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F     ILLINOIS     BULLETIN 

ISSUED  WEEKLY 
MAY  13,  1918  No.  37 

-second-class  matter  Dec.  11,  1012,  at  the  Post   Office  at  Urbana.  111.,  under  the  Aet  of  Aur.  24.  1912.1 


HYDRAULIC  EXPERIMENTS  WITH 

VALVES,   ORIFICES,   HOSE,   NOZZLES, 

AND   ORIFICE   BUCKETS 


BY 


ARTHUR  N.  TALBOT,    FRED  B  SEELY,^ 
VIRGIL  R  FLEMING,   MELVIN  L.  ENGER 


BULLETIN  No.  105 
ENGINEERING  EXPERIMENT  STATION 

PUBLISHED  BY  THE  UNIVERSITY  OF  1      NOIS,  URBANA 


PRICE:     'i  HTRTT-IITB  CENTS 

EUROPEAN  AGENT 
CHAPMAN  &  HALL,  LTD.,  LONDON 


CHANGE 


Wtfttf? 


UNIVERSITY  OF  ILLINOIS 
ENGINEERING  EXPERIMENT  STATION 

BULLETIN  No.  105  MAY,  1918 


HYDRAULIC    EXPERIMENTS   WITH   VALYES, 

ORIFICES,    HOSE,    NOZZLES,    AND 

ORIFICE   BUCKETS 


PART  I 
Loss  OF  HYDRAULIC  HEAD  IN  SMALL  VALVES 

BY  ARTHUR  N.  TALBOT 

PROFESSOR  OF  MUNICIPAL  AND  SANITARY  ENGINEERING 
IN  CHARGE  OF  THEORETICAL  AND  APPLIED  MECHANICS 

AND 

FRED  B   SEELY 

ASSISTANT  PROFESSOR  OF  THEORETICAL  AND  APPLIED  MECHANICS 

PART  II 
THE  FLOW  OF  WATER  THROUGH  SUBMERGED  ORIFICES 

BY  FRED  B   SEELY 
ASSISTANT  PROFESSOR  OF  THEORETICAL  AND  APPLIED  MECHANICS 

PART  III 

FIRE  STREAMS  FROM  SMALL  HOSE  AND  NOZZLES 
BY  VIRGIL  R  FLEMING 

ASSISTANT  PROFESSOR  OF  APPLIED  MECHANICS 

PART  IV 

THE  ORIFICE  BUCKET  FOR  MEASURING  WATER 

BY  MELVIN   L.  ENGER 
ASSOCIATE  PROFESSOR  OF  MECHANICS  AND  HYDRAULICS 


ENGINEERING  EXPERIMENT  STATION 

PUBLISHED  BY  THE  UNIVERSITY  OF  ILLINOIS,  URBANA 


PREFACE 

AS  a  part  of  the  experimental  work  conducted  in  the  Hydraulic 
-*"*•  Laboratory  of  the  University  of  Illinois  a  number  of  problems 
has  been  investigated  which  has  not  been  large  enough  in  scope  to  war- 
rant publication  as  separate  bulletins.  It  seems  well,  however,  to  put 
on  record  the  results  of  such  experiments,  and  this  bulletin  presents 
a  record  of  four  of  these  problems.  It  is  believed  that  the  four  papers 
will  be  found  to  be  of  use  in  various  aspects  of  engineering  practice 
even  though  the  experiments  are  not  exhaustive  investigations. 

The  investigations  for  the  most  part  have  been  the  outgrowth  of 
experimental  work  begun  by  students,  largely  as  thesis  work,  and  car- 
ried on  over  a  period  of  several  years. 

The  variety  of  conditions  under  which  the  flow  of  water  takes 
place,  the  possibility  of  large  changes  in  the  state  of  the  flow  due  appar- 
ently to  small  changes  in  the  form  of  the  passages  through  which  the 
water  flows,  and  the  necessity  of  persistent  effort  in  subjecting  assump- 
tions and  analytical  deductions  to  experimental  verification,  make  it 
desirable  to  report  all  hydraulic  experimental  results  which  are  believed 
to  be  reliable. 

A  part  of  the  experimental  results  herein  reported  has  appeared 
in  the  publication  of  a  technical  society.  The  material,  however,  has 
been  expanded  in  this  bulletin  and  will  be  found  in  a  more  convenient 

form  for  use. 

ARTHUR  N.  TALBOT 

FRED  B  SEELY 

Editors 


PART  I 
LOSS  OF  HYDRAULIC  HEAD  IN  SMALL  VALVES 

BY  ARTHUR  N.   TALBOT 
PROFESSOR  OF  MUNICIPAL  AND  SANITARY  ENGINEERING 
IN  CHARGE  OF  THEORETICAL  AND  APPLIED  MECHANICS 

AND 

FRED   B   SEELY 

ASSISTANT  PROFESSOR  OF  THEORETICAL  AND  APPLIED  MECHANICS 


387318 


CONTENTS 

PART  I 
LOSS   OF  HYDRAULIC   HEAD   IN  SMALL  VALVES 

PAGE 

I.  INTRODUCTION 7 

1.  Preliminary 7 

2.  Acknowledgment 7 

II.  APPARATUS  AND  METHOD  OF  EXPERIMENTING       ....  8 

3.  Valves 8 

4.  Method  of  Experimenting 8 

III.  EXPERIMENTAL  RESULTS  AND  DISCUSSION        .      .      .      .      .  10 

5.  Loss  of  Head 10 

6.  Earlier  Experiments  on  Gate  Valves 18 

7.  Coefficients  of  Discharge  for  Gate  Valves       ....  20 

8.  Summary 21 


LIST  OF   FIGURES 

NO.  PAGE 

1.  Longitudinal  Sections  of  Valves  Tested 9 

2.  Arrangement  of  Apparatus .     11 

• 

3.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

1-inch  Gate  Valve     ....'... 13 

4.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

2-inch  Gate  Valve 13 

5.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

1-inch  Globe  Valve .14 

6.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

2-inch  Globe  Valve 14 

7.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

1-inch  Angle  Valve 15 

8.  Curves  Showing  the  Relation  between  the  Velocity  and  Head  Lost  in 

2-inch  Angle  Valve 15 

9.  Curves  Showing  the  Relation  between  Coefficients  of  Loss  and  Valve 

Openings 16 

10.     Curves  Showing  the  Effect  of  Gradual  Change  of  Section  through  2-inch 

Globe  Valve   .  17 


LIST  OF  TABLES 

1.  Experimental  Values  of  Coefficients  of  Loss 16 

2.  Values  of  the  Coefficient  of  Loss  for  Gate  Valves  of  Various  Diameters 

Due  to  Partial  Closure  Only 19 

3.  Experimental  Values  of  the  Coefficients  of  Discharge  for  Gate  Valves  .     20 


HYDRAULIC  EXPERIMENTS 

WITH 

VALVES,  ORIFICES,  HOSE,  NOZZLES,  AND 
ORIFICE  BUCKETS 


PART  I 
LOSS  OF  HYDRAULIC  HEAD  IN  SMALL  VALVES 


I.     INTRODUCTION 

1.  Preliminary. — Part  I  of  this  bulletin  presents  the  results  of 
experiments  on  the  flow  of  water  through  1-in.  and  2-in.  gate  valves, 
1-in.  and  2-in.  globe  valves,  and  1-in.  and  2-in.  angle  valves.     The  loss 
of  head  caused  by  each  valve,  expressed  in  terms  of  the  velocity  head 
in  the  pipe,  is  given  for  four  different  ratios  of  the  height  of  the  valve 
opening  to  the  diameter  of  the  full  valve  orifice,  namely,  M,  /^,  H, 
and  1.     The  coefficients  of  discharge  are  also  given  for  the  gate  valves 
for  each  of  the  four  valve  openings. 

In  a  long  pipe  line  the  total  amount  of  lost  head  is  caused  chiefly 
by  pipe  friction,  the  resistance  due  to  a  valve  being  comparatively  small 
except  for  very  small  valve  openings. 

In  a  variety  of  cases,  however,  where  valves  are  used  on  compara- 
tively short  pipe  lines  as,  for  example,  in  hydraulic  elevator  service,  in 
office  buildings,  and  in  special  apparatus  it  is  important  to  know  the 
lost  head  caused  by  small  valves  of  different  kinds  when  set  at  various 
positions.  Very  few  experimental  results  have  been  published  on  this 
subject,  particularly  for  globe  and  angle  valves.  Any  experimental 
work,  furthermore,  which  helps  to  indicate  the  laws  governing  the  flow 
of  water  should  prove  of  value.  With  these  facts  in  mind  the  results 
herein  recorded  have  been  prepared. 

2.  Acknowledgment. — The  experiments  herein  considered  were  per- 
formed as  student  thesis  work  in  the  Hydraulic  Laboratory  of  the  Uni- 
versity of  Illinois  by  M.  E.  THOMAS,  class  of  1906,  under  the  direction 
of  PROFESSOR  ARTHUR  N.  TALBOT.     Unusual  care  in  the  experimenting  is 
reflected  in  the  congruity  of  the  data  presented  in  Mr.  Thomas'  thesis. 

7 


ILLINOIS    ENGINEERING     EXPERIMENT    STATION 


II.     APPARATUS  AND  METHOD  OF  EXPERIMENTING 

3,  Valves. — The  valves  used  were  bought  in  the  open  market 
and  tested  just  as  received.     The  passages  through  the  2-in.  globe 
valve  were  then  modified  by  the  use  of  plaster  of  paris  to  give  a  more 
gradual  change  of  section  (see  Fig.  10),  and  this  valve  was  tested  again. 
The  types  or  forms  of  the  interiors  of  the  valves  and  the  dimensions  of 
some  of  the  passageways  through  the  valves  are  shown  in  Fig.  1.     The 
1-in.  globe  valve  and  the  1-in.  angle  valve  were  made  by  the  Western 
Tube  Company.     All  the  other  valves  were  made  by  the  Crane  Company. 

4.  Method  of  Experimenting. — The  arrangement  of  the  apparatus 
is  shown  in  Fig.  2.     The  test  valve  was  placed  in  a  horizontal  pipe  to 
which  water  was  supplied  from  a  standpipe  under  a  static  head  of  about 
50  feet.     The  quantity  of  water  discharged  through  the  valve  was 
regulated  by  another  valve  downstream  from  the  test  valve.     The 
volume  discharged  in  a  certain  time  was  measured  in  a  calibrated  pit 
and  the  time  taken  with  an  ordinary  watch  from  which  the  rate  of 
discharge  was  calculated.     Three-way  gage  connections  for  obtaining 
the  pressure  head  in  the  pipe  were  made  at  a  section  one  foot  upstream 
and  one  foot  downstream  from  the  valve.     Care  was  taken  to  avoid 
having  these  connections  project  into  the  interior  of  the  pipe.     It  was 
found  by  experiment  that  when  any  two  of  the  three  pressure  connec- 
tions at  either  section  were  closed,  the  same  difference  of  head  was 
registered  as  when  all  three  connections  at  either  section  were  open. 
The  three-way  connections  were  used,  however,  in  all  the  experiments. 
The  difference  in  the  pressure  heads  at  the  two  sections  was  measured 
by  a  differential  mercury  gage.     A  Crosby  pressure  gage  was  also 
attached  at  each  section  to  serve  as  a  rough  check  on  the  differential 
gage.     The  lost  head  due  to  the  pipe  friction  for  the  two  feet  of  pipe 
between  the  two  sections  was  assumed  to  be  as  given  in  Weston's  Tables 
of  Friction  of  Water  in  Pipes.     This  amount  of  lost  head  was  subtracted 
from  the  reading  of  the  differential  mercury  gage  in  determining  the  loss 
of  head  caused  by  the  valve. 

The  loss  of  head  and  the  corresponding  rate  of  discharge  and 
velocity  in  the  pipe  were  determined  for  each  of  four  valve  openings  for 
each  of  the  six  valves  tested.  The  valve  openings  used  were  such  that 
the  heights  of  the  openings  were  one-fourth,  one-half,  three-fourths,  and 
one  times  the  diameter  of  the  full  valve  orifice. 


HYDRAULIC     EXPERIMENTS 


One- Inch  Gate  Valve 


Two-Inch  Gate  Valve 


One-Inch  Angle  Valve  Two-Inch  Angle  Valve 

FIG.  1.     LONGITUDINAL  SECTIONS  OF  VALVES  TESTED 


10  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


III.     EXPERIMENTAL  RESULTS  AND  DISCUSSION 

5.  Loss  of  Head. — In  Fig.  3  to  8  values  of  the  lost  head  caused 
by  the  valve  are  plotted  as  abscissas  and  the  mean  velocity  in  the  pipe 
as  ordinates.  The  assumed  value  of  the  friction  head  for  the  two  feet 
of  pipe  between  pressure  connections  is  subtracted  from  the  differential 
mercury  gage  reading  in  plotting  the  abscissas.  There  is,  of  course, 
some  doubt  concerning  the  correct  allowance  to  be  made  for  this  pipe 
friction.  The  loss  of  head  due  to  this  cause,  however,  will  be  relatively 
small  except  for  the  larger  valve  openings.  It  will  be  noted  from  the 
curves  in  Fig.  3  to  8  that  the  range  of  velocity  in  the  pipe  varied  of 
course  with  the  kind  of  valve  and  with  the  amount  of  valve  opening. 
The  smallest  mean  velocity  in  any  case  was  about  %  ft.  per  sec.,  while 
the  maximum  mean  velocity  was  about  40  ft.  per  sec. 

The  curves  in  Fig.  3  to  8  give  values  of  the  loss  of  head  caused 
by  the  valves  which  vary  as  the  square  of  the  velocity  in  the  pipe,  that 
is,,  the  lost  head  due  to  the  valve  may  be  expressed  in  terms  of  the 
velocity  head  in  the  pipe.  This  fact  is  shown  very  clearly  by  plotting 
the  values  from  the  curves  in  Fig.  3  to  8  on  logarithmic  paper;  the 
curves  showing  the  relation  between  the  lost  head,  h,  and  the  velocity 
in  the  pipe,  v,  become  parallel  straight  lines  with  a  slope  varying  but 
little  from  two,  the  slope  indicating  the  exponent  in  the  equation 
h  —  kvn.  That  is,  h  =  kv2  or,  when  expressed  in  terms  of  the  velocity 

head  in  the  pipe,  h  =  -~-  in  which  m  is  called  the  coefficient  of  loss. 

Values  of  the  coefficients  of  loss  for  the  valves  with  the  various  valve 
openings  as  obtained  from  the  curves  in  Fig.  3  to  8  are  given  in  Table  1. 
These  values  have  been  plotted  in  Fig.  9  as  abscissas  against  the  valve 
openings  as  ordinates.  From  these  curves  and  also  from  Table  1  the 
resistance  to  flow  caused  by  the  three  kinds  of  valves  may  be  com- 
pared at  various  valve  openings.  It  will  be  noted  that  the  loss  of  head 
varies  in  a  quite  different  manner  with  the  amount  of  valve  opening  for 
these  three  kinds  of  valves,  for  instance,  a  comparison  of  the  results 
for  the  valves  when  completely  opened  shows  that  a  globe  valve  causes 
more  than  twice  as  much  loss  of  head  as  the  corresponding  size  of  angle 
valve,  while  a  gate  valve  causes  markedly  less  loss  than  either  a  globe  or 
an  angle  valve,  the  velocity  in  the  pipe  being  the  same  in  the  three 
cases.  As  the  valve  is  gradually  closed,  the  resistance  to  flow  of  the 
angle  valves  increases  the  least  (decreasing  at  first)  while  the  resistance 


T      -, 


FIG.  2.     ARRANGEMENT  OF  APPARATUS 


HYDRAULIC    EXPERIMENTS 


13 


02-46       8-     IO      12     14      16     18     2O     22     24    26     28   JO     32     34    36    38   <4O 

Head  Lost ,    /? 

FIG.  3.     CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  I-INCH  GATE  VALVE 


30     32     34    36     38    4O 


24       6       8       10      12      14      16     18     20     22     24    26 

head  Lost  t  ft. 

FIG.  4.     CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  2-iNCH  GATE  VALVE 


14 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


0     2      4      6      6      10     12     14     16     18     20    22    24    26     28    3O    32    J4    36    38 


FIG.  5.     CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  I-INCH  GLOBE  VALVE 


FIG.  6.    CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  2-iNCH  GLOBE  VALVE 


HYDRAULIC     EXPERIMENTS 


15 


O     2     4     6     8      10    IZ    14     16    18     2O    22    24    26    28   JO    32   34  36   38  40 

head  Lost.  ft. 

FIG.  7.     CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  I-INCH  ANGLE  VALVE 


23 


6       B       IO     12      14      IS     /8      2O     22     24     26     28     3O    32     34     36     38   4O 

/lead  Lost,  ft 

FIG.   8.     CURVES  SHOWING  THE  RELATION  BETWEEN  THE  VELOCITY  AND 
HEAD  LOST  IN  2-iNCH  ANGLE  VALVE 


16 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


of  the  gate  valves  increases  the  most  rapidly,  although  the  rate  of 
increase  in  any  case  is  comparatively  small  until  the  valve  is  at  least 
one-half  closed. 


10 


^0  30  40  SO  60 

Coefficientofioss-  m  /n  h=mj- 


70 


FIG.  9.     CURVES  SHOWING  THE  RELATION  BETWEEN  COEFFICIENTS  OF 
Loss  AND  VALVE  OPENINGS 

Fig.  9  also  indicates  that  the  proportions  or  form  or  shape  of  the 
passageways  of  the  valve  of  a  given  type  or  kind  is  a  very  important 
factor  in  causing  loss  of  head.  This  fact  is  shown  by  a  comparison  of 
the  results  for  the  1-in.  globe  valve  with  those  for  the  2-in.  globe  valve 
and  also  by  a  comparison  of  the  results  of  the  1-in.  angle  valve  with 
those  of  the  2-in.  angle  valve.  Each  of  these  1-in.  valves  was  of  a 
somewhat  different  form  from  that  of  the  corresponding  2-in.  valve  as 
may  be  seen  in  Fig.  1.  It  will  be  noted  from  Fig.  9  and  Table  1  that 

TABLE  1 
EXPERIMENTAL  VALUES  OF  COEFFICIENTS  OF  Loss 

Values  of  m  in  h  =  -= — 


Gate  Valves 

Globe  Valves 

Angle  Valves 

Ratio  of  Height  of  Valve- 
Opening  to  Diameter  of 
Full  Valve  Opening 

1-inch 
Diameter 

2-inch 
Diameter 

1-inch 
Diameter 

2-inch 
Diameter 

1-inch 
Diameter 

2-inch 
Diameter 

73.0 

18.8 

16.6 

60.0 

5.00 

7.3 

/4 

7.0 

2.94 

9.62 

10.9 

2.90 

1.70 

% 

1.84 

1.06 

8.75 

6.84 

2.72 

1.44 

1 

0.74 

0.35 

7.12 

6.0 

3.23 

1.70 

HYDRAULIC    EXPERIMENTS 


17 


for  the  smaller  valve  openings  the  1-in.  globe  valve  and  the  1-in.  angle 
valve  cause  less  resistance  to  flow  than  the  corresponding  2-in.  valves. 
The  difference  is  especially  large  in  the  case  of  the  globe  valves.  This 
unexpected  result  seems  to  be  due  chiefly  to  the  better  shaped  dis- 
charge passages  (more  gradual  expansion)  as  the  water  makes  its 
exit  from  the  1-in.  globe  valve. 

Experiments  were  made  on  the  2-in.  globe  valve  to  see  if  a  more 
gradual  change  in  sections  through  the  valve  would  cause  less  loss  of 
head.  This  gradual  change  was  made  by  filling  in  part  of  the  passage- 
way with  plaster  of  paris,  as  shown  in  Fig.  10.  This  modified  valve  was 
then  tested  with  the  valve  one-half  open  and  wide  open,  the  results  for 
which  are  shown  in  Fig.  10.  It  will  be  seen  that  this  modification  had  no 


/6  80 

Head  lost  jn  Feet 


36 


40 


FIG.  10.     CURVES  SHOWING  THE  EFFECT  OF  GRADUAL  CHANGE  OP  SECTION 
THROUGH  2-INCH  GLOBE  VALVE 

effect  on  the  amount  of  head  lost.  This  suggests  that  the  lost  head  in 
a  small  globe  valve  is  caused  more  by  the  form  or  shape  of  the  passage- 
way at  exit  from  the  valve  than  by  the  form  of  the  passages  through  the 
valve.  Other  valve  openings  and  other  modifications  of  the  passage- 
ways, however,  may  give  better  results. 

In  the  case  of  angle  valves  the  loss  of  head  is  not  a  minimum  for 
the  greatest  valve  opening  as  is  shown  in  Table  1  and  in  Fig.  9.  For 
the  2-in.  angle  valve  the  lost  head  is  the  same  when  the  valve  is  only 
one-half  open  as  it  is  when  the  valve  is  wide  open,  the  velocity  in  the 
pipe  for  the  two  valve  openings  being  the  same,  that  is,  the  coefficient 


18  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

of  loss  is  the  same  for  these  two  valve  openings.  When  this  valve  is 
three-fourths  open,  however,  the  coefficient  of  loss  is  about  20  per 
cent  less  than  when  the  valve  is  one-half  open  or  wide  open.  The  1-in. 
globe  valve  caused  a  smaller  amount  of  lost  head  when  it  was  one-half 
and  three-fourths  open  than  it  did  when  wide  open,  the  velocity  in  the 
pipe  being  the  same  for  each  of  the  valve  settings.  The  difference, 
however,  between  the  coefficients  of  loss  for  these  three  valve  openings 
is  not  large.  The  reason  that  the  minimum  loss  of  head  in  the  angle 
valves  occurs  when  the  valve  is  about  three-fourths  open  is  probably 
because  at  this  opening  the  water  can  flow  through  comparatively  large 
openings  all  around  the  valve  disc  meeting  with  less  abrupt  changes  of 
directions  than  when  the  valve  is  wide  open.  In  the  latter  case  there 
is  much  turbulent  action  due  to  the  impact  of  the  water  against  the  bot- 
tom of  the  valve.  As  the  valve  opening  decreases  from  the  three-fourths 
open  position,  the  greater  resistance  due  to  the  narrowing  passages 
causes  the  lost  head  to  increase  again. 

The  assumption  is  sometimes  made  that  for  comparatively  small 
valves  of  like  type  or  kind  the  loss  of  head  varies  inversely  with  the 
diameter  of  the  valve.  For  the  larger  valve  openings  this  assumption 
is  probably  approximately  true,  but  from  the  foregoing  results  and  dis- 
cussion it  would  seem  that  at  least  for  globe  and  angle  valves  the  form 
or  shape  of  the  passages  of  the  valve  is  a  determining  factor  in  the 
amount  of  head  lost  at  the  smaller  valve  openings. 

6.  Earlier  Experiments  on  Gate  Valves. — Among  the  first  reliable 
published  results  on  valves  were  those  by  Weisbach.*  The  largest 
gate  valve  used  by  Weisbach  was  a  little  less  than  two  inches.  Globe 
and  angle  valves,  at  least  of  modern  construction,  were  not  tested. 
Other  experiments  on  gate  valves  have  been  reported  by  Magruderf 
on  %-in.,  K-in.,  M-in.,  1-in.,  and  IM-in.  gate  valves,  by  FolwellJ  on 
a  4-in.  gate  valve,  by  Kuichling^f  on  a  24-in.  gate  valve,  and  by  J.  Waldo 
Smith  §  on  a  30-in.  gate  valve.  In  Smith's  experiments  the  30-in. 
valve  was  located  in  a  42-in.  pipe  with  increaser-shaped  or  Venturi- 
shaped  approaches,  and  in  Kuichling's  experiments  the  valve  was 
placed  in  one  branch  of  a  Y  only  a  few  feet  from  the  section  where  the 
Y  started  to  branch.  The  methods  of  determining  the  lost  head  in  the 


*  Mechanics  of  Engineering  (Coxe's  translation). 

t  Engineering  Record,  Vol.  XL,  p.  78,  1899. 

t  Engineering  News,  Vol.  XLVII,  p.  302,  1902. 

1  Trans.  Am.  Soc.  Civ.  Eng.  Vol.  XXVI,  p.  439,  and  Vol.  XXXIV. 

§  Trans.  Am.  Soc.  Civ.  Eng.  Vol.  XXXIV,  p.  235  (p.  243),  1895. 


HYDRAULIC    EXPERIMENTS 


19 


various  experiments  were  also  different.     For  these  reasons  it  is  obvi- 
ous that  the  results  of  these  experiments  are  not  directly  comparable. 


TABLE  2 

VALUES  OF  THE  COEFFICIENT  OF  Loss  FOB  GATE  VALVES  OF  VARIOUS 
DIAMETERS  DUE  TO  PARTIAL  CLOSURE  ONLY 


Ratio  of  Height 
of  Opening  to 
Diameter  of 
Full  Valve 
Orifice 

Weisbach 

Kuichling 

Smith 

Folwell 

This  Bulletin 

2^-inch 
Diameter 

24-inch 
Diameter 

30-inch 
Diameter 

4-inch  Diameter 

2-inch  and  1-inch 

Parallel 
Sides 

Parallel 
Sides 

Parallel 
Sides 
Venturi- 
Shaped 
Ap- 
proaches 

Parallel 
Sides 

Wedge 
Shaped 

Parallel  Sides 

2-inch 
Diameter 

1-inch 
Diameter 

0 

3/100 



950.0 

1/10 

128.0 



K 

98.0 

90.0 

72.3 

104 

M 

17.0 

22.7 

17.0 

16.8 

20.5 

18.45 

72.3 

N 

5.5 

8.63 

7.5 

6.19 

8.0 

7.01 

16.  01 

H 

2.1 
0.81 

3.27 
1 

1.09 

3.5 
1.5 

2.58 
1.22 

2.72 
1.5 

2.59 
1.21 

6.26 
2.51 

H 

0.26 

0.25 

0.50 

0.55 

0.66 

0.71 

1.10 

H 

0.07 

0.019 

0.19 

0.20 

0.16 

0.151 

0.701 

i 

0.00 

0.00 

0.00 

0.00 

0.00 

0.00 

0.00 

1  Interpolated  from  curve. 

In  Table  2  are  given  the  values  of  the  coefficients  of  loss  as  obtained  by 
the  various  experimenters  mentioned  previously,  as  well  as  the  values 
obtained  in  the  experiments  herein  reported.  These  values  of  the 
coefficients  of  loss  are  those  due  to  partial  closure  of  the  valves  only, 
that  is,  in  excess  of  the  loss  of  head  caused  by  the  valve  when  wide 
open.  Smith's  experiments  are  the  only  ones  in  which  valve  openings 
less  than  one-eighth  were  used.  There  is  considerable  chance  for 
error  in  the  results  obtained  for  the  very  small  valve  openings,  due 
chiefly  to  the  uncertainty  in  securing  the  valve  setting  desired.  Table  2 
indicates  a  rather  close  agreement  in  the  coefficient  of  loss  for  all 
the  gate  valves  having  diameters  of  2  in.  or  greater,  and  for  valve 


20 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


openings  of  K  or  perhaps  H  and  greater.  The  values  for  the  1-in. 
valve  show  a  considerable  increase  in  the  lost  head  over  that  for  valves 
of  2-in.  diameter  and  greater.  It  is  probable  also  that  there  is  consid- 
erable variation  in  the  smaller  valves  of  any  one  type  and  size. 

7.  Coefficients  of  Discharge  for  Gate  Valves. — In  order  to  determine 
the  rate  of  discharge  through  a  pipe  a  partially  closed  valve  has  some- 
times been  used.  This  requires  the  values  of  the  coefficients  of  dis- 
charge of  the  valve  for  various  valve  openings  since  the  rate  of  discharge, 
q,  is  found  from  the  expression,  cA^2gh,  in  which  c  is  the  coefficient 
of  discharge,  A  the  area  of  the  valve  opening,  and  h  the  difference  in 
pressure  heads  on  the  two  sides  of  the  valve  (lost  head),  velocity  of 
approach  being  neglected.  The  average  values  of  the  coefficients  of 
discharge  for  the  1-in.  and  2-in.  gate  valves  as  found  in  the  experi- 
ments reported  in  this  bulletin  are  given  in  Table  3.  The  value  of  the 


TABLE  3 

EXPERIMENTAL  VALUES  OF  THE  COEFFICIENTS  OF  DISCHARGE  FOR 
GATE  VALVES 


Ratio  of  Height  of  Valve- 
Opening  to  Diameter  of 
Full  Valve-Opening 

Coefficient  of  Discharge 

Area  of  Valve-Opening 
Square  Inch 

1-inch  Valve 

2-inch  Valve 

1-inch  Valve 

2-inch  Valve 

\i 

.48 

.88 

.195 

.826 

y* 

.67 

1.00 

.450 

1.80 

K 

,88 

1.12 

.660 

2.67 

i 

1.16 

1.70 

.785 

3.14 

coefficient  varied  somewhat  with  the  velocity  for  any  given  valve  open- 
ing. Because  of  the  uncertainty  of  obtaining  the  exact  valve  setting 
desired  and  the  corresponding  uncertainty  in  the  area  of  the  valve 
opening,  the  values  of  the  coefficients  of  discharge  given  in  Table  3 
cannot  be  considered  as  refined  determinations. 

It  will  be  noted  that  the  coefficient  of  discharge  increases  directly 
with  the  valve  opening  for  each  of  the  gate  valves  for  a  range  of  valve 


HYDRAULIC     EXPERIMENTS  21 

openings  of  34  to  Y±  or  perhaps  greater.  The  more  the  valve  is  opened 
the  greater  is  the  velocity  of  approach  toward  the  valve  and  since  the 
velocity  of  approach  is  not  considered  in  the  calculation  of  the  coeffi- 
cient of  discharge  the  value  of  the  coefficient  increases  with  the  valve 
opening.  The  coefficient  of  discharge  for  the  valves  used  by  Kuichling 
and  Smith  decreased  slightly  until  the  valve  was  about  one-fourth  open 
and  then  increased  rapidly  for  further  openings  of  the  valve.  Gibson 
with  a  2j/2-in.  flat  disc  stop  valve  found  nearly  a  constant  coefficient 
of  discharge  of  0.80.  These  variations  in  the  coefficients  of  discharge 
are  not  surprising  considering  the  wide  range  of  conditions  covered  by 
the  experiments.  They  suggest,  however,  that  if  gate  valves  are  to 
be  used  for  determining  the  rate  of  discharge  in  pipes  with  reasonable 
accuracy  much  more  experimenting  is  required,  or  better,  where  it  is 
possible,  experiments  should  be  performed  under  sendee  conditions  to 
calibrate  the  particular  valve  to  be  used. 

8.  Summary. — The  following  brief  summary  is  given  as  applying 
to  1-in.  and  2-in.  valves  of  the  three  kinds  tested  (gate  valves,  globe 
valves,  and  angle  valves)  with  valve  settings  ranging  from  one-fourth 
open  to  wide  open. 

(1)  The  loss  of  head  caused  by  small  valves  varies  as  the 
square  of  the  velocity  in  the  pipe  for  all  the  valve  openings;  hence 
the  lost  head  may  be  expressed  as  a  constant  times  the  velocity  head 

.     .,       .       (j     mvz\ 
in  the  pipe,  ^/i  =  — j. 

(2)  When  wide  open  a  globe  valve  causes  more  than  twice  as 
much  loss  of  head  as  an  angle  valve  of  the  same  size,  while  a  gate 
valve  causes  much  less  loss  of  head  than  either  a  globe  or  an  angle 
valve,  the  velocity  in  the  pipe  being  the  same  in  the  three  cases. 

(3)  The  loss  of  head  for  an  angle  valve  is  somewhat  less  when 
about  three-fourths  open  than  when  wide  open,  the  velocity  in  the 
pipe  being  the  same  in  each  case. 

(4)  The  loss  of  head  for  each  valve,  as  the  valve  is  closed  from 
a  wide-open  position,  varies  comparatively  little  with  the  valve 
opening  until  the  valve  is  at  least  one-half  closed.     As  further 
closure  takes  place  the  loss  of  head  of  the  globe  valves  and  gate 
valves  increases  rapidly  and  is  considerably  larger  than  that  of  the 
angle  valves. 

(5)  The  form  or  shape  of  the  passageways  through  a  globe  or 
angle  valve  has  a  large  influence  on  the  loss  of  head  for  the  small 


22  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

valve  openings.  The  portion  of  the  passageways  in  which  the  form 
seems  of  greatest  importance  is  in  the  exit  from  the  valve  rather 
than  in  the  passageways  leading  to  the  valve  disc  or  seat.  On 
account  of  the  influence  of  the  form  or  shape  of  the  valve  no  law 
giving  the  relation  of  the  lost  head  to  the  diameter  of  the  valve  can 
be  stated  for  valve  settings  less  than  five-eighths  open.  For  larger 
valve  openings  than  this,  the  lost  head  seems  to  vary  approximately 
inversely  as  the  diameter. 

(6)  The  use  of  the  lost  head  through  a  partially  closed  valve 
as  a  means  of  determining  the  flow  can  be  only  a  very  rough  method 
of  measurement  unless  the  particular  valve  to  be  used  is  calibrated 
under  service  conditions.  Even  then  the  difficulty  in  obtaining 
the  desired  valve  setting  may  introduce  considerable  uncertainty 
in  the  results. 


PART  II 

THE  FLOW  OF  WATER  THROUGH   SUBMERGED 
ORIFICES 

BY  FRED   B   SEELY 
ASSISTANT  PROFESSOR  OF  THEORETICAL  AND  APPLIED  MECHANICS 


CONTENTS 
PART  II 

THE  FLOW  OF  WATER  THROUGH  SUBMERGED 
ORIFICES 

PAGE 

IV.  INTRODUCTION 27 

9.     Preliminary .      .      .  '   .  27 

10.  Acknowledgment 28 

V.  APPARATUS  AND  METHOD  OF  EXPERIMENTING       ....  29 

11.  Orifices -  29 

12.  Tank  Used  and  Method  of  Experimenting     ....  30 

13.  Method  of  Calculating  the  Coefficient  of  Discharge       .  33 

VI.  EXPERIMENTAL  RESULTS  AND  DISCUSSION 34 

14.  Coefficients  of  Discharge 34 

15.  Results  Obtained  by  Earlier  Experimenters  ....  37 

16.  Comparison  with  Discharge  into  Air 39 

17.  Summary        , 40 


25 


LIST  OF  FIGURES 

NO.  PAGE 

11.  Tank  Used  and  Arrangement  of  Apparatus 31 

12.  Diagrams  Showing  Values  of  Coefficients  of  Discharge  of  Circular  Sub- 

merged Orifices  for  Various  Velocities 34 

13.  Diagrams  Showing  Values  of  Coefficients  of  Discharge  of  Square  Sub- 

merged Orifices  for  Various  Velocities 34 

14.  Diagrams  Showing  Values  of  Coefficients  of  Discharge  of  Rectangular  Sub- 

merged Orifices  for  Various  Velocities .      .     35 

15.  Curve  Showing  the  Relation  between  Coefficient  of  Discharge  for  Circular 

Orifice  and  Diameter  of  Orifice 36 

16.  Curve  Showing  the  Relation  between  Coefficient  of  Discharge  for  Square 

Orifice  and  Side  of  Orifice 36 

17.  Curve  Showing  the  Relation  between  Coefficient  of  Discharge  of  Rectan- 

gular Orifice  and  Short  Side  of  Orifice  (other  Side  being  Six  Inches,  in 
Each  Case)       .".......' 36 

18.  Curves  Showing  Relation  between  Coefficient  of  Discharge  and  Area  of 

Orifices  37 


LIST  OF  TABLES 

4.  List  of  Orifices  Used 29 

5.  Values  of  Coefficient  of  Discharge  for  Submerged  Orifices  for  Velocities 

from  One-half  to  Five  Feet  per  Second 35 

6.  Results  Obtained  by  Earlier  Experimenters  on  Submerged  Sharp-edged 

Orifices  38 


26 


HYDRAULIC    EXPERIMENTS  27 


PART  II 

THE   FLOW  OF  WATER  THROUGH  SUBMERGED 
ORIFICES 


IV.     INTRODUCTION 

9.  Preliminary. — Part  II  of  this  bulletin  presents  the  results  of 
experiments  on  submerged  sharp-edged  orifices  of  various  shapes  and 
sizes  discharging  under  moderately  low  and  under  very  low  heads. 
The  orifices  used  were  of  three  shapes,  circular  orifices  with  diameters 
from  1  in.  to  6  in.,  square  orifices  with  sides  from  K  in.  to  &A  in.,  and 
rectangular  orifices  having  one  side  range  from  Y*  in.  to  2  in.,  the  other 
side  being  6  in.  in  each  case.  The  coefficient  of  discharge  is  given  for 
each  orifice  for  a  velocity  range  of  approximately  ^A  ft.  per  sec.  to 
4  ft.  per  sec.  This  range  corresponds  roughly  to  a  range  of  head  on 
the  orifice  of  0.006  ft.  to  0.08  ft. 

Considerable  experimenting  has  been  done  on  orifices  discharging 
into  air,  particularly  on  sharp-edged  circular  orifices  of  rather  small  size 
although  the  results  are  somewhat  discordant.  Comparatively  little 
experimental  work,  however,  has  been  carried  out  on  submerged  orifices. 
While  the  orifice  has  lost  some  of  its  importance  as  a  water  measuring 
device  due  to  the  development  of  other  methods,  it  is,  nevertheless,  of 
importance  to  determine  how  the  rate  of  discharge  is  affected  by  the 
shape  and  the  size  of  the  orifice  and  also  by  the  head  on  the  orifice, 
particularly  the  effect  of  very  low  heads  which  the  submerged  orifice 
makes  possible. 

The  submerged  orifice  may  be  of  particular  importance  in  cases 
which  require  the  measurement  of  water  with  as  small  a  loss  of  head  as 
possible  as,  for  example,  in  determining  the  discharge  from  a  water 
turbine  when  operating  under  a  low  head.  The  decrease  in  the  avail- 
able head  on  the  turbine  made  necessary  by  the  proper  setting  of  a  weir 
may  be  an  important  factor  in  the  installation. 

There  is  a  feeling  among  some  engineers  that  the  importance  of 
the  so-called  standard  orifice  (sjiarp  edges,  complete  contraction  without 
velocity  of  approach,  etc.)  has  been  over-emphasized  and  that  beveled- 
edged  orifices  are  better  adapted  at  least  to  conditions  where  the  orifice 
may  be  obstructed  and  the  edge  soon  worn  off,  as,  for  example,  in 
measuring  the  water  supplied  to  water  wheels  through  flume  or  bulk- 


28  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

head  openings.  There  exist,  no  doubt,  some  grounds  for  this  feeling. 
A  sharp  edged  orifice  (an  opening  in  a  thin  plate),  however,  is  subject 
to  less  variation  in  its  construction  than  a  beveled-edged  orifice.  This 
fact  is  of  considerable  importance  where  accuracy  is  essential.  It  is 
felt  that  the  submerged  orifice,  both  beveled-edged  and  sharp-edged, 
is  worthy  of  more  attention  than  has  been  accorded  it. 

10.  Acknowledgment. — The  experimenting  was  done  in  the  Hyd- 
raulic Laboratory  of  the  University  of  Illinois.  Some  of  the  results 
herein  presented  have  been  taken  from  the  theses  of  W.  R.  ROBINSON 
of  the  class  of  1906  and  G.  D.  PHILLIPS  of  the  class  of  1907,  and  some 
of  the  results  also,  particularly  at  the  low  heads,  have  been  taken 
from  a  second  thesis  presented  by  Mr.  Robinson  in  1909.  All  the 
thesis  work  was  conducted  under  the  direction  of  PROFESSOR  ARTHUR 
N.  TALBOT.  The  careful  way  in  which  this  preliminary  experiment- 
ing was  done  has  made  the  results  of  the  theses  of  much  value.  Dur- 
ing 1914  and  1915  the  writer  spent  considerable  time  in  checking  the 
results  of  the  theses  work  and  extending  certain  parts  of  the  investi- 
gation. 


HYDRAULIC     EXPERIMENTS 


29 


V.  APPARATUS  AND  METHOD  OF  EXPERIMENTING 

11.  Orifices. — The  orifices  used  were  of  three  different  shapes. 
Four  of  the  orifices  were  circular  with  diameters  of  1  in.,  2  in.,  4  in., 
and  6  in.  Five  were  square  with  sides  of  %  in.,  1  in.,  2  in.,  4  in.,  and 
5K  in.  Three  were  rectangular  with  dimensions  of  %  in.  by  6  in., 
1  in.  by  6  in.,  and  2  in.  by  6  in.  In  each  case  the  orifice  was  formed 
in  a  cast  iron  plate  H  in.  thick  and  lO^  in.  in  diameter,  a  sharp  edge 
being  formed  by  beveling  at  45  degrees.  Except  for  a  few  small  nicks 
the  edges  were  sharp  and  the  areas  closely  true  to  shape.  The  dimen- 
sions of  the  orifices  were  carefully  determined  (except  for  the  1-in. 
circular  orifice)  by  an  inside  micrometer  for  dimensions  greater  than 
1  in.  and  inside  screw  calipers  for  dimensions  less  than  1  in.  A  list  of 
the  orifices  used  and  the  areas  as  determined  from  the  measured  dimen- 
sions are  given  in  Table  4.  The  1-in.  circular  orifice  was  broken  before 


TABLE  4 
LIST  OF  ORIFICES  USED 


Form  of  Orifice 

Nominal  Size 

Measured  Area 
square  feet 

1  in.  diam. 

not  measured 

Circular 

2  in.  diam. 
4  in.  diam. 

0.0219 
0.0883 

6  in.  diam. 

0.1967 

J^  in.  by    H  in. 

0.001735 

1  in.  by      1  in. 

0.00698 

Square 

2  in.  by      2  in. 

0.0279 

4  in.  by      4  in. 

0.1109 

5J3  in.  by  5^  in. 

0.2105 

J^  in.  by  6  in. 

0.0206 

Rectangular 

1  in.  by  6  in. 

0.0418 

2  in.  by  6  in. 

0.0838 

its  dimensions  were  taken  so  that  the  nominal  diameter  (1  in.)  has 
been  used  in  the  calculations.  There  may  be  some  error,  therefore, 
in  the  results  for  this  orifice. 


30  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

12.  Tank  Used  and  Method  of  Experimenting. — The  same  tank 
was  used  in  all  the  experiments,  the  dimensions  and  general  arrange- 
ment of  which  is  shown  in  Fig.  11.*  The  tank  was  divided  into  two 
compartments  by  a  vertical  partition  in  which  the  orifice  was  placed, 
holding  the  orifice  in  a  vertical  plane. 

The  water  coming  from  the  laboratory  standpipe  was  supplied 
to  the  tank  through  a  6-in.  supply  pipe  and  also  through  a  M~m- 
pipe,  the  latter  making  possible  a  finer  adjustment  in  maintaining  a 
constant  head.  After  passing  through  baffle  boards  the  water  flowed 
through  the  orifice  and  finally  left  the  downstream  compartment  by 
passing  out  through  small  openings  in  the  end  of  the  tank,  the  flow 
through  which  was  regulated  by  placing  stoppers  in  some  of  the  holes. 
These  holes  were  arranged  in  two  narrow  portions  in  the  end  of  the 
tank,  one  near  each  side  of  the  tank,  and  the  stoppers  were  arranged 
so  as  to  give  nearly  a  uniform  distribution  from  each  of  the  two  sets  of 
openings.  This  arrangement,  it  was  found,  helped  to  maintain  steady 
conditions. 

The  quantity  of  water  discharged  was  determined  by  weighing  for 
the  small  discharges  and  by  measuring  in  a  pit  for  the  larger  discharges. 
The  pit  was  about  6  ft.  deep,  and  7.995  ft.  in  diameter.  The  value 
for  the  diameter  is  the  average  of  a  large  number  of  readings  of  a 
micrometer  attached  to  a  rigid  stick.  The  rise  in  the  pit  was  deter- 
mined by  a  vertical  graduated  rod  which  could  be  read  directly  to 
0.02  ft.  and  to  0.004  'ft.  by  estimating.  A  float  was  attached  to  the 
bottom  of  the  rod  and  a  still  basin  was  provided.  The  water  was 
wasted  into  another  pit  through  a  movable  spout  until  the  surface 
of  the  water  in  the  measuring  pit  became  fairly  still  so  that  an  accurate 
reading  of  the  rod  could  be  taken.  A  hook  gage  was  used  to  test  the 
accuracy  of  the  float  and  rod.  At  the  end  of  the  experiment  the  water 
was  again  wasted  in  the  same  manner.  A  calibrated  stop  watch  gave 
the  time  corresponding  to  the  rise  in  the  pit. 

The  head  causing  flow  through  the  orifice  is  the  difference  in  the 
levels  of  the  water  surfaces  in  the  two  compartments  of  the  tank. 
This  head  was  measured  in  nearly  all  the  experiments  by  means  of  hook 
gages.  These  gages  were  read  directly  to  0.001  ft.  and  to  0.0005  ft. 
by  estimating.  Vertical  2-in.  pipes  attached  toward  the  bottom  of 
the  tank  served  as  still  basins  for  the  hook  gages.  The  level  of  the 
water  in  the  upstream  compartment  was  determined  by  the  use  of  one 


*A  view  of  the  tank  is  shown  in  Fig.  5  of  Bulletin  No.  96  of  the  Engineering  Experiment  Station 
of  the  University  of  Illinois. 


HYDRAULIC     EXPERIMENTS 


31 


u       '<            TO" 

\J 

\\            °  a 

l|                       Measuring  Pif 
\\ 
II 
II 

U 

Lower  Floor  tine  --^ 

FIG.  11.     TANK  USED  AND  ARRANGEMENT  OF  APPARATUS 


32  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

hook  gage  only,  while  two  gages  were  used  on  the  downstream  com- 
partment in  the  earlier  experiments.  It  was  found,  however,  that  for 
the  lower  heads  the  two  gages  gave  practically  the  same  result,  while 
for  the  higher  heads  the  gage  nearer  the  partition  gave  less  fluctuation. 
For  these  reasons  and  because  of  less  difficulty  in  getting  simultaneous 
readings  of  only  two  gages,  it  was  decided  to  take  readings  with  one 
gage  only  on  each  compartment. 

Zero  readings  of  the  hook  gages  were  obtained  by  reading  the 
gages  when  the  tank  was  nearly  full  and  when  no  water  was  allowed 
to  escape,  the  levels  of  the  water  surfaces  in  the  two  compartments 
then  being  the  same.  Zero  readings  were  taken  frequently  during 
the  experimenting. 

For  most  of  the  heads  above  0.3  ft.,  the  head  was  measured  by 
two  vertical  peizometer  glasses,  one  attached  near  the  bottom  of  each 
compartment,  the  difference  in  readings  of  which  (corrected  for  zero 
reading)  gave  the  head  to  0.001  ft.  These  two  methods  overlapped 
somewhat  so  that  certain  heads  were  measured  by  both  methods. 

Leakage  from  the  tank  and  from  the  measuring  pit  was  determined 
several  times  during  the  progress  of  the  experimenting  and  was  found 
to  be  negligible. 

An  experiment  or  run  consisted  of  the  following:  A  sufficient 
number  of  stoppers  was  removed  from  the  end  of  the  tank  to  give  the 
desired  discharge  and  the  inflow  through  the  6-in.  and  %-in.  pipes 
was  then  adjusted  until  the  difference  in  levels  of  the  water  surfaces 
in  the  two  compartments  of  the  tank  became  constant.  The  M-in. 
supply  pipe  was  used  to  make^the  final  adjustment  of  the  head  and  to 
hold  the  head  constant  throughout  the  experiment.  After  obtaining 
a  constant  head,  the  waste  pipe'shown  in  Fig.  11  was  pulled  from  beneath 
the  discharge  pipe,  thus  allowing  the  water  to  discharge  into  the  meas- 
uring pit  until  the  rise  in  the  pit  was  sufficient  to  allow  its  measurement 
without  appreciable  error  and  also  to  allow  time  for  an  accurate  meas- 
urement of  the  head.  The  head  was  taken  as  an  average  of  from  two 
to  ten  readings  of  the  hook  gages,  the  larger  number  being  necessary 
with  the  higher  velocities  on  account  of  the  greater  fluctuations  of  the 
water  levels  due  to  the  more  turbulent  conditions  of  the  water,  espe- 
cially in  the  downstream  compartment.  Each  experiment  was  repeated, 
as  a  rule,  three  times,  although  in  some  cases  as  many  as  eight  or  ten 
runs  were  made. 


HYDRAULIC    EXPERIMENTS  33 

13.  Method  of  Calculating  the  Coefficient  of  Discharge.  —  The  head, 
h,  causing  flow  through  the  orifice  is  the  difference  in  the  levels  of  the 
water  surfaces  in  the_two  compartments  of  the  tank.  The  ideal  rate 
of  discharge  is  A  ^J2gh  in  which  A  is  the  area  of  the  orifice  in  square 
feet  and  g  is  the  acceleration  due  to  gravity  in  feet  per  second  per  second  ; 
hence  the  coefficient  of  discharge,  c,  is  found  from, 


where  q  is  the  measured  rate  of  discharge  in  cubic  feet  per  second,  as 
determined  from  the  measured  weight  or  volume  discharged  and  the 
corresponding  time. 


34 


ILLINOIS     ENGINEERING     EXPERIMENT     STATION 


VI.     EXPERIMENTAL  RESULTS  AND  DISCUSSION 

14.  Coefficients  of  Discharge. — Fig.  12,  13,  and  14  show  the 
experimental  values  of  the  coefficients  of  discharge  for  the  various 
orifices  tested.  Each  plotted  point  represents  the  average  of  from  two 
to  ten  experiments  at  practically  the  same  head.  It  will  be  noted  that 


/  a  3  4 

Velocity  through  Orifice -ft  per  sec. 

FIG.  12.     DIAGRAMS  SHOWING  VALUES  OF  COEFFICIENTS  OF^DISCHARGE 
OF  CIRCULAR  SUBMERGED  ORIFICES  FOR  VARIOUS  VELOCITIES 


.65 
.60 


.70 

|  ' 

65 
.60 


0.5 


/  2  3  4 

Velocity  throw/7  Orifice  -  ft  per  sec 

FIG.  13.     DIAGRAMS  SHOWING  VALUES  OF  COEFFICIENTS  OF  DISCHARGE  OF 
SQUARE  SUBMERGED  ORIFICES  FOR  VARIOUS  VELOCITIES 


S 


HYDRAULIC     EXPERIMENTS 


35 


^»*j 


60 


0.5 


^  3  4 

Ve/oc/ty  through  Orifice  -ft  per  sec. 


FIG.  I&.    DIAGRAMS  SHOWING  VALUES  OF  COEFFICIENTS  OF  DISCHARGE  OF 
RECTANGULAR  SUBMERGED  ORIFICES  FOR  VARIOUS  VELOCITIES 

for  any  given  orifice  the  coefficient  is  constant  for  the  whole  range  of 
velocity  used  in  these  experiments  which  in  most  of  the  cases  is  about 
%  ft.  per  sec.  to  4  or  5  ft.  per  sec.  This  velocity  range  corresponds 
roughly  to  a  range  in  head  of  0.008  to  0.08  ft.  and  as  may  be  expected 
the  values  of  the  coefficient  show  the  greatest  variation  at  the  very 
low  heads. 


TABLE  5 

VALUES  OF  COEFFICIENT  OF  DISCHARGE  FOR  SUBMERGED  ORIFICES  FOR  VELOCITIES 
FROM  ONE-HALF  TO  FIVE  FEET  PER  SECOND 


Kind  of  Orifice 

Nominal  Size 

Coefficient  of  Discharge 

1  in.  diameter 

0.6351 

2  in.  diameter 

0.615 

Circular 

4  in.  diameter 

0.600 

6  in.  diameter 

0.600 

%  in.  by    ^  in. 

0.620 

1  in.  by      1  in. 

0.610 

Square 

2  in.  by      2  in. 

0.610 

4  in.  by      4  in. 

0.605 

5H  in.  by  5%  in. 

0.600 

^  in.  by  6  in. 

0.635 

Rectangular 

1  in.  by  6  in. 

0.635 

2  in.  by  6  in. 

0.635 

1  Probably  somewhat   in  error   since  diameter   was  not  measured;  nominal  diameter  used  in 
calculations. 


36 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


Table  5  and  Fig.  15,  16,  and  17  show  how  the  coefficient  of  dis- 
charge for  the  orifices  of  any  given  shape  varies  with  the  diameter  or 


^  3  456 

D/ctrr?efer  of  C/rcu/ar  Orifices- in. 

FIG.  15.     CURVE  SHOWING  THE  RELATION  BETWEEN  COEFFICIENT  OF 
DISCHARGE  FOR  CIRCULAR  ORIFICE  AND  DIAMETER  OF  ORIFICE 


FIG.  16. 


3  4  S  6 

5ide  of  Square  Orifices  -  in 

CURVE  SHOWING  THE  RELATION  BETWEEN  COEFFICIENT  OF  DIS- 
CHARGE FOR  SQUARE  ORIFICE  AND  SIDE  OF  ORIFICE 


as 


i          2          3         4 

Vertical  Side  of  Reef  angu  Jar  Orifices  -in. 


FIG.  17.     CURVE  SHOWING  THE  RELATION  BETWEEN  COEFFICIENT  OF  DIS- 

CHARGE OF  RECTANGULAR  ORIFICE  AND  SHORT  SIDE  OF  ORIFICE 

(OTHER  SIDE  BEING  Six  INCHES  IN  EACH  CASE) 

side  of  the  orifice,  while  from  Fig.  18  a  comparison  may  be  made  between 
the  coefficients  of  discharge  for  the  different  shaped  orifices  on  the 
basis  of  their  areas.  These  figures  show  that  the  coefficient  of  discharge 
for  circular  and  square  orifices  decrease  as  the  size  increases  until  an 
area  of  8  or  10  square  inches  is  reached  after  which  the  coefficient  has 
a  constant  value  of  not  far  from  0.60.  This  indicates  that  complete 
contraction  does  not  take  place  with  the  smaller  orifices.  Because  of 
the  uncertainty  of  the  exact  diameter  there  is  some  doubt,  however, 
concerning  the  correct  value  for  the  1-in.  circular  orifice.  It  will  be 
noted  also  that  the  coefficient  of  discharge  for  the  rectangular  orifices 


HYDRAULIC     EXPERIMENTS 


37 


.65 


4      6     8     10    tf     14    16     16    ^O 
Area  of  Orifice  -sq.  in. 


E6    ^Q   3O  3^ 


FIG.  18.    CURVES  SHOWING  RELATION  BETWEEN  COEFFICIENT  OF 
DISCHARGE  AND  AREA  OF  ORIFICES 

remain  constant  for  the  range  of  areas  used  in  these  experiments  and 
that  its  value  is  larger  than  that  for  circular  and  square  orifices  of  the 
same  area.  Fig.  18  indicates  furthermore  that  as  the  area  of  the  orifices 
decreases  below  8  sq.  in.,  the  coefficient  of  discharge  for  circular  orifices 
increases  faster  than  that  for  square  orifices.  These  observations 
suggest  that  the  longer  side  of  the  rectangular  orifices  has  a  controlling 
influence  in  determining  the  rate  of  discharge  for  a  given  head  and 
that  the  corners  of  a  small  square  orifice  are  inefficient  in  discharging 
water  as  compared  with  the  form  of  a  circular  orifice  of  the  same  area. 

15.  Results  Obtained  by  Earlier  Experimenters. — In  order  to  com- 
pare the  results  given  in  this  bulletin  with  those  of  earlier  investigations 
and  to  extend  the  study  to  include  higher  heads  and  velocities,  the 
results  given  in  Table  6  have  been  condensed  from  available  published 
data.  It  will  be  noted  that  the  results  are  not  entirely  concordant, 
but  considering  the  different  arrangements  and  methods  of  measuring 
the  head  and  the  rate  of  discharge,  the  results  show  a  very  good  agree- 
ment. The  low  value  of  the  coefficient  of  discharge  found  by  Francis 
is  due  no  doubt  to  the  fact  that  the  rate  of  discharge  was  measured 
over  a  weir  on  which  the  head  was  rather  small.  From  Table  6  it  will 
be  seen  that  in  some  of  the  earlier  investigations  the  coefficient  of 
discharge  increased  slightly  with  the  head  while  in  others  the  coeffi- 
cient decreased,  and  in  still  others  it  showed  no  systematic  change. 
In  all  cases  the  value  of  the  coefficient  of  discharge  is  not  far  from 
0.60.  The  small  square  orifice  (1.2  in.  by  1.2  in.)  used  by  Hamilton 
Smith  gave  a  slightly  larger  coefficient  than  the  circular  orifice  with 
a  diameter  of  1.2  inches.  This  result  is  the  reverse  of  that  found  in 
the  experiments  described  in  this  bulletin.  The  values  also  of  the 
coefficient  of^discharge  for  circular  and  square  orifficesjas  found  by 


38 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


TABLE  6 

RESULTS  OBTAINED  BY  EARLIER  EXPERIMENTERS  ON  SUBMERGED 
SHARP-EDGED  ORIFICES 


Circular  Orifices 

Square  Orifices 

Source 

Diam- 
eter 
inches 

d 

Head 

feet 

h 

Coeffi- 
cient 
of 
Dis- 
charge 
c 

Source 

Dimen- 
sions 
inches 

Head 
feet 

h 

Coeffi- 
cient 
of 
Dis- 
charge 
c 

Francis 

1.22 

1.024 
1.324 
1.490 
1.499 
1.514 

.592 
.592 
.592 
.593 
.591 

Hamilton  Smith,  Jr. 

0.6  by  0.6 

0.35 
2.21 
4.06 

.6201 
.6092 
.6068 

Hamilton  Smith,  Jr. 

1.2  by  1.2 

0.207 
0.410 
0.771 
1.52 
2.32 
3.11 
3.95 

.6117 
.6091 
.6053 
.6055 
.6040 
.6052 
.6048 

Hamilton  Smith,  Jr. 

0.6 

0.437 
2.16 
4.08 

.6183 
.6041 
.6016 

Hamilton  Smith,  Jr. 

1.2 

0.250 
0.648 
0.985 
1.51 
2.00 
2.58 
2.99 
3.57 
3.97 

.6048 
.6027 
.6025 
.6006 
.6006 
.5997 
.5989 
.5987 
.5992 

Ellis 

12  by  12 

2.32 
3.92 
7.99 
11.58 
14.31 
16.22 
18.45 

.600 
.602 
.606 
.605 
.611 
.606 
.606 

Ellis 

12.0 

2.60 
4.71 
6.41 
8.10 
8.80 
12.09 
14.25 
16.29 
18.66 

.607 
.590 
.606 
.599 
.600 
.600 
.601 
.602 
.599 

Balch 

12  by  12 

0.363 
0.750 
0.771 
0.826 
0.905 
1.134 
1.371 
2.097 
2.636 
3.220 
3.975 

.  5940 
.5940 
.  5932 
.5982 
.5950 
.5960 
.5970 
.6056 
.6105 
.6095 
.6148 

Balch 

12.0 

0.145 
0.469 
0.851 
1.254 
1.612 
2.012 
2.421 
2.949 
3.410 
4.015 

.5909 
.5902 
.5912 
.5993 
.5921 
.5924 
.5954 
.5967 
.6006 
.6054 

Stewart 

48  by  48 
(3.  72  in. 
thick) 

.05 
.10 
.15 
.20 
.25 
.30 

.626 
.608 
.605 
.605 
.606 
.610 

Rectangular  Orifices 

Hamilton  Smith,  Jr. 

0.6  by  3.6 

0.614 
1.63 
2.77 

.6219 
.6207 
.6188 

HYDRAULIC    EXPERIMENTS  39 

Hamilton  Smith  are  slightly  less  than  those  herein  reported  in  Table  5. 
Omitting  the  values  as  given  by  Francis  it  will  be  observed  that  there 
is  very  little  difference  between  the  coefficients  for  the  small  and  the 
large  orifices,  the  value  of  the  coefficient  varying  only  slightly  from 
0.60.  From  the  results  obtained  in  the  present  investigation  as  given 
in  Table  5  and  in  Fig.  12,  13,  and  14,  it  will  be  seen  that  the  coefficient 
varies  more  with  the  size  of  the  orifice  than  is  shown  by  the  results  of 
the  earlier  experiments,  as  given  in  Table  6. 

It  will  be  observed  also  that  the  coefficient  of  discharge  for  the 
rectangular  orifice  used  by  Hamilton  Smith  is  somewhat  smaller  than 
that  herein  reported.  It  may  seem  that  the  diverging  sides  of  the 
orifices  used  in  the  experiments  reported  in  this  bulletin  (orifice  plate 
M-in.  thick)  would  form  a  diverging  mouthpiece,  particularly  in  the 
case  of  the  smaller  orifices,  but  experiments*  on  diverging  mouth- 
pieces have  shown  that  a  mouthpiece  having  a  total  angle  of  divergence 
of  90  degrees  has  very  little,  if  any,  effect  on  the  rate  of  discharge. 

16.  Comparison  with  Discharge  into  Air. — The  experiments  on 
sharp-edged  orifices  with  discharge  into  air  are  more  numerous  than 
for  submerged  discharge.  The  experiments  of  Bilton  and  to  a  less 
degree  those  by  Judd  and  King,  and  those  by  Mair  and  by  Ellis  indicate 
that  there  is  a  critical  head  for  each  circular  orifice  above  which  the 
coefficient  remains  constant.  Bilton  concludes  that  "circular  orifices 
of  2>£-in.  diameter,  and  over,  under  heads  of  17  in.,  and  over,  have  a 
common  coefficient  of  discharge  lying  between  0.59  and  0.60  but  which 
is  probably  about  0.598  (subject  to  the  head  being  not  less  than  2  or 
3  diameters)."  The  results  of  the  experiments  of  Hamilton  Smith,  as 
is  well  known,  indicate  that  the  coefficient  of  discharge  gradually 
decreases  as  the  size  of  the  orifice  increases,  and  also  decreases  as  the 
head  increases  until  at  a  head  of  100  ft.  all  orifices,  regardless  of  the 
size  or  the  shape,  have  a  common  coefficient  of  discharge. 

The  results  of  the  experiments  on  submerged  orifices  herein  reported 
seem  to  indicate,  as  previously  noted,  that  orifices  having  diameters 
greater  than  about  2^  in.  (or  sides,  if  square)  have  a  common  co- 
efficient of  discharge  which  is  very  close  to  0.60.  There  seems,  how- 
ever, to  be  no  evidence  of  a  critical  head  since  the  coefficient  remains 
constant  for  the  whole  range  of  head  used,  nor  is  there  evidence  of  a 
critical  head  in  the  results  obtained  by  earlier  experimenters  on  sub- 
merged orifices  as  given  in  Table  6. 


*"The   Effect   of   Mouthpieces   on   the    Flow    of   Water  Through   a  Submerged  Short  Pipe." 
Univ.  of  111.  Eng.  Exp.  Sta.,  Bui.  96,  1917. 


40  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

From  a  study  of  the  experimental  results  on  orifices  with  discharge 
into  air  it  is  believed  that  the  coefficient  of  discharge  for  submerged 
orifices  are  the  same  as  those  for  discharge  into  air  for  the  same  heads 
and  sizes  and  shapes  (except  for  very  small  heads).  It  is  doubtful  if 
the  statement  sometimes  made,  namely,  that  the  coefficient  of  discharge 
for  submerged  orifices  is  about  one  per  cent  less  than  that  for  free  dis- 
charge, is  justified. 

17.  Summary. — The  following  brief  summary  is  given  as  applying 
to  submerged  sharp-edged  orifices  for  velocities  from  K  to  5  ft.  per  sec. 

(1)  The  coefficient  of  discharge  for  a  circular,  a  square,  or 
a  rectangular  submerged  orifice  does  not  vary  with  the  velocity. 

(2)  Circular   and   square   submerged   orifices  having  areas 
greater  than  about  10  sq.  in.  have  a  common  coefficient  of  dis- 
charge varying  but  little  from  0.60. 

(3)  Rectangular  submerged  orifices  having  one  side  from  3  to 
12  times  the  other  side  have  a  constant  coefficient  of  discharge 
which  is  larger  than  that  for  circular  and  square  orifices  of  the 
same  size,  particularly  for  the  larger  areas,  at  least  up  to  a  size 
of  12  sq.  in. 

(4)  The  flow  of  water  through  submerged  sharp-edged  ori- 
fices is  very  nearly  the  same  as  that  for  the  same  kind  of  orifices 
with  discharge  into  air,  provided  the  head  is  not  less  than  2  or  3 

.  diameters  when  the  discharge  is  jnto  air. 


PART  III 
FIRE  STREAMS  FROM  SMALL  HOSE  AND  NOZZLES 

BY  VIRGIL  R  FLEMING 

ASSISTANT  PROFESSOR  OF  APPLIED  MECHANICS 


CONTENTS 

PART  III 
FIRE  STREAMS   FROM  SMALL  HOSE  AND   NOZZLES 

PAGE 

VII.  INTRODUCTION      .     .     ...     ...     ...   ,     .     .     .     .     .     45 

18.  Scope  of  Experiments       .      .      .     .      .      .      .      .      .45 

19.  Acknowledgment '.      .      .      .     46 

VIII.  APPARATUS  AND  METHOD  OF  EXPERIMENTING    ....     47 

20.  Hose  and  Nozzles .      .     .,    .    • .     .    .  .     .     .     .  •    .     47 

21.  Method  of  Experimenting     ........     48 

IX.  EXPERIMENTAL  RESULTS  AND  DISCUSSION     .     .     .     .     .  49 

22.  Results  from  Freeman's  Experiments    .                       .  49 

23.  Experimental  Data .49 

24.  Friction  Factors    .     ...           .      .      .     ...  53 

25.  Coefficients  of  Discharge 54 

26.  Height  and  Horizontal  Distance  of  Jets     .      ...      .  55 

27.  Effect  of  Cylindrical  Tip 56 

28.  Requirements  for  Temporary  Fire  Protection  for  the 

Interior  of  Buildings       . 57 

29.  Summary .........     59 


43 


LIST  OF   FIGURES 

NO.  PAGE 

19.  Longitudinal  Sections  of  Nozzles  Tested    .     ...     .     .      .     .     .     .  47 

20.  Cross-section  of  Piezometer  Coupling 48 

21.  Diagram  Showing  Friction  Factors  in  Rubber-lined  and  Unlined  Hose   .  53 

22.  Diagram  Showing  Coefficients  of  Discharge  of  Nozzles 54 


LIST  OF  TABLES 

7.  Freeman's  Results  for   1-in.,  1^-in.  and  l}4-in.   Nozzles    Attached   to 

2^-in.  Hose       .     .     '. .     .     .     .     50 

8.  Results  of  Experiments  at  University  of  Illinois  with  y\  6-m->  Ke-m->  a^d 

in.  Nozzles  Attached  to  1 3^-in.  Hose        51 


44 


HYDRAULIC    EXPERIMENTS  45 

PART  III 
FIRE  STREAMS   FROM   SMALL  HOSE  AND   NOZZLES* 


VII.     INTRODUCTION 

18.  Scope  of  Experiments. — Part  III  presents  the  results  of  experi- 
ments on  IK-in.  hose  and  nozzles.  Both  rubber-lined  hose  and  un- 
lined  linen  hose  were  used.  Three  sizes  of  conical  nozzles  were  tested, 
the  diameters  of  the  nozzle  openings  being  ^fe  in.,  Ke  in.,  and  K  in. 

The  loss  of  head  in  the  hose  due  to  friction  and  the  corresponding 
friction  factor  are  given  for  each  hose  for  a  range  in  velocity  from 
about  4  to  8  ft.  per  sec.  The  coefficient  of  discharge  for  each  nozzle 
is  recorded  for  a  range  in  pressure  at  the  base  of  the  nozzle  from  about 
10  to  85  Ib.  per  sq.  in.  The  height  and  the  horizontal  distance  which 
the  jets  reached  are  also  recorded.  The  influence  of  a  cylindrical  tip 
on  a  nozzle  is  brought  out  and  some  discussion  is  given  concerning 
the  quantity  of  water  required  for  temporary  fire  protection  for  the 
interior  of  buildings. 

The  importance  of  adequate  fire  protection  has  become  so  well  rec- 
ognized that  most  buildings,  even  those  of  moderate  size,  are  equipped 
with  some  sort  of  fire  apparatus  for  immediate  service  in  case  of  fire  in 
the  interior  of  the  building  and  until  the  city  fire  department  arrives. 
The  ordinary  water  buckets  and  portable  chemical  fire  extinguishers 
have  in  a  large  measure  been  supplemented  with  small  fire  hose.  Few 
data  are  available  concerning  the  hydraulics  of  small  fire  streams. 
Many  inquiries  concerning  the  discharge  from  small  nozzles  and  the 
loss  of  head  in  small  hose  led  to  the  tests  which  are  herein  described. 
The  tests  were  undertaken  with  the  object  of  acquiring  data  and  putting 
the  results  into  so  workable  a  form  that  it  would  be  easy  to  compute 
the  quantity  of  water  delivered  by  a  nozzle  of  the  size  ordinarily  used 
in  the  fire  protection  of  the  interior  of  buildings  or  to  compute  the 
pressure  necessary  in  the  mains  to  give  an  effective  fire  stream  from 
such  nozzles,  and  also  to  throw  some  light  upon  the  quantity  of  water 
which  would  be  considered  sufficient  for  temporary  protection. 

*  The   experiments   used   in    Part   III    of    this  Bulletin  were  reported  in  the   Proceedings  of 
the  Fifth  Meeting  of  the  Illinois  Water  Supply  Association,  p.  170,  1913. 


46  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

19.  Acknowledgment. — The  experiments  here  used  were  con- 
ducted at  the  University  of  Illinois  under  the  direction  of  the  writer 
by  E.  O.  KORSMO  and  A.  B.  NEININGER  of  the  class  of  1911  as  thesis 
work.  Much  credit  is  due  them  for  the  care  and  thought  given  the 
problem  and  the  thoroughness  with  which  they  did  their  work.  The 
water  for  the  experiments  was  drawn  from  the  University  mains. 
The  experiments  for  determining  the  height  and  the  horizontal  dis- 
tance the  jets  would  reach  were  conducted  out  of  doors.  The  other 
experiments  were  carried  on  in  the  Hydraulics  Laboratory. 


HYDRAULIC     EXPERIMENTS 


47 


VIII.     APPARATUS  AND  METHOD  OF  EXPERIMENTING 

20.  Hose  and  Nozzks. — Rubber-lined  cotton  hose  and  unlined 
linen  hose  having  a  nominal  diameter  of  \^A  in.  were  used,  the  length 
of  the  test  section  for  determining  the  lost  head  being  50  ft.  in  each 
case.  The  hose  taken  was  from  the  racks  in  the  University  buildings 
and  is  representative  of  hose  of  this  size  commonly  in  use. 

Three  IJ-in.  conical  nozzles  having  different  sizes  of  openings, 
as  shown  in  Fig.  19,  were  tested.  The  first  nozzle  had  a  diameter  of 


out  smooth 


FIG.  19.     LONGITUDINAL  SECTIONS  OF  NOZZLES  TESTED 


Me  in.  The  second  nozzle  had  a  diameter  of  0.428  in.,  which  is  ap- 
proximately KG  in.,  and  in  compiling  the  tables,  corrections  were  made 
so  as  to  apply  to  a  Ke-in.  nozzle.  The  third  nozzle  had  a  diameter 
of  Yz  in.  The  Me-in.  nozzle  was  12  in.  long  while  the  other  two  were 
only  6  in.  long  (see  Fig.  19).  The  Me-in.  and  the  Ke-in.  nozzles  were 
rough  on  the  interior  surfaces,  having  been  left  just  as  ihey  came 
from  the  molds,  the  prints  of  the  sand  core  being  plainly  visible. 
The  tips  had  been  smoothed  slightly  by  running  a  drill  through  the 


48 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


opening,  but  the  cylindrical  portion  made  by  the  drill  was  very  short 
in  both  cases.  The  M-in.  nozzle  was  made  from  a  Ke-in.  nozzle.  The 
entire  inner  surface  was  machined  smooth  and  a  K-in.  reamer  was  run 
through  the  opening  making  a  cylindrical  portion  K  in.  long. 

21.  Method  of  Experimenting. — The  loss  of  head  was  measured 
over  a  length  of  fifty  feet  of  the  hose  by  means  of  a  differential  mercury 
gage.  The  average  pressure  at  a  section  of  the  hose  was  obtained  with 
a  piezometer  connection  or  coupling  of  the  Freeman  type.  A  cross- 
section  of  one  of  these  couplings  is  shown  in  Fig.  20.  The  discharge 


Openings, -3  of/a, 

Sec  f /on  fl-ft 

FIG.  20.     CROSS-SECTION  OF  PIEZOMETER  COUPLING 


through  the  hose  when  determining  the  lost  head  in  the  hose  was  meas- 
ured with  a  calibrated  nozzle.  When  determining  the  coefficient  of 
discharge  for  the  nozzles  the  discharge  was  measured  by  weighing. 
The  pressure  at  the  base  of  the  nozzle  was  measured  with  a  calibrated 
pressure  gage. 

The  vertical  heights  attained  by  the  streams  were  determined  by 
means  of  a  transit  and  the  horizontal  distances  reached  were  found 
by  measuring  with  a  tape  from  stakes  which  were  driven  in  the  ground 
at  frequent  intervals  and  at  known  distances  from  the  nozzle. 


HYDRAULIC    EXPERIMENTS  49 


IX.     EXPERIMENTAL  RESULTS  AND  DISCUSSION 

22.  Results  from  Freeman's  Experiments. — In  1888  John  R.  Free- 
man conducted  an  extensive  series  of  tests  upon  2M-in.  fire  hose  and 
nozzles.*     In  general,  Freeman  arrived  at  the  following  conclusions: 
Smooth  conical  nozzles  give  coefficients  of  discharge  as  high  as  any 
other  form  of  nozzle,  the  jets  reach  farther  and  the  streams  remain 
solid  for  greater  distances  than  for  any  other  form  of  nozzle  of  the 
same  size  of  opening  and  with  the  same  pressure  at  the  base  of  the 
nozzle.     For  smooth  conical  nozzles    IH  or    IH  in.  in  diameter,   a 
coefficient  of  discharge  of  0.977  may  be  taken  with  great  confidence 
that  it  will  not  be  more  than  one-half  of  1  per  cent  in  error.     The 
coefficient  will  be   slightly   larger   for   smaller  nozzles.     The   nozzle 
makes  a  very  convenient  method  of  measuring  water.     The  friction 
is  but  slightly  more  in  smooth  rubber-lined  hose  than  in  clean  iron  pipe 
of  the  same  diameter.     The  friction  in  unlined  linen  hose  is  about 
two  and  one-third  times  as  much  as  in  smooth  rubber-lined  hose. 
A  hose  elongates  from  2  per  cent  to  5  per  cent  with  a  pressure  of  50 
Ib.  per  sq.  in.     This  elongation  produces  a  sinuosity  which  increases 
the  loss  of  head  about  6  per  cent.     Care  should  be  exercised  that 
there  is  no  abrupt  change  of  section  in  the  hose  couplings  and  that 
no  washers  or  gaskets  are  so  left  as  to  impede  the  flow  of  water. 

It  is  frequently  recommended  that  a  250  gal.  per  min.  fire  stream 
be  used  in  business  districts,  while  a  175  or  a  200  gal.  per  min.  stream 
may  be  used  in  a  residential  district.  These  discharges  correspond  to 
a  nozzle  pressure  of  40  to  50  Ib.  per  sq.  in.,  and  a  hydrant  pressure  of 
80  to  110  Ib.  per  sq.  in.  These  values  refer  to  outside  service.  Table 
7  gives  data  for  2M-in.  hose  and  nozzles  for  three  different  sizes  of 
nozzle  openings  taken  from  Freeman's  results.  This  table  is  con- 
venient for  making  calculations  for  outside  fire  protection. 

23.  Experimental  Data. — Table  8  gives  the  more  important  data 
of  the  experiments  with  hose  and  nozzles  herein  reported.     Values  are 
given  for  the  pressures  at  the  base  of  the  nozzles,  the  discharges,  the 
loss  of  head  in  the  hose,  and  the  vertical  and  horizontal  distances  reached 
by  the  jets.     Other  results  discussed  have  been  calculated  from  the 
data  in  this  table. 


*"  Experiments  Relating   to   the    Hydraulics   of   Fire   Streams."     Trans.  Am.  Soc.  Civ.  Eng., 
Vol.  XXI,  p.  304,  1889. 


50 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


TABLE  7 

FREEMAN'S  RESULTS  FOR  I-IN.  I^-IN.  AND  I^-IN.  NOZZLES  ATTACHED 
TO  2^-IN.  HOSE 

1-iNCH  NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose 

Vertical 

Horizontal  Distance 

Pressure 

Height  of 

Base  of 
Nozzle 

Discharge 

Rubber 
Lined 

Unlined 
Linen 

Jet  for 
Good  Fire 
Stream 

Jet  for 
Good  Fire 
Stream 

Extreme 
Drops  at 
Level 

of  Nozzle 

Lb.  per 
sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

132 

5 

10 

35 

37 

77 

30 

161 

7 

15 

51 

47 

109 

40 

186 

10 

20 

64 

55 

133 

50 

208 

12 

25 

73 

61 

152 

60 

228 

15 

30 

79 

67 

167 

70 

246 

17 

35 

85 

72 

179 

NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose 

Vertical 

Horizontal  Distance 

Pressure 

Height  of 

Base  of 
Nozzle 

Discharge 

Jet  for 
Good  Fire 

Jet  for 

Extreme 

Rubber 

Unlined 

Stream 

Good  Fire 

Drops  at 

Lined 

Linen 

Stream 

Level 

of  Nozzle 

Lb.  per 

sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

168 

8 

16 

36 

38 

80 

30 

206 

12 

25 

52 

50 

115 

40 

238 

16 

33 

65 

59 

142 

50 

266 

20 

41 

75 

66 

162 

60 

291 

24 

49 

83 

72 

178  j 

70 

314 

28 

57 

88 

77 

191 

HYDRAULIC     EXPERIMENTS 


51 


NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose 

Vertical 

Horizontal  Distance 

Pressure 

Height  of 

Base  of 
Nozzle 

Discharge 

Jet  for 
Good  Fire 

Jet  for 

Extreme 

Rubber 
Lined 

Unlined 
Linen 

Stream 

Good  Fire 
Stream 

Drops  at 
Level 

of  Nozzle 

Lb.  per 
sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

209 

12 

25 

37 

40 

83 

30 

256 

19 

38 

53 

54 

119 

40 

296 

25 

51 

67 

63 

148 

50 

331 

31 

63 

77 

70 

169 

60 

363 

37 

76 

85 

76 

186 

70 

392 

43 

88 

91 

81 

200 

TABLE  8 

RESULTS  OF  EXPERIMENTS  AT  UNIVERSITY  OF  ILLINOIS  WITH  %6-m., 
AND  H-IN.  NOZZLES  ATTACHED  TO  13-^-iN.  HOSE 

%  6-iNCH  NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose 

Vertical 

Horizontal  Distance 

Pressure 
Base  of 
Nozzle 

Discharge 

Height  of 
Jet  for 
Good  Fire 
Stream 

Rubber 
Lined 

Unlined 
Linen 

Jet  for 
Good  Fire 
Stream 

Extreme 
Drops  at 
Level 
of  Nozzle 

Lb.  per 

sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

12 

.7 

1.3 

28 

15 

53 

30 

15 

1.1 

1.9 

32 

18 

63 

40 

17 

1.5 

2.6 

34 

21 

71 

50 

19 

1.8 

3.2 

35 

23 

78 

60 

21 

2.2 

3.9 

36 

26 

84 

70 

23 

2.6 

4.5 

37 

28 

90 

80 

24 

2.9 

5.2 

38 

29 

96 

90 

26 

3.3 

5.9 

39 

30 

102 

100 

28 

3.7 

6.5 

40 

31 

107 

52 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose         , 

Vertical 

Horizontal  Distance 

T>         pOQ|,rO 

Base  of 
Nozzle  . 

Discharge 

Rubber 
Lined 

Unlined 
Linen 

Jet  for 
Good  Fire 
Stream 

Jet  for 
Good  Fire 
Stream 

Extreme 
Drops  at 
Level 
of  Nozzle 

Lb.  per 
sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

25 

2.8 

5.1 

23 

10 

45 

30 

30 

4.2 

7.7 

27 

13 

54 

40 

35 

5.6 

10.2 

30 

16 

63 

50 

39 

7.0 

12.8- 

32 

18 

70 

60 

43 

8.5 

15.3 

33 

20 

77 

70 

47 

9.8 

17.8 

34 

21 

84 

80 

50 

11.1 

20.3 

35 

23 

94 

90 

53 

12.7 

22.9 

36 

24 

99 

100 

56 

14.1 

25.5 

37 

25 

106 

NOZZLE 


Loss  of  Head  in 
100  Feet  of  Hose 

Vertical 

Horizontal  Distance 

Pressure 
Base  of 
Nozzle 

Discharge 

Height  of 
Jet  for 
Good  Fire 
Stream 

Rubber 
Lined 

Unlined 
Linen 

Jet  for 
Good  Fire 
Stream 

Extreme 
Drops  at 
Level 
of  Nozzle 

Lb.  per 

sq.  in. 

Gallons  per 
minute 

Lb.  per 
sq.  in. 

Lb.  per 
sq.  in. 

Feet 

Feet 

Feet 

20 

33 

5.2 

9.5 

34 

15 

63 

30 

40 

7.7 

14.4 

37 

20 

79 

40 

46 

10.2 

18.8 

38 

25 

91 

50 

52 

12.8 

23.8 

39 

30 

102 

60 

57 

15.4 

28.5 

40 

33 

111 

70 

61 

18.0 

32.7 

41 

37 

120 

80 

65 

20.5 

38.4 

42 

40 

127 

90 

69 

23.0 

42.0 

43 

43 

134 

100 

73 

25.6 

47.0 

44 

46 

140 

HYDRAULIC     EXPERIMENTS 


53 


24.     Friction  Factors. — The  curves  of  Fig.  21  show  the  friction 
factors  for  each  kind  of  hose  used  and  for  velocities  in  the  hose  ranging 


m 


€  8  /O 

-  ft  per  sec. 


FIG.  21. 


DIAGRAM  SHOWING  FRICTION  FACTORS'IN  ^RUBBER-LINED  AND 
UNLINED  HOSE 


from  4  to  8  ft.  per  sec.  These  curves  cover  the  range  of  velocities 
which  would  be  met  in  ordinary  use.  The  friction  factor  /  is  computed 
from  the  formula 

h=d^g 

h  =  head  lost  in  feet  of  water 
I  =  length  of  hose  in  feet 
d  =  diameter  of  hose  in  feet 

v  =  velocity  of  the  water  in  the  hose  in  feet  per  second 
g  =  acceleration  due  to  gravity  in  feet  per  second  per  second 

The  loss  of  head  in  the  rubber-lined  hose  varies  almost  directly 
as  the  square  of  the  velocity  and  is  about  the  same  as  the  loss  of  head 
in  clean  iron  pipe  of  the  same  diameter.  The  friction  factor  for  the 
unlined  linen  hose  decreases  as  the  velocity  increases,  or  in  other  words 
the  loss  of  head  does  not  vary  directly  as  the  square  of  the  velocity, 
the  ratio  of  the  lost  head  to  the  square  of  the  velocity  being  larger  for 
the  lower  velocities.  The  reason  that  the  friction  factor  for  unlined 
linen  hose  decreased  more  rapidly  with  the  velocity  than  does  that  for 
rubber-lined  cotton  hose  may  be  that  the  diameter  of  the  unlined  hose 


54 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


is  increased  more  than  that  of  the  rubber-lined  cotton  hose  by  the 
increasing  pressures  which  accompany  the  increasing  velocities.  This 
would  make  the  value  of  d  larger  and  the  value  of  v  smaller  in  the  equa- 
tion for  /  than  was  actually  used.  It  is  probable,  furthermore,  that  the 
increasing  pressure  decreases  the  roughness  of  the  unlined  linen  hose 
more  than  it  does  for  rubber-lined  hose.  In  general  the  lost  head  in 
the  unlined  linen  hose  is  about  twice  as  great  as  in  the  rubber-lined 
cotton  hose.  If  an  average  value  of  the  friction  factor  (0.06)  is  used 
for  the  unlined  linen  hose,  no  great  error  will  enter  into  the  results 
under  ordinary  circumstances.  The  length  of  hose  will  ordinarily  not 
be  mose  than  100  feet  and  for  this  length  about  10  Ib.  per  sq.  in.  will 
be  the  maximum  loss  of  head  in  the  unlined  linen  hose  under  working 
conditions  with  nozzles  giving  streams  up  to  K  in.  in  diameter.  An 
error  as  large  as  10  per  cent  in  the  calculation  of  the  loss  of  head  in 
the  hose  would  affect  the  nozzle  pressure  not  more  than  one  pound 
per  square  inch. 


O      JO      ^O    3O    4O     5O    6O     7O    SO     9O 

Pressure  a/  fiase  of/Yozz/e-  /£  per  sq.in 
FIG.  22.     DIAGRAM  SHOWING  COEFFICIENTS  OF  DISCHARGE  OF  NOZZLES 

While  the  loss  of  head  in  the  unlined  linen  hose  is  about  twice  as 
great  as  the  loss  of  head  in  the  rubber-lined  hose,  the  linen  hose  has 
several  advantages.  It  is  much  lighter  to  handle,  folds  up  in  less  space 
on  the  wall  racks,  costs  only  about  50  to  60  per  cent  of  the  cost  of 
rubber-lined  hose  and,  in  an  ordinary  building,  its  life  is  much  longer. 

25.  Coefficients  of  Discharge. — The  coefficients  of  discharge  for 
each  of  the  three  sizes  of  nozzles  are  given  in  Fig.  22  for  pressures 


HYDRAULIC    EXPERIMENTS  55 

at  the  base  of  the  nozzle  ranging  from  about  10  to  85  Ib.  per  sq.  in. 
This  range  of  pressures  corresponds  to  a  range  in  the  velocity  of  the 
issuing  jet  from  a  minimum  of  about  35  ft.  per  sec.  with  the  >£-in. 
nozzle  to  a  maximum  of  about  185  ft.  per  sec.  with  the  Ke-in.  nozzle. 
The  coefficient  of  discharge  is  the  ratio  of  the  measured  discharge  to 
the  ideal  discharge.  The  measured  discharge  was  weighed  and  the 
volume  computed  from  the  weights.  The  ideal  discharge  was  com- 
puted from  the  formula 

q  =  A  ij~2gh 

q  =  discharge  in  cubic  feet  per  second.  A  =  area  of  the  opening  of  the 
nozzle  in  square  feet,  g  =  acceleration  due  to  gravity  in  feet  per 
second  per  second.  h  =  pressure  at  the  base  of  the  nozzle  in  feet  of 
water.  The  velocity  of  approach  to  the  nozzle  was  negligible  and 
was,  therefore,  not  considered  in  the  equation  for  the  ideal  discharge. 
The  pressure  at  the  base  of  the  nozzles  was  measured  with  calibrated 
pressure  gages. 

The  coefficient  of  discharge  for  the  Ke-in.  and  the  3^-in.  nozzles 
is  nearly  constant  for  all  pressures  and  averages  0.98.  The  coefficient 
is  slightly  lower  than  0.98  for  the  Ke-in.  nozzle  at  the  higher  pressures. 
The  ^6-in.  nozzle  gives  a  coefficient  of  0.95.  The  Y\  e-in.  nozzle  is  12 
inches  long  while  the  other  two  are  only  6  inches  long,  and  this  greater 
length  adds  somewhat  to  the  friction  and  lowers  the  coefficient  of 
discharge  for  the  ^fe-in.  nozzle. 

The  Me-in.  and  the  Ke-in.  nozzles  were  rough  on  the  interior 
surfaces,  having  been  left  just  as  they  came  from  the  molds.  The 
tips  had  been  smoothed  slightly  by  running  a  drill  through  the  opening, 
but  the  cylindrical  portion  made  by  the  drills  was  very  short  in  each 
case  and  the  nozzles  gave  streams  which  sprayed  badly  a  short  distance 
away.  The  3^-in.  nozzle  was  made  from  a  Ke-in.  nozzle.  The  entire 
inner  surface  was  first  machined  out  in  hopes  that  it  would  prevent 
the  spraying  of  the  jet,  but  the  nozzle  gave  a  stream  which  appeared 
no  better  than  before  machining.  Then  a  1jH*2-in.  reamer  and  finally 
a  M-in.  reamer  were  run  through  the  opening,  each  reducing  the  spray- 
ing. The  >6-in.  reamer  made  the  cylindrical  portion  of  the  opening 
M-in.  long,  and  the  resulting  nozzle  gave  a  very  good  stream.  An 
opening  larger  than  M-in.  could  not  be  made  in  the  nozzle  because 
of  the  thinness  of  the  walls. 

26.  Height  and  Horizontal  Distance  of  Jets. — The  heights  and  the 
horizontal  distances  reached  by  the  jets  from  each  of  the  three  nozzles 


56  ILLINOIS    ENGINEERING     EXPERIMENT    STATION 

used  are  given"  in  Table  8.  As  stated,  the  vertical  heights  were  meas- 
ured by  means  of  a  transit  and  the  horizontal  distances  were  measured 
with  a  tape^from^stakes  which  were  driven  in  the  ground  at  frequent 
known  space  intervals.  The  observations  were  made  when  a  moderate 
wind  was  blowing  which  interfered  with  the  streams  considerably.  A 
stream  was  considered  good  for  the  distance  in  which  practically  all  the 
water  [would  pass  through  a  circle  whose  diameter  was  18  inches. 
The~value  was  an  arbitrary  selection  and  the  streams  might  be  con- 
sidered by  some  as  effective  for  greater  distances  than  those  given  in 
Table  8.  The  streams,  however,  beyond  the  sections  chosen,  diverged 
rapidly  and  the  selection  of  a  circle  larger  than  18  inches  would  have 
added  but  a  few  feet  to  the  distances  given  in  Table  8  in  any  case. 

27.  Effect  of  Cylindrical  Tip. — The  tests  show  clearly  the  impor- 
tance of  a  smooth  cylindrical  opening  at  the  tip  of  the  nozzle.  A  com- 
parison of  the  results  of  the  tests  on  the  Ke-in.  and  the  M-in.  nozzles 
for  vertical  heights  and  horizontal  distances  of  the  jets  will  show  this 
difference.  In  the  case  of  the  Ke-in.  nozzle  with  a  pressure  of  30  Ib. 
per  sq.  in.  at  the  base  of  the  nozzle  the  vertical  height  of  the  jet  was 
27  ft.  as  compared  with  37  ft.  for  the  ^-in.  nozzle  for  the  same  pressure. 
Likewise  the  horizontal  distance  reached  with  the  Ke-in.  nozzle  was 
13  ft.  as  compared  with  20  ft.  with  the  K-in.  nozzle.  Similar  com- 
parisons may  be  made  for  other  pressures  at  the  base  of  the  nozzle. 
The  appearance  of  the  jets  showed  a  much  greater  difference  than 
the  data  would  indicate.  It  must  be  remembered  that  the  two  nozzles 
were  alike  and  gave  streams  which  appeared  to  be  the  same  before 
one  was  reamed  out  to  a  larger  size. 

It  will  be  noted  also  that,  in  the  case  of  the  % e-in.  nozzle  for  a 
pressure  of  30  Ib.  per  sq.  in.  at  the  base  of  the  nozzle,  the  vertical  and 
horizontal  distances  reached  by  the  stream  were  respectively  32  and 
18  ft.,  which  indicate  that  the  improvement  in  the  carrying  capacity 
of  the  K-in.  nozzle  over  that  of  the  Ke-in.  nozzle  was  not  due  to  the 
smoother  condition  of  the  interior  surface  of  the  M-in.  nozzle,  but 
rather  to  the  effect  of  the  cylindrical  tip.  The  condition  of  the  interior 
surface  of  the  nozzle  to  within  one-half  inch  of  the  end  does  not  seem 
to  affect  appreciably  either  the  quantity  of  discharge  or  the  quality 
of  the  stream. 

It  seems  important,  therefore,  that  the  tip  of  the  nozzle  should 
be  reamed  out  for  a  distance  of  at  least  %  in.  in  order  to  obtain  a  good 
fire  stream.  It  is  probably  true  also  that  for  nozzles  somewhat  larger 


HYDRAULIC    EXPERIMENTS  57 

than  those  used  in  these  experiments  the  length  of  the  cylindrical 
portion  should  be  more  than  H  in.,  perhaps  equal  to  the  diameter 
of  the  issuing  stream. 

28.  Requirements  for  Temporary  Fire  Protection  for  the  Interior 
of  Buildings. — Small  fire  hose  and  nozzles  should  be  used  as  a  tem- 
porary protection  and  brought  into  play  until  greater  relief  is  at  hand. 
They  must  necessarily  operate  under  ordinary  working  pressures  in 
the  mains  more  often  than  under  fire  pressures.  With  40  Ib.  per 
sq.  in.  as  an  average  pressure  in  the  mains,  there  should  be,  after 
deducting  for  losses  in  the  hose  and  connecting  pipes,  about  30  Ib. 
per  sq.  in.  at  the  nozzle.  This  pressure,  of  course,  would  be  still 
further  reduced  if  the  nozzle  used  was  at  a  higher  elevation  than  the 
main.  With  a  nozzle  pressure  of  30  Ib.  per  sq.  in.  the  K-in.  nozzle 
will  discharge  40  gal.  per  min.,  the  Ke-in.  and  the  Y\  e-in.  nozzles  will 
discharge  30  and  15  gal.  per  min.,  respectively.  It  is  felt  that  the 
discharge  from  the  two  smaller  nozzles  is  not  great  enough  for  effective 
work.  It  is  true  that  the  pressure  at  the  nozzle  for  the  smaller  sizes 
with  a  given  pressure  in  the  main  will  be  somewhat  greater  than  for 
the  M-in.  nozzle,  because  of  the  decreased  velocity  in  the  hose  which 
will  give  a  smaller  loss  of  head,  but  this  difference  in  pressure  will  not 
be  enough  to  increase  the  discharge  materially  for  an  ordinary  length 
of  hose.  The  discharge  from  the  iKe-in.  nozzle  is  too  small  to  be  very 
effective  even  at  higher  pressures.  The  discharge  for  a  pressure  of 
100  Ib.  per  sq.  in.  is  but  28  gal.  per  min.  It  is  recommended  that 
M-in.  nozzles  be  used  with  IM-in.  hose.  For  nozzles  larger  than  M 
in.,  the  discharge  would  become  greater  and  increase  the  loss  of  head 
in  the  hose  to  such  an  extent  that  there  would  not  be  enough  nozzle 
pressure  left  to  produce  a  stream  which  would  carry  a  sufficient  distance. 

With  the  aid  of  the  tables  the  discharge  for  any  of  the  nozzles 
may  be  readily  computed  for  any  pressure  in  the  mains.  If  the  nozzle 
is  at  a  higher  elevation  than  the  main,  subtract  from  the  pressure  in 
the  main  an  amount  equal  to  0.434  times  the  difference  in  elevation  in 
feet  between  the  nozzle  and  the  main.  Take  a  discharge  from  the 
table  for  any  pressure  at  the  base  of  the  nozzle  for  the  size  of  nozzle 
used,  then  take  the  corresponding  value  of  the  head  lost  in  the  kind  of 
hose  used,  multiply  this  value  by  the  length  of  hose  in  feet  used  and 
divide  by  100.  The  result  gives  the  total  loss  in  the  hose  for  the 
assumed  discharge.  If  there  is  any  connecting  pipe,  the  loss  in  it  will 
be  the  same  as  the  loss  in  a  corresponding  length ^of  rubber-lined  hose. 


58  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

Add  the  losses  in  the  pipe  and  hose  to  the  pressure  at  the  base  of  the 
nozzle  for  the  assumed  discharge  to  obtain  the  pressure  in  the  main 
(corrected  for  the  difference  in  elevation)  necessary  to  produce  this 
discharge.  The  discharge  will  vary  as  the  square  root  of  this  pres- 
sure. Letting  qf  =  the  assumed  discharge,  P'  =  the  pressure  in  the  main 
(corrected  for  the  difference  in  elevation)  which  will  produce  this  dis- 
charge, 5  =  the  discharge  to  be  determined,  P  =  the  actual  pressure  in 
the  mains  and  H  =  difference  in  elevation  between  the  nozzle  and  the 
main  in  feet  gives  the  relation 

P^QAZIH 

P' 
which  gives  the  required  discharge. 

To  illustrate  the  use  of  the  formula  the  following  assumptions  are 
made.  Pressure  in  mains,  P  =  60  Ib.  per  sq.  in.,  80  ft.  of  linen  hose, 
50  ft.  of  IK-in.  connecting  pipe,  elevation  of  nozzle  above  main  30  ft. 
and  M-in.  nozzle  used. 

Assume  a  discharge  of  46  gal.  per  min.  and  from  the  table  the 
following  values  are  obtained: 

Nozzle  pressure  =  40 

.    ,  80X18.8 

Loss  in  hose  =  — r^r —  =  15.0 

50X10.2 
Loss  in  pipe  =  — r^—  =  5.1 


Total     =  P'  =  60l 

Substituting  in  the  formula 

5  =  40.7  gal.  per  min. 

The  following  method  may  be  used  to  determine  the  discharge 
for  any  size  of  nozzle  for  any  pressure  in  the  mains.  Assume  any 
pressure  at  the  base  of  the  nozzle,  hf,  in  feet  of  water.  The  discharge 
for  this  pressure  may  be  determined  by  the  formula 


q'  =  discharge  in  cu.  ft.  per  sec. 

c  —  coefficient  of  discharge  and  may  be  taken  as  0.98 
A  =  area  ofjDpening  of  nozzle  in  sq.  ft. 
20  =  64.4  ft.  per  sec.  per  sec. 

Determine  the  velocity  in  the_hose  for  this  discharge  from  the 
formula 


HYDRAULIC    EXPERIMENTS  59 


- 


v  —  velocity  in  hose  in  ft.  per  sec. 
a  =  area  of  hose  in  sq.  ft. 
Determine  the  loss  in  the  hose  from  the  formula 


/z2  =  head  lost,  in  feet 
f=  friction  factor  which  may  be  taken  as  0.03  for  rubber  lined 

hose  or  0  .  06  for  unlined  linen  hose 
I  =  length  of  hose  in  feet 
d  =  diameter  of  hose  in  feet 
v  =  velocity  in  hose  in  ft.  per  sec. 
20  =  64.4  ft.  per  sec.  per  sec. 

If  there  is  any  pipe  connecting  the  hose  to  the  main,  the  loss  for 
it  may  be  computed  by  the  same  formula  as  for  the  hose,  using  0.03 
for  the  friction  factor  for  IM-in.  pipe.  Call  this  lost  head  hz. 

The  pressure  in  the  main  to  give  the  assumed  nozzle  pressure  is 


This  pressure  will  be  in  feet  of  water.     Then  using  the  relation 


-'VI 


gives  the  required  discharge.     If  the  main  is  below  the  nozzle,  subtract 
the  difference  in  elevation  in  feet  from  H  in  the  formula. 

It  is  recognized  that  this  method  is  not  strictly  accurate  since  the 
head  does  not  vary  exactly  as  the  square  of  the  discharge,  but  the 
results  obtained  will  be  close  enough  for  practical  use. 


- 


29.     Summary. — The  following  brief  summary  is  given  as  applying 
small  hose  and  nozzles  with  velocities  in  the  hose  ranging  from  about 
4  to  8  ft.  per  sec.  and  with  pressures  at  the  base  of  the  nozzle  ranging 
from  about  10  to  85  Ib.  per  sq.  in. 

(1)     The  friction  factor  (/  in  the  equation  for  the  lost  head, 

7      9    \ 

h  =f  -j^r- I  for  rubber-lined  hose  varies  but  little  with  the  velocity 
d  Zcj  / 

in  the  hose  and  is  nearly  the  same  as  for  clean  iron  pipe  of  the  same 
diameter. 


60  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

(2)  The  friction  factor  for  unlined  linen  hose  decreases  as 
the  velocity  increases.     In  general  the  loss  of  head  in  unlined  linen 
hose  is  about  twice  as  great  as  in  rubber-lined  hose  of  the  same 
diameter  and  for  the  same  velocity. 

(3)  The  nozzle  should  have  a  smooth  cylindrical  tip  at  least 
one-half  inch  long  to  keep  the  jet  from  spraying.     A  cylindrical 
tip  is  a  much  more  important  factor  in  securing  a  good  fire  stream 
than  a  smooth  surface  in  the  interior  of  the  nozzle. 

(4)  Nozzle  openings  commonly  in  use  to  supply  fire  streams 
in  the  interior  of  buildings  seem  too  small  for  adequate  temporary 
fire  protection.     It  is  recommended  that  a  nozzle  with  a  M-in. 
opening  be  used  with  a  IK-in.  hose  in  order  to  secure  a  sufficient 
quantity  of  water  for  an  effective  fire  stream. 

(5)  The  coefficient  of  discharge  of  a  small  conical  nozzle 
varies  but  little  with  the  velocity  and  is  close  to  0.98.     The  value 
of  0.95  obtained  with  the  %6-in.  nozzle,  which  was  12  in.  long  as 
compared  with  6  in.  for  the  other  nozzles  tested,  indicates,  how- 
ever, that  the  nozzle  should  be  short  to  obtain  the  value  of  0.98. 
A  cylindrical  tip  on  the  nozzle  seems  to  have  little  influence  on 
the  coefficient  of  discharge. 


PART  IV 
THE  ORIFICE  BUCKET  FOR  MEASURING  WATER 

BY  MELVIN  L.  ENGER 

ASSOCIATE  PROFESSOR  OF  MECHANICS  AND  HYDRAULICS 


CONTENTS 

PART  IV 
THE  ORIFICE  BUCKET  FOR  MEASURING  WATER 

PAGE 

X.  INTRODUCTION 65 

30.  Purpose 65 

31.  Acknowledgment 66 

XI.  APPARATUS  AND  METHOD  OF  CALIBRATING 67 

32.  Orifice  Bucket    .      . 67 

33.  Method  of  Calibrating  Orifice  Bucket 71 

XII.  EXPERIMENTAL  DATA  AND  DISCUSSION 72 

34.  Fifteen-inch  Orifice  Bucket  having  Fifty-six  Orifices    .  72 

35.  Fifteen-inch  Orifice  Bucket  having  Only  Three  Orifices  73 

36.  Twenty-inch  Orifice  Bucket  having  Nineteen  Orifices  .  73 

37.  Conclusions  .  76 


LIST  OF   FIGURES 

NO.  PAGE 

23.  Fifteen-inch  Orifice  Bucket  having  Fifty-six  Orifices 67 

24.  View  Showing  Orifice  Bucket  in  Use 69 

25.  Twenty-inch  Orifice  Bucket  having  Nineteen  Orifices 68 

26.  Calibration  Curves  for  15-inch  Orifice  Bucket  having  Fifty-six  Orifices  .  72 

27.  Calibration  Curves  for  15-inch  Orifice  Bucket  having  Only  Three  Orifices  74 

28.  Calibration  Curves  for  20-inch  Orifice  Bucket  having  Nineteen  Orifices  .  75 


64 


HYDRAULIC    EXPERIMENTS  65 

PART  IV 
THE  ORIFICE  BUCKET  FOR  MEASURING  WATER 


X.    INTRODUCTION 

30.  Purpose. — The  purpose  of  Part  IV  is  to  describe  a  method 
of  measuring  water  by  means  of  a  simple,  portable,  and  inexpensive 
device,  here  called  an  orifice  bucket,  and  to  present  experimental  data 
applying  thereto  for  a  range  of  conditions  sufficient  to  indicate  that 
the  device  is  reliable  for  use  in  engineering  practice.  An  orifice  bucket 
is  a  cylindrical  vessel  into  which  water  to  be  measured  falls  vertically 
and  passes  out  through  a  number  of  holes  or  orifices  in  the  bottom. 
A  vertical  glass  tube  placed  just  outside  the  bucket  is  connected  to  the 
sides  of  the  bucket  near  the  bottom,  and  the  height  of  the  water  in 
the  tube  indicates  the  head  on  the  orifice. 

The  orifice  bucket  was  devised  for  the  purpose  of  measuring  the 
discharge  of  several  artesian  wells  pumped  by  means  of  air  lift,  the 
water  from  each  of  which  discharged  into  a  separate  cistern  or  small 
reservoir  through  a  vertical  pipe.  In  each  case  the  water  left  the  pipe 
with  considerable  blast  and  momentum.  Several  possible  methods 
for  the  measurement  of  the  discharge  were  considered  but  were  thought 
to  be  impracticable  for  various  reasons  or  inapplicable  for  the  particular 
case.  After  some  preliminary  laboratory  experimenting  an  orifice 
bucket  was  devised  which  served  very  satisfactorily  in  determining  the 
discharge  from  each  of  the  wells.  It  was  at  first  feared  that  the  water 
would  enter  the  bucket  with  such  a  blast  that  entrained  air  would  enter 
the  vertical  glass  tube  and  cause  trouble  in  determining  the  height  of 
water  in  the  bucket.  There  was,  however,  no  trouble  from  this  cause 
and  the  fluctuations  of  the  water  level  in  the  glass  tube  offered  no  seri- 
ous difficulties. 

The  orifice  bucket  has  also  given  satisfaction  in  tests  made  to  deter- 
mine yields  of  well  pumps  of  the  reciprocating  type.  It  should  give 
satisfactory  results  in  the  field  where  simplicity  of  construction  and 
portability  are  desirable  and  where  extreme  accuracy  is  not  of  great 
importance. 


66  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 

31.  Acknowledgment. — The  orifice  bucket  was  developed  by  the 
writer  through  experimental  work  in  the  Hydraulic  Laboratory  of 
the  University  of  Illinois  during  1910  and  1911.*  Considerable  im- 
provement has  been  made  in  the  arrangement  of  certain  parts  of  the 
bucket  by  I.  W.  FISK,  P.  S.  BIEGLER,  and  P.  J.  NILSEN,  of  the  de- 
partment of  electrical  engineering,  in  connection  with  tests  on  electric 
motor-driven  deep-well  pumps.  Some  of  the  experimental  data  herein 
presented  were  obtained  by  them,  to  whom  acknowledgment  is  made. 


*  A  part  of  the  results  here  presented  was  published  in  the  Proceedings  of  the  Third  Meeting  of 
the  Illinois  Water  Supply  Association,  p.  87,  1911. 


HYDRAULIC    EXPERIMENTS 


67 


XL    APPARATUS  AND  METHOD  OP  CALIBRATING 

32.  Orifice  Bucket. — Fig.  23  shows  the  construction  and  dimen- 
sions of  one  of  the  first  orifice  buckets  used  in  the  experiments,  and 
Fig.  24  shows  the  bucket  in  use.  This  bucket  weighed  23  Ib. 

As  previously  stated  an  orifice  bucket  is  a  cylindrical  vessel  having 
holes  or  orifices  in  its  bottom  and  into  which  water  to  be  measured 


nd 
fo 


I 

I 


FIG.  23.     FIFTEEN-INCH  ORIFICE  BUCKET  HAVING  FIFTY-SIX  ORIFICES 


68 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


falls  vertically,  the  head  of  water  on  the  orifices  being  indicated  by 
the  height  of  the  water  in  a  vertical  glass  piezometer  tube  attached 
near  the  bottom  of  the  bucket. 

Fig.  25  shows  the  construction  of  the  most  elaborate  orifice  bucket 
which  has  been  used.  It  is  provided  with  a  short  tube  checker-work 
to  smooth  out  the  flow  of  the  water  on  its  way  to  the  orifices  in  the 


$'6age  g/ass  on 
sca/e  graduated 
'*  £*s  feef 


ga/v.  /'ron  s/r/ps  4 


crisscrossed 
to  form  tubes 
G0/K  w/naow  screen 
so/denzd  to  fop- 


ftezomefer  press,  chamber. 


Bottom  of,%"6oi/erp/afe 
r/ise/ed  and  so/derec/ 


fio/es. 


FIG.  25.    TWENTY-INCH  ORIFICE  BUCKET  HAVING  NINETEEN  ORIFICES 


FIG.  24.    VIEW  SHOWING  ORIFICE  BUCKET  IN  USE 


HYDRAULIC    EXPERIMENTS  71 

bottom  of  the  bucket.  The  vertical  glass  tube  is  connected  to  a 
piezometer  chamber  or  ring  around  the  base  of  the  bucket,  pressure 
being  transmitted  to  the  piezometer  ring  through  a  large  number  of 
small  holes. 

The  orifice  bucket  may  be  adapted  for  the  measurement  of  water 
for  a  considerable  range  in  the  discharge  by  varying  the  head  on  the 
orifices  and  also  by  varying  the  number  of  holes  which  are  stopped  or 
plugged  with  corks  or  wooden  stoppers.  The  range  in  the  capacities 
of  the  orifice  buckets  which  have  been  used  is  from  about  40  to  1000 
gal.  per  min. 

33.  Method  of  Calibrating  Orifice  Bucket. — In  calibrating  the  ori- 
fice bucket  it  was  hung  underneath  a  vertical  pipe  as  shown  in  Fig.  24. 
The  quantity  of  water  discharged  was  measured  with  a  6-in.  Venturi 
meter  in  most  of  the  calibration  tests  although  a  calibrated  measuring 
pit  was  used  in  some  of  the  tests  to  determine  the  volume  discharged 
in  a  given  time. 

With  a  given  number  of  holes  open,  the  flow  in  the  orifice  bucket 
was  regulated  by  means  of  a  valve  between  the  Venturi  meter  and  the 
bucket  until  the  height  in  the  bucket  remained  constant.  The  Venturi 
meter  reading  and  the  head  on  the  orifices  were  then  taken.  This 
procedure  was  repeated  for  several  different  heads  and  for  different 
numbers  of  orifices  open. 

The  effect  of  varying  the  conditions  of  flow  was  investigated  some- 
what. The  height  of  the  free  fall  of  the  water  from  the  inflow  pipe  to 
the  orifice  bucket  was  varied;  likewise  different  sizes  of  pipe  were  used 
giving  different  velocities  to  the  stream  entering  the  bucket.  The 
stream  was  also  allowed  to  enter  near  to  one  side  of  the  bucket  instead 
of  at  the  center.  Different  groupings  of  the  open  orifices,  furthermore, 
were  tried,  and  different  methods  were  employed  in  attempting  to 
spread  or  distribute  the  inflowing  stream. 

In  using  the  orifice  bucket  it  is  necessary  to  estimate  the  average 
head  shown  in  the  glass  tube  because  there  is  some  fluctuation.  The 
amount  of  the  fluctuation  may  be  reduced  by  throttling  the  valve  in 
the  connection  of  the  glass  tube  to  the  orifice  bucket.  If  the  proper 
conditions  are  observed,  there  should  be  little  trouble  from  this  source. 
It  should  be  remembered  that  the  rate  of  discharge  is  proportional  to 
the  square  root  of  the  head  and  that  the  effect  of  the  error  which  might 
occur  in  the  head  reading  itself  is  thus  reduced  in  determining  the 
discharge. 


72 


ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


XII.     EXPERIMENTAL  DATA  AND  DISCUSSION 

34.  Fifteen-inch  Orifice  Bucket  Having  Fifty-six  Orifices. — Fig.  26 
shows  the  calibration  curves  for  the  15-inch  orifice  bucket  shown  in 
Fig.  23  and  24.  There  were  fifty-six  1-in.  holes  in  the  bottom  of  the 
bucket  giving  a  maximum  capacity  of  about  1000  gal.  per  min.  With 
all  the  orifices  open  the  rate  of  discharge  was  varied  from  about  600 
to  1000  gal.  per  min.  by  varying  the  head  from  about  %  ft.  to  2  ft. 
With  thirty-two  orifices  open  the  discharge  had  a  range  of  about  300 
to  600  gal.  per  min.  by  varying  the  head  from  about  Y*  ft.  to  2.5  ft. 
In  closing  the  twenty-four  orifices,  corks  were  used  of  such  size  that 
they  projected  but  little  into  the  bucket.  It  was  found  that  in  filling 
the  orifices  a  symmetrical  arrangement  gave  somewhat  steadier  action, 
particularly  when  the  orifices  near  the  circumference  were  the  ones 
filled.  The  inflowing  stream  was  discharged  from  an  8-in.  pipe.  A 


1000 


0.5 


/-O  /.f  2.O 

/iead  in  feet 


3.0 


FIG.  26.     CALIBRATION  CURVES  FOR  15-iNCH  ORIFICE  BUCKET  HAVING 
FIFTY-SIX  ORIFICES 


HYDRAULIC    EXPERIMENTS  73 

3-in.  pipe  was  also  tried  but  did  not  give  satisfactory  results,  on  account 
of  the  high  velocity  which  produced  an  extremely  agitated  condition 
of  the  water  in  the  bucket.  This  condition  may  be  overcome,  however, 
by  use  of  a  deflector  or  distributor,  such  as  an  open  bag  or  sack  attached 
to  the  end  of  the  discharge  pipe. 

The  rate  of  discharge  for  any  other  number  of  open  orifices  for  this 
bucket  may  be  obtained  from  the  equation 


which  represents  fairly  well  the  relation  between  the  quantity,  q,  in 
gal.  per  min.,  the  number  of  orifices  open,  n,  and  the  head  in  the 
bucket,  h,  in  ft.  The  experiments  give  an  average  coefficient  of  dis- 
charge for  the  1-in.  orifices  of  this  bucket  of  about  0.63. 

35.  Fifteen-inch   Orifice   Bucket   Having   Only    Three    Orifices.  — 
Fig.  27  shows  an  orifice  bucket  of  the  same  dimensions  as  the'  one  just 
described  but  with  three  iron  tubes  about  1  in.  long  inserted  in  a  1-in. 
wooden  bottom.     It  was  provided  with  two  screens  through  which  the 
water  passed  on  its  way  to  the  orifices  hi  the  bottom  of  the  bucket. 

Fig.  27  also  shows  the  calibration  curves  for  this  orifice  bucket. 
It  will  be  noted  that  the  discharge  ranges  from  about  35  to  115  gal. 
per  min.  This  orifice  was  constructed  and  calibrated  for  immediate 
use  and  not  for  experimental  purposes.  The  calibration  curves  are  of 
value  in  indicating  the  reliability  of  the  orifice  bucket  under  a  rather 
wide  range  in  the  details  of  its  construction. 

36.  Twenty-inch    Orifice   Bucket   Having   Nineteen   Orifices.  —  An 
illustration  of  the  most  elaborate  orifice  bucket  used  in  the  experi- 
ments is  shown  in  Fig.  25,  the  capacity  of  which  is  about  1000  gal. 
per  min.     It  contains  a  checkerwork  of  vertical  tubes  through  which 
the  water  flows  in  passing  to   the  orifices.     The  gage  glass  which 
indicates  the  head  on  the  orifices  is  connected  to  a  piezometer  ring  or 
chamber  around  the  base  of  the  bucket.     The  pressure  of  the  water  in 
the  bucket  is  transmitted  to  the  piezometer  chamber  through  a  large 
number  of  M-in.  holes.     The  bottom  of  the  bucket  consists  of  jKe-in. 
boiler  plate  in  which  nineteen  1%-in.  circular  holes  are  drilled. 

The  calibration  curves  for  this  orifice  bucket  are  shown  in  Fig.  28, 
for  all  holes  open  and  for  ten  holes  open.  The  discharge  for  any  other 
number  of  orifices  open  may  be  found  with  a  fair  degree  of  accuracy 
from  the  equation 


IZU 

no 
too 

\  90 

I 

i" 

r 

x 

r 

60 
SO 
40 
3O 

/ 

> 

/ 

i 

<gcree/7 

i 

/ 

/ 

• 

/ 

s 

. 

</ 

/ 

/ 

(2? 

w 

?' 

|f- 

n 

A) 

. 

1 

1 

fl 

i 

&^ 

IJ 

r 

c^ 

f 

^ 

^ 

ft 

/ 

/ 

^ 

*\ 

/ 

^ 

1- 

/ 

/ 

x 

/^x 

X 

<* 

/ 

s 

(* 

r 

$ 

F 

x 

^^ 

/ 

Ix*3 

o 

1C 

"6 

aa 

^ 

S 

c 

IP^ 

4$ 

<* 

* 

,  ^t 

^ 

/ 

• 

= 

/ 

/ 

tfe&d  /n  feet 

FIG.  27.     CALIBRATION  CURVES  FOR  15-iNCH  ORIFICE  BUCKET  HAVING 
ONLY  THREE  ORIFICES 


HYDRAULIC    EXPERIMENTS 


75 


if 


Ho/es  Plugged  thus: 


.6     .8     /.O 


.         .        . 
Head  in  feef 


ZO    2 


FIG.  28.     CALIBRATION  CURVES  FOR  20-iNCH  ORIFICE  BUCKET  HAVING 
NINETEEN  ORIFICES 


76  ILLINOIS    ENGINEERING    EXPERIMENT    STATION 


in  which  q  is  expressed  in  gal.  per  min.,  n  is  the  number  of  holes  open, 
and  h  is  the  head  on  the  orifices  in  feet.  The  average  coefficient  of 
discharge  for  the  1%-in.  orifices  of  this  bucket  is  0.61. 

The  curves  in  Fig.  28  were  obtained  when  the  bucket  was  supported 
firmly  in  an  upright  position  with  the  stream  to  be  measured  discharging 
vertically  in  the  center  of  the  bucket  and  with  the  free  fall  into  the 
bucket  small.  The  velocity  of  the  inflowing  stream,  furthermore,  was 
not  high  (2  or  3  ft.  per  sec.),  thereby  causing"  but  little  agitation  of 
the  water  in  the  bucket.  Experiments,  however,  in  which  more  or  less 
variation  from  these  conditions  were  allowed  indicated  that  no  serious 
errors  resulted. 

37.  Conclusions.  —  The  conditions  under  which  the  discharge  of 
water  has  to  be  measured  are  so  varied  and  the  purpose  or  aim  in  deter- 
mining the  discharge  differs  so  much  in  different  problems  that  nearly 
any  one  of  the  many  common  methods  of  measuring  water  has  a  rather 
restricted  field  of  usefulness,  while  some  methods  apply  only  to  very 
special  conditions. 

The  orifice  bucket  is  designed  to  meet  rather  special  conditions. 
It  is  peculiarly  adapted  for  the  measurement  of  water  where  a  device 
which  is  portable  (light  weight  and  small  size),  simple  in  construction, 
and  low  in  cost  are  essential  features.  The  measuring  capacity,  more- 
over, covers  a  considerable  range.  The  orifice  bucket  is  particularly 
fitted  for  the  measurement  of  water  when  the  water  discharges  with 
considerable  blast  and  momentum  from  the  end  of  a  vertical  pipe,  in 
such  a  manner  that  the  spray  covers  the  entire  surface  of  the  water  in 
the  bucket,  as  in  the  case  of  air  lift  pumping.  When  so  used  the  orifice 
bucket  gives  results  which  should  be  correct  within  5  per  cent  if  the 
proper  precautions  are  observed  in  its  use,  as  is  shown  by  the  calibration 
curves,  and  correct  within  10  per  cent  for  the  more  unfavorable  condi- 
tions to  be  met  in  the  field.  The  highest  accuracy  is  obtained  when 
the  orifice  bucket  is  supported  rigidly  in  an  upright  position  with  the 
center  of  the  discharging  stream  vertically  over  the  center  of  the  bucket. 
The  free  fall  of  the  water  should  be  as  small  as  possible  and  the  velocity 
of  the  water  as  it  enters  the  bucket  should  not  be  large,  unless  the  stream 
is  distributed,  so  as  to  avoid  high  local  velocities  in  the  bucket.  The 
orifice  bucket,  however,  gives  very  satisfactory  results  even  when  there 
are  considerable  deviations  from  these  desirable  conditions  and  renders 
a  service  for  which  other  measuring  devices  may  not  be  adapted. 


LIST  OF 
PUBLICATIONS  OF  THE  ENGINEERING  EXPERIMENT  STATION 


Bulletin  No.  1.     Tests  of  Reinforced  Concrete  Beams,  by  Arthur  N.  Talbot,  1904.    None  available. 
Circular  No.  1.     High-Speed  Tool  Steels,  by  L.  P.  Breckenridge.     1905.     None  available. 

Bulletin  No.  2.  Tests  of  High-Speed  Tool  Steels  on  Cast  Iron,  by  L.  P.  Breckenridge  and  Henry 
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Circular  No.  2.     Drainage  of  Earth  Roads,  by  Ira  O.  Baker.     1906.     None  available. 

Circular  No.  3.  Fuel  Tests  with  Illinois  Coal  (Compiled  from  tests  made  by  the  Technological 
Branch  of  the  U.  S.  G.  S.,  at  the  St.  Louis,  Mo.,  Fuel  Testing  Plant,  1904-1907),  by  L.  P.  Breckenridge 
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1906.  Forty-five  cents. 

Bulletin  No.  5.    Resistance  of  Tubes  to  Collapse,  by  Albert  P.  Carman  and  M.  L.  Carr.     1906. 

None  available. 

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Bulletin  No.  7.  Fuel  Tests  with  Illinois  Coals,  by  L.  P.  Breckenridge,  S.  W.  Parr,  and  Henry  B. 
Dirks.  1906.  None  available.  • 

Bulletin  No.  8.  Tests  of  Concrete:  I,  Shear;  II,  Bond,  by  Arthur  N.  Talbot.  1906.  None 
available. 

Bulletin  No.  9.  An  Extension  of  the  Dewey  Decimal  System  of  Classification  Applied  to  the 
Engineering  Industries,  by  L.  P.  Breckenridge  and  G.  A.  Goodenough.  1906.  Revised  Edition 
1912.  Fifty  cents. 

Bulletin  No.  10.  Tests  of  Concrete  and  Reinforced  Concrete  Columns,  Series  of  1906,  by  Arthur 
N.  Talbot.  1907.  None  available. 

Bulletin  No.  11.  The  Effect  of  Scale  on  the  Transmission  of  Heat  through  Locomotive  Boiler 
Tubes,  by  Edward  C.  Schmidt  and  John  M.  Snodgrass.  1907.  None  available. 

Bulletin  No.  12.  Tests  of  Reinforced  Concrete  T-Beams,  Series  of  1906,  by  Arthur  N.  Talbot. 

1907.  None  available. 

Bulletin  No.  13.  An  Extension  of  the  Dewey  Decimal  System  of  Classification  Applied  to  Archi- 
tecture and  Building,  by  N.  Clifford  Ricker.  1907.  None  available. 

Bulletin  No.  14.  Tests  of  Reinforced  Concrete  Beams,  Series  of  1906,  by  Arthur  N.  Talbot. 

1907.  None  available. 

Bulletin  No.  15.  How  to  Burn  Illinois  Coal  Without  Smoke,  by  L.  P.  Breckenridge.  1908. 
None  available. 

Bulletin  No.  16.  A  Study  of  Roof  Trusses,  by  N.  Clifford  Ricker.     1908.     None  available. 

Bulletin  No.  17.  The  Weathering  of  Coal,  by  S.  W.  Parr,  N.  D.  Hamilton,  and  W.  F.  Wheeler. 

1908.  None  available. 

Bulletin  No.  18.  The  Strength  of  Chain  Links,  by  G.  A.  Goodenough  and  L.  E.  Moore.  1908. 
Forty  cents. 

Bulletin  No.  19.  Comparative  Tests  of  Carbon,  Metallized  Carbon  and  Tantalum  Filament 
Lamps,  by  T.  H.  Amrine.  1908.  None  available. 

Bulletin  No.  20.  Tests  of  Concrete  and  Reinforced  Concrete  Columns,  Series  of  1907,  by  Arthur 
N.  Talbot.  1908.  None  available. 

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cents. 

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Fifteen  cents. 

*Bulletin  No.  24-  The  Modification  of  Illinois  Coal  by  Low  Temperature  Distillation,  by  S.  W.  Parr, 
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Bulletin  No.  26.  Lighting  Country  Homes  by  Private  Electric  Plants,  by  T.  H.  Amrine.  1908. 
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78  PUBLICATIONS    OF    THE    ENGINEERING    EXPERIMENT   STATION 

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Bulletin  No.  27.  Tests  of  Brick  Columns  and  Terra  Cotta  Block  Columns,  by  Arthur  N.  Talbot 
and  Duff  A.  Abrams.     1909.      Twenty-five  cents. 

Bulletin  No.  28.  A  Test  of  Three  Large  Reinforced  Concrete  Beams,   by  Arthur  N.   Talbot 
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*Bulletin  No.  31.  Tests    with    House-Heating    Boilers,    by    J.    M.    Snodgrass.     1909.     Fifty-five 
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*Bulletin  No.  59.  Tests  of  Washed  Grades  of  Illinois  Coal,  by  C.  S.  McGovney.     1909.     Seventy- 
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1916.  Thirty-five  cents. 

^Bulletin  No.  86.  The  Strength  of  I-Beams  and  Girders,  by  Herbert  F.  Moore  and  W.  M.  Wilson 
1916.  Thirty  cents. 

*Bulletin  No.  87.  Correction  of  Echoes  in  the  Auditorium,  University  of  Illinois,  by  F.  R.  Watson 
and  J.  M.  White.  1916.  Fifteen  cents. 

Bulletin  No.  88.  Dry  Preparation  of  Bituminous  Coal  at  Illinois  Mines,  by  E.  A.  Holbrook.     1916- 
Seventy  cents. 

*A  limited  number  of  copies  of  bulletins  starred  is  available  for  free  distribution. 


80  PUBLICATIONS    OF   THE    ENGINEERING    EXPERIMENT   STATION 

*Bulletin  No.  89.  Specific  Gravity  Studies  of  Illinois  Coal,  by  Merle  L.  Nebel.  1916.  Thirty 
cents. 

*Bulletin  No.  90.  Some  Graphical  Solutions  of  Electric  Railway  Problems,  by  A.  M.  Buck.  1916. 
Twenty  cents. 

*Bulletin  No.  91.  Subsidence  Resulting  from  Mining,  by  L.  E.  Young  and  H.  H.  Stock.  1916. 
None  available. 

*Bulletin  No.  92.  The  Tractive  Resistance  on  Curves  of  a  28-Ton  Electric  Car,  by  E.  C.  Schmidt 
and  H.  H.  Dunn.  1916.  Twenty-five  cents. 

^Bulletin  No.  93.  A  Preliminary  Study  of  the  Alloys   of   Chromium,    Copper,  and  Nickel,  by 

D.  F.  McFarland  and  O.  E.  Harder.     1916.     Thirty  cents. 

*Bulletin  No.  94.  The  Embrittling  Action  of  Sodium  Hydroxide  on  Soft  Steel,  by  S.  W.  Parr. 
1917.  Thirty  cents. 

^Bulletin  No.  95.  Magnetic  and  Other  Properties  of  Iron-Aluminum  Alloys  Melted  in  Vacuo,  by 
T.  D.  Yensen  and  W.  A.  Gatward.  1917.  Twenty-five  cents. 

*Bulletin  No.  96.  The  Effect  of  Mouthpieces  on  the  Flow  of  Water  Through  a  Submerged  Short 
Pipe,  by  Fred  B.  Seely.  1917.  Twenty-five  cents. 

*  Bulletin  No.  97.  Effects  of  Storage  Upon  the  Properties  of  Coal,  by  S.  W.  Parr.  1917 
Twenty  cents. 

^Bulletin  No.  98.  Tests  of  Oxyacetylene  Welded  Joints  in  Steel  Plates,  by  Herbert  F.  Moore. 
1917.  Ten  cents. 

Circular  No.  4.  The  Economical  Purchase  and  Use  of  Coal  for  Heating  Homes,  with  Special 
Reference  to  Conditions  in  Illinois.  1917.  Ten  cents. 

*Bulletin  No.  99.    The  Collapse  of  Short  Thin  Tubes,  by  A.  P.  Carman.   1917.    Twenty  cents. 

*Circular  No.  5.  The  Utilization  of  Pyrite  Occurring  in  Illinois  Bituminous  Coal,  by  E.  A. 
Holbrook.  1917. 

*Bulletin  No.  100.  Percentage  of  Extraction  of  Bituminous  Coal  with  Special  Reference  to 
Illinois  Conditions,  by  C.  M.  Young.  1917. 

^Bulletin  No.  101.    Comparative  Tests  of  Six  Sizes  of  Illinois  Coal  on  a  Mikado  Locomotive,  by 

E.  C.  Schmidt,  J.  M.  Snodgrass,  and  O.  S.  Beyer,  Jr.     1917.     Fifty  cents. 

*Bulletin  No.  102.  A  Study  of  the  Heat  Transmission  of  Building  Materials,  by  A.  C.  Willard 
and  L.  C.  Lichty.  1917. 

^Bulletin  No.  103.  An  Investigation  of  Twist  Drills,  by  B.  Benedict  and  W.  P.  Lukens.  1917. 
Sixty  cents. 

*Bulletin  No.  104.  Tests  to  Determine  the  Rigidity  of  Riveted  Joints  of  Steel  Structures,  by 
W.  M.  Wilson  and  H.  F.  Moore.  1917.  Twenty-five  cents. 

Circular  No.  6.      The  Storage  of  Bituminous  Coal,  by  H.  H.  Stock.     1918.     Forty  cents. 

Circular  No.  7.  Fuel  Economy  in  the  Operation  of  Hand  Fired  Power  Plants.  1918.  Twenty- 
five  cents. 

*BulletinNo.  1 05.  Hydraulic  Experiments  with  Valves,  Orifices,  Hoze,  Nozzles,  and  Orifice 
Buckets,  by  Arthur  N.  Talbot,  Fred  B  Seely,  Virgil  R  Fleming  and  Melvin  L.  Enger.  1918. 
Thirty-five  cents. 


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THIS  BOOK  IS  DUE  ON  THE  LAST  DATE 
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1 

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