Abstract
Two profiles of weakly podzolised, well drained soils of abraded moraine plains in northwestern Russia are studied. The profiles are located at the edges and on the upper parts of slopes. They are developed upon two-layered rocks: stony sand-sandy loam deposite of complex genesis, underlain with reddish brown bouldery moraine loam. This determines a clear differentiation of the profile in terms of particle size distribution and bulk chemical composition, and also in terms of the mineralogical composition of the clay fraction.
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