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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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above the calcareous Ck or IICk horizons . <strong>The</strong>clay enriched B horizons usually have s<strong>and</strong>y loamtextures, while the Ck or IICk horizons usuallyhave gravelly coarse s<strong>and</strong> or gravelly s<strong>and</strong>textures.Soil reaction ranges from slightly acid toneutral in the Ap horizons, to mildly alkaline inthe IICk horizons. Soil classification is typicallyBnuiisolic Gray Brown Luvisol.Soil VariabilityBurford soils mainly occur in areas which arenear or adjacent to the Thames River <strong>and</strong> largecreeks which run through the <strong>County</strong>. Frequentlythe upper materials contin gravel which mayrange as high as 20% in some soils . Occasionallythe upper lacustrine materials have loam textures,or the underlying fluvial materials consist <strong>of</strong>alternating layers <strong>of</strong> s<strong>and</strong>y <strong>and</strong> gravelly materials.Brisbane (BI) or Caledon (CA) soils may occur inl<strong>and</strong>scapes where Burford soils were mapped .L<strong>and</strong> Use/Management CommentsBurford soils are rated Class 2FM for commonfield crops when topography is not a limitation.<strong>The</strong>y fiend to be draughty because <strong>of</strong> their lowwater holding capacities . Burford soils aresuitable for a wide range <strong>of</strong> special crops if thesurface slopes are not too steep . Withsupplemental irrigation, they are highly suitablefor many fruit <strong>and</strong> vegetable crops. Suitabilityratings for selected special crops are given inTables 6, 7, <strong>and</strong> 8.Burford soils are susceptible to wind erosion.Planting cover crops, establishing windbreaks, <strong>and</strong>carrying out management practices whichmaintain organic matter levels, will aid inreducing the risk <strong>of</strong> wind erosion. Conservationtillage practices, particularly no-till practices,should be considered for these soils .Caledon <strong>Soils</strong> (CA)L<strong>and</strong>form <strong>and</strong> TopographyCaledon soils have developed on 40 to 100 cmthick veneers <strong>of</strong> coarse textured lacustrinematerials which are underlain by gravelly coarsetextured fluvial outwash materials. <strong>The</strong>y usuallyoccur on upper to crest slope positions, especiallyin l<strong>and</strong>scapes where imperfectly or poorly drainedsoils also occur. <strong>The</strong> topography associated withCaledon soils ranges from nearly level to verygently sloping or undulating. Slopes generallyrange from 1 to 5% .Soil Moisture CharacteristicsCaledon soils are well drained <strong>and</strong> rapidlypermeable. <strong>The</strong>y have low water holdingcapacities <strong>and</strong> slow surface run<strong>of</strong>f, except onslopes greater than 5% where run<strong>of</strong>f may bemoderate.General Soil Characteristics<strong>The</strong> Ap horizons usually have s<strong>and</strong>y loam orloamy s<strong>and</strong> textures. <strong>The</strong> textures <strong>of</strong> the s<strong>and</strong>yBm horizons are usually loamy s<strong>and</strong> or s<strong>and</strong> .Clay enriched Bt or IIBt horizons, which usuallyhave s<strong>and</strong>y loam textures, commonly occur abovethe calcareous IICk horizons . <strong>The</strong> IICk horizonsfrequently have gravelly coarse s<strong>and</strong> or gravellys<strong>and</strong> textures.Soil reaction ranges from slightly acid toneutral in the Ap horizons, to mildly alkaline inthe IICk horizons . Soil classification is typicallyBrunisolic Gray Brown Luvisol.Soil VariabilityCaledon soils mainly occur in areas which arenear or adjacent ,to the Thames River <strong>and</strong> largecreeks which run through the <strong>County</strong>. Frequentlythe upper s<strong>and</strong>y materials have been windmodified . Occasionally Caledon soils have rapiddrainage when the Bt or 11Bt horizons are weaklydeveloped <strong>and</strong> the upper materials also containsignificant amounts <strong>of</strong> gravel. <strong>The</strong> underlyingIICk materials <strong>of</strong> some Caledon soils consist <strong>of</strong>alternating layers <strong>of</strong> s<strong>and</strong>y <strong>and</strong> gravelly materials .Fine phase Caledon soils (CA.F) were mappedwhere 15 to 40 cm <strong>of</strong> clay loam or silty clay loamtextured material overlies the s<strong>and</strong>y <strong>and</strong> gravellymaterials . Caledon (CA) soils were most <strong>of</strong>tenmapped in combination with Camilla (CM) soils.Fox (FX) <strong>and</strong> Brady (BY) soils may occur inl<strong>and</strong>scapes where Caledon soils were mapped .L<strong>and</strong> Use/Management CommentsCaledon soils are rated Class 2FM forcommonfield crops when topography is not a limitation .<strong>The</strong>y have fertility limitations <strong>and</strong> also tend to bedraughty. With supplemental irrigation, they arehighly suitable forawide range <strong>of</strong> special crops ifthe surface slopes are not too steep. Suitabilityratings for selected special crops are given inTables 6, 7, <strong>and</strong> 8.Caledon soils are susceptible to wind erosion.Planting cover crops, establishing windbreaks, <strong>and</strong>carrying out management practices whichmaintain organic matter levels, will aid inreducing the risk <strong>of</strong> erosion by wind .

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