Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada
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Soil Moisture Characteristics : Columbia soils are well to rapidly drained . They are rapidly pervious an d<br />
have slow surface run<strong>of</strong>f <strong>and</strong> low water holding capacity. They are droughty during most summers .<br />
General Soil Description :<br />
Columbia soils usually have 5 cm or less <strong>of</strong> forest litter on <strong>the</strong> soil surface . This i s<br />
underlain by a thin (less than 2 cm), discontinuous, grayish, s<strong>and</strong>y, leached layer, which, in turn, is underlain b y<br />
about 15 cm <strong>of</strong> s<strong>and</strong>y or loamy, friable, reddish-brown, brown or yellowish-brown material . This material grade s<br />
to about 40 cm <strong>of</strong> similarly coloured, loose gravel or gravelly s<strong>and</strong> . Below about 80 cm, unwea<strong>the</strong>red, loose ,<br />
stratified gravel <strong>and</strong> gravelly s<strong>and</strong> occur. Stones <strong>and</strong> cobbles are common throughout . Soil reactions rang e<br />
from strongly acid in <strong>the</strong> surface layers to medium or slightly acid in <strong>the</strong> lower subsoil . Soil classification is Orthic<br />
Humo-Ferric Podzol.<br />
Commonly Associated <strong>Soils</strong> :<br />
Abbotsford, Lynden, Lehman <strong>and</strong> Defehr soils <strong>of</strong>ten occur in soil complexes<br />
with Columbia soils or occupy adjacent l<strong>and</strong>s . Abbotsford soils differ from Columbia soils by having 2 0<br />
to 50 cm <strong>of</strong> silty material over gravel or gravelly s<strong>and</strong> . Lynden soils are s<strong>and</strong>y ra<strong>the</strong>r than gravelly in texture whil e<br />
Lehman <strong>and</strong> Defehr soils respectively, are poorly <strong>and</strong> imperfectly drained .<br />
Vegetation :<br />
Large areas have been cleared <strong>and</strong> are utilized for agricultural or urban uses . Uncleared areas<br />
support a mixed forest which includes coast Douglas-fir, western hemlock, gr<strong>and</strong> fir, red alder, birch <strong>and</strong> maple .<br />
The understory includes salai, bracken, thimbleberry <strong>and</strong> various mosses . O<strong>the</strong>r than impediments imposed<br />
by <strong>the</strong> gravelly subsoil, no restrictions to rooting occur to depths <strong>of</strong> 100 cm or more .<br />
General L<strong>and</strong> Use Comments :<br />
(1) <strong>Agri</strong>culturally, Columbia soils are limited by low water holdin g<br />
capacity, relatively low fertility <strong>and</strong> stoniness . With adequate fertilization <strong>and</strong> irrigation (<strong>and</strong> stone picking a s<br />
required), most crops can be produced satisfactorily. (2) Columbia soils are well suited for urban <strong>and</strong> simila r<br />
uses . They are well drained <strong>and</strong> have good bearing strength <strong>and</strong> level topography . However, effluent fro m<br />
numerous septic tanks can potentially contaminate groundwater through incomplete filtration in <strong>the</strong> coarse -<br />
textured, gravelly subsoil . Columbia soils are usually good sources <strong>of</strong> aggregate . (3) Forest production o n<br />
Columbia soils is moderate . Limited plot data indicates growth <strong>of</strong> coast Douglas-fir to be about 6 to 8 m 3/ha/yr.<br />
Droughtiness during <strong>the</strong> latter parts <strong>of</strong> <strong>the</strong> growing season seems to be <strong>the</strong> main growth limitation .<br />
(CL)<br />
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