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Detailed Soil Survey of the Mount Revelstoke Summit Area.

Detailed Soil Survey of the Mount Revelstoke Summit Area.

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(D1) Rapidly drained - soil moisture content seldom exceedsfield capacity in any horizon except immediately afterwater additions .(D2) Well drained - soil moisture content does not normallyexceed field capacity in any horizon except possibly <strong>the</strong>C, for a significant part <strong>of</strong> <strong>the</strong> year .(D3)Moderately well drained - soil moisture in excess <strong>of</strong> fieldcapacity remains for a small but significant period <strong>of</strong> <strong>the</strong>year .(D4) Imperfectly drained - soil moisture in excess <strong>of</strong> fieldcapacity remains in subsurface horizons for moderatelylong periods during <strong>the</strong> year .(D5)Poorly drained - soil moisture in excess <strong>of</strong> field capacityremains in all horizons for a large part <strong>of</strong> <strong>the</strong> year .(D6) Very poorly drained - free water remains at or within 12inches <strong>of</strong> <strong>the</strong> surface most <strong>of</strong> <strong>the</strong> year .Specific reference tosurface drainage may be designatedin terms <strong>of</strong> run-<strong>of</strong>f and described ashigh, medium, low, or ponded .Similarly, specific reference to<strong>the</strong>characteristics <strong>of</strong> horizonswithin <strong>the</strong> pr<strong>of</strong>ile may be designatedin terms <strong>of</strong> permeability orpercolation and described asrapid, moderate, slow, very slow,and none .4 . HORIZON BOUNDARIESThe lower boundary <strong>of</strong> each horizon is described by indicatingits distinctness and form as suggested in <strong>the</strong> U .S . Department<strong>of</strong> Agriculture <strong>Soil</strong> <strong>Survey</strong> Manual (1951) .

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