TRANSFORMATION OF MICA TO HIGH-CHARGE SMECTITE, DEPENDING ON THE PARTICLE SIZE, IN A YELLOW-BROWN SOIL OF CHINA
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Clay mineralogical composition of a Yellow-brown soil of China was examined. Common to the A and C horizons, micas and their transformation products dominated the clay fraction. The transformation products of micas were, however, different between the fine (<0.2μm) and coarse (0.2-2μm) clay fractions. Irregularly interstratified mica/smectite or mica/vermiculite/smectite of the smectite-rich phase was found in the fine clay fraction, while smectite and regularly interstratified mica/smectite were detected in the coarse clay fraction. The endo-type and exo-type K-replacement models were proposed to explain the different transformation products between the two clay fractions.
- 日本粘土学会の論文
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