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Soils of the - Agriculture and Agri-Food Canada

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GLOSSARY<br />

absorbed water : Water held mechanically in a soil mass <strong>and</strong> having physical properties similar to ordinar y<br />

water at <strong>the</strong> same temperature <strong>and</strong> pressure .<br />

acid soil : A soil material having a pH <strong>of</strong> less than 7 .0 .<br />

adsorbed water : Water held in a soil mass by physicochemical forces <strong>and</strong> having physical propertie s<br />

substantially different from absorbed water or chemically combined water at <strong>the</strong> same temperature an d<br />

pressure .<br />

aeration, soil : The process by which air in <strong>the</strong> soil is replaced by air from <strong>the</strong> atmosphere . In a well-aerate d<br />

soil, <strong>the</strong> soil air is similar in composition to <strong>the</strong> atmosphere above <strong>the</strong> soil . Poorly aerated soils usuall y<br />

contain a much higher percentage <strong>of</strong> carbon dioxide <strong>and</strong> a correspondingly lower percentage <strong>of</strong> oxyge n<br />

than <strong>the</strong> atmosphere . The rate <strong>of</strong> aeration depends largely on <strong>the</strong> volume <strong>and</strong> continuity <strong>of</strong> pores in <strong>the</strong> soil .<br />

aggregate : S<strong>and</strong>, gravel <strong>and</strong> o<strong>the</strong>r similar mineral material suitable for use in construction (i .e. for road<br />

surfaces, concrete, pavement) .<br />

aggregate, soil : A group <strong>of</strong> soil particles cohering in such a way that <strong>the</strong>y behave mechanically as a unit .<br />

alkaline soil : Any soil that has a pH greater than 7 .0 .<br />

alkalinity, soil : The degree or intensity <strong>of</strong> alkalinity <strong>of</strong> a soil expressed by a value greater than 7 .0 on <strong>the</strong> p H<br />

scale .<br />

alluvial fan : A fan-shaped deposit <strong>of</strong> alluvium laid down by a stream where it emerges from an upl<strong>and</strong> into les s<br />

steeply sloping terrain .<br />

alluvium : Material such as clay, silt, s<strong>and</strong>, <strong>and</strong> gravel deposited by modern rivers <strong>and</strong> streams .<br />

amorphous mineral : (i) A mineral that has no definite crystalline structure . (ii) A mineral that has a definit e<br />

crystalline structure, but appears amorphous because <strong>of</strong> <strong>the</strong> small crystal size .<br />

anthropogenic : Man-made, or strongly man-modified, soil materials .<br />

apron : A relatively gentle slope at <strong>the</strong> bottom <strong>of</strong> a steeper slope, <strong>and</strong> formed <strong>of</strong> materials similar to those on th e<br />

upper slope (i .e . alluvial fan apron).<br />

arable soil : Soil suitable for plowing <strong>and</strong> cultivation .<br />

aspect : A measure <strong>of</strong> <strong>the</strong> orientation <strong>of</strong> a slope by means <strong>of</strong> compass points .<br />

Atterberg Limits (Plastic Limits) : The range <strong>of</strong> water content over which a soil exhibits plastic behaviour. Th e<br />

Lower Atterberg Limit is <strong>the</strong> water content at which <strong>the</strong> soil is not plastic when worked <strong>and</strong> crumbles o n<br />

application <strong>of</strong> pressure . The Upper Atterberg Limit is <strong>the</strong> water content at which <strong>the</strong> soil changes fro m<br />

plastic to flow behaviour .<br />

available nutrient : The portion <strong>of</strong> any element or compound in <strong>the</strong> soil that can be readily absorbed an d<br />

assimilated by growing plants . ('Available should not be confused with "exchangeable" . )<br />

available water : The portion <strong>of</strong> water in a soil that can be readily absorbed by plant roots ; usually considered<br />

to be <strong>the</strong> water held in <strong>the</strong> soil against a pressure <strong>of</strong> up to approximately 15 bars .<br />

bar : A unit <strong>of</strong> pressure equal to one million dynes per square centimeter .<br />

base saturation percentage : The extent to which <strong>the</strong> adsorption complex <strong>of</strong> a soil is saturated wit h<br />

exchangeable cations o<strong>the</strong>r than hydrogen <strong>and</strong> aluminum . It is expressed as a percentage <strong>of</strong> <strong>the</strong> tota l<br />

cation exchange capacity .<br />

beach deposits : Sediments that are modified in <strong>the</strong>ir degree <strong>of</strong> sorting, or surface relief, or both, by <strong>the</strong> actio n<br />

<strong>of</strong> waves in forming beaches .<br />

bearing capacity (bearing strength) : The average load per unit area that is required to rupture a supportin g<br />

soil mass .<br />

bedrock : The solid rock that underlies soil <strong>and</strong> <strong>the</strong> regolith or that is exposed at <strong>the</strong> surface .<br />

blanket : A mantle <strong>of</strong> unconsolidated material thick enough to mask minor irregularities in <strong>the</strong> underlying roc k<br />

or o<strong>the</strong>r deposits, but which still conforms to <strong>the</strong> general underlying topography .<br />

bog : An area covered, or filled with, peat material which generally consists <strong>of</strong> undecomposed to moderatel y<br />

decomposed mosses .<br />

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