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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lithic layer : Bedrock under <strong>the</strong> control section <strong>of</strong> a soil . In Organic soils, bedrock occurring within a depth o f<br />
between 10 cm <strong>and</strong> 160 cm from <strong>the</strong> surface, while in mineral soils it occurs between 10 <strong>and</strong> 100 cm <strong>of</strong> th e<br />
surface .<br />
loamy : Intermediate in texture <strong>and</strong> properties between fine-textured <strong>and</strong> coarse-textured soils . It includes al l<br />
textural classes having "loam" or "loamy" as a part <strong>of</strong> <strong>the</strong> class name, such as clay loam or loamy s<strong>and</strong> .<br />
loess : Material transported <strong>and</strong> deposited by wind <strong>and</strong> consisting <strong>of</strong> predominantly silt-sized particles .<br />
Luvisolic : An order <strong>of</strong> soils that have eluvial (Ae) horizons, <strong>and</strong> illuvial (Bt) horizons in which silicate clay is th e<br />
main accumulation product . The soils developed under forest or forest-grassl<strong>and</strong> transition in a moderate<br />
to cool climate .<br />
map, soil : A map showing <strong>the</strong> distribution <strong>of</strong> soil mapping units related to <strong>the</strong> prominent physical <strong>and</strong> cultura l<br />
features <strong>of</strong> <strong>the</strong> earth's surface .<br />
medium texture : Intermediate between fine-textured <strong>and</strong> coarse-textured soils . It includes <strong>the</strong> followin g<br />
textural clases : very fine s<strong>and</strong>y loam, loam, silt loam, <strong>and</strong> silt .<br />
mesic layer : A layer <strong>of</strong> organic material at a stage <strong>of</strong> decomposition between that <strong>of</strong> <strong>the</strong> fibric <strong>and</strong> humi c<br />
layers .<br />
metamorphic rock : Rock derived from pre-existing rocks, but differing from <strong>the</strong>m in physical, chemical, an d<br />
mineralogical properties as a result <strong>of</strong> natural geological processes, principally heat <strong>and</strong> pressure ,<br />
originating within <strong>the</strong> earth . The pre-existing rocks may have been igneous, sedimentary, or ano<strong>the</strong>r for m<br />
<strong>of</strong> metamorphic rock .<br />
mineral soil : A soil consisting predominantly <strong>of</strong>, <strong>and</strong> having its properties determined predominantly by ,<br />
mineral matter. It contains less than 17% organic carbon except for an organic surface layer that may b e<br />
up to 40 cm thick .<br />
miscellaneous l<strong>and</strong> type : A mapping unit for areas <strong>of</strong> l<strong>and</strong> that have little or no natural soil .<br />
moder : A zoogenous forest humus form made up <strong>of</strong> plant remains partly disintegrated by <strong>the</strong> soil fauna ( F<br />
layer), but not matted as in raw humus . It is transitional to a zone <strong>of</strong> spherical or cylindrical microejections o f<br />
arthropods that is permeated by loose mineral particles in its lower part <strong>and</strong> <strong>of</strong>ten throughout . Incorpora -<br />
tion <strong>of</strong> organic matter is shallow <strong>and</strong> <strong>the</strong> mixing <strong>of</strong> organic <strong>and</strong> mineral particles is purely mechanical .<br />
moderately coarse texture : Consisting predominantly <strong>of</strong> coarse particles . In soil textural classification, i t<br />
includes all <strong>the</strong> s<strong>and</strong>y loams except very fine s<strong>and</strong>y loam .<br />
moderately fine texture : Consisting predominantly <strong>of</strong> intermediate-sized soil particles with or without smal l<br />
amounts <strong>of</strong> fine or coarse particles . In soil textural classification, it includes clay loam, s<strong>and</strong>y clay loam ,<br />
<strong>and</strong> silty clay loam .<br />
moraine (glacial till) : The materials transported beneath, beside, on, within <strong>and</strong> in front <strong>of</strong> a glacier ;<br />
deposited directly from <strong>the</strong> glacier <strong>and</strong> not modified by any intermediate agent .<br />
morphology, soil : (i) The physical constitution, particularly <strong>the</strong> structural properties, <strong>of</strong> a soil pr<strong>of</strong>ile a s<br />
exhibited by <strong>the</strong> kinds, thickness, <strong>and</strong> arrangement <strong>of</strong> <strong>the</strong> horizons in <strong>the</strong> pr<strong>of</strong>ile, <strong>and</strong> by <strong>the</strong> texture ,<br />
structure, consistence, <strong>and</strong> porosity <strong>of</strong> each horizon . (ii) The structural characteristics <strong>of</strong> <strong>the</strong> soil or any o f<br />
its parts .<br />
mottles : Spots or blotches <strong>of</strong> different colour or shades <strong>of</strong> colour interspersed with <strong>the</strong> dominant colour . The y<br />
are described in terms <strong>of</strong> abundance (few, common, many), size, (fine, medium, coarse) <strong>and</strong> contras t<br />
(faint, distinct, prominent) . Mottling in soils indicates poor aeration <strong>and</strong> lack <strong>of</strong> good drainage .<br />
mottling : Formation or presence <strong>of</strong> mottles in <strong>the</strong> soil .<br />
mull : A zoogenous forest humus form consisting <strong>of</strong> an intimate mixture <strong>of</strong> well-humified organic matter an d<br />
mineral soil that makes a gradual transition to <strong>the</strong> horizon underneath . It is distinguished by its crumb o r<br />
granular structure, <strong>and</strong> because <strong>of</strong> <strong>the</strong> activity <strong>of</strong> <strong>the</strong> burrowing micr<strong>of</strong>auna, partly decomposed organi c<br />
debris does not accumulate as a distinct layer (F layer) as in mor <strong>and</strong> moder .<br />
Munsell colour system : A colour designation system specifying <strong>the</strong> relative degrees <strong>of</strong> <strong>the</strong> three simpl e<br />
variables <strong>of</strong> colour : hue, value, <strong>and</strong> chroma .<br />
order, soil : The highest category in <strong>the</strong> Canadian system <strong>of</strong> soil classification . All <strong>the</strong> soils <strong>of</strong> <strong>Canada</strong> have<br />
been divided into nine orders : Chernozemic, Solonetzic, Luvisolic, Podzolic, Brunisolic, Regosolic ,<br />
Gleysolic, Organic, <strong>and</strong> Cryosolic . All <strong>the</strong> soils within an order have one or more characteristics i n<br />
common .<br />
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