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eluviation

   Also found in: Financial, Encyclopedia, Wikipedia 0.01 sec.
e·lu·vi·a·tion  (-lv-shn)
n.
The lateral or downward movement of dissolved or suspended material within soil when rainfall exceeds evaporation.


eluviation [ɪˌluːvɪˈeɪʃən]
n
(Earth Sciences / Physical Geography) the process by which material suspended in water is removed from one layer of soil to another by the action of rainfall or chemical decomposition
[from eluvium]

eluviation  (-lv-shn)
The lateral or downward movement of the suspended material in soil through the percolation of water. Eluviation differs from leaching in that it affects suspended, not dissolved, material and usually results only in the movement of the material from one soil horizon to another.


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The SOC flow in the composition of organic matter begins with litter falling on or into the soil, continues with its disintegration, transformation into humus and accumulation, and ultimate disappearance, via consumption by soil organisms, complete mineralization or illuviation into the subsoil, or eluviation out of the soil cover.
0) B brown weathering Be = "earthy" (coagulated fabric), Bl = "loamy" (dispersed fabric) E eluviation of colloids Eg = by gleying, El = by lessivation, Ep = by podzolization I illuviation of colloids Ia = argillic, Ih = humic, If = ferric G ground-water influence Go = oxidative, Gr = reductive P pseudogleying M mother substrate (unweathered), Mw = weakly weathered Two prefixes are used here: p means ploughed, r indicates relict horizons.
Morphological features of clay eluviation, formation of evident clayskins, and presence of argillic properties are still lacking.
 
 
 
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