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Estimation of Physical Properties of Reclaimed Ground with coal ash using Resistivity, IP, and Micro-gravity Surveys

机译:使用电阻率,IP和微重量调查估算煤灰煤灰的物理性质

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摘要

It has been conventionally difficult to estimate the physical properties of inhomogeneous grounds such as the reclaimed ground that consists of several kinds of coal ash by means of geophysical surveys. By laboratory test using artificial samples, we confirmed that resistivity of the ground was related to saturation. We also confirmed that IP was measured at the ground composed of much ignition loss rate. Physical tests of the samples showed that porosity and water content were related to unconfined compressive strength due to ignition loss rate. Based on these relationships, we demonstrate a flowchart to derive physical properties by combining resistivity, IP and micro-gravity survey data. Then, we have carried out these surveys in a area of 62 m X 30 m at a reclaimed site with coal ash, which contains two areas reclaimed by different operation methods. To estimate conductivity of pore water, specific gravity, and water content, several samples were collected from the survey area. We calculate water-saturation, porosity, and compressive strength profiles in the survey area using the flowchart. As a result, we can classify two reclaimed areas by these physical profiles. The compressive strength profiles roughly matched the dynamic strength estimated from N-values by the penetration tests within the area. These profiles can help us to estimate the distribution of compressive strength for reclaimed grounds.
机译:通常难以估计不均匀理由的物理性质,例如通过地球物理调查由几种煤灰组成的再生地面。通过使用人造样品的实验室测试,我们证实了地面的电阻率与饱和度有关。我们还确认IP在地面上测量,由较大的点火损失率组成。样品的物理测试表明,由于点火损失率,孔隙率和水含量与未缠绕的抗压强度有关。基于这些关系,我们通过组合电阻率,IP和微重量调查数据来证明流程图以导出物理性质。然后,我们在具有煤灰的回收位点在62米×30米的区域进行了这些调查,其中包含由不同操作方法再生的两个区域。为了估算孔隙水,比重和含水量的电导率,从调查区域收集了几种样品。我们使用流程图计算测量区域中的水饱和度,孔隙度和压缩强度曲线。因此,我们可以通过这些物理配置文件分类两个再生区域。压缩强度曲线大致匹配了该区域内的渗透试验从n值估计的动态强度。这些简档可以帮助我们估算再生地面的压缩强度分布。

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