O0:PT &@ LL-9T-T ‘00: 0 LL-P-T 00202 8 Lé-£-T “00:61 8 Ld-£-— ‘SOWT2 9 porindd0 070 uoTILIS IZ Axonuep oy Xvui ANoYy-T ai “LL-TE-ZT puw “21-61 -2E “22-01-21 ‘2L-6-21 » :sowyta p posznd20 ¢29 UOTILIS YL aaquasoq AOF XVM ANOY-YZ Oy, (soysuy) 100], (soysuy) [vaoL (S) LL/vt/S| L£L/St/v LL/T/S) £4/92/2 (1) o34Ud 20° 82° 62° 92° yr 0° SOYDUT) *XUY ANO]-pZ LL/21/9 LL/vt/S| LL/2t/P LL/T/£| LL/22/Z L2/61/21 o3nt] 1 oc” Lc. Re v0° SOYDUT) *XC\Y ANO|]-¥Z 00:2T 00:91 00:01 00:61 00:20 (LSW) own LL/¥2/9 LL/St/S} LL/1T/¥ LL/92/2 LL/01/21 ong 20° ome! | Ot° L0° £0° (soysuy) *Xujy 4Nno}j-T LL/21/9 LL/ST/S} LL/L2/b LL/22/2 /S2/21 o7eg 00:2T 00:61 00:12 00:20 00:€1 Cis) ony (2) 91 i yt* Ca 0° £0° 20° (soysuy) *XtY ANO]]-f TLLNOW (dud urna TuryFLom YILM poansroay) ¥SNOLIVIS OML JV NOLIN IORd dO AUVANNS 02-8 il 9TAPL (S) (v) (<) (2) (T) “*$20 uolaTIs 3” YLGT “9 toquiodog ple 070 UOTICIS Ie OLGT “ET ABqUOd9q TTIUM po ITITUT Jou sem OSes ures SuTyTtom yIIM uotaeqtdtaoud jo Jursoqwugyy 68°G. $2'6 NOTLV.LS [fk B-26 fabke bib —7b SOLAR RADIATION STATION 023 Total Daily Ave. Highest Daily Lowest Daily Month Langleys (Langleys) Total/Date Total/Date 11/26 6725 2202 307/1 5/13 12/76 5685 183.4 242/1 73/5 1/77 6043 194.9 376/25 54/5 2YUT 7850 280.4 409/27 92/22 S/T 7 10737 | 346.4 523/27 110/17 4/77 12870 429.0 598/10§24 90/19 5/17 16228 525<5 714/39§31 209/14 6/77 18590 619.7 744/19 381/7 WaT 14526 518.8 75/10 180/22 8/77 13970 450.6 674/1 172/47 The above values have not been modified to include radiation received during downtime (instrument calibration, computer downtime, etc.). IE B-27 ejyeg SuISSTW (2) ATuQ eieq [etz1eg = (T) (3) “Say ATInoY ‘uM * TOY Nd Tofefofol sume (fol efofo falar o (%) “UTW ATAnoy ‘uM “TOY (%) *xeW ATInoy ‘*umY * Toy le (ig ) o8ei1o0Ay ATANOL] ‘oinzetoduoy, eis ) umwtuty ATIno}] ‘9injze1odusy, (J ty) unuTxEy ATANO}] ‘ain er1oduoy, 4 2% eS ee OSPLOAY (3y8TOH 3005 O¢) €70 uoTzeIS ALIGIWNH SALLVISY GNV FUALVYEdWAL = AUVWWNS TVOISOTOUOSLAN €c-d Il SLIeL II B-28 LOW ALTITUDE | METEOROLOGY CORRECTIONS TO INTERIM MONITORING REPORT VOLUME Ii II B-2 Low Altitude Meteorology Table/Figure No. Description Text Figure II B-3 Quarterly and Annual Wind Roses for the Meteorological Tower 100' Elevation Gust Analysis No. of 5-Minute Samples Table II B-82 a.) 50) Level Table II B-82 b. .100' Level Table’ 1T-B-82 Gee 200m Level Table II B-83 Average Hourly Stability Classes for the Meteorological Tower and Pyranometer Table II B-84 Meteorological Summary: Stability Class Frequencies (%) Wind. Persistence at Specified Stability Table If B-126a Monthly Values for Each Stability Class 41265 August 1977 Table Tl B-127 Ten Month Summary, November 76 - =132 August 77 lable IF B=-135 Cumulative Summary Since November 1974 =158 Mal ala Page I B-89 EI B-96 ii B-91 ie B=92 iP B-93 II B-94 B= I5 II B-138a to 138f II B-139 to 144 It B=145 to 150 THIS PAGE LEFT BLANK INTENTIONALLY II B-2 Low Altitude Meteorology Low altitude meteorological tower data are obtained at 8', 30', 100', and 200' for wind direction and speed, relative humidity, and temperature. Barometric pressure and daytime solar radiation are obtained at ground level. Temperature differences are obtained between the 30' and 100' levels and between the 30' and 200' levels. Basic low altitude meteorological data through August 1977 are contained in Refs. 1-10 at the end of this section. Table/Figure No. Description Page Figure? Ii |B=5 Wind Rose Diagram it B-90 This figure presents the wind roses for the 100' level of the meteorological tower for the quarter. fabte if B=82 Gust Analyses Cumulative number of 5-minute samples from November 1, 1974 thru August 1977. an SOLnE- II B-91 bes 100 £t2 Ii B-92 e. 200 ft! II B-93 Table II B-83 Atmospheric Stability II B-94 This table presents Pasquill-Gifford average hourly atmospheric stability class for each month. Ranges of dT/dz (variation of tem- perature with height) corresponding to each class are defined on the table. The sources are the temperature difference from 200' to 30' on the meteorological tower, designated DT2 corrected for wind speed (30') and the pyranometer. Table II B-84 This table shows the stability class frequency II B-95 distribution for each month. it 5-389 QUARTERLY WIND ROSE - 100’ LEVEL SEPT. °76 - NOV. °76 Total 3 of Calms Distributed (3.263) Total No. of 5-Min. Samples - 21165 QUARTERLY WIND ROSE - 100' LEVEL APRIL '77 - MAY '77 Total $ of Calms Distributed (].08%) Total No. of S-Min. Samples - 15080 Wh, ee Bits, Is QUARTERLY WIND ROSE - 100’ LEVEL DEG mOmee FEB. 77 A Total % of Calms Distributed (2.94%) = Total No. of S-Min. Samples - 15629 Oo Pe = 20% ae 20% 15% WIND SPEED (MPH) “ y vA at <3 7-12 18-24 hi S% Sal 12-18 a ANNUAL WIND ROSE - 100' LEVEL SEPT '76 - AUGUST '77 Total $ of Calms Distributed (2.11%) Total No. of 5-Min. Samples - 66955 mil, i as QUARTERLY WIND ROSE -100"' LEVEL JUNE '77 - AUGUST '77 | Total ¢ of Calms Nistributed (0.66%) Total No. of 5-Min. Samples - 15(81 ais Figure II B-3 METEOROLOGICAL TOWER 7GC’ ELEVATION QUARTERLY AND ANNUAL WIND ROSES 1975-1977 II B-90 Table II B-82 GUST ANALYSIS - NO. OF 5-MIN. SAMPLES \ ae 30 Ft. Level WIND SPEED RANGE (MPH) (WS, -WS.) ToE=.No. Month 36-40 41-45 46-50 TOTAL Expectation P (exceeding WS,) * Missing Data ii B-91 Expectation | Table II B-82 GUST ANALYSIS - NO. OF S-MIN. SAMPLES b. 100 Ft. Level WIND SPEED RANGE (MPH) (WS, -WS.,) Tot. No. of 5-Min. Month 36-40 41-45 46-50 51-35 56-60 61-65 Samples TOTAL 219/550 * Missing Data TE B-92Z Table II B-82 GUST ANALYSIS - NO. OF 5-MIN. SAMPLES eG. 200 Pe. Level WIND SPEED RANGE (MPH) (WS,-WS.) Month 36-40 41-45 46-50 St=55 56-60 61-65 Samples Nov. '74 1 8239 Dec. '74 5088 Jai. “475 2 7036 Feb. '75 z 6338 May. "75 L 5324 Apr: S75 2 7452 May '75 1 8102 June "75 3 6848 July '75 4 7619 Aug. '75 1 7694 Sept.'75 1 7203 Oct. "75 2 7932 Nov.. “975 1 7791 Dec As 2 7191 Jan. "76 4376 Feb. '76 3 7811 Mar. 7/6 4 7754 Apr. '76 3 6729 May '76 1 6920 June '76 Z ddd July '76 Aug. '76 2 7549 Sept. '76 1 7129 (Ves eee A 1 7113 Nov. '76 6558 Dec. '76 i 7203 Jan.."77 7385 BH 226,281 Expectation P (exceeding; 1.5027 x WS.) tog * Missing Data Ebb =95 Table II B-83 AVERAGE HOURLY STABILITY CLASSES Temperature Differences Between 200 ft. and 30 ft. on the Met Tower (Adjusted for Wind Speed) SOURCE: a4 eS — Pyranometer (Daylight Only) SOURCE : : “Partial Data Onl IMissing Data Unstable Class y 2No Data. (Lightning strike) - (D] Neutral Stable Class Key: Ti °B-=94 Table II B-84 METEOROLOGICAL SUMMARY: STABILITY CLASS FREQUENCIES (%) Source: Met. Tower! (30' to 200°) ’ Pasquill- dT/dz Range! Stability pepiity cless 1974 1975 Anmal Class (°C/100m) Nov.2 Dec.2 Jan. ‘Feb. Mar. Apr. May June July? Aug. Sept. Oct. Mean A <-1.9 8.5 1.0 ot 12.0 7.4 8.6 0.0 2.4 5.8 8.1 6.1” B -1.9 to -1.7 S65 4.4 10.3 235-59 | S0KG 25.6 85.75 1925 23.4 20.6 18.1 Cc 17) tonal 5 4.1 2.4 16.3 6.9 9.3 6.9 14.3 6.1 5.0 5.7 7.0 D -1.5 to -0.5 33.0 43.4 60.9 36.3 30.0 27.0 Os0 y 2528 V5.4" 92853 535-1 E -0.5 to +1.5 SES) SNS 11.4 TSeL NZL 18.0 03064 17-5 24.4 18.6 21.1 F >1.5 US sSie 1220 0.0 See 10.6 13.9 0.0 29.7 28.0 18.7 14.6 Total Percentage 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 Pasquill- dT/dz Range? Gifford for this Stability Stability Class 1975 1976 Annual Class (°C/100m) Nov. Dec. Jan. Feb. Mar. Apr. May June July Aug. Sept. Oct. Mean A <-1.9 15.6 18.8 Zante alsjets} 19.4 9.5 7/65) 4.6 10.3 7.4 1321-91556 14.0 B -1.9 to -1.7 19.7 20.7 ZS mice: 27.0 7a 26.3 17.4 30.5 18.4 255) 2056 22.6 Cc -1.7 to -1.5 6.9 7.4 5.6 7.7 7.9 9.7 6.0 10.0 5.6 6.7 6.1 5.6 Yorl D -1.5 to -0.5 Za Z1S5 1656) 9355.7 28.7 S552 21.0 SZe7, 14.1 27.6 Wfosy tbe 24.4 E -0.5 to +1.5 2209) 2365 2120'- F1S.8 15.6 17.0 15.6 17.6 19.5 23.0 20s) we 2iaz 19.5 F >1.5 Abts 72 8.1 10.6 6.9 1.4 6.9 13.6 17.6 20.0 16.9 Weak 7Aloal 12.6 Pasauill- dt/dz Range™ Gifford for this Stability Stability Class 1976 1977 Annual Class (°C/100m) Nov. Dec. Jane brebs Mar. Apr. May Jume5 July®> Aug? Sept. Oct. Mean A <-1.9 18.6 1255 18.0 12.9 12.9 12.6 5.9 O37 15552 B =9) CO) da, 19.8 20.7 BE = 747057 21.6 29.6 13.3 14.8 21.6 Cc =e7. tO = 155 4.3 feat 6.8 Hos 7.9 8.1 9.12 se Ur D -1.5 to -0.5 i255 16.2 ZO Sie ele 30.1 19.0 46.6 S525 22.5 E -0.5 to +1.5 27.4 exe 25a ROS 19.3 18.1 17.8 20.6 22.6 F >1.5 17.4 20.0 10.4 Sir 8.2 12.6 Mae 20.6 12.8 Total Percentage 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 100.0 1 adjusted for wind speed Data are suspect and, therefore, not included 3 Partial data “ Averaged from January-October, excluding July Missing data Averaged from November-July IT B-95 WIND PERSISTENCE AT SPECIFIED STABILITY: Table/Figure No. Description Page Tables II B-85 Monthly Values for Each Stability II B-97 | =126£ Class to-156f fables 11 °B- 127 Ten Month Summary, November 1976 - II B-139 2132 August 1977 to-144 Tables II B-133 Cumulative Summary Since November II B-145 eae 1974 to- 150 Note: No stability class data were calculated for June 1977 or for July 1977 Ii B-96 ‘STABILITY IND PERSISTENCE AT SPECIFIED i STABILITY A Max, DurATION HRS» AS DEPAAA AAAS Aa) SONTONINOONE [eels MONTH August 1977 = Ta ” Lu ” ” = ” ey = eon Lid Lu Lut ice) [7e) Ww (7a) ”Y aS a3 AS DERECTION NV II B-138a Ni Wino PERSISTENCE AT Spectriep STABILITY - STABILITY B IT B-138b SANA VONTH ___August 1977 __ tC ™ ™ ™ = = ™ (op) NS NS — SS N \O Max, DURATION at a DIRECTION A OFECI Pep OPABLe drs WIND PERSISTENCE SraBILITY C za = i ee MED i E DiRECTION | i -B-135S8e WIND FERSISTENCE AT SPECIFIED STABILITY STABILITY D ~ os a —_ ae) Aug MonTH E \ Max, DURATION HRs, DIRECTION - Pegi wi Nh WA AIATATATATA eee S/ a7 30/77 ae | 8/ 9750/77 ae \ aM \ iT B-138d | POHRYsIIYIee MI YreLbL ily yvinvirtris Wii STABILITY E t 1977 Au MONTH —= ‘ (=) 28 DIRECTION | II B-138e STABILITY WIND rERSISTENCE AT SPECIFIED STABILITY F uy co ~s r 1 ~Q kH KH ONE IRANI ANONICER oh DN ron) eS ae : WW : > 2 4 ee Max, DURATION ~ DIRECTION | NE ENE ESE SE SSE DIRECTION _—, — E r Anwh -— -— <= Y oe tw —- --— SES om Plax, DURATION - Hes, — Dae wn +! — wn aa — = ! oO ' ~ OV Nh ra) ~ ~ \ al ! Sy ON r ~s OV 1 ™~! ~~) STABILITY A MonTH Nov, 1976 to Aug 1977 3 15-16-76 > po jee) 1 ~ ~) { ul e ' — te 1 ~!] ~! ROMANS Ranh 2-897). (1) The wind pattern of ESE-ESE-E-E- ESE- ESE* ESE was recorded as 5 hrs. @ ESE rand Z hrs. -@ E for January. II B-139 WLW POROLOICNLO AL GCUIFICU IJIADILIIT STABILITY B II B-140 2=26-77 1 i Ti-23-76 — { ™ ™ ™ ' ‘ ™ N re | ' ' ' — Wy N NS \O ™ ™ \O ™ ' ™ 1 co ! \O ct ™ H 1 N ra N ' as at reo N ro \O ™ ™ ™ NS ' ! ™ WwW ' N GN ' sr Ln rH MONTH _Nov. 1976 to Aug. Sate eG 1-28-77 Sa gee 2-22-77} 12-19-76 lO 1-8-77 2-25-77 Max, DURATION “IND PERSISTENCE AT SPECIFIED STABILITY STABILITY C ‘ flax, DURATION tRECTION | iv h eee MonTH Nov. 1976 fp August 1977 TE {B-141 WIND rERSISTENCE AT SPECIFIED STABILITY STABILITY J CM ~~ op) 4 : xt () pis) ‘oO ™ n (= S © a I ES — = Max, DURATION DIRECTION = \: II B-142 STABILITY E Max, DURATION NOH 7 MONTH Nov. 1976 to Aug. DIRECTION E \V\ n (ae 22 2 rae \ \ JAE) =25-77 Be ee 5 5 a. 2 Z : La 2 ate, ae Ti 6 -T-11 S= 50-77 8-29-77 5 te se \ te pe te WIND rERSISTENCE AT OPECIFIED oTABILITY STABILITY F ™ ™ Oo: rc F Z e) a) \O ™ n ce S oO Ga 3 = FE = = S| ae §\ pae = = ae ee DIRECTION 3 7-13-76 5 s ie II B-144 er ee Prat 6 Loa es ee STABILITY A ™ ~ oO ra bt =i = i a ™ a eH ns @ i= © S 5 Z & , DURATION Max (1) The wind pattem of ESE-ESE-E-E- ESE-ESE-ESE was recorded as 5 hrs. . @ ESE and 2 hrs. E ey E for January 5-75 I=] _-< ae (1) Z 5 7- II B-145 STABILITY B Max, DuRATION DIRECTION ™ ™ (op) ra =| 2G { = ™ nD ro S {e) aq = BRS» Tyre (1) The wind pattern o: NNE-NE-NNE-NE-NNE was recorded as 4 4 Pe, ae ay ee 3 3(1 ae ee Bee eos Paget 8-4-76 s 9-27-75 NINE @ NNE and @ NE for March '77. S tirs: 2. hese =a 4 Be cae II B-146 STABILITY C Aug 1977 November 1974 - MONTH Hrs Max, DuRATION on rr ae & Se Lu oO: neal f = ae 16, 2 ie i acl ths i i Lil Lu iS) 2 Ra Aug. 1977 MONTH November 1974 - of S-S-S-SSE- SSE-SSE-S was credited as 3 hrs. @ SSE ag (2) The wind patte: 4 hrs. @ S. (3) The wind patte: 2 NNE NE ENE of SSWv-SSW-S-S c was credited as @ SSW an S-SSW-SSW-SSW- 5S. 3.hrs.)€ Ghrs- a 8-30-76 ]12-17-76 cc li Be 3 ESE SW ce gs 12-25-76 Va ay / 7) is ai pl ae 6-5-75 7S 3 7-76 2 j=) iva) ah pQ i bt » €o Fa texas 2 ris Kent . ei ae . RPORATION DCN 77-100-484-7-171-05 (100-152) AIR MONITORING REPORT FOR G=-b SHALE OFL PROJECT SUB 97 7 Report No. 35 EXOeEtober 11.977 Presented to: G-p. Shale O01) Project United Bank Tower Denver, Colorado 80202 il B-1940 \ 8500 Shoal Creek Blvd./P.O. Box 9948/Austin, Texas 78766 /(512)454-4797 mADIAN CORPORATION jee JG ese VI. TABLE OF CONTENTS Page GENERAL DESCRIPTION OF AIR MONITORING PROGRAM--------- II B-1949 DESCRIPTION OF INSTRUMENT SYSTEMS--------------------- 1951 A. Air Quality Instrumentation----------------------- “1951 B Gallitonsetilen Pee eSeiies a4 Me Ss =S= SS se 5 ogee eo -1952 C. Data Acquisition System--------------------------- -1954 D. Meteorological Instrumentation-------------------- =1955 MICROMETEOROLOGICAL AND TERRAIN FEATURES-------------- Sis fel OPERATING TIME ANALYSIS FOR EACH SITE----------------- | -1963 MCNTHLY METEOROLOGICAL SUMMARY------------------------ -1967 A. Summary of the Meteorological Conditions over North America during July 1977-------------------- *=1967 B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during July 1977----------------------------------------- =1969 ¢. Summary of the Meteorological Conditions in the Oil Shale Tract C-b Region during July 1977--- suo 0 DATA PRESENTATION AND SUMMARY------------------------- -1974 II B-1941 RADIAN CORPORATION TABLE I TABLE I1 TABLE III LIST OF TABLES DOWNTIME HOURS FOR C-b SHALE OIL PROJECT le of = pA fen Site 023--------------------------------~---- Sate (2 ya a a a a ee ee ee ee ee FEDERAL AND COLORADO STANDARDS -------------- AVERAGES FOR JULY 1 THRU 31 Buerogen. Oxides QUO )aaos- ss - Pesos oas Nitric Oxide (NO) -------------------~-------- Nitrogen Dioxide (NO,)---------------------- Sulfur Dioxide (S02) ------------------------ PY eaome Cea — = === = —— pS ss Sea aS ne ee Se a Sulfur Dioxide (S0,)------------------------ BWeh SAIN skegehate Felela a) 210 | ae ee Non-Methane Hydrocarbons-------------------- Carbon Monoxide----------------------------- Barometric Pressure------------------------- Total Precipitation------------------------- Particulate----------------------~---------- Wind Speed---------------------------------- Wind Direction------------------- bo eee ae Relative Humidity--------------------------- Temperature--------------------------- ys eee iP B-1987 Page -1965 RADIAN CORPORATION LIST OF TABLES (contd) Page TABLE IV DAELY AVERAGES FOR JULY 1 THRU 31 Nitroren Oxides (NO, )s—o-oSa- 2p See 425-5 >= II B-1985 Nitcre Oxide. (NO) - ~~ ~~ > a aa -1985 Nitrogen Dioxide (NQ,)---------------------- -1985 Sulfur Dioxide (S02) ------------------------ Missing Pyranometer-- --------- +--+ ern Missing Sulfur Dioxide (S02)------------------------ Missing Total Hydrocarbons-------------------------- =1987 Methane------------------------------------- -1987 Non-Methane Hydrocarbons -------------------- Oey Carbon Monoxide----------------------------- -1988 Ozone- -------------------------------------- -1988 Barometric Pressure------------------------- ; -1988 Total Precipitation------------------------- —IS59 Particulate--------------------------------- -1989 Wind Speed---------------------------------- -1990 Wind Direction------------------------------ -1991 Temp erature--------------------------------- 1992 Relative Humidity--------------------------- =1993 TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR JULY 2 THRU 31 Nieroten Oxides) (lO j= —--o-=—— = - aa =s =a -1995 Nitric Oxide (NO) --------------------------- -1996 Nitrogen Dioxide (NO, )---------------------- -1997 Sulfur Dioxide (S0O,)------------------------ -1998 Pyranometer---------------------- eer -1999 Sabian, Diode (SOs) =o == —2=— ae eee -2000 Total Hydrocarbons-------------------------- -2001 Mepnane= =e eos os bee tee -2002 Nom-Methane Hydrocarbons------------=------— -2003 Gazbon Monoxide=—==-=—->---—=----_ = = = 22 = -2004 Ozone- -- ------------------------------------ - 2005 Barometric Pressure—-——-—--=-—--=--—--=—-_- === 2006 i B-1943 RADIAN CORPORATION LIST OF TABLES. (contd) Page TABLE V (contd) TABLE VI TABLE VII Total Precipitation------------------------- II B-2007 Wind Speed - Wind Direction----------------- -2008 Temperature-----------------~--------------- -2009 Relative Humidity--------------------------- -2010 THE FIVE MAXIMUM INDEPENDENT SLIDING AVERAGES FOR JULY I THRU St Nitrogen Oxides-----------------~------------ =Z012 Nigeria Ueda ee ee eee Nitrogen Dioxide-------------~--------------- -2012 Sulfur Dioxide------------------------------ =2045 Total Hydrocarbons -------------------------- -2014 jie F al iis eS a SB SEE EE 72015 Non-Methane Hydrocarbons-------------------- -2016 Carbon Monoxide----------------------------- -2017 Carbon Monoxide- 8-hour--------------------- -2018 Ozone- -------------------------------------- 2019 DERARE ema SS Se SS ee ee ee -2020 FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION Ni Cropen, Cxedes “NO jena -2022 Nitric Oxide---------------~---------------- -2023 Nitrogen Dioxide (NO,)---------------------- -2024 Sulfur Dioxide (S0O,)------------------------ -2025 Sulfur Dioxide (S0,)------------------------ -2026 Total Hydrocarbons -------------------------- =20Z7, Methane-- ----------------------------------- -2028 Non-Methane Hydcocarbons---- 2. se ese a= ------ -2029 Caron Monoxide- ----------------------------- -2030 Ozone- -------------------------------------- -2031 II B-1944 RADIAN CORPORATION LEST OF TABLES (Ccontd) TABLE VIII DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Oxides------------------------------ Nitric Oxide--------------------------------- Nitrogen Dioxide----------------------------- Sulfur Dioxide------------------------------- Sulfur Dioxide-----------------=------.------ Total Hydrocarbons--------------------------- WE SY a Ee Non-Methane Hydrocarbons --------------------- Carbon Monoxide------------------------------ Precipitation---------~---~------------------ Wind Speed 20) HaaPsSeboaos oo eSs Se oo soo SSeS eee ae OO) Bese SS SeeSe 26s sae eS SSeS Ses DOG) Sei Ses se oS BOO Se Se Wind Direction 80 (pects s—5-— = oe eee eae ooo eee ees BAG \0 Saed = 2) a a II B-1945 RADIAN CORPORATION Lio, OF) TABLES. (eontd) Page Solar Radiation-------------------~----~------- II B-2060 Relative Humidity---------------------------- -2061 Barometric Pressure-------------------------- -2062 Nitrogen Oxides------------------------------ ~2063 Nitric Oxide--------------------------------- -2064 Nitrogen Dioxide----------------------------- -2065 Sulfur Dioxide------------------------------- -2066 Sulfur Dioxide------------------------------- Missing Total Hydrocarbons --------------------------- -2067 Methane---------------------- (eee ---------- -2068 Non-Methane Hydrocarbons--------------------- -2069 Carbon Monoxide------------------------------ -2070 OZON Cm — 3 = = en er rn nn en nn en === === -2071 Hour iseilotal Pecetps male one === oe Wind Speed at 8 feet------------------------- -2073 30 feet------------------------ -2074 100 feet----------------------- -2075 900 ~fiet< <2 ene santas = osec5e- -2076 Wind Direction at 8 feet--------------------- -2077 30 feet------------------------ -2078 100 feet----------------------- -2079 200 feet------------~------------ - 2080 Temperature at 8 feet-~---------------------- -2081 30 feet-------------------~----- -2082 100 feet----------------------- =Z083 200 feet----------------------- -2084 jeleGeleyen sues ealiel 1a gsi Sy -2085 II B-1946 RADIAN CORPORATION List JOF FABLES (Ceontd) Page Solar Radiation----------------------------- II B-2086 Relative Humidity FSU a Sag SS a I tgp i pega a -2087 Stability Class Determination Using Pyranometer Recording----------------------- -2088 APPENDIX A - STABILITY WIND ROSE DIAGRAMS---------------- -2089 8-foot level - Stability Class A------------ -2093 Class B------------ -2094 Class C------------ -2095 Class D------------ -20S6 Class E------------ -2097 Total-------------- - 2098 30-foot level - Stability Class A----------- -2099 Class B------------ -2100 Class C------------ -2101 Class D------------ -2102 Class E------------ -2103 Total-------------- -2104 100-foot level - Stability Class A---------- -2105 Class B------------ -2106 Class C------------ -2107 Class D------------ -2108 Class E------------ -2109 Total-------------- -2110 200-foot level - Stability Class A---------- =74 4d Class B------------ -2112 Class C------------ -2113 Class D--~---------- -2114 Class E------------ -2115 Total-------------- =~Z116 Pie b-oay RADIAN CORPORATION LIST OF TABLES (contd) Percertaze for 8-foot 30-foot 100-foot 200-foot Page of Occurrence of Wind Direction level---------------------------- IT B-Z1i7 level---------------------------- =Z2118 level---------------------------- -Z119 level-------------------~--------- -2120 Il B-1948 RADIAN CORPORATION E GENERAL DESCRIPTION OF AIR MONITORING PROGRAM Radian Corporation, under contract to the C-b Oil Shale Project, is performing the data compilation and reporting of air quality and meteorological data at one monitoring site in Northwest Colorado. The site measures and records concen- trations of particulates, sulfur dioxide, oxides of nitrogen, hydrogen sulfide, total hydrocarbons, methane, and carbon monoxide. A 200-foot meteorological tower provides wind direction, wind speed, temperature, and relative humidity data at four levels (8, 30, 100, and 200 feet). Other meteorological variables measured at the tower site are insolation, barometric pressure, and precipitation. Figure I shows the configuration of the monitoring station. The station provides a sturdy and protective covering for the monitoring equipment. I] B-1949 NOILVLIS ONIYOLINON 79 NOILVYNDIANOD ‘I WUNOLA SIVYYOLS AYILIVA . . CJ e, Py ~ ‘ : ee <---> f-- ——— zl 2) KOON ITLL0a aw) i hea ey | ! ¥aunaK0o| Vauv INSHNULSHT Ovi | | | | ee aans {1% waayaanzf aNotN | 3DV M aay ngs i} Sa\s | = ULV OLIaZ Ig jeans mou lTeie | lee ET O 5 ULV OUAZ Id (B-1950 RADIAN CORPORATION Loe DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle and continuously monitors both NO, and NO. A SuUbDCrTaction Ci1rcuLtein sbhe Lnstrument provides a-continuous NG> output, bUE TS net wsed in-Radian"s system.~ NOz is cal= culated once a second by the computer by subtracting the NO value from the NOx value, thus avoiding any drift which might occur in the NO, output of the instrument. This instrument has a minimum detectable sensitivity of 5 ppb (parts per billion) and a linearity of +1%. Sulfur dioxide is measured with the Meloy SA185-2A analyzer while hydrogen sulfide is measured with the Meloy SA185-2 analyzer. The hydrogen sulfide analyzer uses a Meloy Model S0O7-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H,S-1 hydrogen sulfide scrubber. The Model SA185-2 is a continuous analyzer and utilizes the flame photometric principle of operation. The minimum detectable sensitivity for the Model SA185-2 is 5 ppb with a linearity of +1% and the minimum detectable sensitivity for the Model SA185-2A is 2 ppb with a linearity of 1%. Ozone is measured with a Meloy Model OA350 analyzer. This instrument, based on the chemiluminescent principle, pro- vides continuous measurement of ozone. The minimum detectable Senstteavacy 25 08S ppp.and the Jinearity is “21%. Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument, which uses a plume ionization detector, has a Minimum detectable sensitivity of 5 ppb for all three components. The Model 8200 works on a five-minute cycle, i.e., one air sample is analyzed every five minutes, and the results are dis- played for five minutes via a sample and hold circuit. ib B-195l RADIAN CORPORATION The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, through which a constant air flow is provided by an air pump rated at 60 cfm at 0" head pressure. The manifold has sampling ports to which 1/4" teflon lines to the instrument are connected. All joints in the sampling system are secured by O-ring compression fittings. The manifold is contained in a heated (100°F) chamber to prevent condensation of moisture. The teflon lines from the manifold to the instruments are insulated with 1/8" wall thickness rubber tubing. The trailer has four heavy duty high volume particu- late samplers (Hi-Vols). Fiberglass filter paper is used for the collection of particulate samples, after which each filter is brought to a controlled humidity before weighing. Each Hi- Vol has a flow recorded to permit correction for changes in air. flow as the filter becomes loaded’ with particulates. Each Hi- Vol runs for a 24-hour period (midnight to midnight) and is turned on and off by the computer. The Hi-Vols, which were manufactured by Radian, were designed following guidelines re- commended by the Environmental Protection Agency. In addition to the normal Hi-Vol particulate samples, a duplicate Hi-Vol sample is collected every sixth day on special filter paper for trace element analysis. Once each quarter these samples are composited and analyzed for gross radioactivity and trace element content. B. Calibration Procedures The trailer contains a Meloy Model RAD-1 calibration ULES This Tnstrument provides a. zero sairosluppiy. SO>p—span eas from an SO, permeation tube, and NO span gas obtained by precisely te p-LO52 RADIAN CORPORATION diluting bottled NO span gas. The computer-controlled calibration of all instruments is automatically performed once atday., ‘shach Instrument is first switched to zero’; the ‘computer monitors the output of each channel and takes a new zero reading after a stable zero signal has been reached. This zero reading is compared by the computer to the zero reading obtained 24 hours betore, and if «a dritce in excess of 10 ppb has occurred, an excess Zerg Gdrict light for the channel in question is turned on on the System Status Panel. Next, span gas is supplied to each channel and the computer decides when a stable span value has been reached. This value is recorded and compared to the previous day's value >> Am excess span drift light on the System Status’ Panel is turned on if a drift exceeding 10 ppb occurs. The instruments are then seturned co *che™moni tor mode-and- after two minutes the “eom= puter resumes data taking. The bottled NO gas used at each site was obtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO, analyzers. The SO, permeation tubes were manufactured by Metronics Association, Inc. Their output has been verified by comparison to the output of National Bureau of Standards tube 10-42. Both SA185 analyzers in each trailer are calibrated with the SO, from the permeation tube. This instrument responds to the number of sulfur atoms per molecule; thus, SO, can be used to calibrate both the H2S and SO, monitors. The Model 0A350 ozone analyzer has its own calibration system which provides a zero check and a span check. The ozone calibration system is verified by comparison to a calibrated ozone generator maintainec in Radian's laboratory in Rifle. Tt B-1953 RADIAN CORPORATION The Model 8200 total hydrocarbon, methane, and carbon monoxide analyzer is calibrated with undiluted span gas obtained from AirCo's Rare and Specialty Gas Division. This span gas con- tains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. The Model 8200 is zeroes with air from a Bendix Model 8834. zeronalreunit. Im additions, the instrument. is ‘ebectronically re-zeroed at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. Gos. Data Acquisition System The basis of the data acquisition system is a Data General NOVA 1200 minicomputer. The NOVA, which has a basic cycle time of 1.2 psec, is equipped with automatic program load and power fail/automatic restart features. The computer utilizes 16K 16-bit words of core memory. Analog-to-digital conversion is accomplished via an ADC built by Radian Corporation. The input/output unit for the system is Texas Instrument's KSR 733 keyboard/printer. This model teletype provides keyboard entry and hardcopy printed output. The data are also recorded on a cassette magnetic tape unit with three drives. The cassette unit is utilized for program storage and loading as well as for recording. To reduce wear on mechanical parts, the power to the teletype and cassette units is turned on only when the unit(s) is (are) to be used. Several important functions in the instruments as well as in the computer and the trailer are monitored by means of lights on a System Status Panel. These data lights are written onto cassette tape to monitor the complete status of the system every five minutes. The Data Acquisition System also monitors the presence of 100V power from the power lines. In its absence, the computer, which is powered by batteries, switches all trailer TP B=1954 RADIAN CORPORATION systems to battery-provided power. If the line voltage is restored before the batteries are discharged to a specified level, the trailer system is switched back to line power. D. Meteorological Instrumentation 200-Foot Meteorological Tower The tower has instrumentation at four levels: 8 feet, 30 feet, 100 feet, and 200 feet. At all four levels, there are: wind speed, wind direction, and temperature and relative humidity sensors in a power-aspirated radiation shield. Temperature difference thermistors (also in power-aspirated radiation shields) and their associated circuitry take lapse rate measure- ments for the 30-foot to 100-foot layer and the 30-foot to Z00-foot Jliayer.- In addition, .this site, has .a,.Precision, Spectral Pyranometer, a barometer, and a tipping bucket rain/snow gage. The wind direction and speed apparatus used at each measurement level of the tower is the Model 1074-2 wind sensor by Meteorological Research, Inc. (MRI). This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This sensor is rugged, with an all-weather coaxial cup and damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. The wind sensors on the tower have been specially treated with a black paint which will promote warming of the exposed surfaces of the sensor and thereby reduce ice and snow accumulations on the moving parts of the apparatus. The specifications on the Model 1074-2 are as follows: ki B-1955 RADIAN CORPORATION Wind Speed Starting Threshold: 0.75 mph. Response Distance: 18 feet (63% recovery). Flow Coefficient: 7.9 feet/Revolution. Accuracy: +0.4 mph or 1% (whichever is greatest) Wind Direction Starting Threshold. 90°73 mph - Delay Distance: 4 feet (50% recovery). Damping Ratio: 0:5 te 0.6. Accuracy (540° system): +1%. Range 5.0 to 540... The relative humidity and temperature sensors are mounted within a power-aspirated radiation shield at each tower level. All aspirators and sensors are of the Model 840 Series by MRI. The aspirated shielded housing is designed to provide maximum radiation protection to the sensor. Ambient air is drawn into the shield and across the sensors at approximately 15 feet per second. This intake air is essentially sampled from a hemispherical space which is approximately 3-inch radius from the tube opening. Speed of the incoming air at the perhiphery of this hemisphere is approximately 1 mph. The temperature sensor is comprised of a dual thermistor and resistor network. This circuit provides a linear resistance change with an air temperature change. The relative humidity sensor is placed alongside the temperature elements inside the shield where it is exposed to a constant flow of air. Circulation to both sides of the sensing element produces accurate monitoring with a good response time. The specifications on the sensing ele- ments are as follows: it B-1956 RADIAN CORPORATION Temperature Accuracy: +0.25°C. Range: -50°C to +50°C. Humidity Accuracy: £3.07 RH. Range: 0% to 100% Relative Humidity. Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot and the 30-foot to 200-foot layer. The thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The use of separate thermistors and circuitry to measure AT allows £6m much greater accuracy and resolution in the measurements, which is necessary for stability assessments. Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot level. All of these AT thermistors are mounted within power-aspirated radiation shields. The specifications on the AT instrumentation are as follows: Accuracy: +0.1°C. Range of AT Circuit (Lower Level-Upper Level): +9F° to -9F°. All instrumentation, except at the ground level, is mounted at the end of 12-foot retractable booms. These booms are 3-inch box beams which are on rollers and can be retracted to the instrument platforms for instrument maintenance. The meteorological tower itself is a 200-foot Rohn Model 80 Guyed Tower, designed for 40 pounds per square foot wind Load with = of radial ice, per ELA Standard RS-222-B, to Iie B- 1957 RADIAN CORPORATION support four levels of meteorological equipment. The material consists of tower sections with a tapered base, three retractable booms 12-feet long, three outside work platforms, an inside ladder for climbing, two base ground kits and one anchor ground kit. The cable-type Safety Climbing Device consists of a cable and attachment mechanisms with a locking sleeve and safety belt. The tower is lighted and painted according to FAA specifications. The signals from the tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of the tower. After signals have been converted to analog signals, they are fed into a junction box, also at the tower base, where they are assimilated into one coaxial cable. The signals are then run underground within 3" PVC conduit to the A-to-D assembly, where they are processed. The transmitters are shielded and insulated from the elements. The signal cable is run underground in PVC conduit in order to minimize damage from the weather or from various rodents in the region. The auxiliary equipment at the tower site consists of a heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model P511-E unit by Weather Measure. In the case of this gage, the durability and reliability of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all- purpose precipitation sensor. This gage may be used to measure both snowfall and rainfall. An insulating cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The thermostatic control is adjustable from 0 to 35°C. Snow falling into the inlet funnel is melted. The resulting water (from rain or snow) drains into a precision tipping bucket mechanism which activates a mercury switch each time the bucket fills and tips... The gage is .constructed. of durable tconsosion-— resistant materials to provide many years of service. The Tt B-1956 { RADIAN CORPORATION specifications for this gage are as follows: Orifice: 8 inches. Calibration.) 07019inch.. Aecuracy:, 0.5), (Calibrated at 0.5. in/hr). Sensor: Chrome-plated tipping buckets. Switch: Mercury, 0.l-second closure. Heat Control: Thermostat adjustment, 0 to 95°63 The barometer is the B242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly proportional to pressure. The specifications on this instrument, which is mounted inside the monitoring trailer at the site, are as follows: Range: Specially designed for the 100 millibar interval from jZ> mililibars to. $25 millibars . Resolution: Infinite. Linearity: +0.5 millibar, over the 100 millibar interval. The pyranometer at the site is the Eppley Precision Spectral Pyranometer. This instrument is used for the measure- ment of sun and sky radiation totally or in defined wavelength bands. The pyranometer is levelled and mounted atop a wooden stand 4% feet from the ground surface. Care has been taken to eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: Sensitivity: 5 mv. per cal/cm°/min. Independence: 300 ohms. Temperature dependence: Sensitivity constant to within +l percent over the ambient temperature range from -20 to +40°C.. II B-1959 RADIAN CORPORATION Linearity: Response linear up to intensities of 4 ‘eal en*/ min. Response time: 1 second (i/e signal). All instrumentation is factory-calibrated and is field- calibrated at various intervals. Sling psychrometers are used to calibrate the humidity sensors; known temperatures and/or resis- tances are used to calibrate the thermistors; and an rpm cali- brating unit is used to calibrate the anemometers. The wind direction instrumentation is aligned to true north (reference direction) by means of a surveyor's transit. II B-1960 RADIAN CORPORATION FEL. MICROMETEOROLOGICAL AND TERRAIN FEATURES The Piceance Creek Valley and C-b Shale Oil Tract are Situated such that many microscale meteorological phenomena affect the region where the ambient air monitoring unit is located. Trailer 023 and its associated 200-foot meteorological tower are located atop a plateau to the south of the valley, high enough to be affected mostly by gradient flow conditions. The elevation at the meteorological tower site (Trailer 023) is 6940 feet above sea level. The largest gradients in eleva- tion in this area, of course, occur at the Piceance Creek Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. The Piceance Creek Valley decreases in elevation from east to west in this area, so that nighttime katabatic cold-air drainage flows advect from east to west. Site 023 is approximately 2.5 miles south of the Piceance Creek Valley. This location is relatively high com- pared to its surroundings, with the nearest point having an eleva- tion greater than 7000 feet being .5 miles to the south of the tower. The tower itself is on the top of a small knoll located between Scandard and Sorghum Gulches. Because of its location and the irregularities of the surrounding terrain, meteorological patterns are varied here. Wind instrumentation is mounted at four levels of the meteorological tower: 8 feet, 30 feet, 100 feet, and 200 feet. The top level of the tower generally remains in gradient wind flow. That is, the winds at that level are normally generated IT B-1961 RADIAN CORPORATION by synoptic-scale features and are usually separated from terrain ‘ features and micrometeorological circulations. Occasionally, a weak anabatic flow influence is experienced. However, such is not the case with the three lowest measurement levels. To varying degrees, these levels are influenced by both the katabatic and anabatic circulation cells. However, when strong pressure gradient forces exist in the region and the synoptic-scale wind flow is strong, all four tower levels will reflect a gradient wind flow as the winds increase in strength and height. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries rapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. In the Piceance Creek Valley, the terrain is fairly grassy and flat, with steep valley walls on either side. Surface winds are normally rather light in this valley unless channeling effects occur. During clear nights with rather light pressure gradient- induced winds, rapid radiational cooling will occur in the region because of the barren nature of the terrain and the generally dry .character ofthe air.in this portion of, the country. As a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20F° lower than they are on the plateau during the early morning hours. HBS oZ RADIAN CORPCRATION LY OPERATING TIME ANALYSIS FOR EACH SITE thas“ sectton™presents the* operating statistics for each of the major subsystems contained in the monitoring station. Table I shows the specific number of hours that each of these subsystems were inoperative for the month. The columm labeled "DIGITIZING SYSTEM" indicates the entire data acquisition system; therefore, downtime hours appearing in this columm means total . loss of data. These instances include, in addition to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner malfunctions. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. 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Tat i Z 0 u 0 tj 0 0 e W gv ve 0 v ‘i j d yy) 6 6 s 8 t 5 a s s ‘ r) a a « rt ty fi Q a) T t @ i) f 2) iY v2? v 4) i) W A « i/Z é 6 r) ry r é e ry ‘ a e a a ° ° ' 7 0 0 1 g a 7) v ) ¢ be Y v 7) \) ' ‘ Qi7Z S ® L) é 8 e ‘py ‘ *y "> *¢ « vy ° ° ¢ / au i) Y) t A Q , ”) 2 v W vl ‘ L/ d 8 8 4 6 s s, . 6 a C) é ° a ‘] Q id. £0 Y) i} t ” A 0 Q be 7) v A (4 0 . Ria ‘ r ® é ‘ ‘ ° a ate ‘ ‘ 4) a / O09 @ Fi 7 HY 4 a 8 38 a 4 J i bart(y ibe DHI G 0 ) v ? be 0 ¢ 7) ) e ae bi/ 8 s ‘ ‘ r é e é a ° 1 rs Z DHL v Y v v pe A “4 0 \ . b/Z ia *¢ “y "? bye "Y Y “Vv *u ext oe zs OA Ae ‘ a é P) ar: ia ° ® {) Vi. Zug ) a _é ,@ ae up a a ih rh/Z YAd v ‘ve ? i a xe ae e., ahs he 4) ig a be ay ‘| SL dé 0) a we i an ee SM uj ti " ° [Pv als “4 a ° Gere “9 ' ] 14 t Z (ony Q wy Demi ih »ON 7 ele 1 PM) Ses 5 Ve 1d quvu (vee 4 Ips ea d 7 Ob Aly HE ye: Ree OH = { 3W dns wt e I gv nolwHod uo> ENT STG TI TY PT ye oeceeesewserersk @eewFresee#see#eeeree«ese SSSBsSse SSB eGGSTeOOGSS FZ’ ESM ddbl. LISLGNd VIO S3IVHS 889 YNA SYNOH BhiIhegil “u du A OTIS 7. ie eect Bagged 8 ee Perit Mo *g a) "ce Pe ee. we i ee aq 6 Pe "ve "Re “po °ve he "we > a os “ha “ve aia |: abs *) *y *A *¢ % bi "9 *p2 *0 *yZ *Q wate *9 *y2 *0 "pz “9 "pz "0 pie *9 *ve "2 "te "4 *pz *9 *p2 *D "pe *8 Sue *0 ae “0 cad *¢ nue *0 “ve "A "ve fGSA EQsH *y “A “Re- ve *pe ‘p2 eee “re. =ee Soe "Pe ne pe sk ae a Va - "re "Pere i aaa *g “4 *8 *v et Sey wpe. “pe “ve Pe Pie. tote “we “pe “oa "we “oo “are he. vie Cre “ve a> ee aie.- = be “he *0.01 inch) occurred on the 4th, 5th, the 18th through the 22nd, the 24th, and the 27th. The region received 75 percent of the possible monthly sunshine. Sky cover by cloudiness averaged 4.7 out of a possible 10 during the daylight hours and 4.5 out of a possible 10 during the entire month. The region had twelve clear days, twelve partly cloudy days, and seven cloudy days during the month. Air mass changes occurred in the region with a frequency of about once every five days during July. Temperatures were warm and slightly above normal. Transport winds were not as strong as those winds which prevailed in the area during June. Six cold fronts, all of maritime polar origins, passed through the region during July. These cold frontal passages occurred ommulyesrd,» 7th, Loth,) [4th 23rdi1 and: 30th. Di B=1969 RADIAN . CORPORATION bil Summary of the Meteorological Conditions in the OL) -Shalée Trace “€=b Region during July 1977 Several short waves moving through an essentially zonal flow pattern accounted for the above normal precipitation total in the Tract C-b region during July. Precipitation occurred on. “thé -4th 6th oe hSéneg-19th, 23rd) 'Z4thy;- andvthel29th) ss Tempera- tures in the Tract C-b region were near normal compared to the above normal temperatures recorded east of the Rocky Mountains. Six maritime polar cold frontal passages occurred during July. These frontal passages occurred on the 3rd, 7th, 10th, 14th, 23rd, and 30th. There is no temperature data at the 30- and 100-foot levels of the tower after the 19th because of a lightning strike. The 8-foot level became operative again on the 23rd. The 200-foot level was inoperative during all of July except for the one week period from July llth through the 19th. Nevertheless, monthly average temperatures recorded at the meteorological tower during July were 67.9°F at 8 feet, 69.5°F at 30 feet, and 69.2°F at 100 feet. These averages are approximately 2F° higher than those recorded during June. The warmest days of the month were the 9th, 10th, and the 12th through the 17th. The coolest days were the 4th, 5th, 23rd, and the 24th. The highest temperature recorded at the meteorological tower during July was 88°F at the 8-foot level on the 8th. The coldest temperature recorded at the meteorological tower was 48°F at the 8-foot level on the morning of the 28th. | Relative humidity data was obtained only at the 8-foot level of the meteorological tower during July. Data was obtained until the L9th of July when lightning struck the tower. The average relative humidity for this period was 31.6 percent. The most humid days at the 8-foot level were the 4th, 5th, and the II B-1979 RADIAN CORPORATION 19th. The driest days were the 8th through the 12th. Wind speed and wind direction data was obtained at the meteorological tower from July lst through the 19th. Resultant wind vectors at the meteorological tower during July were as follows: 213.6 degrees at 4.1 miles per hour at 8 feet; 205.9 degrees at 5.5 miles per hour at 30 feet; 204.2 degrees at 6.3 miles per hour at 100 feet; and 213.8 degrees at 7.2 miles per hour at 200 feet. The scalar average wind speeds associated with these resultant wind vectors were 6, 9, 10, and 11 miles per hour, respectively. The Ekman spiral and Ekman effect, i.e., a veering in direction and increase in speed as a function of increasing height above the surface, were in evidence during most of July. A reference to the July wind rose for the meteorological tower indicates that the winds at that location were primarily south- southwesterly with a high percentage of southwesterly winds in addition. The windiest days of the month at the meteorological tower were the 9th, 10th, and the 13th. The days having the lightest winds were the l6th and the 17th. The highest five- minute average wind speed recorded at the tower during July was 44 miles per hour at the 200-foot level on the lst. Precipitation totals in the Tract C-b monitoring net- work during July were generally above normal. During July. .0:..89 inch of precipitation was recorded at the meteorological tower. The largest daily precipitation total recorded in the network during July was 0.23 inch on July 23rd. The greatest five-minute precipitation total recorded druing the month was 0.11 inch (a precipitation rate of 1.32 inches/hour), recorded on the 23rd. Measurable precipitation (>.01 inch) was recorded at the meteoro- logical tower on the 4th, 6th, 18th, 19th, 23rd, 24th, and the 29th. II B-1971 RADIAN CORPORATION The monthly average station pressure during July was 794.2 millibars at the meteorological tower. This reading is 2.9 millibars higher than the June average station pressure of 791.3 millibars. The highest daily average station pressures occurred on the 25th through the 28th and the 3lst. The lowest daily average station pressures occurred on the 2nd, 3rd, 4th, and the 10th. Cloudiness increased in the Tract C-b region during July, compared to the June cloud cover and insolation statistics. The region received an insolation total of 14,515.9 langleys during a 27-day period, which is equivalent to a daily average insolation total of 538 langleys/day. This average is below the normal for July of 610 langleys/day in the Tract C-b region. On a diurnal basis, the greatest solar radiation rates occurred between 1100 and 1200 hours. The greatest daily radiation totals were received on the 10th, llth, and the 12th. The lowest daily solar radiation totals were received on the 4th, 23rd, and the 27th. The greatest five-minute radiation total received during July was 8.75 langleys (a rate of 1.75 langleys/minute), which occurred on the lst. The largest hourly insolation total re- ceived during July was 85 langleys, which occurred on the 10th between 1200 and 1300 hours. Because of the progressively decreasing solar elevations and the increasingly shorter periods of daylight that prevailed during July, the total possible solar radiation which could be received during a day decreased monotonically throughout the month. The increase in cloudiness which affected the Tract C-b during July caused the "very unstable" stability classes to LB 1972 RADIAN CORPORATION become less common than they had been in June. Using the Pasquill method of stability determination, "D" stability (neutral sta- bility) was the most common stability, occurring during 144 daytime hours, or 55 percent of the time. In decreasing order of fre- quency, "C™ “slightly unstable)° stability, occurred, during, /9 hours, or 30 percent of the time, and "B" (very unstable) stability occurred during 37 hours, or 14 percent of the time. "A" (ex- tremely unstable) stability did not occur. There is no lapse rate method of stability data since the Ss sensors were inoperable for the entire month. Using the standard deviation of the horizontal wind (55) method of stability determination, "EO Stability was the most common stability classification at the 30-, 100-, and 200- foot levels due to the moderately strong winds at those levels. At the 8-foot level, the "D" stability classification was the most common stability classification. The stability distributions for the 30-, 100-, and 200-foot levels were similar. The 8-foot level of the tower exhibited higher percentages of the unstable classes because cf excessive mechanical turbulence. No vertical direction wind data was obtained from the bivanes during July. The bivane at the 200-foot level was in- operable during the entire month, and the other two bivanes were being repaired. Also, no comparison may be made of To values between the bivanes and the standard wind instrumentation. IT B-1973 RADIAN CORPORATION Wie DATA PRESENTATION AND SUMMARY This section includes summaries for various recorded data at the monitoring sites. The data presentations indicate the variability of pollutant concentrations and meteorological parameters with location and time. In addition, the presenta- tions indicate the functional dependence of pollutant concentra- tion with wind direction. All data except suspended particulates (24-hour samples) are sampled once each second, but recorded as five-minute arithmetic averages of the one-second samples. This averaging technique tends to smooth instantaneous maximum values, and is especially evident when comparing wind gusts to local weather bureau data. Inherent to any data acquisition system is random noise both from the recording instruments and quantization in the ana- log-to-digital conversion. The lower threshold for all analytical instruments is twice the maximum noise level generated by the instruments. This lower threshold is 5 ppb for all instruments, except for the ozone analyzer, for which it is 0.5 ppb. There- fore, any values appearing in the data presentations that are less than 5 ppb indicate only a trace of pollutant in question and should not be construed to be absolute levels. In addition, the recorded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. All pollutant data (except for particulate data) is taken at the monitoring site in integer parts per billion (ppb) but is presented here in micrograms per cubic meter (yg/m’*) II B-1974 RADIAN CORPORATION assuming standard temperature and pressure of 25°C and 760 mmHg C012 Ping ia bars), cespectavely.+.cthe. scale, factors, required to convert wg/m*® at standard conditions back to ppb for the various pollutants are given in the following table. TO CONVERT vg/m? AT 25°C POLLUTANT AND 760 mmHg TO ppb MULTIPLY BY The units of the meteorological parameters are given in the table. It should be noted here that inside temperature is monitored and recorded as a functional part of the system but is not presented in this report. Table III displays the monthly statistics for each monitoring station for the month. To insure statistical"sig- HS6acance cand to reduce, ithe possibility “of introducing a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of i Bao RADIAN CORPORATION samples present for a particular channel is defined as the total possible number of five-minute samples for the averaging time less the computer downtime less the channel downtime less the channel calibration time. The averages in Table III are arith- metic averages with the following exceptions: « Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. e Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 75 percent. A blank entry indicates an insufficient number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same way as described in Table III. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum expected for that channel on that day. Table VI indicates the five largest averages for various averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments IT B-1976 RADIAN CORPORATION are independent. The maximum averages reported are found using a 'sliding average’ technique with the exception of the 24-hour particulate average, which is computed from midnight to midnight. For averaging times less than or equal to three hours, the slid- ing average is stepped one five-minute sample at a time. For longer averaging times the step size is twelve samples or one hour. For averaging times less than or equal to one hour 100 percent of the five-minute samples must be present to compute an average. Averaging times greater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A shows the stability wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy. It was originally based on the effects of various wind speeds on the amount of canvas that a full-rigged frigate of the period could carry, but has since been modified and modernized. Im its present form for international meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; Ba Lo77 Source: RADIAN CORPORATION (c) descriptive terms; and (d) visible effects upon land objects or the sea surface. One land adaptation is the NRM wind scale. The six basic wind speed classifications used in the 1-3 “knots; “4-6 knots ; 7-10 knets?e-11-16 4eniots; and winds of greater than 21 knots. report are: l7=ZL. knots, table is a complete description of the Beaufort Wind Scale, by Helmut Landsberg, 1969. The following taken from Physical Climatology, BEAUFORT WIND SCALE FOR OBSERVATIONS AT LAND STATIONS Explanatory 1 -grd. Ti | Mi/hr. | Knots Km/hr.. Mi/hr. | Knots! Km/hr.| M/sec. 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(144g ) (ieiar— 7) alva ay? ARleTS ALIOLWOH SATLY 1448 CSSHINI@NOLTAVLTdIID9SNd PSYVET TITRA SNNSS aed CSABVIINV) TWidkeeaadeuavadd $HLYON SHL OL 193d83H HLIM S3SXDFG*NOILISFMHIYU Guin CVISHNSNHYY GISMNZU Ae VN dF fYNUH Y3d SAVWed3adds ANIM (NZIaH JLGND Yad SWVNSOMIT HW ShOT eM INADNUDICL ING) TE NYHL Y AWLP Mud SHOVRSAV ALY SAI 37bV1 NOE ROOHO? VET Ae ae RADIAN CORPORATION. | | | | | | | | TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR JULY 1 THRU 31 IT B-1994 SA 61-4 Lt Chie ei = t O77 Sa2 eB Sew ae Bee SBOE BSS SESH BBE DBAS HSSHBSASKHBSE BABS 2 Be SS & OO & MO we & & OO BF ey Oe Om mm wm © Ob em is Be mh Om se oe CG igre aie isin a VES ZL UGierane, pier al Gis Z Coie tes Tt Wasd Cie Zab en at LeveL EN Hey dal VT fay sae bold (we tv pan LTE (Guede Jue arty AM A Cui etiee ies yay ae Si oa at Sie Oi aaa Cow t : SA VATE maw eS Sena Kt dt Bema enna ade ae 22a 2 SS ww & & HM OF wm © ot Ok Oe me Oe 68 OE oe OO Fe BD OE OR oe es Ot OF eB. 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II B-2033 | OXIDE CUG/Maed) PERIND( 7/ 1/77 TO OF MITRIC DIURNAL, TRAILER NO, BP SREB OES CORPORATION ae VARTATIGN DIS77) 4 ¢ 7 ‘ 23 e HOUR 20 24 22 23 24 MEAN 19 1s rw 4 J sy wi ¥ = =x = x2 *= =x x ® * = © oo al = = ® = x * = = =a & = = =z + * * ® x * => + * « as =x + $3 ot! “a =x = «x = « a 8 FT OwnN © o 26 «3 13 14 ha) 19 17 145 19 2a we a «3 ee 23 24 ' © oo wi en 27 26 = ay 34 4 A A i) MEA Me MEAN NJMBER OF OBSERVATIONS = 7511, TOTAL INSTRUMENT MINIMUM DETECTABLE. LIMUT OF THE CALISR ATION DURING THE WOR * CENNTES & VALTO SAMPLE HELOW THE INDICATES ET 6B-2054 24 MEAN 19 24 7/33/77) DIOXIDE CUG/Mawd) VARIATION OF NITROGEN MRACKISEIRY NOt Sette 3 VEPERINO C7 7° 1777 ° FO HOUR w 8 NT URMAL. 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Average Values Stability. Pasquill Tg a Classification Categories (degrees) Extremely Unstable A 25,-Os Moderately Unstable B 20% Oe Slightly Unstable C 15.466 Neutral D TOe0= Slightly Stable E 530 Moderately Stable F 245° Stability wind roses obtained at the trailers in the monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of stability categorization (or with instruments at higher levels). Table 1 depicts the frequency distribution of Pasquill 9 from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant stability categories based on co (Actual Standard Deviations. of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 9-13, A974). Three distinet range patterns of stability class II B-2090 RADIAN CORPORATION distributions were observed: low, mid, and high, according to the height at which the Og Measurements were taken. TABLE 1 FREQUENCY DISTRIBUTION OF PASQUILL STABILITY CATEGORIES Stability Cateseries based sa c. one Se B C 0 E F G 3 a G5 s23- 1a S2t Stt Lot 98 L6 hos See LHe e@LtI ROT 1S2 BLE TET ¢9 L9 Ge eke tid. 6 lL L2 gt Le if V2 l2 02 22d hI MSM MS SS S§ ass NOILIJINIG IGNIM GCELIBVAE O08 LEAN 7 OORKad (I u 40 4 40 40 40 39vVINIINAd JOVINAIDNId JOVINADN|Ad J9ViN3du4d JOVINIINId JAQOHY GFLNGTULSIO Swivd 40 NFAWAN DWVLOL @ee¢esesbeteoaseseeeoweeseeaeseee eee se see boanseoeseebaeseseoseeaesese eed 91 35 *b * ie, 2 c22 29t whet ot oo ap) pS Opt ue On 1s ioe Ot 1 ee Ay itl eh St 382 2 3N3 3N 1334 @ = 739037 LIarOdd WO 3WHS G=9 WYUYSVIG JSON ONTIM ALTITAVIS OTs : IN3943d Cot Goh = AAO 5 aD (=) iS Se 3 ¢ La > ~O 9S 69 : ik = § = UT 62 3 el ev / 2 2 3 QT - 2] 3 re - Qf . : he 19 HdW 2t ct GQaadS XVW dfNoud JNN ON IviOl = SSV19 ALITIAVIS NOIWHOANOD ~ DT ACa ey a eee CROCKER OHHH E HEHEHE RH HOF HE RHEHHKRHEHHKOHRHEHHKEHHHEHHOHEHHEHHE HEH HHO HH HHH HEH HHS HH HHH HH HHHHOHH SHEE HEHHOSD nt I Lt fe Ofe f. tt 09 3 02 4 9 ol . 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Se °s we Gre 92 Wore Lys Gs tee ell Siitt-—Q2S\ ¢S2 901 ne he 2 G2 I2 oF He t2 Civ ray 92 6S S9 Qh 6h 16 QL Me 66 oat Wel LH $6 00T 68 9L O1t Dati FO 20 le -v6 ok 02 RF. 6h 9 Gots "8d Glee =26 26 09 92 ol Gt 61 he We Moe L9e= OL. fare g 6 S Te wit a6 OF 2 h c$. S¢ PICA ad 7 OF ef 92 Ke Lt | MN MNM oM MGM MS MSS § Acc 38 isa Jj NOTLOINIG UNIT CLE7OI7L OL LEAL O00TH3d «Ladd 00¢= LO3fOUd VIO JIWHS Hed WYHYOVEIQ JSON GNIM ALIVIAVIS Ee a : IN39Y3d Tht eit 3 WlOl oO co G2 02 $ g 17 me aa 29 © 6950.2 r Ee ee | ¢2 On H 21 = / I tt t gt - 21 2 2 te - gt : he 19 Hdw ct gt aqagadS XVH dNOUd JINN ON Wwilol = SSV19 ALITIAVLS MOMWNOANMOD PIO By an RADIAN CORPORATION PERCENTACE OF OCCURRENCE OF WIND DIRECTION FCR- 8 FOCT LEVEL 1 igi PALEY RADIAN CORPORATION Wore PERCENTAGE GF GCCURRENCE OF WIND DIRECTION FOR 30 FOOT LEVEL II B-2118 RADIAM CORPORATION fey PERCENTACE OF OCCURRENCE OF WIND DIRECTION FOR 100 FOOT LEVEL i B- 2119 RADIAN CORPORATION 1. PERCENTAGE OF OCCURRENCE OF WIND DIRECTION FCR 200 FOOT LEVEL £1 B=21:20 THIS PAGE LEFT BLANK INTENTIONALLY II B-2120a ee Aad AIR MONITORING REPORT FOR C=b; .SHALE. OLL} PROJECT AUGUST 1977 Report No. 36 19 October 1977 Presented to: Cb iShatlies Oa, Psoject United Bank Tower Denver, Colorado 80292 Prepared by: Redaanr Start ie B= 22d 8500 Shoal Creek Blvd./P.O. Box 9948/Austin, Texas 78766 /(512)454-4797 RADIAN CORPORATION TABLE. OF CONTENTS PAGE I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM-------- Il B-Z130 II. DESCRIPTION OF INSTRUMENT SYSTEMS-------------------- 59433 A. Air Quality Instrumentation---------------------- =2132 B. Calibration Procedures--------------------------- =71 35 C. Data Acquisition System-------------------------- =2436 D. Meteorological Instrumentation------------ ------- -2136 III. MICROMETEOROLOGICAL AND TERRAIN FEATURES------------- -2142 IV. OPERATING TIME ANALYSIS FOR EACH SITE---------------- ~2144 V. MONTHLY METEOROLOGICAL SUMMARY----------------------- -2148 A. Summary of the Meteorological Conditions over North America during August 1977----------------- -2148 B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during August 1977-------------------------------------- -2150 C. Summary of the Meteorological Conditions in the Oil Shale Tract C-b Region during August 1977-------------------------------------~------- -2151 VI. DATA PRESENTATION AND SUMMARY------------------------ -2157 Ti BeZ122 RADIAN CORPORATION TABLE I TABLE~ TE TABLE TEE LEST OF TABLES DOWNTIME HOURS FOR C-b SHALE OIL PROJECT AVERAGES FOR AUGUST 1 THRU 31 Nitrogen Oxides (NO) a aa a aaa Nitric Oxide (NO) --------------------------- Nitrogen Dioxide (NO,)---------------------- Sulfur Dioxide (S0O2)------------------------ Pyranomet Cf ----- ----- 2-9 en a hydrogen Suita die=--s =< ---=-T ieee aw == === Total Hydrocarbons-------------------------- Methane------------------------------------- Non-Methane Hydrocarbons -------------------- Carbon Monoxide----------------------------- Barometric Pressure------------------------- Total Precipitation------------------------- PartereulLate———--5—— = — ee Wind Speed---------------------------------- Wasnd:=DiaseC@ tt ON=——— a an ere eee Sia Relative Humidity--------------------------- Temperature-------------------~------------- Lip Be 275 Page RADIAN CORPORATION List OF TABLES (contd) Page SABLE LV DATLY AVERAGES FOR AUGUST 1 THRU 31 Hero pen Omides (0) -—— == Il B-2168 Nitric Oxide (NO) --------------------------- -2168 Nitrogen Dioxide (NO,)---------------------- -2168 Sulfur Dioxide (S0.2)------------------------ -2169 Pyranomet €f =~ «<= << 99- 9 oe en 8 HR SG 8S Sen Heo -2169 Hydrogen Sulfide----------------------------- -2169 Total Hydrocarbons-------------------------- -2170 Methane- ------------------------------------ -2170 Non-Methane Hydrocarbons-------------------- -2170 Carbon Monoxide----------------------------- -2171 OZONe - ~- -- - = 2 Ha ne ne -- -2171 Barometric Pressure------------------------- -2171 Total Precipitation------------------------- -2172 Particulate--------------------------------- -2172 Wind Speed-------------------~+-------------- -2173 Wind Direction------------------------------ -2174 Temperature--------------------------------- -2175 Relative: Humidity n= a ee me -2176 TABLE V MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE FOR AUGUST 1 THRU 31 Niprogem Oxides--CiO pe => 2a <= = - === -2178 Nitric Oxide (NO) --------------------------- =2179 Nitrogen Dioxide (NO,)---------------------- -2180 Sulfur Dioxide (S0,)------------------------ -2181 Pyranometer- -------------------------------- -2182 Hydrogen” Sul fides --} Saas Saas as -2183 Total Hydrocarbons -------------------------- -2184 Methane- ------------------------------------ -2185 Non-Methane Hydrocarbons--------------+----- ~2186 Carbon Monoxide----------------------------- =2187 OZONE = <= = 9 8 9 on ae === === -2188 Barometric Pressure------------------------- -2189 II B-2124) | RADIAN CORPORATION BRST OF TABLES Ccontd) Page TABLE V C€congd) TABLE VI TABLE. VEL WOE TESS a ola Set So) Qe a 11B-2190 Wind Speed - Wind Direction----------------- -2193 SRG an SBN EC =Z2195 Relative Humidity------------------------ --- =21953 THE FIVE MAXIMUM INDEPENDENT SLIDING AVERAGES BORVAUGUST 1 THRU. 31 Nitrogen Oxides----------------------------- =Z195 Nitric Oxide-------------------------------- =Z2195 Nitrogen Dioxide---------------------------- -2195 Sulfur Dioxide------------------------------ -2196 Total Hydrocarbons -------------------------- =2197 Methane- ------------------------------------ - 2198 Non-Methane Hydrocarbons-------------------- +2199 Carbon Monoxide----------------------------- -2200 Carbon Monoxide- 8-hour--------------------- -2201 OZ ORC = = = nm mn i nn = ne -2202 Particulate--------------------------------- -2203 FUNCTIONAL DEPENDENCE OF RECORDED PARAMETERS UPON WIND DIRECTION Nitrogen Oxides (NO) )osssge-Gor-->- >>> >" >> -2205 Nitric Oxide-------------------------------- -2206 Nitrogen Dioxide (NO, )---------------------- -2207 Sulfur Dioxide (S0O,)--------~---------------- -2208 DyGrOpenL sul tideo52 lo oeeee as > > SSS -2209 Total Hydrocarbons -------------------------- S220 Methane------------------------------------- =o Non-Methane Hydrocarbons-------------------- Lae Caron Monoxide------------------------------ =2215 Ozone- -------------------------------------- =Z244 i B=2025 RADIAN CORPORATION Gtsr OF TABLES. (contd) Page TABLE sv EES DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS Nitrogen Oxides------------------------------ IE BL2716 Nitric Oxide--------------------------------- Be) Nitrogen Dioxide----------------------------- <77T8 Sulfur Dioxide------------------------------- -2219 Pyaropen” Sul bates: = ae mee re et wee eee ree -2220 Total Hydrocarbons--------------------------- -2221 Me thane- ------------------------------------- ~727? Non-Methane Hydrocarbons --~------------------ =2795 Carbon Monoxide------------------------------ -2224 Ozone---------------------------------------- -~2225 Precipitation-------------------------------- Missing Wind Speed 8 feet-------------------------------- -2226 30 feet-------------------------------- Bi | 100 feet-------------------------------- -2228 200 feet-------------------------------- =~ 7996 Wind Direction 8 feet-------------------------------- -2230 30 feet-----------------~--------------- -2231 100 feet-------------------------------- -2232 200 feet-------------------------------- -2233 Wind Direction Standard Deviation 8 feet------~-------------------------- ~2234 30 feet-------------------------------- =20535 100 feet-------------------------------- -2236 200 feet-------------------------------- =2257 Temperature 8 feet-------------------------------- -2250 30 feet-------------------------------- -2239 100 feet-------------------------------- -2240 200 feet-------------------------------- -2241 It B-2126 ie FAD Ata CORPORATION LIST OF TABLES (contd) } Pace TABLE VIEL (eonud) Solar Radiation------------------------------- II B-2242 Relative Humidity----------------------------- -2243 Barometric Pressure-----------------+--------- -2244 Hom_Zontal Wind Direction Standard Deviation at 30 feet-------------------------- -2245 Vertical Wind Direction Standard Deviation at 30 feet-------~------------------- -2246 Temperature Change from 30' to 200'----------- -2247 Bi-Vane Wind Speed at 100 feet---------------- -2248 Horizontal Bi-Vane Wind Direction at 30 feet-- -2249 Nitrogen Oxides------------------------------- =2250 Nitric Oxide---------------------------------- —LLo4 Nitrogen Dioxide-----------------+------------ =2252 Sulfur Dioxide-------------------------------- iS 2255 Hydrogen Sulfide------------------------------ ~2254 Total Hydrocarbons ---------------------------- =2255 Methane- -------------------------------------- =2956 Non-Methane Hydrocarbons---------------------- -2257 Carbon Monoxide------------------------------- -2258 Ozone----------------------------------------- -2259 Total Precipitation--------------------------- -2260 Wind Speed - 8 feet--------------------------- -2261 30 feet--------------------------- -2262 100 feet--------------------------- %2263 200 feet---------~------------------ - 2264 Wind Direction - 8 feet----------------------- -2265 30 feet----------------------- -2266 100 feet----------------------- -2267 200 feet----------------------- -2268 IT B-2127 RADIAN CORPORATION MST OF TABLES (contd) Page TABLE ViLI (Ceontd) APPENDIX A - Temperature at 8 feet------------------------ Il. B= 2769 30 feet------------------------ - 2970 100 feet------------------------ ey al 200 feet------------------------ =2979 Barometric Pressure-------------------------- -297% Solar Radiation------------------------------ -2274 Relative Humidity---------------------------- =2275 Bi-Vane Wind Speed at 100 feet--------------- ~ 2976 Horizontal Bi-Vane Wind Direction at 30 feet- = Ze Stability Class Determination Using Pyranometer Recording------------------------ -2278 Stability Class Determination Using DT/DZ (Level 2)------------------------------------ -2279 STABILITY WIND ROSE DIAGRAMS ----------------- =2292 8-foot level - Stability Class A------------- - 2296 Class B------------- -2297 Class C------------- -2298 Class D------------- -2299 Class E------------- -2300 Total--------------- -2301 30-foot level - Stability Class A------------ -2302 Class B------------- -2303 Class C------------- -2304 Class D------------- -2305 Class E------------- - 2306 Total--------------- -2307 100-foot level - Stability Class A----------- - 2308 Class 8=——————— = -2309 Class C------------- -2310 Class D------------- = Snell Claes f= === === -2312 Total--------------- = 46S I) B= 24:28 RADIAN CORPORATION LUST OF TARLES.Geonit.d,) Page APPENDIX A (contd) Z00EEecotelewel ~SS5tabi trey sCbass j/A==2—==---= 1 B-2514 Class B------------ ~2315 Class C------------ -2316 Class D------------ at 7, Class E------------ -2318 Total-------------- -2319 Percentage of Occurrence of Wind Direction for 8-foot level---------------------------- -2320 30-foot level---------------------------- -2321 100-foot level---------------------------- -2322 200-foot level---------------------------- L525 IB =21-29 RADIAN CORPORATION td GENERAL DESCRIPTION OF AIR MONITORING PROCRAM Radian ‘Corporation; fuuder contractoteithe C-b Oil Shale Project, is performing the data compilation and reporting of air quality and meteorological data at one monitoring site in Northwest Colorado. The site measures and records concen- trations of particulates, sulfur dioxide, oxides of nitrogen, hydrogen sulfide, total hydrocarbons, methane, and carbon monoxide. A 200-foot meteorological tower provides wind direction, wind speed, temperature, and relative humidity data at four levels (8, 30, 100, and 200 feet). Other meteorological variables measured at the tower site are insolation, barometric pressure, and precipitation. Figure I shows the configuration of the monitoring station. The station provides a sturdy and protective covering for the monitoring equipment. PLB =21350 T oandty SIVVOLS AUZLIVE E HONIG HONIG ] ee eee ee 39vdS NUON [ae ey — | | SWNULSNI : r ¥I310EO9 a YaNGNay HOV O ! eee tty Poo oP aaa | 3.104V govds muon |) “2 ey ak cq rv oraz Ok oe ne ee ome ee ee oe oe fleas oot —on ne ee ee owe ! a, r (SIC ee ae ee Sea et Bo Claw = ©) O © O e | Gee) GR) GST | ae Gan (| ae | EEE | GE 5 Sea 4 YVIV OU3Z is B= 2050 RADIAN CORPORATION ip es DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA520 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle and continuously monitors both NO, and NO. A subtraction circuit in the instrument provides a continuous NO2 output, but is not used in Radian's.system. NO? is cal- culated once a second by the computer by subtracting the NO value from the NOx value, thus avoiding any drift which might occur in the NO, output of the instrument. This instrument has a minimum detectable sensitivity of 5S ppb (parts per billion) and a linearity of 41%. Sulfur dioxide is measured with the Meloy SA185-2A analyzer while hydrogen sulfide is measured with the Meloy SA185-2 analyzer. The hydrogen sulfide analyzer uses a Meloy Model S0O2-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H,S-1 hydrogen sulfide scrubber. The Model SA185-2 is a continuous analyzer and utilizes the flame photometric principle of operation. The minimum detectable sensitivity for the Model SA185-2 is 5 ppb with a linearity of +1% and the minimum detectable sensitivity for the Model SA185-2A is 2 ppb with a linearity of +1%. Ozone is measured with a Meloy Model OA350 analyzer. This instrument, based on the chemiluminescent principle, pro- vides continuous measurement of ozone. The minimum detectable sensitivity_is 0.5 ppb and the linearity is #1%. Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. This instrument, which uses a plume ionization detector, has a minimum detectable sensitivity of 5 ppb for all three components. The Model 8200 works on a five-minute cycle, i.e., one air sample is analyzed every five minutes, and the results are dis- played for five minutes via a sample and hold circuit. i BZ a2 RADIAN CORPORATION The air sample is drawn in through a glass cane and manifold supplied by the Ace Glass Company. The system has a 25mm diameter, through which a constant air flow is provided byean ainepump rated at) 60 cim at OY head pressure. \£ The manifold has. sampling ports to which 1/4" teflon lines to the instrument are connected. All joints in the sampling system are secured by O-ring compression fittings. The manifold is contained in a heated (100°F) chamber to prevent condensation of moisture. . The teflon lines from the manifold to the instruments are insulated with 1/8" wall thickness rubber tubing. The trailer has four heavy duty high volume particu- late samplers (Hi-Vols). Fiberglass filter paper is used for the collection of particulate samples, after which each filter is brought to a controlled humidity before weighing. Each Hi- Vol has a flow recorded to permit correction for changes in air flow as the filter becomes loaded with particulates. Each Hi- Vol runs for a 24-hour period (midnight to midnight) and is turned on and off by the computer. The Hi-Vols, which were manufactured by Radian, were designed foliowing guidelines re- commended by the Environmental Protection Agency. In addition to the normal Hi-Vol particulate samples, a duplicate Hi-Vol sample is collected every sixth day on special filter paper for trace element analysis. Once each quarter these samples are composited and analyzed for gross radioactivity and trace element content. B. Calibration Procedures The trailer contains a Meloy Model RAD-1 calibration unit... Thispanstrument; provides, ai zero air supply, SO span gas from an SO, permeation tube, and NO span gas obtained by precisely ET B21 35 RADIA CORPCRATION diluting bottled NO span gas. The computer-controlled calibration of all instruments is automatically perfcrmed once a day. Each instrument is first switched to zero; the computer monitors the output of each channel and takes a new zero reading after a stable zero signal has been reached. This zero reading is compared by the computer to the zero reading obtained 24 hours before, and if a drift in excess of 10 ppb has occurred, an excess zero’ drift light for the channel in question is’ turned ’on on the System Status Panel. Next, span gas is supplied to each channel and the computer decides when a stable span value has been reached. This value is recorded and compared to the previous day's value.\ “An excess span drifce light on the System Status Panel is turned on if a drift exceeding 10 ppb occurs. The instruments are then returned to the monitor mode and after two minutes the con- puter resumes data taking. The bottled NO gas used at each site was obtained from Precision Gas Products. Pre-purified grade hydrogen is used in the SO, analyzers. The SO» permeation tubes were manufactured by Metronics Association, Inc. Their output has been verified by comparison to the output of National Bureau of Standards tube 10-42. Both SA185 analyzers in each trailer are calibrated with the SO, from the permeation tube. This instrument responds to the number of sulfur atoms per molecule; thus, SO, can be used to calibrate both the HS and SO, monitors. The Model OA350 ozone analyzer has its own calibration system which provides a zero check and a span check. The ozone calibration system is verified by comparison to a calibrated ozone generator maintainec in Radian's laboratory in Rifle. IM B-2134 RADIAN CORPORATION The Model 8200 total hydrocarbon, methane, and carbon monoxide analyzer is calibrated with undiluted span gas obtained from AirCo's Rare and Specialty Gas Division. This span gas con- tains methane and carbon monoxide in air, the methane being used to calibrate both the total hydrocarbon channel and the methane channel. The Model 8200 is zeroes with air from a Bendix Model 83834 zero air unit. ..lImeaddition, the.instrument is electronically re-zeroed at the start of every five-minute cycle. The Hi-Vol particulate samplers were calibrated using a Calibration Kit from General Metal Works. C. Data Acquisition System The basis of the data acquisition system is a Data General NOVA 1200 minicomputer. The NOVA, which has a basic cycle time of 1.2 usec, is equipped with automatic program load and power fail/automatic restart features. The computer utilizes 16K 16-bit words of core memory. Analog-to-digital conversion is accomplished via an ADC built by Radian Corporation. The input/output unit for the system is Texas Instrument's KSR 733 keyboard/printer. This model teletype provides keyboard entry and hardcopy printed output. The data are also recorded on a cassette magnetic tape unit with three drives. The cassette unit is utilized for program storage and loading as well as for recording. To reduce wear on mechanical parts, the power to the teletype and cassette units is turned on only when the unit(s) is (are) to be used. Several important functions in the instruments as well as in the computer and the trailer are monitored by means of lights on a System Status Panel. These data lights are written onto cassette tape to monitor the complete status of the system every five minutes.” The Data Acquisition System also monitors the presence of LO00V power from the power lines. In its absence, Ehe scomputer, “whieh is powered by batteries, switches all trailer kp B-ZE35 z?ADAN CORPORATION systems to battery-provided power. If the line voltage is restored before the batteries are discharged to a specified level, the trailer system is switched back to line power. D. Meteorological Instrumentation 200-Foot Meteorological Tower The tower has instrumentation at four levels: 8 feet, 30:feet >: 100*feet,, “and ZOO feet: “At-akilVfour® Levels ,. there. are, wind speed, wind direction, and temperature and relative humidity sensors in a power-aspirated radiation shield. Temperature difference thermistors (also in power-aspirated radiation shields) and their associated circuitry take lapse rate measure- ments for the 30-foot to 100-foot layer and the 30-foot to 200-foot layer. In addition; this site Ras ‘a Precision Spectral Pyranometer, a barometer, and a tipping bucket rain/snow gage. The wind direction and speed apparatus used at each measurement level of the tower is the Model 1074-2 wind sensor by Meteorological Research, Inc. (MRI). This sensor has a 540° potentiometer for wind direction and a light chopper for wind speed. This sensor is rugged, with an all-weather coaxial cup and damped vane assembly. The prototype model has been in operation for years under the most demanding weather conditions, performing continuously with the utmost reliability. The wind sensors on the tower have been specially treated with a black paint which will promote warming of the exposed surfaces of the sensor and thereby reduce ice and snow accumulations on the moving parts of the apparatus. The specifications on the Model 1074-2 are as follows: et B=-2456 RADIAN CORPORATION Wind Speed Stareime Thresholds 0.75 mph. Response Distance: 18 feet (63% recovery). Flow Coefficient: 7.9 feet/Revolution. Aceusacy: £0.4 mph or 17 Cwhichever is greatest) Wind Direction Starting “Threshold: “0.75 mph. Delay Distance: 4 feet (50% recovery). Damping” Ratvo= “O85-te 70. 6S Accuracy (540° system): 17%. Range: 0° to 540°. The relative humidity and temperature sensors are mounted within a power-aspirated radiation shield at each tower level. All aspirators and sensors are of the Model 840 Series by MRI. The aspirated shielded housing is designed to provide maximum radiation protection to the sensor. Ambient air is drawn into the shield and across the sensors at approximately 15 feet per second. This intake air is essentially sampled from a hemispherical space which is approximately 3-inch radius from the tube opening. Speed of the incoming air at the perhiphery of this hemisphere is approximately 1 mph. The temperature sensor is comprised of a dual thermistor and resistor network. This circuit provides a linear resistance change with an air temperature change. The relative humidity sensor is placed alongside the temperature elements inside the shield where it is exposed to a constant flow of air. Circulation to both sides of the sensing element produces accurate monitoring with a good response time. The specifications on the sensing ele- ments are as follows: i B-2S7 RADIA CORPORATION Temperature Accuracy: +0.25°C. Ranga ~.50 46 }to +50° CG; Humidity Aceurdey; “23.07 Ra. Range: 0% to 100% Relative Humidity. Measurements of temperature difference are taken for two layers, the 30-foot to 100-foot and the 30-foot to 200-foot layer. The thermistors and circuitry used for these measurements are separate from the thermistors measuring air temperature. The use of separate thermistors and circuitry to measure AT allows for much greater accuracy and resolution in the measurements, which is necessary for stability assessments. Two AT thermistors are at the 30-foot level, one is at the 100-foot level, and one is at the 200-foot level. All of these AT thermistors are mounted within power-aspirated radiation shields. The specifications on the AT instrumentation are as follows: Accuracy: +0.1°C. Range of AT Circuit (Lower Level-Upper Level): +9F° to -9F°. All instrumentation, except at the ground level, is mounted at the end of 12-foot retractable booms. These booms are 3-inch box beams which are on rollers and can be retracted to the instrument platforms for instrument maintenance. The meteorological tower itself is a 200-foot Rohn Model 80 Guyed Tower, designed for 40 pounds per square foot wind load with %" of radial tee per ENA Standard RS-Z222-5 to II B-2138 RADIAM CORPORATION support four levels of meteorological equipment. The material consists of tower sections with a tapered base, three retractable booms 12-feet long, three outside work platforms, an inside ladder for climbing, two base ground kits and one anchor ground kit. The cable-type Safety Climbing Device consists of a cable and attachment mechanisms with a locking sleeve and safety belt. The tower is lighted and painted according to FAA specifications. The signals from the tower instrumentation are fed from multiple signal cables into transmitters mounted at the base of the tower. After signals have been converted to analog sPenals, “they “are field tito Ya “junetion box ftaliso at the tower base, where they are assimilated into one coaxial cable. The signals are then run underground within 3" PVC conduit to the A-to-D assembly, where they are processed. The transmitters are shielded and insulated from the elements. The signal cable is run underground in PVC conduit in order to minimize damage from the weather or from various rodents in the region. The auxiliary equipment at the tower site consists of a heated tipping bucket rain/snow gage, an analog barometer, and a Precision Spectral Pyranometer. The rain/snow gage is the Model P511-E unit by Weather Measure. In the case of this gage, the durability and reliability of a tipping bucket gage are combined with heavy-duty electric heaters to make this an all- purpose precipitation sensor. This gage may be used to measure both snowfall and rainfall. An insulating cover of poly-vinyl chloride and a thermostatic control insure the proper gage temperature. The thermostatic control is adjustable from 0 to 35°C. Snow falling into the inlet funnel is melted. The resulting water (from rain or snow) drains into a precision tipping bucket mechanism which activates a mercury switch each time the bucket filis and tips. The gage isteonstructéed obidirable corrosion- resistant materials to provide many years of service. The IT B-2139 RADIAN CORPORATION specifications; fox, this, gage.are as, follows.: Onrefices, 8) dmches. Gal. i-bra tiom:-.9 0,014 nien . Aecuracys <0..5% (Calibrated..at,..0:.5,in/hr). Sensor: Chrome-plated tipping buckets. Switch: Mercury, 0.l-second closure. Heat Control: Thermostat adjustment, 0 to 35°C. The barometer is the B242 Analog Output Barometer by Weather Measure. This barometer provides an output voltage that is linearly proportional to pressure. The specifications on this instrument, which is mounted inside the monitoring trailer at the site, are as follows: Range: Specially designed for the 100 millibar interval from $/25, milLlibars.to 825 .millibans. Resolution: Infinite. Linearity: +0.5 millibar, over the 100 millibar interval. The pyranometer at the site is the Eppley Precision Spectral Pyranometer. This instrument is used for the measure- ment of sun and sky radiation totally or in defined wavelength bands. The pyranometer is levelled and mounted atop a wooden stand 4% feet from the ground surface. Care nas been taken to eliminate the effects from all outside influences, such as reflection or shadows, on the pyranometer. The instrument characteristics are as follows: Sensi.bivity jwe wivic per cal/em°/min. Independence: 300 chms. Temperature dependence: Sensitivity constant to within +l percent over the ambient temperature range from -20 to +40°C. IIT B-2140 RADIAN CORPORATION Linearity: Response linear up to intensities Or realy em (mim, Response seine: I second (4/e signal). All instrumentation is factory-calibrated and is field- calibrated at various intervals. Sling psychrometers are used to calibrate the humidity sensors; known temperatures and/or resis- tances are used to calibrate the thermistors; and an rpm cali- brating unit is used to calibrate the anemometers. The wind direction instrumentation is aligned to true north (reference direction) by means of a surveyor's transit. PE Ba2148 RADIAMz CORPORATION KI Hi tH MICROMETEOROLOGICAL AND TERRAIN FEATURES The Piceance Creek Valley and C-b Shale Oil Tract are situated such that many microscale meteorological phenomena affect the region where the ambient air monitoring unit is located. Trailer 023 and its associated 200-foot meteorological tower are located atop a plateau to the south of the valley, high enough to be affected mostly by gradient flow conditions. The elevation at the meteorological tower site (Trailer 023) is 6940 feet above sea level. The largest gradients in eleva- tion in this area, of course, occur at the Piceance Creek Valley walls. However, the northern valley walls are slightly steeper than those at the southern boundary of the valley, which then slopes upward gradually toward the C-b Tract. The Piceance Creek Valley decreases in elevation from east to west in this area, so that nighttime katabatic cold-air drainage flows advect from east EO WesSE. Site’ O23) 1s approximately 2.5 miles south of the Piceance Creek Valley. This location is relatively high com- pared to its surroundings, with the nearest point having an eleva- tion greater than 7000 feet being .5 miles to the south of the tower. The tower itself is on the top of a small knoll located between Scandard and Sorghum Gulches. Because of its location and the irregularities of the surrounding terrain, meteorological patterns are varied here. Wind instrumentation is mounted at four levels of the meteorological tower: 8 feet, 30 feet, 100 feet, and 200 feet. The top level of the tower generally remains in gradient wind flow. That is, the winds at that level are normally generated II B-2142 Fe ADA CORPORATION by synoptic-scale features and are usually separated from terrain features and*micrometeorological circulations. —-Oecasionally,«a weak anabatic flow influence is experienced. However, such is not the case with the three lowest measurement levels. To varying degrees, these levels are influenced by both the katabatic and anabatic circulation cells. However, when strong pressure gradient forces exist in the region and the synoptic-scale wind flow is strong, all four tower levels will reflect a gradient wind flow as the winds increase in strength and height. The terrain atop the plateau is generally barren and fairly rugged, with a few scattered small trees. The topsoil dries sapidly and is very fine, resulting in blowing dust when dry, windy conditions exist. In the Piceance Creek Valley, the terrain is fairly grassy and flat, with steep valley walls on either side. Surface winds are normally rather light in this valley unless channeling effects occur. During clear nights with rather light pressure gradient- induced winds, rapid radiational cooling will occur in the region because of the barren nature of the terrain and the generally day character Of the air In. this portion@of the ‘country. *As’a result, the diurnal range of temperatures will be extremely large. Because of the katabatic flow in the valley, nighttime temperatures will generally be lower in the valley than on the plateau. During the winter, especially, temperatures in the valley may be 20F° lower than they are on the plateau during the early morning hours. i, Be 25 RADIAN CORPORATION LY. OPERATING TIME ANALYSIS FOR EACH SITE This section presents the operating statistics for each of the major subsystems contained in the monitoring station. Table I shows the specific number of hours that each of these subsystems were inoperative for the month. The column labeled "DIGLTIZING SYSTEM" indicates the entire data acquisition system; therefore, downtime hours appearing in this column means total loss of data. These instances include, in addition to computer downtime, power failures, no power available, and self-automated shutdown periods such as during air conditioner malfunctions. Calibration time is not considered to be downtime and is, therefore, not included in the downtime figures. The amount of time used in calibrating the instruments is given at the bottom of the downtime analysis table and is reported as total calibration hours for each channel for the entire month. As is evident in the calibration figures, channels can be calibrated independently of one another. No calibration time is given for particulate monitoring since Hi-Vol calibration occurs infre- quently and only during the off-duty cycle for each Hi-Vol while another Hi-Vol is taking data. 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COA he 7 eS 6 ‘5 \/¥ 1 /¥ /1/* WLW GIs Vt 7 S1/H en An I {/ 43 OLS (a) Se / /¥ 7 /}3 42 / J 78 7 4iVad ee Ul) $115 “ho mate Oe (ne? “he >On Oe "ne y (6 “Pe “tid the tee Bole ° 22 Wie Ste etid She Satie Ste, *he tre "th? *He wulte *t2 *h2 “ne “ne SdSH e fe tre HT ne 2 AT V2 he ne 22 Se red n? he ph? nr? We ne? tie 1? he hd h2 he n2 ph? ne ne CASA Uv © tie a ike stie “tid “the oy it “te *he “67 “Hie “te “ne rca “Se wee “he = tie wile "2 "Ae it ba fied tic *te “ne *te “ne “ne nid “te “re 7 USH *() “td "tid aitie wre * the wig an | °GI *6I *ne *t2 matae 2a. “Se, *22 “he “We "he “the one wilted *he mike “ihe "ne “re *t2 the *td *ne *n2 TOSA "Qi “ci Fen Gal a * te "ne Peer mace ae hie “he *tre * tre *ne Pie “tric *te * tie otic. aati "Hi “ne * tid “tre “te Tas =) U0 sitar *h2 “te “ne “tie. “te *ph2 “tie a tn) *re *he HaUSM oy) wt) ert) mal} *\) Sed) 1) =) eri() oa(') Sait Or) a) edt) 0) a) oul een Ole sa Od Op th? (A) Ste ae 0 ae © y ~iGeee ei) “ae. « 0 re A ie ew *h2 0) “he a) Lip wee ell vite Ss" tid Bi weir: Ste ae: tie ire we 2 cic. wakes ie. Ste HS ie “We ee tie one + @ ine "ie tid "fear the Ste eae Nie FASM 2agn al Ste pec *t? “he "ue *te oie “12 *ne wide Ei hed fdSn LO9L0MNd VW 47 a tHe *te 2 tie "te =the a3), "ne? etre Soul ene ehie “ne 22 Voc wae * 2 Siti “he wine Pie Ete *tre 072 "he Site hie 2 "te Sie We wa elte! =0 = () Shia Ste eee ual “te le) milion’ °n2 Sri OWI SRT idan aaire “te aihte oA | mG | Be. Sind sve. mic Siiee lic See ee aSey me’ pcan ace ties ratte, aie atic, Shee - ihe Slide entice “ne “hd Hic male Ye Oe ees tne sities 3 ine Ses EM Stice mit ne. —for-whach,1t_s-.0..5.ppb.— There- fore, any values appearing in the data presentations that are Bess Elan > ppb anareate only a trace of pollutant in. question and should not be construed to be absolute levels. In addition, the recorded quantity is simply random noise and averages tend toward zero. Thus, when concentrations are below the lower threshold of the analytical instruments they may appear as a zero entry in the data presentation which does not indicate absolute zero concentration. ALT pollutant data (except for particulate: data),is taken at the monitoring site in integer parts per billion (ppb) but is presented here in micrograms per cubic meter (yg/m°) EE BZ 157 RADIAN CORPORATION . = = ‘@) T assuming standard temperature and pressure of 25°C and 760 mmHe (1013.2. millibars), respectively, The sealbe factors nequired to convert wg/m’* at standard conditions back to ppb for the various, pollutants.are given in the. following table. TO CONVERT ug/m? AT 25°C AND 760 mmHg TO ppb MULTIPLY BY POLLUTAN The units of the meteorological parameters are given in the table. It should be noted here that inside temperature is monitored and recorded as a functional part of the system but is not presented in this report. fable, lad idisplays,.the monthly.statistics foreach monitoring station for the month. . To insure statistical sig- nificance, and to reduce the possibility o£ introducing a bias in the presentation, averages are computed only when at least 50 percent of the samples are present, except for relative humidity and temperature, in which case 75 percent of the samples are required. If less than the required samples are present for a particular parameter, that entry will be blank. The number of iT B-Z2458 RADIAN CORPORATION samples present, for a particular channel is defined as the total possible number of five-minute samples for the averaging less the computer downtame less the channel downtime less th channel calibration time. The averages in Table III are metic averages with the following exceptions: - Wind speed and wind direction are computed using a vector averaging technique where the wind speed is treated as the vector magnitude. - Particulate averages are computed as the geometric mean. Table IV displays the daily averages. Again, 50 percent of the five-minute samples are required in order to compute an average except for the cases of relative humidity and temperature which require 75 percent. A blank entry indicates an insufficient number of five-minute samples present for that day. Wind speed, wind direction, and particulate averages are computed the same way, as described in Table III. Table V presents the maximum daily five-minute average retained in the data base as well as the time of occurrence. A five-minute maximum average is printed if any samples are present for that day. Therefore, the maximum five-minute average for a channel which experienced considerable downtime or calibration time during the day in question may be misrepresentative of the maximum expected for that channel on that day. Table VI indicates the five largest averages for varlous averaging times. The table shows the period of time covered by the average. Maxima are chosen so that time segments te B=2159 mADIAM CORPORATION are independent. The maximum averages reported are found using a 'sliding average' technique with the exception of the 24-hour particulate average, which is computed from midnight to midnight. For averaging times less than or equal to three hours, the slid- ing average is stepped one five-minute sample at a time. For longer averaging times the step size is twelve samples or one hour. For averaging times less than or equal to one hour 100 percent of the five-minute samples must be present to compute an average. Averaging times greater than one hour require 90 percent. Whether or not a sliding average is computed is solely determined by the number of samples present in that averaging time and is independent of daily and monthly averaging criteria. To demonstrate the functional dependence of recorded parameters upon wind direction, Table VII shows pollutant con- centration displayed in a bi-variate distribution with wind direction. The tables display the total number of five-minute samples occurring in each concentration and wind speed class. The mean concentration for all samples occurring in each wind class are also shown. This distribution demonstrates the dependence of high pollutant concentrations upon wind direction. Appendix A shows the stability wind rose diagrams. The wind speed classifications used in Appendix A are based on the Beaufort wind scale classification system. This is a system of estimating and reporting wind speeds, invented in the early nineteenth century by Admiral Beaufort of the British Navy. It was originally based on the effects of various wind speeds on the amount of canvas that a full-rigged frigate of the period could carry, but has since been modified and modernized. In its present form for international meteorological use it equates: (a) Beaufort force (or Beaufort number); (b) wind speed; 1198-2160 —— RADIAN CORPORATION Ce) deseniptive terms; and (d) visible effects upon land objects or the sea surface. One land adaptation is the NRM wind scale. The six basie wind’ speed classifications used inuthe Fepore are-." l-3 knots. "4-6" knots; 7-LOM knots, ° 11-165 knotss 17-21 knots, and winds of greater than 21 knots. The following table is a complete description of the Beaufort Wind Scale, taken from Physical Climatology, by Helmut Landsberg, 1969. 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OS ‘4 >, pare ate ee EY oss Lf q A RADIAN CORPORATION TABLE VIII DIURNAL VARIATION OF VARIOUS RECORDED PARAMETERS ieBa225 ee. 23 ed MEAN at 16:5 9 8/31/77) PERTOOL 87 1777 “10 23 HOUR DIURNAL VARIATION OF NITROGEN OXIDES(UG/M*43) TRAILER NO, 4 : 6 wT t 4 YW ae y i q i doe. ba Co kbad EL ee DLS } ye 5 es LL wy i : mu wk ay’ DAY =U” 0 10 Ne) 14 ce Lad ee ce ec 19 20 21 ee ee ee oe oe ee eo ) () 26 28 \) 29 1, DETECTABLE LIMIT OF THE INSTRUMENT BELOW THE MINIMUM TOTAL NUMBER OF OBSERVATIONS CALIBRATION DURING THE HOUR, DENOTES A VALID SAMPLE TES INDICA x ° . () i B=2216 MEAN 50 31 () 24 MEAN 23 OF AST TO @7SY777) PERIOD ( HOUR ~ 23 NO. DIURNAL VARTATION OF NITRIC OXIDE(UG/M«*x%3) TRAILER () *y ee * 3 ay 0 = So ee ee 0 1. MEAN 7039, NUMBER OF OKRSERVATIONS TOTAL LIMIT OF THE INSTRUMENT BELOW THE MINIMUM DETECTABLE HOUR DURING THE SAMPLE CALIBRATION 45 ad's COUNPOIATROWN b i § “ad a Ve De bee j 1] dj DENOTES A VALID INDICATES x () MEAN DAY 10 11 1e 13 14 1S 16 17 18 19 20 el 2s 24 25 26 el 28 29 30 31 Q 24 MEAN 18. 109 20 Pet Pee srs BALAVT THO 8873AV77) PERTOD( HOUR —s235 DIURNAL VARIATION OF NITROGEN DIOXIDE (CUG/Mxx3) TRAILER NO, bd a Oop, / Rea ca wee Sf bf nl oF Fe) CORP OR NVI ak ‘Gat. DAY 10 Gt lig ee) 14 15 16 17, 18 19 20 Q) ee oe xt se ec ‘KY el 22 23 So xy ce =) 24 ay 25 26 eT 28 x eo 29 30 0 0. DETECTABLE LIMIT OF THE INSTRUMENT 7031. ) 0 HOUR NUMBER OF OBSERVATIONS TOTAL 0) DENOTES A VALIO SAMPLE BELOW THE MINIMUM INDICATES CALIBRATION DURING THE x () II B-2218 MEAN a 23 24 WEAN 9) () () Q 0 19 2) () 8/31/77) 16 WT The 15 14 () 0) () SULFUR DIOXIDE (CUG/M**3) VARIATION OF = 23 PERIOD( 8/ HOUR 0% 03 0) () () DIURNAL TRAILER NO, () u () Q) () O$ () 0) 0) Q 0) () () 0 0) () 0 () \) Q 0) 0 0 0) () 0. THE HOUR 0 () 0 () 0 () ’ iy ' Ma 0) Lae, Ey 0) () () () 0 Hit fe tal CONF UORAVICH iy () 0) ¢) 0) ()3 0 () 0) () () () van ~~ i ayy haw. 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AL TEAS. 3 NOLTLOIGNYTO ONY ONIM ATYNOH GEESE U8 LEAN ARE DOOD (2 W9A91) Zasiad OYNTSN NOTIVNIivasida SSv19d ALITIHVLS JLIS YAMOL WITHOWHNILSwH LOSLONd TIO FIVHS feo —, RMOIAWHOCAMOD mrccunenss 6szz-a Il 1g/R UL/R 6¢c/8 wos L2/ 92/8 G¢2/# 1e/R ae/4 22/7? 12/4 U2 61/4 RT/7R LI/8 he te a le 02 6} Gree Lele O* Git ots 8 gl> JT” Of 6 8 L o) S n Cc ¢ yYNOH SSV19 ALIN HVIS 4 NOTLOSYIG UNV GNIM ATVYNOH COLI NITPS” “OL LL 1 £89 COT dad (2 VW4A37) ZO/1O SONTSN NOTLYNIWH3130 SSV19 ALTVIvls ALIS HIMOL WITSOWHOFLIW LISFOMNd VIO 3AWHS wed MOAT MOdkios Ry Oe oh 622-4 II 91/8 S73 HI £ 1/8 2/4 11/8 OT/# 6 Y 72 “3 /® /% 74 J" /# /# /® “SS MSS 6 L MSS MS MSS MSS 8 ety 6 JN3 MSM 4S 0 0 S Jo saao) ae I € £ SS Om A evans. sa NOTLIOSYTA GNY GNIM AVYNOH (LL/TE/8 OU EEA 7 Re 00 ee Sic) MS Sadiog lo aac h 9 193r0u¥d VIO AIVHS Hd SS MSS MS (2 V9A31) 20/710 SONISN NOTLYNIWNALSO SSvV ID ALTIIGVIS S31TS MAMOL WITDOWNOSL SAY 7 9 ¢ i re ¢. 3$3 3N3 “GM WS 3S4 N 0) I I J () ¢e MS MS MSS 2 1 2 NOULWUEOAMOD Day ICH al leccad 1 RADIAM CORPORATION APPENDIX A STABILITY WIND ROSE DIAGRAMS cieB— ies) bo 9 bo RADIAN CORPGRATION APPENDIX A STABILITY WIND ROSE DIAGRAMS According to the data presented in AEC Safety Guide No. 23, the relationships between stability classes and Og are as follows (the values shown are averages for each stability classification...o, is the standard deviation of horizontal wind direction fluctuations). Average Values Stability Pasquill re Classification Categories (degrees) Extremely Unstable A 25 406 Moderately Unstable B 20: 408 Slightly Unstable é 15/40 Neutral D 100° Slightly Stable E SO. Moderately Stable F a5° Stability wind roses obtained at the trailers in the monitoring network are displayed in the following tables. Because of the relatively low heights above the surface (9 meters) at which the wind data is taken, the stability distributions are skewed toward the unstable end of the spectrum. That is, the unstable classes (A, B, and C) have a much higher frequency of occurrence than would be obtained with the Pasquill method of Stability categorization (or with instruments at higher levels). Table 1 depicts the frequency distribution of Pasquill stability categories based on T5 from data collected by M. M. Pendergast and T. V. Crawford at the Savannah River Plant ("Actual Standard Deviations of Vertical and Horizontal Wind Direction Compared to Estimates from Other Measurements", Symposium on Atmospheric Diffusion and Air Pollution, September 9-13, 1974)..--three distinet range patterns of stability class IE B-2293 RADIAN CORPORATION distributions were observed: low, mid, and high, according to the height at which the 6 measurements were taken. TABLE 1 FREQUENCY DISTRIBUTION OF PASQUILL STABILITY CATEGORIES Stability Ceteseries based sa ¢ ee B D E F G “B Gg 223 18 se, <23 Ws, <12 8c, <22 4 <5, <8 2 <3; <7 «8, <2 10 22.5 13.3 218 23.5 2.9 0.4 3.5 33 49.3 11.3 19.4 22.6 15.9 ge (0.5 Oe 91 9.6 6.7 ESE, Sor J 29.5 15.5 265 37 98 5.8 11.7 2.2 28.5 i ce 182 7.0 pee] 6.5 17.1 23.9 <5.6 33.7 253 ot $.3 9.4 17 .t 27.6 22.9. 10.4 HIGH RANGE 334 762 EP 8.0 7.2 iP | 23.9 tL Also, Figure 1 (from D. H. Slade, Meteorology and Atomic Energy, 1968, p. 52) demonstrates that the line represent- ing very stable conditions (which by their nature are associated with light winds) branches into three separate lines near the ground. The curve at the left represents the smallest values of 59 usually observed. The curve that branches off to the right reflects the contribution of very low-level wind direction meander to the total standard deviation. These meandering oscillations decrease in amplitude very rapidly with height under stable conditions. The central curve represents typical inversion conditions. Actually, for a given stability condition, values of 56 will always be greater when the wind is light than when it is strong. This phenomena is most noticeable in the lowest layers. II B-2294 RADIAN CORPORATION €09 om oe er ope ae eee qraset veny stand vworcasamuy HOUTAAL very Unter’ HCIGHY (f1) wooraavay Uusteere fe} e s . .7 : Ce] 5 ite) 15 20 ao 39 STANOAAD CEVIATICN Ce LATERSLL WING ClarcTice C3 (e09) wr FIGURE 1 The vertical variation of the lateral wind- direction standard deviation (0,) for various stability regimes. The curves represent average or typical con- ditions with the exception of the two outer "very stable" lines, which represent extremes. The large surface values of 56 for unstable conditions do not decrease very rapidly with height. As in the case of very stable conditions, the greatest lateral fluctuations during a very unstable thermal structure occur with very light winds. As a general rule, for a given insolation condition, increasing wind speeds are associated with profiles of ore that tend toward neutral stability. The majority of the trailers in the network recorded very light winds throughout the month. Therefore, the stability distributions had a predominance of high To values and, hence, unstable classifications. Those trailers with the highest average winds (and fewest nearby obstacles to the flow) generally had the more reasonable and representative low-level stability class distributions. IT B-2295 II B-2296 Ct Se LT = JAN08Y GILAKINLSTIG SWIVD 40 NFHWNN AWILOlL esevseeeeeoevoe see eee veoeaseeeseeeeenueeseseseeoeoeeeeeveeceevaseoeaeeeseceoseeaeereeepeeeeeaseeaeeeeveeeeseeesee eens oaeaaesens "oo! | es | °6 me *9 me a °S oS °9 es) a] *9 *9 Pile rile *Q 3 LN49NGd 80S ¢ 4 Lb L¢ 82 $¢ 1 Le L2 62 we ed #2 ay Le 9g 6¢ : VWiot en Gee § OT 9I nt ki OT £1 6 om LA BT GI 91 LI QT Tor 149! : ¢ ial "Gh ete % te Le 6T GI OT SI sal | 9 6 OT S ea SI RT G2 02 ° l - § poe eB te 7 iy] = g ¢ Q 3 g J if Q : Z| -~ 1 *0 3 3 at ~ 2] “0 : : te - et WIN g g tT Q g 6 Ot iT Ot 9 L S 9 L 9 6 G34IdS XVW dod) % WiliOL MNN- MN MNM M MSM MS MSS — § 4ass 43s 4as3 3 43N3Q. 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Kee A mr "9 - Wa ne a ey A> imo ar — ee a INTERIM MONITORING REPORT RADIAN CORRECTIONS THIS PAGE LEFT BLANK INTENTIONALLY RADIAM CORPORATION fel. DESCRIPTION OF INSTRUMENT SYSTEMS A. Air Quality Instrumentation Nitrogen oxides are measured with a Meloy Model NA5S20 analyzer. This dual-channel analyzer is based on the chemilu- minescent principle and continuously monitors both NO, and NO. KA Subtraction Circuit in the instrument provides a continuous NO? ovltput, but as mot used in Radian's system. NOz is cal- culated once a second by the computer by subtracting the NO value from the NO, value, thus avoiding any drift which might occur in the NO, output of the instrument. This instrument has a minimum detectable sensitivity of 5 ppb (parts per billion) and a linearity of y2ly. Sulfur dioxide is measured with the Meloy SA185-2A analyzer while hydrogen sulfide is measured with the Meloy SA185-2 anablyzen. the hydrogen sulfide analyzer uses a Meloy Model SO7-1 sulfur dioxide scrubber and the sulfur dioxide analyzer uses a Meloy Model H5S-1 hydrogen sulfide scrubber. The Model SA185-2 1S a continuous analyzer and utilizes the flame photometric principle of operation. The minimum detectable sensitivity for the Model SA185-2 is 5 ppb with a linearity of +1% and the minimum detectable Sensitivity for the Model SAI85-2A is 2 ppb with 2 linearwvety of 21a. Ozone is measured with a Meloy Model OA350 analyzer. This instrument, based on the chemiluminescent principle, pro- vides continuous measurement of ozone. The minimum detectable SCnSMtavaey, us 05 ppb and the lineartty 1s, 21%. Total hydrocarbons, methane, and carbon monoxide are monitored with a Bendix Model 8200 gas chromatograph analyzer. Thais instrument. whieh uses a plume Gonazation detector, has a minimum detectable Sensitivity ot 5 ppb for all three components. The Model 8200 works on a five-minute cycle, i.e., one air sample is analyzed every five minutes, and the results are dis- played for five minutes via a sample and hold circuit. THUS PAGE REPEACES PAGE S (OF WHE APRIL 1977, MAY 41977, AND JUNE 1977 RADIAN REPORTS. THIS PAGE LEFT BLANK INTENTIONALLY ‘Mg DEN 7/=L090-152-03 AIR MONITORING REPORT FOR C=b SHALE OFE PROJECT APRIL. L977 REPORE NO; 32 REVISED LO Octope= 91977 Presented to: C=b Shale” Oil” Proyect United Bank Tower Denver, Colorado 80202 Prepared by: Radian Stat Note: Only revised page changes from original report are included here. Bir B= 15115 8500 Shoal Creek Bivd./P.O. Box 9948/Austin, Texas 78766 (512)454-4797 RA DIAS CORPCRATION TABLE OF CONTENTS I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM------- II. DESCRIPTION OF INSTRUMENT SYSTEMS------------------- A. Air Quality Instrumentation--------------------- B. Calibration Procedures-~------------------------- c. Data Acquisition System------------------------- D. Meteorological Instrumentation--~---------------- IIZ. MICROMETEOROLOGICAL AND TERRAIN FEATURES------------ IV. OPERATING TIME ANALYSIS FOR EACH SITE--------------- V. MONTHLY METEOROLOGICAL SUMMARY---------------------- A. Summary of the Meteorological Conditions over North America during April 19/77----------------- B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during April 1977-------------------------------------- C..2 Summary of the Meteorolioeical Conditions in the Oil Shale Tract C-b Region during April 197/7---------------------------~---------- VI. DATA PRESENTATION AND SUMMARY------- lla etna Teter TI B-15%6 Page II B-1325 -1327_ -13e7 -1328 -1330 ~133t =1357 - hae -1343 -1343 -1345 -1346 “1352 RADIAN CORPORATION TABLE I1if AVERAGES FOR APRIL 1 THRU 30 II B-1559 it 9B =1560 si bg hee A) ou ZLLS divwigtlavd HOLIVItd igh Wild BROS SS ABS OEMRSSBHRRHABDSABRKDAHABDKAARESMR SRS HS SAHSSHSSEHRHESSHHRABOR BADR ADAH SAH SDS MINNA RNS B EHR DWP eee Be wae we e682 i 9* ue C2v a”) OGY | ss BuNnsSsaudd ILTYLIWOYNVE 3NO0Z0 SULXONGChH KOYWNT SAAN EB RRBSHSASARAHSSSBSHASHABASHSANRHRSDSHSKE BD BEARASSHSHHASSHHKSBARSAH BSS KBS HS STHBABESSAAGSSHBAHAANH SAR DORR SHH RADE SNE UaNee ease w e*zee sa vw It6 G* Enel ¢2u 22 eeu are SNOGYVYIONGAK SNVHI3WeNUN ANVRL3W SNOUMVIUAUAH wind SRO BSA HESSHAASHRRBDNHSEA SSBB HSHASHSHS SS ASBRRHSBDSKASSSH HARSHEST SRS SASRSRAASDH RS ASRS ORME ET SS Bo & mm om | yp? a S*pgudl ey ecu Eo@ cr 3145S (208) 30rxO10 YNnsINS HALSWONVYAd (2uS)SUTAOLQ Spd dis 2 OOOH ABE DORRDEA ABABA ES SESH REH EHH EBARARSHRSHKHS ST SEES SHSHSRAH BATH ORHDOHASHRS ASSAD DRDSE SHS SSS SH ee 2 aDenn na ae = Oo ee oe Sill ae agi | Ge c2u eeu gee Ali (ZON) 30LXOTU NADOMLIN (UN) 3GIKXO JIYIIN CXUNJESCIAO NAGS I~ (SIHINI@NOLTL vi dI99Nd (SHVETIIIFANSdNSS aid ESADTONGT Wildbemt 2 duOnvedd fHLMON SHL OL 193dS3Y HLIM SZAYISMGeNOTLOISSIO ONIN FLL 3HWNSSHVA SAStUSUMSeN LVM ad Ad {YNOH Hd SAWWO33SdS GNImM PesL39W DIEND &Sd SwryQUdIT@SNCLivddr sono ure die) PE NYHL 7 MdvV Hud SADVNZAV “ILS 318vd NOoMwuNoOAdHOD DOP RCa Ue aa rt 6 lool _ aie 0° De Of /h 7 Q*y bape b2/h aaa O* 06 Q2e/h 0°2 n* bh*2 Le/h G*2t Oke G*2t 92/h g's pre ey S2/h Gi 0° 6° hesh fan 0° nye ¢2/ Cast 0° Zt 22/h et RY 0°S te/n p Oe oh a om On bd ot Gh O4 tm Ob Bs Ob dm ny > ad © OD Ot Ot ad GF) 08 DD me oh OD On GF mm OA ae A) GD C8 C8 th G&D 68 Of Gn the Ge OR A i AE OS 08 68 00 oe of Oe Oh te ft OD BD ES oD OS OD GE BS 8 OD ME > GD OD OR OD OD OD OS om On Ot OD OO On Ob Oe 08 Oe ft OE ot OS 00 OS OS OB OS ae we Ok mm oe ot ‘I 9° lee 02/h tat ei 6°2 61/h et ft 9°2 eed Waly) ly 0° Lady) BAW Ay) a’ Gre G°@ 91/1 ie G°s¢ 9°sG GSI/h (yy We et bish 10° G* eam Ct/h iy ee Gt 2t/t oe eos coat Tt /b 0° g* Ole Ol/t o* Oe ihe 6 /h Of 9° 9° Q /f Oh 9° Gs Loli g°e2 72 R'2 9 /h ot t. et G /h 0! ey ies h /h 1° 2 \ he Cush pe oe Q° 2/4 ¢‘ OF oa aw) Jiva €20 £20 20 J11S (20N) 3QIX0IO NFJNOULIN (ON) 30IXO JILIN (XON)SJAIXO NIDONLIN (SJHINTSNOTIVITdALTISNd {SUVELVIIW*SYNSSINd (SAFTONVA WILOL*YILIWONVNAd fHLYON BHL OL LIO3d89Y HLIM SAAMDIO=NOTLIIYIG ONIM FLTSHNINHVA SAINOFIIG@ZUNIVUJdWSL (YNOH YFd SIVNGIIdS GNIM {HALIN IIGNI YAd SNYUIOUITN=SNOTLVYLNAINOIISLINN) O£ NYHL tT dv NOs SAE 3AV ATIVG “AT 378V1 ’ MOMWUOAYLOD ~ wel 1 f Sissies oe ee NCTC eT) % - re Q bas oa | a° 9°26G be eye B* G°aKG a° Gerr a e-tTT¢? ue beso n° 6°¢e? v° Le/b as V°ter Ce yesy a° . 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Box 9948/Austin. Texas 78766 /(512)454-4797 RADIAN CORPORATION TABLE OF CONTENTS I. GENERAL DESCRIPTION OF AIR MONITORING PROGRAM------ II. DESCRIPTION OF INSTRUMENT SYSTEMS------------------ A. Air Quality Instrumentation-------------------- B Calibration Procedures------------------------- C. Data Acquisition System------------------------ D. Meteorological Instrumentation----------------- IIL. MICROMETEOROLOGICAL AND TEFRAIN FEATURES----------- IV. OPERATING TIME ANALYSIS FOR EACH SITE-------------- V. MONTHLY METEOROLOGICAL SUMMARY----------------- ---- A. Summary of the Meteorological Conditions over North America during May 1977------------------ B. Summary of the Meteorological Conditions in Northwestern and West Central Colorado during May 1977------------~-------------------------- C. Summary of the Meteorological Conditions in the Oil Shale Tract C-b Region during May 1977--------------------------------------- Vi.. DATA. PRESENTATION AND SS Il B- 1542 Page II B-1550 a ” Be ADADIN CORPORATION TABLE EL PABLE LEE LEST OF TABLES Page DOWNTIME HOURS FOR C-b SHALE OIL PROJECT Site 023------------------------------------ TIB=41565 et nn a -1566 Site 023------------- - - rr ~1567 FEDERAL, AND. COLORADO STANDARDS -————=——-—=———— -1583 AVERAGES FOR MAY 1 THRU 31 Nuree On en Odes NO ec cal lane -1585 Nitric Oxide (NO) --------------------------- ~1585 Nitrogen Dioxide (NO,)---------------------- * =-1585 Sulfur Dioxide (S02) ------------------------ ~. - 1585 Pyranometer-- --~ - --- = - en e- -1585 Sulfur Dioxide (SO,)------------------------ -1585 Total Hydrocarbons---------------=----------- -1585 NSE) Ne SI I SIS -1585 Non-Methane Hydrocarbons-------------------- - 1585 Carbon Monoxide----------------------------- Sa egl oso Ozone------------------------------~--------- -1585 Barometric Pressure--~----------------------- -1585 Total Precipitation------------------------- “-1585 Particulate-------~--------------------~------ -1585 Wind Speed---------------------------------- -1586 LeBel Bla oy ep oa ay 2 ee wo eee A SP SS6 Relative Humidity--------------------------- . -1586 Temperature---------------- rchpceptel pedsat cee nee . 27596 TT B=1543 mA OIA CORPORATION LISt OF TABLES (Ceontd) Page DABLE LV DAILY AVERAGES FOR MAY fs 5 ee TABLE V Nitrogen Omides (NO Meas 9242-2 = II B-1588 Nitric Oxide (NO) --------------------------- - 1588 Nitrogen Dioxide (NO,)---------------------- -1588 Sulfur Dioxide (S0,)------------------------ -1589 Pyranometer- --------------- ee nn en enn nae -1589 Sulfur Dioxide (SO,)------------------------ -1589 Total Hydrocarbons-------------------------- -1590 Me thane- ------------------------------------ - 1590 Non-Methane Hydrocarbons-------------------- -1590 Carbon Monoxide----------------------------- -1591 OZ OTC a a am a a i ir ee a - 159% Barometric Pressure--<----------<-<-----<-=---- =159% Total Precipitation------------------------- =1592 Particulate--------------------------------- =1592 Wind Speci =n. se pee es See nee -1593 Wind Direction---------------------<-----<-- -1594 MUS utes 2 eS aS SS SS -1595 SASS a SN) 9 ice 6 a) i a ale te -1595a MAXIMUM FIVE-MINUTE AVERAGES AND TIME OF OCCURRENCE? 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SL/STS SL/97/T> SL/9T/9 @SL/91/9 SL/9T/9 SZ/9T/9 SZ/9T/9 out | /21eq Pats g°2¢ eas C' ys p°ss 0°9S ¢°09 Z°S9 8°S9 6°19 (,w/3n) uotjetqUedu0D 120 LOT a 681 Sit 98T LST SIT int 61T 96 UuoTIDOAITG PUT T S OT S OT I L L 9 ¢ (ydu) poods put Sp:00 G2: 9¢ OL: It So:¢ SO:0T (HeRISNE 0$:22 Op:12 gg: 00:¢ $L/8/¢ SG) tae SULLA S/S SL/L / Se SLI PELE 9L/L1/6 IL/L1/6 92/81/6. 92/8 /6 out 1/93 vq O'S Oon O°TEe mais 8°2E 6°S¢ €°78 «= 8°60T )=s«s TTT )=—ssT'68T = (gS) uotzesquadu0D 020 OT 6 8 l 9 S p ¢ Z if 93TS ANITESVa ONTUNd SdOVUaAV “OS UNO JNO ISHHOIH NIL 8T-f STIPL 435 so Table 3-19 2 1- HOUR MAXD2¥ CONCENTRATIONS Constituent (1974-1975) By Month Dec. | Jan. Feb. Mar. Apr. May- June July _—= Aug. Sept. © Value (¢/m3) 3.6 17.4 2.6 7.6 32.8 7 (Pa: 7.6 20.8 33.9 12.4 9.1 20. ° Date 11/1 12/8 1/14 2/20 “3/7 4/12 5/30 6/23 7/14 8/4 9/27 — 10/2 Time (ST) 13:50 21:48 16:10 10:55 10:05 11:35 14:50 4:45 13:10 13:20 11:30 8:30 Wind Direction (Deg.) 204 102 134 275 190 266 292 134 157 299 318 182 Wind Speed (MPH) 5 1 5 12 8 3 7 7 1 5 6 9 Value (ug/m3) 0.2 97.9 50.6 5.0 i252 8.2 72 337 13.2 59.9 9.3 7.6 Date 11/1 12/21 1/1 2/20 3/29 4/5 5/4 6/23 7/28 8/20 9/1 10/° Time (MST) 21S “LSS 14:30 11:30 22:05 10:05 11:00 12:45 19:15 4:15 8:45 232555 Wind Direction (Deg.) 191 156 358 236 201 184 186 199 184 171 211 228 Wind Speed (MPH) 8 7 4 18 3 18 27 ll 1l 2 12 10 Value (ug/m3) 32.8 25.8 53.4 2352 AS 2167 4434255 567.9 18.2 16.9 1163 200 Date 11/1 12/19 1/26 = 2/21 3/25 4/25 S/S 6/16 7/11 8/17 9/2 10/: Time (MST) 1:35 15:45 14:05 5:00 9:00 20:25 10:50 13:45 22:55 12:35 19:00 23: Wind Direction (Deg.) 123 324 176 156 154 288 147 304 127 219 116 125 Wind Speed (MPH) 5 7 10 5 8 ll 5 15 5 7 3 2 Value (ug/n3) 13.0 20.8 5.9 De ele T 2.6 18.2 27.4 14.5 16.3 2.4 13.¢ Date 11/6 =: 12/20 1/25 2] 2Z mn 8/5 4/7 “\5/25— B6/az 7/23 8/17 9/17 —-:10/ Time (MST) 17:00 = 1:15 14:25 8:45 8:30 3:30 20:55 0:00 0:40 14:10 4:55 6:1 Wind Direction (Deg.) 120 127 275 107 110 291 82 123 114 275 88 121 Wind Speed (MPH) 1 6 9 2 5 5 1 7 7 5 2 7 Value (ug/m3) 5.2 128.5 Sae3' | 3825 _ “S0.8 49.1 S6.4 33.0 10.6 26.5 20.6 41.7 Date 11/29. 12/10 ~=—-1/S 2/26. 3/3 4/13 5/2 6/23 7/17 8/2 9/7 10/é Time (MST) 21:10 6:20 11:50 2:25 22:50 17:35 3:20 9:20 19:55 11:05 4:25 4:20 Wind Direction (Deg.) 80 12 178 63 60 284 103 212 170 317 114 218 Wind Speed (MPH) 3 0 9 0 3 5 0 5 8 7 7 10 (1975-1976) 020 Value (ug/m}) : ’ 2 3.5 12.4 1st 7.6 9 189.1 10.6 Date 11/15 2 2/1734 4/4 5/22 7 6/1 7/13 8/24 9/18 10/17 Time (MST) 18:10 1:35 14:25 9:45 9:45 4:35 4:00 11:35 11:55 3:00 4:35 Wind Direction (Deg.) 113 99 296 175 173 102 123 279 255 96 86 Wind Speed (MPH) 4 3 10 8 8 (2) (2) (2) 6 3 7 vale’ (ley?) 0 19.1 51.4() 7.20) 54.6 Ize "135. 2559 7.2 2.6 9.6 13.5 Date 11/18" 912/156 ol /S 2/6 /22 4/28 «5/18 s) 6/5: 7/18 8/3 9/7 10/2 Time (MST) 12:40 7:10 11:10 11: 14:20 6:40 10:05 13:15 13:00 10:20 8:15 3:35 Wind Direction (Deg.) 241 139 129 311 144 271 221 194 315 198 72 161 Wind Speed (MPH) 12 5 14 3 9 1 13 22 14 15 2 3 Value (ug/m3) 11477 5-2 28.2 1058 - 25.40 Je x2 618. 2 F2.8 14.3 4.1 8.5 5.2 Date 11/12 12/6 1/5 2/1 3/13 4/10 5/16 6/8 7/11 8/12 9/4 10/3 Time (MST) 11:20 23:40 7250= 210200 | 1230'S 3250" e3600.. 2220 3:20 15:10 5:50 2:10 Wind Direction (Deg.) 298 108 132 JCM 128 104 99 46 89 156 349 107 Wind Speed (MPH) 4 5 6 7 l 4 1 2 7 0 8 Value (yg/m3) 13.7 13.5 16.9 eee pup Y3E0) 6.7 1.5 13.7 6.5 6.3 (2) Date 11/1 12/7 1/8 2/1 3/14 4/16 = 55/3 6/17 7/6 8/6 9/23 (2) Time (MST) 13235. 14:35 ‘“Selo§ 7255 -. 0-10 10:25 5:40 2:15 2:55 4:50 7:55 (2) Wind Direction (Deg.) 266 125 101 115 CALM 266 117 96 88 118 116 (2) Wind Speed (MPH) 6 2 5 10 6 8 2 1 7 5 (2) Value (ug/m3) 2281 451020 5.9 3.0 4.6 4.3 4.6 8.7 10.0 16.1 13-7) 14eS Date Wy Sezy14 1/1 2/4 3/14 4/8 5/20 6/15 7/16 8/29 9/9 10/5 Time (MST) 3:20) 232550 14:20 12:30 4:30 9:55 5:10 8:10 5:15 125 5:35 oes 342 179 330 119 179 123 106 3 4 2 4 7 1 0 Wind Direction (Deg.) 103 291 286 148 163 Wind Speed (MPH) 4 9 6 19 7 (1) Side-by-side monitoring of H2S in Trailer 023 and of SO> in Trailer 021 was initiated, as a data reliability check, for three months beginning 1 “January , 1976. SO, analyzer at 021 are reported in the row for 023 for January, February, and March. (2) Missing Data. *\11 data below minimm detectable limit. Therefore, no SOp data were taken at 023. 456 The data from the second Bw A + 4 i BIOLOGICAL BASELINE STUDIES TRACT C-b Ti-ci THIS PAGE LEFT BLANK INTENTIONALLY Table ET C-4 Pi¢-s ie (C=60 i G7 i C=s iy E-9 it ¢-10 ee C= 11 TABLE OF CORRECTIONS* AND ADDITIONS IL C-1,, Jerrestrial Wildlife, Studies Interim Monitoring Report Corrections Description Production and Utilization of Bitterbrush in the Pinyon-juniper Habitat, 1976-77. Estimates are based on lengths of new shoots. Production and Utilization of Bitterbrush in the Chained Pinyon-juniper Habitat, 1976-77. Estimates are based on lengths of new shoots. Production and Utilization of Mountain Mahogany in the Pinyon-juniper Habitat, 1976-77. Estimates are based on lengths of new shoots. Production and Utilization of Mountain Mahogany in the Chained Pinyon-juniper Habitat, 1976-77. Estimates are based on lengths of new shoots. Production and Utilization of Bitterbrush in the Pinyon- juniper Habitat, 1976-77. Estimates are based on weights of new shoots. Production and Utilization of Bitterbrush in the Chained Pinyon-juniper Habitat, 1976-77. Estimates are based on weights of new shoots. Production and Utilization of Mountain Mahogany in the Pinyon-juniper Habitat, 1976-77. Estimates are based on weights of new shoots. Production and Utilization of Mountain Mahogany in the Chained Pinyon-juniper Habitat, 1976-77. Estimates are based on weights of new shoots. Page IT i Dy DT TE 1 | it it * Corrected tables bear the same table and page numbers assigned to them in the October 14, 1977 Interim Monitoring Report. bY Cris Cy C6 Cas) C-10 G-ald: C-1z C4 TABLE OF CORRECTIONS* AND ADDITIONS il C-2,, Aquatic. Stidies Interim Monitoring Report Additions Table Description Page fi C-1 Periphyton Biomass at Piceance Creek, it C-4 October 20, 1977 to C-6 Oa Benthic Study - October, 1976 Il C-7 Ti C-3 Benthic Study - January, 1977 It G6 1 a Benthic Study - February, 1977 Einge8 TiNC=5 Benthic Study - March, 1977 II C-10 G G-ai i C-o Benthic Study <“April, 1977 iM Cei2 G C=13 GS Benthic Study - May, 1977 LE G-14, 5% C-15 Ii ¢-8 Benthic Study - June-July, 1977 PL C-96.4 G-17 RC Benthic Study - August, 1977 Td €-18:°6 g-19 LT ACSLO Benthic Study - November, 1977 ci C-20 TL -C-1% Fish Population Sampling, it €-21 7G November, 1977 - P-3 C-22 i C-12 Fish Population Sampling, II C-23 November, 1977 - S-1 eiC=15 Fish Population Sampling, il C74 November, 1977 - P5-A LI sG=4 Fish Population Sampling, Piica75 November, 1977 - S-2 4 we Corrected tables bear the same table and page numbers assigned to them in the October 14, 1977 Interim Monitoring Report. i C-i94 TERRESTRIAL WILDLIFE STUDIES Lanes ‘Ob es a CEDEN CAA to i hes © oa \; ra i yt. 2 [sts pay eS PS - a VN ode, Pee er OUR ee 2.2¢ one ie AS ty, ee gw re ru yi BN. es > Aer ees ’- A ty Se a oer oe * pas «@ qi a oe ou iy sh Pe 7 ed prey) fs be 4 bs >, . wae 7 tek ar ae i ma Se. Bit Py go yt eae ott “7 r oe 7 > > 7 : st j ra | . ie : ee ee a ee Pop ae a fc a eae hk rier & ta iu be by oy a Se er +) ven ~ F Ly ive) x ie a Tee hele) t Je eed ew, ibe ont cg ae ins nen : “sane . > eee We Cake ale Be DP c * a. Aine a ° = oe he & Ar rq we t 7 yf LM Pe oes nD on oe : J ~ - wy = ae - iy “ ves * w a wr 4 Shs Fy 1° 7 vir ae fr Sen ee ¥ ht ; 7 we ae fins) ot wie ae rd “~e es Chet id Na \ pray 4 iF. 4 she! He ny oe 7 hy 2 wy v alk a > hee ett oe! iat Bes its ii at 4 Af 1+ ag ie oS ea fe al ¥ i eh a oo we - 4 iy ; Lon vi, , ees ats ? Sire oa ai ee en iy Aa Ae t>. y fh s Es Oe fea OT Nee © eh Oe Tt etl, Ta ly Mag a oh ie me Fe! A Paria Fn) ore Ld yb ued A er Ae, a’ ren wi “) Al - Pests H = , ua oe a r . ‘ eae me a) Pil ms q 3 ae take . oats Fe) By) } yw tie Th, 4, 0) ee oe >| ‘oa %,, fe © eee raid. ee tnst fo TE a i ae ee aN CE mt vf we a ag! ch Caeiene Orbe reas se ao. yarn Tad > Potir Man ae eA Beatty te of i Sihalirts =G . wor ela " a al APer okt et ee tu bad ie ati fay. ie we ’ ar aon me ina . 4a si oy ; Pe 7 .*s ‘" g« y “a 7 A ve nae ras \ rp in, 4 ay he ve S o 4 \ i \ oe ee A 9 FO To oe ee aa ow a Oe Aro Pit a aR! Rie Pree ao ee es 4ap lal aes “iy - x a PB AP bai he _ { ; ip, ae. ~ wees mo Te oe ae . cl ’ bay 7 aie ‘Y ne tee \ LTS ia ies @ Fs ye ie is, ww hl a jg a, Wag: a ‘ Sy : “) “vp ana a ae i seats et fa AY ie (ha Py eee ag Eh 3; ean) . Laue ae eR O 4 p fy Nee PLT Naor ; Pe oN , 2 ia ate Rte | phn . - a ee aie 7 b ee iy BAN ad * a. re Sa Becta ; , Shey Laan ee ive. 2 A et os es Fe aT eN carla POPs Ie ar an f Bie GEN i 9 ee » he ae hai sy ear I BO ; ath ah mas iia Ct Poe ener Eb Biology II C-1 Terrestrial Wildlife Studies Introduction Shrub Production and Utilization The following data updates the tables found in the October 14, 1977 Interim Monitoring Report, in which some of the tabulations were incomplete. The tables retain the same table and page numbers as in the Interim Monitoring Report. JE Gaal THIS PAGE LEFT INTENTIONALLY BLANK Pies 2 INTERIM MONITORING REPORT CORRECTIONS THIS PAGE LEFT BLANK INTENTIONALLY Table C 11-4 Production and Utilization of Bitterbrush in the Pinyon— juniper Habitat, 1976-77. Estimates are based on lengths of new shoots. A 3 C PRODUCTION: lensth Lenztn of snoots UTILIZATION : of new shoots in remaining in in percent fal pean) soring (mn) ome Transect liean + SE (H) veam = So Ci) C= == X 100 P/ i-C=7 8327 (100) 5525 (106) 61 ey i—C—2 10546 (10C) 36+5 (100) 66 P/J-C-3 107x9 (100) 42+4 (100) 61 ey jae 4 64+5 (100) 2642 (100) 59 Pp/jJ-T-2 115415 (100) 29+4 (100) 74 ey ness} 85+7 (100) 2643 (100) 69 Tie —7 Ch-T-1 Ch-T-2 Tabte I TiS Production and Utilization of Bitterbrush in the Chained Pinyon-juniver Havitat, 1976-77. Estimates are based on lengths of new shoots. a B CG PRODUCTION: length Length of shoots UTILIZATION: of new shoots in remaining in in percent fall (mm) soring (mm) Mean + SE (i!) Mean + SE (N) c= 52x 400 426412 (100) 47+5 (100) 62 196+23 (100) 65+8 (100) 67 41349 (100) 1622. (100) 86 485422 (160) 42+4 (160) TT 308429 (100) 56z5 (100) 82 P7As26 (C1GO)! | 96+12 (100) 65 if C-8 ~~ Table € 11-6 Production and Utilization of itountain Mahogany in the Pinyon—juniner Habitat, 1976-77. Estimates are based on lengths of new snoots. A B C PRODUCTION: length Length of shoots UTILIZATION: of new snoots in remaining in in percent fall (mn) soring (mm) Transect Mean + SE (&) Mean + S= (i) c= “52 x 100 P/s5-C—1 5143 (100) 26+3 (100) 49 P/J-C-2 76z5 (100) 3525)(90) 56 P/I-C-3 6446 (100) 2142" C150) 67 P/J-T-1 5724 (100) - 1422 (100) is) P/J-T-2 5544 (100) 28+4 (100) 49 P/J-T-3 5743 (100) 22+2 (100) 61 Pi C-9 Table C II-7 Production ana Utilization of Mountain Fahnogany in the Chained Pinyon-juniver Habitat, 1976-77. Estimates are pasead on lengths of new snoots. A - <5 C PRODUCTION: length Length of shoots UTILIZATION: of new shoots in remaining in ; in percent fall (mm) spring (mm) Transect Mean + SE (33) Mean + S= (N) c= AS? x 400 Cx-C=1 6543 (100) 20+2 (100) 68 Ch-C-2 7845 (100) 2643 (100) 67 Ch-C-3 10929 (160) 2543 (90) 77 Ch-T-14 1172135 (100) 34+7 (100) 69 Ch-T-2 Gt29 (70C) 1922 (100) 73 Ch-T-5 114415 (100) 3945 (90) 66 if C-1€ ef ern, Table II C-8 Produccrion ana Uvulyzatiom OL Bitterorush im the Panyon— juniver Habitat, 1976-77. Estimates are based on weights Of new snoots. A PRODUCTION: weigat Of Pew SNOOtTS 1.7 B Verght Of “Snoots remaining in C UTILIZATION : in percent fa liens) spring (g) Treansect Hean = Se (im) Mean + SE (i) c= “52 x 100 D/s-C=4 0792.007 (100) .055+.006 (100) 30 P/J—-C-2 .128 (100)* .075 (100)** 41 P/J-C-3 .132 -(100)* .067 (100)** 49 P/j-7-1 052 (100)* 031 (100)** 40 P/j—2-2 M10626011 (100) -045+.009 (100) 57 Py gan-s .104+.011 (100) .047%.006 (100) 54 * Estimates obtained from linear regression equation ** Estimates are means of all n shoots combined TCL fable di; C€-9 a Production and Utilization of Bitterbrush in the Cnained Pinyon-juniner Habitat, 1976-77. Estimates are based on weights of new shoots A 3 C PRODUCPION: weight Weight of shoots UTILIZATION : of new snoots in remaining in ~ in percent fa. Ga) soring (g) Rransect Mean + SS (3) Mean 4SB (i) c= 452 x 100 Ch-C— . 168 (00)* 086.0100) *4 49 Ch-C—2 .300 (100)* 1751000 }F* 42 Ch-C-3 aes. C14C100) -029+.004 (100) 82 Cn-T—1 2708 GL00))* 073+ (100) = 74 Ch-T-2 -383+.039 (100) ©153+.018 (100) 60 Ch-T-5 2 3734.040 (99) »2754.041 (100) 26 * Estimates obtained from linear regression equation ** Estimates are means of all n shoots combined bs ET C2 fabie Li C- 10 Production and Utilization of Mountain Majoseny in the Pinvon-—junioer Habitat, even stinates are basec on weishts of new shoots. : F ee TE A B C PRODUCTION: weight Weight of shoots UTILIZATION: of new snoots in Semen s an in vercent fata ie) sprinz (=) Transect ean = Ss (#) Iiean + SS (1) c= == x 100 P/I-c—1 .086 (100)* 053 (90) == 38 ?/g-C-2 ~ 1872.022 C100) -0289+.015 (50) ; 55 P/i-C-3 2125+.009 (1C0) - -052+.C058 (99) 59 P/j-T—1 0144+.018 (100) BOsZ2 08> (100) 76 P/J—-B-2 2095) (100) = 071 (LOOvSs ZS P/J-T—3 - 102 (100) * -074 (100) ** ZT * Estimates obtained from linear regression equation ** Estimates are means of all n shoots combined Te C13 Table C II-ll Production and Utilization of Bitterbrush in the Chained Pinyon—juniner Havitat, 1975-77. Estimates are based on | lengths of new shoots. ~ h B C PRODUCTION: weight Weight of shoots UTILIZATION: of new shoots in revainaAns- in * in percent fall (gs) spring (2) Transect Hean + SE (K) Mean + SE (H) c= 42 x 100 Cn=C=4 . 1062; 010; £100) -0514.005 (100) 52 Gn=ae—2 .156 (100)#* .080 (100)** 2 * eS Ch—-0—5 .236 (100)* .094 (90)** 60 Ch-T~1 .240 (100)* .068 (100)** 72 | Ch—T~2 ~2854.028 (100) .065+.009 (100) Fi Ch_-T-3 © 2722.058 (100) .049=.026 (90) Bo * : : : : 3 Estimates obtained from linear regression equation ** Estimates are means of all n shoots combined a& Pali a ET Ca AQUATIC STUDIES Te”. €=2 Aquatic Studies Introduction The following are data that were not available for the October 14, 1977 Interim Monitoring Report. The scope of the studies and methods can be found in the above mentioned report. The benthos data furnished by the U.S.G.S. is a draft, with indentifications of some species tentative. 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Gi 0°OOLT = ULraW 0°9¢ vST S°S Sv 0°9P SOL S°8 6L 0°OLT SEC S°9 cL 0°9T ZI[T 0°86 86T Sc 5. os 0°02 02L 0°9T O71 0°9 eye Sav, L9 0°8Z 9¢T Ors 69 OF Lt aie (3) 2UusTOM (uur) YAsUST (3) 3yYsTOM SUdT (3) 1ysTOM (ul) YISUST yNoL], Yoo1g aoeq-popTyoods SLoyons UuTe}UNOW T-S NOLLVIS LL6T YAGWSAON ‘HINO LYVMALS AO ONITAWVS NOILVINdOd HSIAd él-9 Il SEGeL Po DOTTOO YSTF ON V-Sd NOILVLS LL61 UAAWHAON “WSIIYO AONVADId AO ONI'TdWVS NOILVINdOd HSI eso il SL aeL Id. C-24 POD9T TOD YSTF ON é-S NOILVLS LL6T MAQWHAON “NATUD LYVMALS JO ONITANVS NOILVINdOd HSI pT-O II 9TqeL IT C-25 = Se t 7 a = i Tes, Y Tit OTHER STUDIES Only two of the programs in the Other Studies categories were included in the Interim Monitoring Program. These are the Revegetation and Microenvironmental Studies. The other programs were completed during the Baseline period, including the Fish and Wildlife Management Plan, Scenic Studies, Aerial Photographic Studies, and Archaeological Studies. Corrections to both of these studies are contained in this supplemental report. The entire revegetation section has been corrected, and completely replaces the revegetation report in the Interim Monitoring Report. The table and page numbers are the same as those which appeared in the Interim Monitoring Report. iti THIS PAGE LEFT BLANK INTENTIONALLY INTERIM MONITORING REPORT CORRECTIONS I-ET-'-B Revegetation Program Introduction Evaluation of disturbed areas revegetated during the baseline period was begun in 1976. These studues are designed to measure the progress of the revegetated areas over time and to help evaluate trends occurring in the reestablishment of desirable vegetation cover as defined by the Environmental Lease Stipulations. Scope of Study At the onset of these studies all disturbed areas (mostly drill pads and their access roads) were documented using photographic techniques; seed bed treatments, seed mixtures, and methods were also recorded. In 1976 each pad was evaluated using a combined occular and clipping method combined with phytosociological sampling techniques. During the Interim Period Monitoring sampling has been refined to include eight drill pad sites that are representative of major vegetation types within the study area. The categories sampled include, disturbed areas within upland sagebrush, bottomland sagebrush, chained pinyon-juniper rangeland, pinyon-juniper woodland, and agri- cultural meadowland. Methods Two major parameters were sampled on each disturbed site: 1) species frequency and cover, and 2) herbaceous standing crop. Species frequency and cover was sampled using 10 one-centare quadrats permanently located in each disturbed site. Frequencies were noted by presence; percent cover of each species, litter, soil, rock, mosses, and lichens were estimated. Herbaceous standing crop was measured at peak season (in August). Five, one-centare quadrats were randomly located in each disturbed site using a random number generator and clipped. Four fractions were clipped to ground level and weighed. The four fractions separated were, annual grasses, annual forbs, perennial grasses, and perennial forbs. In addition to the five clip quadrats, 50 one-centare quadrats, including the clip quadrats, were estimated occularly. Results and Discussion The results of the combined phytosociological and standing crop measurements are presented below. These data have not been subjected to analysis at this time. EYE B=1 ( r, f | X 5°8¢ o7 OL l i 9°5 2°0 I 1 Eee | S*0 ‘ 9°SS 2°16 eae ? Meo) 2 bez 0°¥22 sl AONANOTUA YAOI %) AONINORUS SONRMINIDO (4) UsAOD X UACD zLWIAVNO AALLVISY JALLVITe JO SLOTd JO # 30 dZ1S LLoT dNAr VIVO LOTd NOTAVLEDTARY - ‘ds velospt2s TTY ZIWS ‘ds BIUDoOy uorkdousy AUOITLVO/SITITS T-0S & I! 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OTaPRt Ga OT 570 OT 1E 0 O°T Zul POUTIIOD voodtesovyds AONANOR ~~ USAOD (%) AONENOUNA TONAMUNIIO (s)uqAOD X = UAOD zs LMVIND AUODTLVI/SALOdS UAILVIE = SATJ.VISY 40 SLOTd JO # JO UZIS 9-95 # GNVIS salve ¢ 70 2 (penuryuod) gel TIT Atavus lars AONANOTUA SALLV Ide isa UTAOD SALLVTSY (%) AONENOTYS FONTAUNIIO JO SLOTd JO ae (S$) UdAOD X £46 JNA — WLVCE LOT el womel LV LED EATU ‘ds sodievsti1oydus | ezewos edrt4s ‘ds e[ostts SSUIQ [RTUUdIOg vptouowAy stsdozAig ‘ds untptdoy TTysMOpot eTnddey ST[TOVIZ LVILOTOOY ‘ds etysoy eyeuutd eluteinsseg ‘ds vyquejdArg vosol vtlieuusjUuy umzoydoyst 1} uotkdorsy ~ esd untneodyova uorkdossy ee le] uMTpoU9ZUT UoLAdOIBY UTA) & Lvudvn 1O AZIS UMLOJLOSOpP UdTAdOISY ANOOULVO/SIIIIdS Ts tt ONVIS — weg bie Be 7 qioj TvTuUd.Og UMOWIUN s¢ BIVUOPTL} LTYSANG O's BPTOUDWAY stsdozki9. S72 snojuosie snutdny $° 22 "ds eBtysoy Ges snjzeutumoe stdei19 ; Coe uNnq[e umtpodousy ! 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X wgAod gS LVUCV) RNOYALVO/SAIOdS FAILVIGN =: SATLV ISU , JO SLOTd SO } dO dZ1s L£LGT ANAL 8i-9S # GNVLS VIVO LOTd NOLIWISOSArTe | Cet Thr SEaImp ee LErB-S Byrwoo edtiS “ds eTOs[es ; eptouswAy stsdozA19 ‘ds verysoy wunzoydoyst1} uorAdoisy dete) Ohad cv ¢ umtnesAyoes1y uostAdoisy lee jeod 00T L TTYITWS UOLAGOLOY 19 = 62 2 T0 0'L rut UmtpoulLojzut uorAdorsy ADNANOTUS UAC (%) ADNENOIU FONSMUNIIO (4) UIAOD X YAO) x J.vRicrvno RUODHIVO/SH OAS JALLVI = SATLVISU JO SLOTd 0 4 JO i218 LLGTA ‘ae GI-9S<>, ¥ GNVLS baa! | VIVG LOTd , nu VLAOTARI ee ee il ii ; bat tit 5-9 pee 6*OL 08 ieee 0°S6 i ‘ds vqosTes =a 8 O- TL Of 0°9T STTBVUTITJZJO SNIOTT TOW ZY v0 Sees T tO S'0 i ‘ds uoro31ag Cow. y°0 ene ae iL T’°0 $*0 i ‘ds elureinosag (je LS OT | ii S*0 0°S u RURTOTAOPNT eIsTuoq.y 8°02 S*Y OS ee 9°0 0°9 u Tryytus uotkdordy AONSNOTUS YEACO (%) AONANOTA TONTUUNIIO (s)ugAoD xX wsAOD 2 = Jucivnd AUODTLVO/SHIITdS SALLVIGY = AALLVISY 4O SLOTd JO 4 JO dZ1s VIVG LOTd NOLLVLUDEARY : Ltt B-10 9°2 9°0 SS = I 0 S*0 é (t8unz) stTeqzzng 9°2 o°T 01 i oat T'0 0°T ‘ TTpooy xorg 0°8T Shadal OL Ih b°T 0°rI Fa eBptouowdy stsdozA1g Sor qe at a 2 £°0 gz ‘ unLOTJTSuep umtptdoq ‘ds xouvg wWN10}903 snuio1g umpnvodAyovaiz uorAdoisy AONANORUL YFAOD (%) ANANDA FONTUUNDOO (4) UaAOD X UwAOD x LVuavnd RIOVELVO/SAIOTdS FALLVISY = SATLV ISU dO SLOTd HO # JO d2Is " L“6T fir oT E74 GNVIS tiga VIVE LOT iygsl LVLIOATY ane onc atrant ‘egy ~ III B-11 Ma, Z°2 £°0 OT T T'0 Ean re vv S‘T cone a7 £°0 $*0 ait ade 6°T 0's a7 9°0 O°T — vY yh 02 Z O°L ‘ Gy. 6°28 001 aa a ‘ a5 8° IZ OZ l S" HS i 2% Oa ee i ZU 0°2 yt ADNINOMU ULAOS (%) ANAND TONRRINODO (4) UIAOD X wAOI gs — Lvucvnd UALLVIGY =—- AATLVISY JO SLOTd JO ¥ JO 21S L£26T ANN VLVG LOTd NOILVLESAASU le ( BI vWOD . edtyS BTTOFTSUOT XOTUg SStIN [TeTUUdIOg BptouowAy stsdozAio "ds umutaedsoyjTT BIVISTAD LPTLOTOOY snjeutumoe stdor9 ‘ds eaipucwo) UT. snuueyzosk1yy wN1O}99} snuio1g "ds snuoig ‘ds sn~eseiqsy BIVIUSPTIZ VISTWO LY umtoudoystz3 uorAdorsy TLyjtwms uortkdossy WNT powtojutT uoLrAdoidy uMtoZIOSOp uorAdOIsy AUOVULVO/SILIEdS « youed3 yf CNVLS LEY B=1:2 19-Mi2 0-M13 0-M14 O-MLS 1$-M16 22-M17 DECEMBER 1976 JANUARY 1977 emperature fenperature} °c Precip, aC cm. |Min. Max.| oe eae 1,52 -32 20 1.47 -32 10 0.73 -21 13 0.61 -27 11 0.75 -6 12 1.47 | -17 14 0.81 |-28 24 2.08 232 20 1.33 -34 15 1.83 -29 43 1.78 -30 45 -22 4 1.24 -28 11 “26. 14 | Tar--h-3e 44 -28 40 Sigii/s - 30 12 =55 16 1.87 -33 il -3] 25 1.40 -31 li Missing data July data is missing {5 MICROLNVIRONMENTAL SPOT CUIECK DATA* FEBRUARY 1977 MARGI 1977 temperature ‘emperature Precip. ec Precip. sd 2 cm. cm. Min. Max. Bey Ai Ary 1.98 1.17 -20 17 2.26 1.63 -20 13 2.01 1.42 -20 21 () 1.14 ~}*16° - 1S 1.98 1.65 “11 16 1.73 a0 7 -19 20 () 0.02 |-16 22 1.78 Waa -19 20 2.34 1.05 -20 26 Teo Wody/ “18 17 2.01 1.55 -21 21 i 0.00 {-17 20 1.30 0.91 “17 20 1.60 1.35 -18 20 0.76 G3) -23 DS 1.85 -21 15 APRIL 1977 cmperature Min. Max. iy 20 -18 30 “17 20 -18 32 -18 29 -16 28 =}7 28 15 32 -15 31 -16 31 “17 28 4.79 -16 31 2.24 cpl! 27 2.87 -16 25 3.79 -15 29 202 -20 24 4.16 -17 af TABLE III C-7 MAY 1977 temperature Precip. SU 1.86 2.03 -9 33 1.27 8 30 1.65 -10 36 0.71 “9 31 1.73 -5 32 z.01 -7 30 Ya35 -8 37 1.22 -8 38 2.09 -10 35 1.78 -7 30 1.73 -10 34 1.96 -15 30 1.68 -6 31 1.50 -7 33 1.58 -8 30 1.86 -9 31 JUNE 1977 Temperatur AUGUST 1977 Temperature Precip, em. Min, Max. aie, | areata 1,54 1 40 9,75 2 36 2.46 1 40 4.06 Celie ey 3.18 5 36 $.79 4 38 4.57 6 44 4.65 3 39 5.61 2 32 2.74 5 35 ASA 1 37 3.43 3 33 3. 30 4 35 4.06 5 33 1.78 2 34 2.29 1 31 Bolle MICROENVIRONMENTAL DATA, Table III C-6 TOTAL PRECIPITATION (mm) reer eae lhe tatrl aefoeb tsrall val | coil amallors PINYON JUNIPER WOODLAND sol (6.41 29.91 0-0 | 6.9 | wire CHAINED PINYON-JUNIPER RANGELAND BOTTOMLAND SAGEBRUSH UPLAND SAGEBRUSH *missing data ( ) collected at corresponding spot check stations be al See » r ; 5st LIL. .¢ Microenvironmental Programs Introduction The following microenvironmental data include: 1. The soil moisture data for September, which was not available for the Interim Monitoring Report. 2. Corrections to Table III C-6 of the Interim Monitoring Report. Methods Methods for the soil moisture studies are outlined in the October 14, 1977 Interim Monitoring Report. i Bi Ora THIS PAGE LEFT INTENTIONALLY BLANK ET C22 (A “7 * INTERIM MONITORING REPORT ADDITIONS THIS PAGE LEFT BLANK INTENTIONALLY CN Yable Iti C-1 PLANT-SOIL WATER POTENTIAL DATA September, 1977 PROBE SOIL-WATER VEGETATION TYPE STATION DATE NUMBER POTENTIAL BARS Chained Pinyon-Juniper 1-1M 9/22 is (1) Rangeland 9/22 18 Aree yy) 2-2M 9/23 2 es 9/23 19 . 7-7™M 9/23 i ili 9S) 9/23 24 L235) Pinyon- Juniper 5-5M 9/22 5 a2) Woodland 9/22 22 Ze8 (3) 6-6M 9/22 6 19.0 9/22 ZS - 0-14M 9/23 14 20.0) (2) 9/23 Sil 202502) 0-15M 9/23 15 Sor 9/23 52 * Bottomland Sagebrush 4-4M 9/23 4 Zi as 2) Community 9725 21 Zia 0-9M 9/22 9 Lt 50 9/22 26 L255 0-12M 9/23 12 O60) 9/23 29 5.2 42) Upland Sagebrush 3- 2M 9/22 3 555 Community 9/22 20 13.0 : 0-16M 16 7.5 42) 33 10.8 42) Bunchgrass 20-8M 9/22-23 8 (2) Communi ty , 9/22-23 25 (2) 0-11M 9/22 11 us 9/22 28 * Rabitbrush 0-10M 9/23 10 = Community B25 on * Mixed Mountain 0-13M 9/22 13 9.8 Shrub land 9/22 30 fail Annual Weed 0-17M 9/23 WW dS ae (G2) | Community 9/23 34 (4) bs No reading due to dirty probes (1) faulty probe (2) Improbable reading due to a difference >3uv between read and input short (3) Questionable (4) Broken probe BEinC-3 THIS PAGE LEFT BLANK INTENTIONALLY an INTERIM MONITORING REPORT CORRECTIONS = oo + : t ae