The results of studies of the mineralogical composition, specific surface,
porosity, heat of adsorption, and the surface energy status are presented f
or three types of soils in China (Latosol, Red Earth (Krasnozem), and Yello
w-Brown Earth). A complex of physical methods (X-ray diffractometry, Mossba
uer spectroscopy, magnetic measurements, mercury porosimetry, etc.) was use
d. These soils are specified by a high content of nonsilicate crystalline i
ron oxide compounds. All soils contain hematite and goethite in clay fracti
ons. The content of iron oxides and the hematite/(hematite and goethite) ra
tio decrease in the following sequence: Latosol, Red Earth, and Yellow-Brow
n Earth.