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illuvial horizon

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illuvial horizon [i′lü·vē·əl hə′rīz·ən]
(geology)


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Clay illuviation This process consists in the translocation of claysize particles from eluvial (A, E) to illuvial horizons (mainly Bt, and to a lesser degree, in BA or BC horizons).
A micromorphological comparison of the horizons (Reuter 1964b) proved that the obvious polygenesis can certainly not be a transformation of BrownEarth into Lessive as some other authors have assumed: in the argillic illuvial horizon the clay and silt particles are 90% strongly dispersed.
The interval from 66-112 cm is also now part of the BC horizon of the surface soil and an illuvial horizon (B'X) of the fragipan.
 
 
 
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