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Depositional and geotechnical properties of marine clays in Lianyungang, China

机译:连云港海相粘土的沉积和岩土特性

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摘要

The mineralogy, geochemistry and geotechnical properties of clay samples in Lianyungang, China are presented. The correlations of depositional history, depositional environmental and geotechnical properties are discussed. A series of X-ray diffraction tests show that the principal clay minerals of the soil are illite–smectitemixed-layer mineral and illite. The geochemistry investigation results indicate that the pore water of the Lianyungang marine clay is dominant by sodium. The pH of the soils varies in the range of 7.8 to 8.9. The depositional environment is oxidation condition. The correlations of the geochemistry with the geotechnical properties are examined by the statistic analysis.
机译:介绍了连云港市粘土样品的矿物学,地球化学和岩土工程特性。讨论了沉积历史,沉积环境和岩土性质之间的关系。一系列的X射线衍射测试表明,土壤的主要粘土矿物是伊利石-蒙脱石混合层矿物和伊利石。地球化学调查结果表明,连云港海相粘土的孔隙水以钠为主。土壤的pH值在7.8至8.9之间变化。沉积环境是氧化条件。通过统计分析检查了地球化学与岩土属性的相关性。

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