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Soils of the - Agriculture and Agri-Food Canada

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SHALISH (Continued)<br />

(SH)<br />

General L<strong>and</strong> Use Comments : (1) Excessive stoniness <strong>and</strong> low water holding capacity generally mak e<br />

Shalish soils unsuited for arable agriculture . (2) Urban <strong>and</strong> related uses are moderately to poorly suited fo r<br />

Shalish soils. The stony <strong>and</strong> bouldery nature <strong>of</strong> <strong>the</strong> soil make basements, septic tank disposal fields <strong>and</strong> o<strong>the</strong> r<br />

excavations difficult to construct . Effluent filtration may be incomplete because <strong>of</strong> coarse textures <strong>and</strong> ma y<br />

ei<strong>the</strong>r contaminate groundwater or o<strong>the</strong>r areas downslope . Stream channel shifting or diversion is a significant<br />

hazard in some areas . Shalish soils provide potential sources <strong>of</strong> fill <strong>and</strong> aggregate ; screening is likely to be<br />

required, however. (3) Forest growth is good in spite <strong>of</strong> <strong>the</strong> coarse soil textures <strong>and</strong> low water holding capacity .<br />

Telluric subsoil seepage seems to provide enough moisture during most <strong>of</strong> <strong>the</strong> growing season . Data from a<br />

limited number <strong>of</strong> plots indicates western hemlock <strong>and</strong> Douglas-fir produce about 9 to 15 m3/ha <strong>of</strong> wood/yr. The<br />

higher rates <strong>of</strong> growth are associated with areas receiving <strong>the</strong> greatest amounts <strong>of</strong> seepage .<br />

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