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RM of Springfield Information Bulletin 99-7

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RM of Springfield Information Bulletin 99-7 Rural Municipality of Springfield Information Bulletin 99-7 Rural Municipality of Springfield Information Bulletin 99-7 Page 1 Rural Municipality of Springfield Information Bulletin 99-7 Prepared by: Land Resource Unit, Brandon Research Centre, Research Branch, Agriculture and Agri-Food Canada. Department of Soil Science, University of Manitoba. Manitoba Soil Resource Section, Soils and Crops Branch, Manitoba Agriculture. Printed October, 1999 Page 2 Information Bulletin 99-7 Rural Municipality of Springfield PREFACE ACKNOWLEDGMENTS This is one of a new series of information bulletins for individual Continuing support for this project has been provided by Brandon rural municipalities of Manitoba. They serve to introduce the newly Research Centre and PFRA Manitoba. The project was initiated by developed digital soil databases and illustrate several typical derived the Land Resource Unit under the Canada-Manitoba Agreement of and interpretive map products for agricultural land use planning Agricultural Sustainability. applications. The bulletins will also be available in diskette format for each rural municipality. The following individuals and agencies contributed significantly to the compilation, interpretation, and derivation of the information Information contained in this bulletin may be quoted and utilized contained in this report. with appropriate reference to the originating agencies. The authors and originating agencies assume no responsibility for the misuse, Managerial and administrative support was provided by: alteration, re-packaging, or re-interpretation of the information. R.G. Eilers, Head, Land Resource Unit, Brandon Research Centre, This information bulletin serves as an introduction to the land Research Branch, Agriculture and Agri-Food Canada. resource information available for the municipality. More detailed G.J. Racz, Head, Department of Soil Science, University of information, including copies of the primary soil and terrain maps Manitoba. at larger scales, may be obtained by contacting Technical support was provided by: Land Resource Unit Room 360 Ellis Bldg, University of Manitoba G.W. Lelyk, and P. Cyr, Land Resource Unit, Brandon Research Winnipeg, Manitoba R3T 2N2 Centre, Research Branch, Agriculture and Agri-Food Canada. Phone: 204-474-6118 FAX: 204-474-7633 J. Fitzmaurice, and A. Waddell, Department of Soil Science, University of Manitoba. CITATION G.F. Mills, P. Ag, Winnipeg, Manitoba Land Resource Unit, 1999. Soils and Terrain. An Introduction to the J. Griffiths, and C. Aglugub, Soil Resource Section, Soils and Crops Land Resource. Rural Municipality of Springfield. Information Branch, Manitoba Agriculture. Bulletin 99-7, Brandon Research Centre, Research Branch, R. Lewis, PFRA, Agriculture and Agri-Food Canada. Agriculture and Agri-Food Canada Professional expertise for data conversion, correlation, and interpretation was provided by: W.R. Fraser and R.G. Eilers, Land Resource Unit, Brandon Research Centre, Research Branch, Agriculture and Agri-Food Canada. P. Haluschak and G. Podolsky, Soil Resource Section, Soils and Crops Branch, Manitoba Agriculture. Rural Municipality of Springfield Information Bulletin 99-7 Page 3 INTRODUCTION The location of the Rural Municipality of Springfield is shown in Figure 1. A brief overview of the database information, and general environmental conditions for the municipality are presented. A set of maps derived from the data for typical agricultural land use and planning applications are also included. The soil map and database were compiled and registered using the Geographic Information System (PAMAP GIS) facilities of the Land Resource Unit. These databases were used in the GIS to create the generalized, derived and interpretive maps and statistics in this report. The final maps were compiled and printed using Coreldraw. This bulletin is available in printed or digital format. The digital bulletin is a Windows based executable file which offers additional display options, including the capability to print any portion of the bulletin. Figure 1. Rural municipalities of southern Manitoba. Page 4 Information Bulletin 99-7 Rural Municipality of Springfield LAND RESOURCE DATA Base Layer The soil and terrain information presented in this bulletin was Digital base map information includes the municipality and compiled as part of a larger project to provide a uniform level of township boundaries, along with major streams, roads and land resource information for agricultural and regional planning highways. Major rivers and lakes from the base layer were also used purposes throughout Agro-Manitoba. This information was as common boundaries for the soil map layer. Water bodies larger compiled and analysed in two distinct layers as shown in Figure 2. than 25 ha in size were digitized as separate polygons. Soil Layer The most detailed soil information currently available was selected as the data source for the digital soil layer for each rural municipality. Comprehensive detailed soil maps (1:20 000 to 1:50 000 scale) have been published for many rural municipalities. Where they were available, the individual soil map sheets were digitized and compiled as a single georeferenced layer to match the digital RM base. Map polygons have one or more soil series components, as well as slope and stoniness classes. Soil database information was produced for each polygon, to meet national standards (MacDonald and Valentine, 1992). Slope length classes were also added, based on photo-interpretation. Older, reconnaissance scale soil maps (1:126 720 scale) represented the only available soil data source for many rural municipalities. These maps were compiled on a soil association basis, in which soil landscape patterns were identified with unique surficial geological deposits and textures. Each soil association consists of a range of different soils ("associates") each of which occurs in a repetitive position in the landscape. Modern soil series that best represent the soil association were identified for each soil polygon. The soil and Figure 2. Soil and Base Map data. modifier codes provide a link to additional databases of soil properties. In this way, both detailed and reconnaissance soil map polygons were related to soil drainage, surface texture, and other soil properties to produce various interpretive maps. Slope length classes were also added, based on photo-interpretation. Rural Municipality of Springfield Information Bulletin 99-7 Page 5 SOIL AND TERRAIN OVERVIEW excess of 255 m asl. The generally low surface gradients (0.7 m/km or 3.8 ft/mi) throughout most of the municipality result in poorly The Rural Municipality (RM) of Springfield covers an area of developed surface drainage. In addition, much of the area is approximately 11.5 townships (110 348 ha) extending east from the characterized by high groundwater levels while very poorly drained City of Winnipeg for a distance of 48 km (page 3). The village of organic terrain in the eastern part of the municipality contributes Oakbank is the largest population and service centre with smaller drainage waters to the area throughout the year. Surface waters concentrations of people resident in Dugald, Anola and Vivian. drain slowly in a northwesterly direction via Cooks Creek and Monominto and Prairie Grove are small population centres located northerly via the Brokenhead River in the eastern portion. The Red on the southern boundary of the municipality with the RM of Tache. River Floodway around the east side of Winnipeg is constructed through the municipality. Surface drainage for agricultural purposes The climate in most of the area can be related to weather data from has been improved in parts of the area by a network of man-made Dugald while data from Beausejour best characterize the eastern drains. portion of the area. The mean annual temperature decreases from 1.8°C in the west to 1.6°C in the east and the mean annual Soil materials in the Red River Valley were deposited during the precipitation ranges between 553 mm in the west and 539 mm in the time of glacial Lake Agassiz and consist primarily of deep, clayey east (Environment Canada, 1993). The average frost-free period is lacustrine sediments. In contrast, the Southeastern Plain is 106 days and degree-days above 5°C accumulated from May to characterized by thin, sandy to coarse-loamy lacustrine veneers September average 1597 (Ash, 1991). An evaluation of growing overlying stony, loam textured glacial till. Waterworked, extremely conditions in this region of Manitoba can be related to estimates of calcareous, stony, loam till and local areas of gravelly sand outwash seasonal moisture deficit and effective growing degree-days and beach deposits are common, particularly in the Birds Hills area. (EGDD) above 5°C. The seasonal moisture deficit calculated The eastern edge of the municipality is characterized by extensive between May and September falls between 250 mm and 200 mm organic deposits (page 11). The flat topography throughout the with lower deficits occurring to the east. Similarly, the estimated municipality results in the majority of soils being classified as effective growing degree-days accumulated from May to September imperfectly to poorly drained (page 13). range between 1600 and 1500, with lower values to the east (Agronomic Interpretations Working Group, 1995). These Soils in the municipality have been mapped at a reconnaissance parameters provide an indication of moisture and heat energy level (1:126 720 scale) and published in the soil survey
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