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Hydrogeological investigations in a low permeability claystone formation: the Mont Terri Rock Laboratory

机译:低渗透性粘土岩地层的水文地质调查:蒙特泰里岩石实验室

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摘要

This paper addresses the achievements in understanding the hydrogeological conditions in the low permeability claystone formation of the Opalinus Clay at the Mont Terri Rock Laboratory. The synthesis work consisted of (i) an assessment of clay-specific artifacts which may affect the interpretation of hydraulic tests, (ii) a survey of hydraulic rock properties such as hydraulic conductivity and storage coefficient, and (iii) an assessment of the governing flow laws and definition of hydrogeological units and flow boundaries on the site scale. Drawing on the broad hydrogeological data base, confidence is gained in the hydraulic barrier function of the Opalinus Clay, which effectively prevents groundwater flow between the over- and underlying aquifer systems.
机译:本文阐述了在蒙特Terri岩石实验室了解Opalinus粘土的低渗透性粘土岩层中的水文地质条件方面取得的成就。合成工作包括(i)评估可能会影响水力试验解释的粘土特有制品,(ii)对水力岩石特性(例如水力传导率和储水系数)的调查,以及(iii)流量定律以及现场规模的水文地质单位和流量边界的定义。利用广泛的水文地质数据库,人们对Opalinus粘土的水力屏障功能有了信心,这可以有效地防止地下水在上层和下层含水层系统之间流动。

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