The biogeochemical cycling and chemical transformation of Se in Chinese env
ironments is reviewed, especially with regard to the formation of low-Se en
vironments. The occurrence, distribution, concentration and flux of Se in C
hinese environments are reported in comparison to those in the rest of the
world. Low-Se regions in China can be classified into 4 categories. In the
NE, organic matter in the soil affects bioavailability of Se in soil. In th
e Huabei plain, the concentration of soil Se is strongly influenced by leac
hing acid hydrological transport processes and Se deficient regions are mos
tly located on the hill-slopes due to leaching. In the Loessial Plateau, lo
w-Se soils have developed on the low-Se parent material with a very low flu
x of Se between soil and plants. Low-Se regions in the SW have soils derive
d from weathered materials of lower Se contents. Both the lowest and highes
t concentrations and the Aux of Se in environments are reported For China.
(C) 2001 Elsevier Science Ltd. All rights reserved.