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The Soils of Elgin County - Agriculture and Agri-Food Canada

The Soils of Elgin County - Agriculture and Agri-Food Canada

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eaction ranges from slightly acid to neutral in theAp horizons, to mildly alkaline in the IICkghorizons. Soil classification is typically OrthicHun-dc Gleysol.Soil VariabilityOccasionally Wauseon soils have gravellylayers which occur above the IICkg horizons . Siltloam or loam textured layers also occuroccasionally in the underlying materials . Wauseontill phase (WU.T) soils were mapped where 40 to100 cm <strong>of</strong> coarse textured lacustrine materialswere underlain by fine to very fine textured PortStanley till .Wauseon soils were <strong>of</strong>ten mapped incombination with Berrien (BE) <strong>and</strong> Walsingham(WM) soils . Wauseon till phase soils were <strong>of</strong>tenmapped in combination with Berrien till phase(BE.T) soils.L<strong>and</strong> Use/Management CommentsWauseon <strong>and</strong> Wauseon till phase soils requiretile drainage in order to reach their potentialcapability for common field crop production .<strong>The</strong>y are rated Class 2W . If they are the drained,they are suitable for a wide range <strong>of</strong> special crops .Suitability ratings for selected special crops aregiven in Tables 6, 7, <strong>and</strong> 8.Compaction can occur in Wauseon soils if theyare too wet. Care should be taken, therefore,when using heavy machinery. Conservationtillage practices, particularly no-till practices forfall crops, should be considered for these soils.Miscellaneous L<strong>and</strong> Unit DescriptionsAlluvium (AL)Areas mapped as Alluvium occur mainly inthe floodplains <strong>of</strong> rivers, creeks, <strong>and</strong> streams .<strong>The</strong>y are composed <strong>of</strong> soils which have variabledrainage conditions. Due mainly to theirgenerally low-lying or depressional l<strong>and</strong>scapepositions <strong>and</strong> high water table levels, the soilswhich occur in these l<strong>and</strong> units usually are eitherimperfectly or poorly drained . Many Alluviuml<strong>and</strong> units remain wet for prolonged periods dueto flooding <strong>of</strong> adjacent water courses, or additions<strong>of</strong> surface or seepage water from surroundingl<strong>and</strong>s with steep slopes .<strong>The</strong> soil materials which compose these l<strong>and</strong>units are variable in texture . <strong>The</strong>y may be fairlyuniform in texture throughout the pr<strong>of</strong>ile, or theymay consist <strong>of</strong> alternating layers <strong>of</strong> materialswhich have contrasting textures . When thematerials are fairly uniform, they mainly tend tobe either medium to coarse textured, or finetextured . Silt loam, loam, fine s<strong>and</strong>y loam, or veryfine s<strong>and</strong>y loam textures are common in themedium to coarse textured materials . Silty clayloam or clay loam textures are common in the finetextured materials. When the materials arelayered, the textures are highly variable <strong>and</strong> rangefrom gravelly s<strong>and</strong> to clay. Most <strong>of</strong>ten thematerials are calcareous to . the surface, <strong>and</strong> soilreaction is mildly alkaline .Alluvium l<strong>and</strong> units are generally limited intheir use for agriculture . <strong>The</strong>y are rated Class 31to 51 for common field crops, which is the range <strong>of</strong>soil capability classes which occur. If flooding istemporary <strong>and</strong> generally occurs in early spring,the risk <strong>of</strong> growing common field crops is lower.Those areas are therefore rated Class 31 . Graincorn is frequently grown on some <strong>of</strong> the higher,more extensive floodplains bordering the ThamesRiver <strong>and</strong> large creeks . Many areas which occurwithin these l<strong>and</strong> units are subject to prolongedperiods <strong>of</strong> flooding that frequently occur duringthe growing season. <strong>The</strong>y are rated Class 51, sincethey are best suited for forage crops .Eroded Channel (ER)<strong>The</strong>se l<strong>and</strong> units consist <strong>of</strong> deep "V" shapedchannels which are the result <strong>of</strong> past <strong>and</strong> presenterosion . Small creeks <strong>and</strong> streams, which in someareas may be intermittent, are present in many <strong>of</strong>these l<strong>and</strong> units. <strong>The</strong> soils which occur are highlyvariable in materials <strong>and</strong> drainage. Texture <strong>of</strong> thesoil materials range from gravelly s<strong>and</strong> to clay.Soil drainage ranges from rapidly drained oncoarse textured materials which may occur on thesteep side walls <strong>of</strong> the channel, to poorly drainedon fine to very fine textured materials which mayoccur in the narrow channel bottoms.<strong>The</strong> slopes <strong>of</strong> the steep side walls generallyexceed 30%. Occasionally the slopes may be lesssteep, especially in channels with short side slopes .Many channels have side wall slopes which are sosteep that they have no capability for agriculture.Areas mapped as this l<strong>and</strong> unit are therefore ratedClass 6T to TT for common field crops .Not Mapped (NM)Areas <strong>of</strong> l<strong>and</strong> that were disturbed or modifiedfrom their natural condition, or were permanentlywithdrawn from agricultural use, were designatedas Not Mapped on the soil maps . Such areasinclude golf courses, gravel pits, sewage lagoons,or areas that have been developed for residential,industrial, or commercial uses .53

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