12.07.2015 Views

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

SHOW MORE
SHOW LESS
  • No tags were found...

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

L<strong>and</strong> Use/Management CommentsChurchville soils require tile drainage in orderto reach theirpotential capability for common fieldcrop production . <strong>The</strong>y are rated Class 3W. If theyare tile drained, Churchville soils are suitable forgrowing a fairly wide range <strong>of</strong> special crops .Suitability ratings for selected special crops aregiven in Tables 6, 7, <strong>and</strong> 8.Colwood <strong>Soils</strong> (CWTL<strong>and</strong>form <strong>and</strong> TopographyColwood soils have developed on blankets <strong>of</strong>medium textured lacustrine materials . <strong>The</strong>y occurmainly on lower slopes <strong>and</strong> in depressions inl<strong>and</strong>scapes which have nearly level topography orvery gently undulating topography. Slopes areless than 2%.Soil Moisture CharacteristicsColwood soils are poorly drained . <strong>The</strong>y areusually moderately permeable, but thepermeability decreases in horizons that are clayeyor compacted. Because <strong>of</strong> high water table levels,they tend to remain saturated for prolongedperiods <strong>of</strong> time. <strong>The</strong> water holding capacities <strong>of</strong>Colwood soils are high if permeability is notrestricted. Surface run<strong>of</strong>f is slow.General Soil Characteristics<strong>The</strong> Ap, Bg, <strong>and</strong> Ckg horizons which occurusually have silt loam, loam, or very fine s<strong>and</strong>yloam textures . <strong>The</strong> Ckg horizons are calcareous.Gray gley colours are dominant within thepr<strong>of</strong>ile, <strong>and</strong> prominent yellowish brown to strongbrown mottles are also present. Soil reactionranges from slightly acid to neutral in the Aphorizons, to mildly alkaline in the Ckg horizons .Soil classification is typically Orthic HumicGleysol .Soil VariabilityColwood soils frequently contain layers <strong>of</strong> fineor very fine textured materials . <strong>The</strong> layers arevariable in thickness <strong>and</strong> usually have silty clayloam or silty clay textures. Occasionally, they alsocontain layers <strong>of</strong> coarse textured materials whichusually have fine s<strong>and</strong>y loam textures .Colwood coarse phase (CW.C) soils weremapped where 15 to 40 cm <strong>of</strong> coarse texturedmaterials were present at the surface. Colwoodpeaty phase (CW.P) soils were mapped where 15to 40 cm <strong>of</strong> organic materials were present at thesurface . Most <strong>of</strong>ten Colwood (CW) soils weremapped in combination with Tuscola (TU) soils .L<strong>and</strong> Use/Management CommentsColwood soils require tile drainage in order toreach their potential capability for common fieldcrop production. Colwood <strong>and</strong> Colwood coarsephase soils are rated Class 2W, -<strong>and</strong> Colwoodpeaty phase soils are rated Class 4W. If they aretile drained, Colwood <strong>and</strong> Colwood .coarse phasesoils are suitable for growing a wide range <strong>of</strong>special crops. Colwood peaty phase soils aresuitable for most vegetable crops if they are tiledrained, but they have limited suitability for mostspecial field crops as well as fruit <strong>and</strong> nut crops .Suitability ratings for selected . special crops aregiven in Tables 6, 7, <strong>and</strong> 8.Colwood soils are susceptible to compaction<strong>and</strong> care should be taken not to use heavymachinery when they are too wet . Althoughconventional tillage practices may be best toimprove soil structure <strong>and</strong> enhance drainage,Colwood soils are suitable for a number <strong>of</strong>conservation tillage practices.Ekfrid <strong>Soils</strong> (EK)L<strong>and</strong>form <strong>and</strong> TopographyEkfrid soils have developed on blankets <strong>of</strong> fineto very fine textured lacustrine materials. <strong>The</strong>yusually occur on mid to crest slope positions inl<strong>and</strong>scapes which have nearly level or very gentlyundulating topography . Occasionally the surfaceslopes are steeper <strong>and</strong> the topography is gentlyundulating . Slopes range from 1 to 9%, withslopes <strong>of</strong> 1 to 5% most common.Soil Moisture CharacteristicsEkfrid soils areimperfectly drained <strong>and</strong> slowlypermeable . <strong>The</strong>y have high seasonal water tablelevels, <strong>and</strong> saturated conditions tend to occur inthe upper pr<strong>of</strong>ile for prolonged periods <strong>of</strong> time.Ekfrid soils have medium to high water holdingcapacities, but can be draughty during dry periodsbecause <strong>of</strong> water retention by the clayey soilmaterials . Surface run<strong>of</strong>f is moderate to rapid,depending on the steepness <strong>of</strong> the surface slope.Soil cracks which may develop during the summerwill increase permeability <strong>and</strong> reduce surfacerun<strong>of</strong>f.General Soil CharacteristicsEkfrid soil materials usually contain at least40% clay . <strong>The</strong>y also contain one or more layerswithin the pr<strong>of</strong>ile which contain more than 60%

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!