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Hydraulic conductivity of remolded fine-grained soils versus index properties

机译:重塑细粒土的水力传导率与指数特性

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Hydraulic conductivity is a dominant parameter in the design of engineered waste disposal facilities such as landfill liners and covers, lagoon liners and slurry walls. It is of interest to a geotechnical or geo-environmental engineer to develop a predictive method of determining the hydraulic conductivity of fine-grained soils, in order to assess its suitability as a liner material. To predict the hydraulic conductivity of soils, researchers and geotechnical engineers have attempted to correlate it with index properties of the soils, such as the liquid limit, void ratio and specific surface. Based on the present study a predictive method has been developed in this paper to predict the hydraulic conductivity in terms of void ratio and shrinkage index (Liquid limit - shrinkage limit) for remoulded fine-grained soils. Though the initial conditions for the soil will affect the hydraulic conductivity behaviour to some extent, both the void ratio and soil characteristics are primary factors in affecting the hydraulic conductivity. Therefore for predictive purpose, the study of hydraulic conductivity behaviour of remoulded fine-grained soils as presented in this paper can be found to be useful for compacted soils also.
机译:在设计的废物处理设施(例如垃圾填埋场衬里和覆盖物,泻湖衬里和泥浆墙)的设计中,水力传导率是一个主要参数。对于岩土工程或地球环境工程师来说,开发一种预测方法来确定细粒土壤的水力传导率,以评估其作为衬砌材料的适用性,对岩土工程或地球环境工程师来说很有意义。为了预测土壤的水力传导率,研究人员和岩土工程师已尝试将其与土壤的指数特性(例如液体极限,孔隙率和比表面积)相关联。基于目前的研究,本文开发了一种预测方法,用于以重塑细粒土壤的孔隙率和收缩指数(液体极限-收缩极限)来预测水力传导率。尽管土壤的初始条件会在一定程度上影响水力传导性,但空洞率和土壤特性都是影响水力传导性的主要因素。因此,出于预测目的,如本文所述,对重塑细粒土的水力传导行为的研究也可用于压实土。

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