I. I. Tolpeshta, T. A. Sokolova, E. Bonifacio, G. Falcone
Minerals of the pedogenic chlorite group were studied in the clay fractions
isolated from the mineral horizons of podzolic and gleyic peat-podzolic soils.
In the AE and E horizons of the podzolic soil, pedogenic chlorites are thought
to develop from vermiculite, whereas in the E horizon of the gleyic
peat-podzolic soil, they can be formed from smectite minerals. For estimating
the degree of chlori... hiện toàn bộ