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- W2382271377 abstract "The Xigeda soil is made up of silty loam and silt soil in Panzhihua region, Minerals of which are mainly quartz and plagioclase with clay minerals, montmorillonite, illite and kaolinite. That the REE patterns are similar in different soil layers suggests that REE should be inactive during the pedogenesis. The trace elements, such as Ti, V, Cr, Ni, Cu, Zn, Pb, As and Cd, have high geochemical background contents in the Xigeda soil and are mainly concentrated in the top soil in Panzhihua region. Some elements may be released and pollute the environment while the water leaches the soil. the stability of the Xigeda soil is very weak, which would be easy to induce geological disasters." @default.
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- W2382271377 date "2002-01-01" @default.
- W2382271377 modified "2023-09-28" @default.
- W2382271377 title "PEDOLOGICAL ENVIRONMENTAL GEOCHEMISTRY OF XIGEDA SOIL IN PANZHIHUA REGION" @default.
- W2382271377 hasPublicationYear "2002" @default.
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