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Soils of the - Agriculture and Agri-Food Canada

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Commonly Associated <strong>Soils</strong> : Scat, Nicholson, Albion, Bose <strong>and</strong> Sunshine soils are commonly associated<br />

with Whatcom soils . Nicholson soils are similar to Whatcom soils except that <strong>the</strong> clay-enriched subsoil laye r<br />

occurs between 20 <strong>and</strong> 50 cm <strong>of</strong> <strong>the</strong> surface ra<strong>the</strong>r than at depths below 50 cm . Scat <strong>and</strong> Albion soils differ from<br />

Whatcom soils by being poorly drained <strong>and</strong> are ei<strong>the</strong>r depressional or lie in slightly lower l<strong>and</strong>scape positions .<br />

Bose <strong>and</strong> Sunshine soils differ from Whatcom soils by being, respectively, gravelly <strong>and</strong> s<strong>and</strong>y in <strong>the</strong> surface an d<br />

subsurface layers .<br />

Vegetation : Substantial areas <strong>of</strong> Whatcom soils are cleared <strong>and</strong> utilized for a variety <strong>of</strong> agricultural uses ,<br />

including pasture <strong>and</strong> hay, small fruits <strong>and</strong> vegetables, corn <strong>and</strong> bulb crops . Uncleared areas support second -<br />

growth forest which includes red alder, coast Douglas-fir, western hemlock, western red cedar, vine <strong>and</strong> bigleaf<br />

maple, <strong>and</strong> birch . The understory includes, among many o<strong>the</strong>rs, thimbleberry, salmonberry, cascara, elderbe -<br />

rry, trailing blackberry <strong>and</strong> bracken . Rooting is unrestricted to at least 50 cm <strong>and</strong> more commonly, 75 cm depth .<br />

Below that, root penetration is severely impeded by <strong>the</strong> dense, compact subsoil .<br />

General L<strong>and</strong> Use Comments : (1) Where adverse topography is not restricting, Whatcom soils are suite d<br />

for most agricultural crops. Some susceptible perennials may be adversely affected during <strong>the</strong> winter by<br />

temporary, perched watertables <strong>and</strong> telluric seepage . As with most soils in <strong>the</strong> map area, supplementa l<br />

irrigation is beneficial during most summers . O<strong>the</strong>r soils, especially Scat <strong>and</strong> Albion soils, are <strong>of</strong>ten closely<br />

intermingled with Whatcom soils causing some difficulties in individually managing <strong>the</strong>se soils . (2) Whatco m<br />

soils are moderately to poorly suited for urban uses . The dense, compact subsoil severely impedes septic tan k<br />

effluent disposal while variable soil bearing strengths may require special foundation requirements . Temporar y<br />

perched watertables <strong>and</strong> seepage may cause problems for basements <strong>and</strong> o<strong>the</strong>r excavations . (3) Whatco m<br />

soils potentially produce good forest growth . Limited data indicates wood production by Douglas-fir to b e<br />

between 9 <strong>and</strong> 12 m z/ha/yr, constrained mainly by soil moisture deficiencies during some mid-to-late summers .<br />

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