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Lateritic Soils

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Lateritic Soils 

soils of equatorial and tropical rain forests, characterized by low silica content, high aluminum and iron content, insignificant content of alkalies and alkaline earths, acid reaction, and low cation and high anion absorptive capacity. Since the late 1950’s lateritic soils have more often been referred to as ferralitic soils, and the term “lateritic” has been used for soils that have a horizon of laterite in their profile.



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1c) showed loamy sand and sandy loam A horizons over B horizons typical of lateritic soils, which texture as sandy-loam to sandy clay loam when finely ground but in their native state are cemented with sesquioxides and contain dense ironstone gravel layers (>60% v/v) at the upper margin of the B horizon.
The natural fertility of the leached lateritic soils and deep aeolian sands, on which most P.
Zones identified in the paleosol are similar to those of lateritic soils that develop mostly in tropical climates.
 
 
 
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