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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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Ayr <strong>Soils</strong> (AY)L<strong>and</strong>form <strong>and</strong> TopographyAyr soils have developed on 40 to 100 anthick veneers <strong>of</strong> coarse textured lacustrinematerials which are underlain by gravelly coarsetextured fluvial outwash materials . <strong>The</strong>y usuallyoccur on lower slope positions in l<strong>and</strong>scapeswhich have nearly level or very gently undulatingtopography. Slopes are less than 2% .Soil Moisture CharacteristicsAyr soils are poorly drained <strong>and</strong> rapidlypermeable . <strong>The</strong> poor drainage conditionsassociated with these soils are caused by highwater table levels which are near the surface forprolonged periods during the year. Ayr soils havelow water holding capacities <strong>and</strong> slow surfacerun<strong>of</strong>f .General Soil Characteristics<strong>The</strong> Ap <strong>and</strong> Bg horizons usually occur in theupper s<strong>and</strong>y materials <strong>and</strong> have s<strong>and</strong>y loam,loamy s<strong>and</strong>, or s<strong>and</strong> textures . <strong>The</strong> calcareousIICkg horizons generally occur in lower gravellymaterials commonly have gravelly coarse s<strong>and</strong>,gravelly loamy coarse s<strong>and</strong>, gravelly s<strong>and</strong>, orgravelly loamy s<strong>and</strong> textures .Gray gley colours are dominant in the pr<strong>of</strong>ile,<strong>and</strong> prominent dark brown to dark yellowishbrown mottles are also present. Soil reactionranges from neutral in the Ap horizons, to mildlyalkaline in the IICkg horizons . Soil classificationis typically Orthic Humic Gleysol.Soil Variability<strong>The</strong> aerial extent <strong>of</strong> Ayr soils in the <strong>County</strong> islimited. Ayr fine phase soils (AY.F) were mappedwhere 15 to 40 cm <strong>of</strong> clay loam textured materialsoverly the s<strong>and</strong>y <strong>and</strong> gravelly materials . Ayrloamy phase soils (AY.L) were mapped where 15to 40 cm <strong>of</strong> silt loam <strong>and</strong> loam textured materialsoverly the s<strong>and</strong>y <strong>and</strong> gravelly materials. Ayr soilswere mapped in combination with Camilla soils(CM).L<strong>and</strong> Use/Management CommentsAyr soils require file drainage in order to reachtheir potential capability for common field cropproduction . <strong>The</strong>y are rated Class 2W or 2WT. Ifthey are the drained, Ayr soils are suitable forgrowing a wide range <strong>of</strong> special crops . Suitabilityratings for selected special crops are given inTables 6, 7, <strong>and</strong> 8.Conservation tillage practices should beconsidered for Ayr soils. Ayr fine phase (AY.F)soils, however, are better suited for conventionaltillage practices .Bennington <strong>Soils</strong> (BN)L<strong>and</strong>form <strong>and</strong> TopographyBennington soils have developed on 40 to 100cm thick veneers <strong>of</strong> medium textured lacustrinematerials which are underlain by fine to very finetextured lacustrine materials . <strong>The</strong>y occur inl<strong>and</strong>scapes which usually have gently undulatingtopography, <strong>and</strong> they commonly occur on mid toupper slope positions. Slopes commonly rangefrom 5 to 9% .Soil Moisture CharacteristicsBennington soils are well drained . <strong>The</strong>y areusually moderately permeable through the uppermedium textured materials, <strong>and</strong> slowly permeablein the lower fine to very fine textured materials .<strong>The</strong> water holding capacities <strong>of</strong> Bennington soilsare high. Surface run<strong>of</strong>f is moderate on verygentle slopes, but can be rapid on steeper slopes .General Soil Characteristics<strong>The</strong> Ap <strong>and</strong> Bm horizons usually occur in theupper medium textured materials . <strong>The</strong>y typicallyhave silt loam or loam textures. Clay enriched Btor IIBt horizons commonly occur where themedium textured materials contact the underlyingfine textured materials . Textures <strong>of</strong> those horizonsfrequently are silt loam, loam, silty clay loam, orsilty clay . <strong>The</strong> calcareous IICk horizons usuallyhave silty clay loam or silty clay textures . Soilreaction ranges from slightly acid to neutral in theAp horizons, to mildly alkaline in the IICkhorizons. Soil classification is typically BrunisolicGray Brown Luvisol .Soil VariabilityOccasionally very fine s<strong>and</strong>y loam or fines<strong>and</strong>y loam textures occur in the upper materials .Layers <strong>of</strong> medium textured materials also occuroccasionally in the lower fine textured materials .Bennington till phase 03N T) soils were mappedwhere 40 to 100cm <strong>of</strong> medium textured lacustrinematerials were underlain by fine to very finetextured Port Stanley till. <strong>The</strong> aerial extents <strong>of</strong>Bennington (BN) <strong>and</strong> Bennington till phase(BN.T)soils in the <strong>County</strong> are limited .Bennington soils were mapped in combinationwith Tavistock (TA) soils, -<strong>and</strong> Bennington till

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