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Evidence of localised gas propagation pathways in a field-scale bentonite engineered barrier system: results from three gas injection tests in the large scale gas injection test (Lasgit)

机译:现场气体膨润土工程屏障系统中局部气体传播途径的证据:大规模气体注入试验(Lasgit)中三次气体注入试验的结果

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摘要

Three gas injection tests have been conducted during a large scale gas injection test (Lasgit) performed at the Äspö Hard Rock Laboratory, Sweden. Lasgit is a full-scale experiment based on the Swedish KBS-3 repository concept, examining the processes controlling gas and water flow in highly water-saturated compact buffer bentonite. Three preliminary gas injection tests have been performed. The first two tests were conducted in the lower array of injection filters (FL903). Both of these tests showed similar behaviour that corresponded with laboratory observations. The third gas test was conducted in an upper array filter (FU910), which gave a subtly dissimilar response at major gas entry with an initial pressure drop followed by a secondary gas peak pressure. Lasgit has confirmed the coupling between gas, stress and pore-water pressure for flow before and after major gas entry at the field scale. All observations suggest mechanisms of pathway propagation and dilatancy predominate. In all three gas tests the propagation was through localised features that tended to exploit the interface between the copper canister and the bentonite buffer. Considerable evidence exists for the development of a highly-dynamic, tortuous network of pressure induced pathways which evolves both temporally and geospatially within the clay, opening and closing probably due to local changes in gas pressure and or effective stress.
机译:在瑞典ÄspöHard Rock实验室进行的大规模注气测试(Lasgit)期间,进行了三项注气测试。 Lasgit是一项基于瑞典KBS-3储存库概念的大规模实验,研究了在高度水饱和的紧凑型缓冲膨润土中控制气体和水流的过程。已经进行了三个初步的气体注入测试。前两个测试是在下部的注入过滤器(FL903)中进行的。这两个测试均显示出与实验室观察到的相似的行为。第三次气体测试是在上部阵列过滤器(FU910)中进行的,该过滤器在主要气体进入时给出了略微不同的响应,其初始压降随后为次要气体峰值压力。拉斯吉特(Lasgit)已在田间尺度上确定了主要气体进入之前和之后的气体,应力和孔隙水压力之间的耦合关系。所有观察表明,途径传播和扩张性的机制占主导。在所有三个气体测试中,扩散都是通过局部特征进行的,这些局部特征倾向于利用铜罐和膨润土缓冲液之间的界面。存在大量证据表明,压力诱导路径的高度动态,曲折网络的发展在粘土内随时间和地理空间在演化,可能由于气压和/或有效应力的局部变化而打开和关闭。

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