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Soils of the - Agriculture and Agri-Food Canada

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subsoil : A general term for <strong>the</strong> layer <strong>of</strong> soil (or surficial geologic deposit) which, in <strong>the</strong> context <strong>of</strong> this report ,<br />

underlies <strong>the</strong> surface <strong>and</strong> subsurface soil layers . It begins about 50 cm below <strong>the</strong> surface <strong>and</strong> continue s<br />

downward for about 75 to 100 cm .<br />

subsurface soil : A general term used in this report for <strong>the</strong> approximately 20 to 30 cm thick layer <strong>of</strong> soi l<br />

underlying <strong>the</strong> surface soil .<br />

surface soil : The uppermost part <strong>of</strong> <strong>the</strong> soil that is ordinarily moved in tillage, or its equivalent in uncultivate d<br />

soils . In this report it refers to <strong>the</strong> upper 15 to 20 cm <strong>of</strong> <strong>the</strong> soil .<br />

telluric seepage : Seepage moving through <strong>the</strong> soil on a plane more or less parallel to <strong>the</strong> l<strong>and</strong> surface an d<br />

<strong>of</strong>ten above a restricting area ; <strong>the</strong> waters are usually oxygenated .<br />

terric layer : An unconsolidated mineral substratum underlying organic soil material .<br />

texture, soil : The relative proportions <strong>of</strong> <strong>the</strong> various soil separates (s<strong>and</strong>, silt <strong>and</strong> clay) in a soil as described b y<br />

<strong>the</strong> classes <strong>of</strong> soil texture . The names <strong>of</strong> textural soil classes may be modified by adding suitabl e<br />

adjectives when coarse fragments are present in substantial amounts .<br />

tidal flats : Areas <strong>of</strong> nearly flat, <strong>of</strong>ten barren mud periodically covered by tidal waters . Normally <strong>the</strong>se material s<br />

have an excess <strong>of</strong> soluble salt . A miscellaneous l<strong>and</strong> type .<br />

till (moraine) : Unstratified glacial drift deposited directly by <strong>the</strong> ice <strong>and</strong> consisting <strong>of</strong> clay, s<strong>and</strong>, gravel, an d<br />

boulders intermingled in any proportion .<br />

type, soil : A unit in <strong>the</strong> natural system <strong>of</strong> soil clasification ; a subdivision <strong>of</strong> a soil series consisting <strong>of</strong> o r<br />

describing soils that are alike in all characteristics including <strong>the</strong> texture <strong>of</strong> <strong>the</strong> A horizon .<br />

value, colour : The relative lightness <strong>of</strong> colour, which is approximately a function <strong>of</strong> <strong>the</strong> square root <strong>of</strong> <strong>the</strong> tota l<br />

amount <strong>of</strong> light .<br />

variant, soil : A soil whose properties are believed to be sufficiently different from o<strong>the</strong>r known soils to justify a<br />

new name, but comprising such a limited geographic area that creation <strong>of</strong> a new named soil is not justified .<br />

water table (groundwater) : Elevation at which <strong>the</strong> pressure in <strong>the</strong> water is zero with respect to <strong>the</strong> at -<br />

mospheric pressure .<br />

wea<strong>the</strong>ring : The physical <strong>and</strong> chemical disintegration, alteration, <strong>and</strong> decomposition <strong>of</strong> rocks <strong>and</strong> minerals a t<br />

or near <strong>the</strong> earth's surface by atmospheric agents .<br />

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