PUBLICATION NO. 738 ISSUED SEPTEMBER, 1942 TECHNICAL BULLETIN 44 FIRST PRINTING AN ECOLOGICAL and GRAZING CAPACITY STUDY OF THE NATIVE GRASS PASTURES IN SOUTHERN ALBERTA, SASKATCHEWAN AND MANITOBA by S. E. Clarke, Agricultural Scientist, in charge of Forage Crops and Pasture Studies. J. A. Campbell, Agricultural Supervisor. J. B. Campbell, Agricultural Supervisor. DIVISION OF FORAGE CROPS Dominion Experimental Station, Swift Current, Sask. edby authority of the Hon. JAMES G. GARDINER, Minister of Agriculture, Ottawa, Canada !♦! A9ricu,tur9 Canadian Agriculture Library Canada Bibliotheque canadienne de I'agriculture Ottawa K1 A 0C5 TABLE OF CONTENTS Page Introduction 3 Physical Factors Influencing Botanical Composition and Yield of the Vege- tational Cover 6 Topography 6 Climate 7 Soil 8 Vegetation 9 Short-grass Prairie (Bouteloua-Stipa Association) 11 Mixed Prairie (Agropyron-Stipa-Bouteloua Association) 12 Submontane Mixed Prairie (Festuca-Danthonia Association) 15 Methods Employed in a Study of the Vegetation and in the Determination of Carrying Capacity 16 Pasture Survey Procedure 17 Methods of Sampling 18 Sampling Technique 19 Determination of Carrying Capacity 19 Results of Investigations 23 Short-grass Prairie 23 Mixed Prairie 25 Submontane Mixed Prairie 26 Comparative Yields and Carrying Capacity 28 Yields of Forage Expressed in Terms of Animal Products 29 Summary and Conclusions 30 Literature Cited 31 AN ECOLOGICAL AND GRAZING CAPACITY STUDY OF THE NATIVE GRASS PASTURE IN SOUTHERN ALBERTA, SASKATCHEWAN AND MANITOBA INTRODUCTION In 1937 a survey of the grasslands in Alberta, Saskatchewan and Manitoba was inaugurated as one of the activities of the Prairie Farm Rehabilitation program. The chief purposes of the survey are, to classify the native grasslands according to the botanical composition of the vegetation, to ascertain the carrying capacity of the various grazing districts, and to determine how the native grass pastures should be utilized in order to secure the maximum production of animal products and yet maintain the forage cover. Since the inception of the survey slightly over three million acres have been studied. The area being surveyed is in the southern portion of the three provinces. The Rocky Mountains, the International Boundary between Canada and the United States, and the Red River are respectively the western, southern and eastern borders of the domain; while a line running northwest from Winnipeg, Manitoba, to Lloydminster, Saskatchewan, and from there southwest to the Rocky Mountains in the vicinity of Banff, Alberta, is the northern boundary (plate 1). The region included within these boundaries contains practically all of the prairies and certain adjacent portions of the "Park Belt". It is esti- mated that within this tract of country there are nearly thirty million acres of native grassland used for pasture. The larger blocks of grassland are located close to the western and southern borders of the area, while smaller parcels are scattered over the entire region. The grazing industry in Western Canada had its inception about 1875. From then until about 1900 it developed rapidly. Range was free and grass was abundant. Occasionally the winters were long and cold, but during many years the warm chinook winds kept the pastures partially cleared of snow and the temperatures moderate, thus allowing winter grazing during most seasons. These favourable factors, combined with the apparent possibilities for unlimited expansion induced the movement of capital into the region, first into the Foothill areas and later to the prairies. By 1901 the cattle population of Alberta and Saskatchewan had increased to 590,000 head, while sheep numbered about 153,000. The period of rapid expansion ended with the advent of dryland farmers about 1900. With the inevitable progress of land settlement the trend in ranching was changed from one of open range methods to one of ranch con- solidation. Properties were purchased or leased, fences were constructed, and arable lands cultivated to provide winter feed. From 1900 to 1912 there was a strong local market for horses and cattle created by the demands of the farmer settlers. From 1914 to 1918 the demand induced by the World War main- tained ranch revenues. 3 5*438— 1| Conditions changed about 1920, the high prices for live stock disappeared and grazing resources started to show signs of depletion. An over-grazed condition was developing or had developed on many ranges, and live stock populations were greater than the average grazing capacity of the pastures. Sufficient supplies of winter feed were not being maintained to offset the ranch consolidation and more stock-watering sites were needed on many ranches to obtain more efficient land use. Prolonged summer droughts and severe winters added to the burdens of decreased productivity and dwindling revenue, forcing many ranchers to reduce their herds and flocks and others to liquidate their investments. General concern among stockmen concerning the future of the ranching industry prompted them to request the Dominion Government in 1925, to investigate conditions throughout the range areas In answer to their request an investigation was conducted in 1926, and in the following year the Dominion Range Experiment Station was established near Manyberries, Alberta. At the Manyberries Station, which is located in the heart of the ranching country, extensive studies were inaugurated concerning range management problems. These studies included, the relative merits of different grazing practices, the carrying capacity of range pastures, the distribution of watering places and salt licks, and the development of small irrigation projects for the purpose of producing winter feed. Detailed studies were made of the vege- tational cover of the pastures, including their botanical composition, distribution of plant associations, percentage grass cover, yields of forage species and associations, and the changes brought about by climatic conditions and different grazing practices. A more favourable period was experienced during the years 1927 to 1929. This was followed, however, by a period of dry years extending to and including 1937, which was the driest season on record. The drought resulted in further depletion of pastures and reduction of live stock. These adverse conditions affected stockmen and grain farmers alike, and in an effort to alleviate the situation the Dominion Government enacted legislation in 1935 known as the Prairie Farm Rehabilitation Act. The Act made provision for a cultural program which includes such projects as soil-drift control and related drought problems, the reclamation of eroded lands, and soil, economic and botanical surveys; a land utilization department whose main activities are the estab- lishment of community pastures and the resettlement of farmers on better- quality and irrigated lands; and a water development branch which administers the construction of irrigation projects, stock-watering dams and dugouts. The pasture survey was one of the activities provided for under the cultural section of the Act. This study has been conducted on privately-owned ranches, community pastures and special areas throughout the three provinces. Reports on the areas surveyed have been prepared and presented to owners, managers and other interested parties. These reports embody information relating to the vegetational cover, its botanical composition, density and nutritive value; the carrying capacity of the areas studied; and definite recommendations per- taining to the management of the pastures. This bulletin outlines the nature of the pasture survey studies, and the relationship between these studies and certain physical and biotic factors, such as soil, climate and grazing practices which influence the productivity of the native grasslands. *i* /m ** */:*■ .A I . / _ / PHYSICAL FACTORS INFLUENCING BOTANICAL COMPOSITION AND YIELD OF THE VEGETATIONAL COVER Topography, climate and soil are the principal physical factors affecting the productivity of lands throughout the prairie region of Western Canada. These factors ultimately determine which portions shall be brought under cultivation and used for the production of cereal crops, and which shall be left as native sod and used for grazing purposes. They also determine what crops should be produced and the yields that may be expected. A good understanding of these important factors, and of their effects upon agricultural practices and production is essential in determining how the prairie region can be utilized to the greatest advantage. Topography The topography of the area under consideration is represented as a plain, the highest portion of which is the district adjacent to the Rocky Mountains. From there the plain extends eastward in a series of steppes until the lowest level is reached along the valley of the Red River in Manitoba. Some idea of the differences in elevation may be gained by reference to plate 1. Pincher Creek, Calgary and Lethbridge, all close to the western boundary, have altitudes of 3,773, 3,438, and 2,983 feet respectively. Redcliffe, a town near Medicine Hat but not situated in the river valley has an elevation of 2,439 feet above sea level. Continuing eastward through the provinces of Saskatchewan and Manitoba the following altitudes are recorded: Swift Current — 2,432, Regina — 1,896, Brandon — 1,204, and Winnipeg— 766. The continuity of this great plain is broken by several ranges of hills, including the Cypress Hills, Handhills, Neutral Hills, Touchwood Hills and Wood Mountains. These hills rise from 250 to 2,000 feet above the surrounding prairie. Certain other portions are classified as hilly or rolling prairie. Broad river valleys, from 100 to 500 feet deep are also typical topographical features. These include the North and South Saskatchewan, Bow, Red Deer, Assiniboine, Red, Frenchman and Milk Rivers. The Saskatchewan River, the Red River and their tributaries drain into Lake Winnipeg and Hudson Bay, while the Milk and Frenchman Rivers empty into the Missouri and thus form part of the Mississippi River drainage system. Roughness of topography renders certain areas unfit for cultivation, but well suited for grazing purposes. Usually more favourable growth conditions are encountered at higher altitudes, precipitation being greater, evaporation less and the soil generally productive. These factors induce the development of heavier-producing forage species, thus increasing the carrying capacity of the lands and making them more desirable for the production of live stock. Although roughness of topography is not always associated with greater carrying capacity, there are other factors connected with rough topography which are advantageous to stockmen. Natural stock-watering places are usually abundant, and sites for the development of other water supplies are usually plentiful. There is also more shelter in these rough areas, an element of im- portance to graziers. Owing to these favourable factors areas of rough topo- graphy provide some of the best range pastures. 6 Climate Annual precipitation is the principal climatic factor affecting vegetative growth over the entire prairie area, particularly in the western and southern portions. Not only is it limited in amount, but its distribution is uncertain. Meteorological records indicate that over a period of years about one-half of the annual precipitation occurs during the months April to July inclusive. This, however, is not constant, for as little as one-seventh or as much as four- fifths may fall during the same period in any particular year. In addition, wide yearly variations can be expected. A drop of from 25-28 to 7-64 inches of total precipitation was recorded at Medicine Hat, Alberta, in two successive seasons (1927 and 1928). Other factors including temperature, evaporation and wind velocity add to the complex effects of climate. Selected meteorological data from representative stations are presented in table 1. With the exception of the Manyberries records which are for an eleven-year period, all records of temperature and precipitation are for twenty- six years or more. The selected stations are close to the southern and northern boundaries of the area covered by the survey. All of the stations listed in the table are shown on plate 1. TABLE 1.— TEMPERATURE, PRECIPITATION AND EVAPORATION RECORDS FROM SELECTED STATIONS IN THE PRAIRIE PROVINCES Station Mean A nnual Temp. in O p Average Precipitation Annual April to July Evapo- ration in ins. P:E Ratio Refer. Pincher Creek, Alta. Lethbridge, Alta Medicine Hat, Alta. . Manyberries, Alta. . . Klintonel, Sask.* Swift Current, Sask. Indian Head, Sask. . Morden, Man Brandon, Man Rosthern, Sask Scott, Sask Lacombe, Alta 39 41 42 40 36 38 34 36 34 33 32 35 •52 •96 •75 •71 •90 •22 •32 •05 •84 •62 •40 •27 •96 •05 •76 •36 •61 •04 •30 •92 •52 •43 •27 •67 24-96 33 02 0-64 0-32 3C-08 21-62 23-21 16-19 19-02 21-76 16-44 0-44 0-85 0-84 1-16 0-77 0-62 105 * Klintonel is located in the Cypress Hills. 1. Canada Year Book 1930. 2. Dominion Experimental Farm Reports and Records. Annual precipitation in inches Seasonal evaporation in inches from a free water surface = P:E ratio. (April to August inclusive) The records presented in table 1 indicate that there is an area of low average seasonal and annual precipitation surrounding Medicine Hat and Manyberries. The table further shows that there is a greater average rainfall at stations near the eastern, western and northern margins of the region. Evaporation records are presented for a five-month season (May to Septem- ber inclusive). The data indicate that evaporation from a free water surface is greater at Manyberries than at any other point. The precipitation-evapor- ation ratio is lowest at the same station. Mean temperature as shown by the records decreases from a high of 42° F. at Medicine Hat to a low of 32° F. at Scott. Although these are the extreme temperatures given in the table, they are representative of fairly large districts 8 surrounding the two stations. Thus there is a region which has a mean tem- perature equal or nearly equal to that of Medicine Hat. This area extends westward to the vicinity of Lethbridge, nearly as far east as Swift Current, and northward from the International Boundary to the vicinity of the Red Deer River. The mean temperature at Scott is also representative of tem- peratures over a considerable area. It will be noted that the mean temperature at Rosthern is only one degree higher. A broad picture of the climate within the region would show, first, that there is a district surrounding Medicine Hat which has a low annual precipitation, a high evaporation rate and a high mean temperature, and second, that rainfall increases, while mean temperatures and evaporation rates decrease toward the northern and eastern margins. As stated previously rainfall is the chief climatic factor influencing crop production, but its effects are modified by those of mean temperature, the seasonal distribution of rainfall, the evaporation rate and other climatic factors of less importance. Soil The soils of the region are classified into three major divisions, the brown, dark brown and black soil zones,1 (plate 2). Within each zone the soil varies considerably in texture, large tracts are composed of sand, while others equally large are deposits of glacial lake clay. However, most of the soils are classified as loams which vary from sandy types to those which are composed mostly of clay. These soils are derived largely from glacial deposits, although sedentary types are found in the Foothills and Cypress Hills. Soils in the brown soil zone have developed under the lowest rainfall in the area. They have brown or greyish-brown surface horizons which are lower in organic matter than the corresponding horizons of the other zones. The lime layer, or layer of calcium carbonate accumulation, is encountered generally at from 6 to 14 inches below the surface. In the western portion of the zone the vegetation is dominated by species which characterize the short-grass prairie, while in the eastern portion the dominant species are those of the mixed prairie association. Surface horizons in the dark brown soil zone are dark brown in colour. They contain greater quantities of organic matter than do similar horizons of the brown soil zone. Lime layers are deeper, varying from 10 to 18 inches below the surface. The vegetation is dominated by species which distinguish the mixed prairie association, although at the outer margin stands of submontane mixed prairie are encountered. Soils of the black soil zone have surface horizons which are black or nearly so in colour. They contain more nitrogen and organic matter than do the same horizons in the brown and dark brown zones (table 2). The lime layer is generally more than 18 inches, and is often as much as 30 inches below the surface. While these soils have developed under grass vegetation, there has been a considerable invasion of deciduous trees from the grey forest soils located north of the black soil zone. The chemical compositon of surface soils in the three zones is presented in table 2. Data are taken from the Saskatchewan Soils Survey Eeport No. 10 (12), and are fairly representative of the soils throughout the area. 1 The three soil zones, brown, dark brown and black are comparable to the brown, chestnut and chernozem zonal soils of the United States. 9 TABLE 2.— CHEMICAL COMPOSITION OF TYPICAL BROWN, DARK BROWN AND BLACK SOILS Soil Zone and Series Type Nitrogen % Phosphorus % . Calcium % Brown Soil Zone Sceptre Series " Haverhill Series Hatton Series Dark Brown Soil Zone Regina Series Asquith Series Black Soil Zone Indian Head Series Meota Series Heavy clay Loam Fine sandy loam . Heavy clay Loam Fine sandy loam . Heavy clay Loam Fine sandy loam . 0-22 0-20 0-16 0-27 0-26 0-19 0-40 0-45 0-30 006 005 004 0-07 007 005 009 0-06 0-04 103 0-44 0-37 1-30 0-65 0-70 1-49 0-94 0-81 VEGETATION The vegetational cover over most of the area with which the survey is concerned is a grassland climax (plate 2). The exceptions are regions along the northern and western boundaries, and at certain higher altitudes in the interior, where the vegetation is dominated by shrubs and trees. However, the lands which produce the forest associations are not of great importance to the live stock industry, as they provide a very small percentage of the forage produced. The species which constitute the cover are being collected. To date over 1,100 species have been gathered and placed in the herbarium at the Dominion Experimental Station, Swift Current, Saskatchewan. These species are repre- sentative of 426 genera and 112 families. The families having the largest representation being Poaceae, Cyperaceae, Chenopodiaceae, Carduaceae, Fabaceae, Rosaceae and Brassicaceae. Three main types are recognized within the grassland climax (16). 2 These are classified as follows: 1. Short-grass prairie — Bouteloua-Stipa association. 2. Mixed prairie — -Stipa-Agropyron-Bouteloua association. 3. Submontane mixed prairie — Festuca-Danthonia association (5). Forest formations dominate the vegetation in certain areas. Within the wooded portions of the Foothills and Cypress Hills the vegetational cover is characterized by a lodge-pole pine Pinus contorta lati folia Wat. sub-climax. Along the northern boundary of the area a gradual change from grassland to forest is noted. This ecotone is generally referred to as Parkland. The grasses are still dominant but slightly improved climatic conditions favour the growth of aspen and willow (10). Further north, and beyond the region covered by the survey, the Parkland gives way to coniferous forest, in which the dis- tinguishing species are jack pine, P. Banksiana Lamb., and white spruce, Picea glauca (Moench) Voss. 2 In addition to the three principal grassland types, small areas in southern Manitoba are classified as tall-grass prairie. There are vegetational cover is dominated by big bluestem Andropogon furcatus Muhl., Indian grass Sorghastrum nutan. (L.) Nash, and prairie cordgrass Spartina pectinata Link. 58438—2 10 I \ x n -a a SO Ph CD hh" W CO od u o o CO 3 © •H Fh •H CO ft ft, ©