Clay Minerals in Quaternary Clayey Soil and Its Relation to the Land Subsidencein Kunming Basin Area
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P57; P642.26

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    Abstract:

    Based on X-ray diffraction and scanning electron microscopic analyses of Quaternary clayey soil from Kunming basin area, the authors have extensively studied the combination, mineralogy and micro-textures of the clay minerals, and discussed the relationship between the clay minerals and the land subsidence under the overdraft of the groundwater which may alter the combination, micro-textures and physicochemical conditions of the clay minerals. The results show that, under the same condition, the content, mineral combination and micro-textures of the clay minerals play most important roles in leading to land subsidence.

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薛传东,谈树成,李 峰,刘 星,秦德先,2001,昆明盆区第四系粘性土中的粘土矿物与地面沉降[J].岩石矿物学杂志,20(4):437~440. XUE Chuan-dong, TAN Shu-cheng, LI Feng, LIU Xing, QIN De-xian ,2001,Clay Minerals in Quaternary Clayey Soil and Its Relation to the Land Subsidencein Kunming Basin Area[J]. Acta Petrologica et Mineralogica,20(4):437~440.

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  • Revised:May 16,2001
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