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Hydraulic conductivity of naturally sedimented and reconstituted clays interpreted from consolidation tests

机译:自然沉积和重构粘土的液压导电性解释于固结试验

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摘要

The hydraulic conductivity of naturally sedimented and reconstituted clays is often interpreted using the settlement-time curves measured from consolidation tests. Understanding the accuracy of the interpreted hydraulic conductivity is essential in geological and geotechnical engineering. To the best knowledge of the authors, such a work has been little reported up to now. This study aims at investigating the errors of the interpreted hydraulic conductivity via the comparison between the interpreted values and the measurements. The ratios of the interpreted values of hydraulic conductivity over the measurements are examined based on the data from the consolidation-hydraulic conductivity tests performed in this study in conjunction with those published by our research team. The investigated clays cover wide geological origins and depositional states. The geological origins and depositional states are linked with the errors of the interpreted hydraulic conductivity for understanding the roles of these factors in the uncertainty of the interpreted hydraulic conductivity. The causes responsible for the discrepancy in hydraulic conductivity between the interpretations and the measurements are identified. The probability distribution of the errors of the interpreted hydraulic conductivity is also investigated.
机译:通常使用从固结试验中测量的沉降时间曲线来解释天然沉淀和重构粘土的液压导电性。了解地质和岩土工程中解释的液压导电性的准确性。为了提名的最佳知识,这项工作已经很少报告到现在。本研究旨在通过对解释值与测量的比较来研究解释的液压导电性的误差。根据本研究中的整合 - 液压导电性试验的数据,与我们的研究团队发布的那些,基于来自本研究中的固结 - 液压导电性试验的数据进行了解释值的液压导电性值。调查的粘土覆盖了广泛的地质来源和沉积状态。地质来源和沉积状态与解释的水力传导率的误差相关联,以了解这些因素在解释的液压导电性不确定性中的作用。鉴定了对解释与测量之间的液压导电性差异负责的原因。还研究了解释的液压导电误差的概率分布。

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