-
secondary carbonates starting within 70 cm of the
mineral soil surface.
Kastanozems are
found in
relatively dry
zones with 200 to 450 mm of
rainfall a year...
-
Cambisols Chernozems Ferralsols Fluvisols Gleysols Greyzems Histosols Kastanozems Lithosols Luvisols Nitosols Phaeozems Planosols Podzols Podzoluvisols...
-
Canadian WRB
United States Chernozemic Kastanozem, Chernozem,
Phaeozem Mollisol Brown Chernozem Kastanozem (Aridic)
Aridic Mollisol subgroups (Xerolls...
- Base for Soil
Resources (WRB),
Mollisols are
split up into Chernozems,
Kastanozems and Phaeozems.
Shallow or
gravelly Mollisols may
belong to the Leptosols...
-
Ferralsols G :
Gleysols H :
Phaeozems I :
Lithosols J :
Fluvisols K :
Kastanozems L :
Luvisols M :
Greyzems N :
Nitosols O :
Histosols P :
Podzols Q :...
- Solontsі.
Solonetz zones are ****ociated with Gleysols,
Solonchaks and
Kastanozems. In USDA soil taxonomy,
Solonetz corresponds to sodium-rich Alfisols...
- Resources,
rendzina soils would be
classified as leptosols, chernozems,
kastanozems, or phaeozems,
depending on
their specific characteristics. Rendzina...
-
counterpart of
comparable soils with a high base
saturation (Chernozems,
Kastanozems and Phaeozems).
Umbrisols develop in
weathering material of siliceous...
-
Chernozem (very dark and well-structured topsoil,
secondary carbonates) KS
Kastanozem (dark topsoil,
secondary carbonates) PH
Phaeozem (dark topsoil, no secondary...
- of the 28
groups in the 1988
revised version.
Along with chernozems,
kastanozems, and phaeozems,
these four soil
groups form a set of soil
groups that...
