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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soils which occur in the eastern portion of theCounty . Suitability ratings for selected specialcrops are given in Tables 6, 7, and 8.Plainfield soils are susceptible to wind erosion .Planting cover crops and establishing windbreakswill aid in reducing the risk of erosion by wind .Conservation tillage practices, particularly no-tillpractices, should be considered for these soils.Shedden Soils (SH)Landform and TopographyShedden soils have developed on coarsetextured ice-contact stratified drift materials . Thecoarse texured drift materials usually containlayers of gravelly materials . They commonly arefound on upper and crest slope positions onisolated sandy ridges or knolls which occur inclayey till morainal landscapes . Slopes range from2 to 15%, with slopes of 6 to 15% being mostcommon .Soil Moisture CharacteristicsShedden soils are rapidly drained and rapidlypermeable . They have low water holdingcapacities and slow surface runoff, except onslopes greater than 5% where runoff may bemoderate to rapid .General Soil CharacteristicsThe Ap and Bm horizons usually have loamyfine sand, loamy sand, . or fine sandy loamtextures . Clay enriched Bt horizons, which usuallyhave fine sandy loam textures, usually occurabove the calcareous Ck or IICk horizons .Textures of the Ck horizons is usually fine sand orloamy fine sand. The coarser textured calcareousmaterials which occur at depth usually consist ofalternating layers of sandy and gravelly materials .The sandy layers commonly have loamy fine sand,fine sand, or sand textures. The gravelly layersfrequently have gravelly sand, gravelly coarsesand, or gravelly loamy coarse sand textures.Soil reaction ranges from medium acid toneutral in the Ap horizons, to mildly alkaline inthe underlying calcareous materials. Soilclassification is typically Brunisolic Gray BrownLuvisol.Soil VariabilityShedden soils mainly occur in the northernportion of Southwold Township and in the northeasternportion of Dunwich Township . In thoseareas they are underlain by clayey till materials ofthe St. Thomas Moraine . The layers of coarsetextured materials which occur at depth in thesesoils are variable in thickness. The sandy layerswhich are present in those materials usuallycontain some gravel, which may be greater than10% in some layers . Occasionally loamy or clayeylayers also occur within the profile of someShedden soils.In transition areas between the, sandy ridgesand the surrounding till moraines, occasionallyshallow Shedden soils may occur where theunderlying till materials are present within 100 cmof the surface. Severely eroded Shedden soilsoccur in small portions of some landscapes.Shedden soils were most often mapped incombination with Middlemarch (MI) and Gobles(GO) soils.Land Use/Management CommentsShedden soils are rated Class 2FM for commonfield crops when topography is not a limitation.With supplemental irrigation, they are highlysuitable for a wide range of special crops.Suitability ratings for selected special crops aregiven in Tables 6, 7, and 8.Shedden soils are susceptible to wind erosion .Planting cover crops, establishing windbreaks, andmaintaining high crop residue levels will aid inreducing the risk of erosion by wind .Conservation tillage practices, particularly no-tillpractices, should be considered for these soils.Silver Hill Soils (SL)Landform and TopographySilver Hill soils have developed on 40 to 100cm thick veneers of coarse textured lacustrinematerialswhich are underlainby medium texturedlacustrine materials. They usually occur on lowerslopes and in depressions in landscapes whichhave nearly level or very gently undulatingtopography. Slopes are less than 2% .Soil Moisture CharacteristicsSilver Hill soils are poorly drained . They aremoderately to rapidly permeable in the uppercoarse textured materials, but slowly permeable inthe lower medium textured materials. The poordrainage conditions associated with these soils areoften caused by high water table levels, whichmay occur within 50 cm of the surface forprolonged periods of time. Silver Hill soils havemedium to highwater holding capacities and slowsurface runoff.

General Soil CharacteristicsThe Ap horizons commonly have fine sandyloam, fine sand, or loamy fine sand textures . TheBg and calcareous Ckg horizons usually have finesand or loamy fine sand textures . The calcareousIICkg horizons generally have higher silt or veryfine sand contents and frequently they have siltloam or very fine sandy loam textures .Gray gley colours are dominant within theprofile, and prominent dark yellowish brown todark brown mottles are also present. A zone ofintensive mottling is often present in the sandymaterials 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. They may also contain layers of sandy orclayey materials . Silver Hill soils frequently arefound in landscapes where better drained soilsalso occur.Land Use/Management ContinentsSilver Hill soils require tile drainage in orderto reach their potential capability for common fieldcrop production . They are rated Class 2W . Withtile drainage, they are suitable for a wide range ofspecial crops . Suitability ratings for selectedspecial crops are given in Tables 6, 7, and 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 Soils (SO)Landform and TopographySouthwold soils have developed on blankets offine to very fine textured lacustrine materials.They usually occur in low-lying depressional areasin landscapes which have nearly level topography.Slopes are less than 2% .Soil Moisture CharacteristicsSouthwold soils are very poorly drained andslowly permeable. Saturated conditions occur ator near the surface for prolonged periods eachyear because of high water table levels .Southwold soils have high water holdingcapacities, and surface runoff is slow .General Soil CharacteristicsSouthwold soil materials contain 27% or moreclay. The Ap, Bg, and calcareous Ckg horizonswhich commonly occur usually have silty clayloam or silty clay textures.Bluish gray or gray gley colours are dominantwithin the profile . 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 VariabilityThe aerial extent of Southwold soils in theCounty is limited . The clayey subsoil materialsmay contain layers of medium or coarse texturedmaterials .Southwold soils may occur in areas whereToledo (TO) soils were mapped.Land Use/Management CommentsSouthwold soils require tile drainage in orderto reach their potential capability for common fieldcrop production. They are rated Class 4W . Dueto severe wetness conditions, they are not suitablefor growing most vegetable, fruit, and nut crops .If they are tile drained, they have limitedsuitability for some special field crops includingwhite beans and spring canola .Springwater Soils (SP)Landform and TopographySpringwater soils have developed on blanketsof coarse textured eolian materials . They occuronly in low-lying depressional areas in landscapeswhich have nearly level topography . Slopes areless than 2% .Soil Moisture CharacteristicsSpringwater soils are very poorly drained andrapidly permeable . The very poor drainageconditions associated with these soils are causedby high water table levels which occur at or nearthe surface for prolonged periods each year . Theyhave moderate water holding capacities in thesurface materials which have high organic mattercontents, but the water holding capacities of thesubsoil materials is low. Surface runoff is slow .General Soil CharacteristicsThe Ap horizons usually have fine sand ofloamy fine sand textures, and high organic mattercontents. The subsoil Bg and calcareous Ckghorizons usually have fine sand textures .45

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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