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

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

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

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General Soil Characteristics<strong>The</strong> Ap horizons commonly have fine s<strong>and</strong>yloam, fine s<strong>and</strong>, or loamy fine s<strong>and</strong> textures . <strong>The</strong>Bg <strong>and</strong> calcareous Ckg horizons usually have fines<strong>and</strong> or loamy fine s<strong>and</strong> textures . <strong>The</strong> calcareousIICkg horizons generally have higher silt or veryfine s<strong>and</strong> contents <strong>and</strong> frequently they have siltloam or very fine s<strong>and</strong>y loam textures .Gray gley colours are dominant within thepr<strong>of</strong>ile, <strong>and</strong> prominent dark yellowish brown todark brown mottles are also present. A zone <strong>of</strong>intensive mottling is <strong>of</strong>ten present in the s<strong>and</strong>ymaterials above the point where they contact theunderlying loamy materials . Soil reaction rangesfrom strongly acid to neutral in the Ap horizons,to mildly alkaline in the IICkg horizons . Soilclassification is typically Orthic Humic Gleysol.Soil VariabilityOccasionally the IICkg horizons have silttextures. <strong>The</strong>y may also contain layers <strong>of</strong> s<strong>and</strong>y orclayey materials . Silver Hill soils frequently arefound in l<strong>and</strong>scapes where better drained soilsalso occur.L<strong>and</strong> Use/Management ContinentsSilver Hill soils require tile drainage in orderto reach their potential capability for common fieldcrop production . <strong>The</strong>y are rated Class 2W . Withtile drainage, they are suitable for a wide range <strong>of</strong>special crops . Suitability ratings for selectedspecial crops are given in Tables 6, 7, <strong>and</strong> 8.Compaction can occur in St. Williams soils ifthey are 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.Southwold <strong>Soils</strong> (SO)L<strong>and</strong>form <strong>and</strong> TopographySouthwold soils have developed on blankets <strong>of</strong>fine to very fine textured lacustrine materials.<strong>The</strong>y usually occur in low-lying depressional areasin l<strong>and</strong>scapes which have nearly level topography.Slopes are less than 2% .Soil Moisture CharacteristicsSouthwold soils are very poorly drained <strong>and</strong>slowly permeable. Saturated conditions occur ator near the surface for prolonged periods eachyear because <strong>of</strong> high water table levels .Southwold soils have high water holdingcapacities, <strong>and</strong> surface run<strong>of</strong>f is slow .General Soil CharacteristicsSouthwold soil materials contain 27% or moreclay. <strong>The</strong> Ap, Bg, <strong>and</strong> calcareous Ckg horizonswhich commonly occur usually have silty clayloam or silty clay textures.Bluish gray or gray gley colours are dominantwithin the pr<strong>of</strong>ile . Soil reaction ranges fromslightly acid to neutral in. the Ap horizons, tomildly alkaline in the Ckg horizons. Soilclassification is typically Orthic Hun-dc Gleysol .Soil Variability<strong>The</strong> aerial extent <strong>of</strong> Southwold soils in the<strong>County</strong> is limited . <strong>The</strong> clayey subsoil materialsmay contain layers <strong>of</strong> medium or coarse texturedmaterials .Southwold soils may occur in areas whereToledo (TO) soils were mapped.L<strong>and</strong> Use/Management CommentsSouthwold soils require tile drainage in orderto reach their potential capability for common fieldcrop production. <strong>The</strong>y are rated Class 4W . Dueto severe wetness conditions, they are not suitablefor growing most vegetable, fruit, <strong>and</strong> nut crops .If they are tile drained, they have limitedsuitability for some special field crops includingwhite beans <strong>and</strong> spring canola .Springwater <strong>Soils</strong> (SP)L<strong>and</strong>form <strong>and</strong> TopographySpringwater soils have developed on blankets<strong>of</strong> coarse textured eolian materials . <strong>The</strong>y occuronly in low-lying depressional areas in l<strong>and</strong>scapeswhich have nearly level topography . Slopes areless than 2% .Soil Moisture CharacteristicsSpringwater soils are very poorly drained <strong>and</strong>rapidly permeable . <strong>The</strong> very poor drainageconditions associated with these soils are causedby high water table levels which occur at or nearthe surface for prolonged periods each year . <strong>The</strong>yhave moderate water holding capacities in thesurface materials which have high organic mattercontents, but the water holding capacities <strong>of</strong> thesubsoil materials is low. Surface run<strong>of</strong>f is slow .General Soil Characteristics<strong>The</strong> Ap horizons usually have fine s<strong>and</strong> <strong>of</strong>loamy fine s<strong>and</strong> textures, <strong>and</strong> high organic mattercontents. <strong>The</strong> subsoil Bg <strong>and</strong> calcareous Ckghorizons usually have fine s<strong>and</strong> textures .45

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