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Soil Resistivity Measurements to Predict Moisture Content and Density in Loose and Dense Soil

机译:土壤电阻率测量以预测松散和致密土壤中的水分含量和密度

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In the past, most of the soil electrical resistivity charts were developed based on stand-alone geomaterial classification with minimal contribution to its relationship to some of geotechnical parameters. Furthermore, the values cited a very wide range of resistivity with sometimes overlapping values and having little significance to specific soil condition. As a result, it created some ambiguities during the interpretation of observations which were traditionally based on qualitative anomaly judgments of experts and experienced people. Hence, this study presents soil resistivity values based on laboratory experiment with a view to predict the soil moisture content and density in loose and dense soils. This study used a soil box and a resistivity meter to test a clayey silt soil, increasing its water usage from 1-3% based on 1500 gram of dry soil. All the moisture contents and density data were observed concurrently with 25 electrical soil resistance observations being made on the soil. All testing and formula used were in accordance with that specified in BS1377 (1990). It was apparent that the soil resistivity value was different under loose (L) and compact (C) condition with moisture content (w) and density (ρ_(bulk)) correlations being established as follows; ρ_((bulk)(C))= 2.5991ρ~(-0.037), ρ_(bulk) (L) = -0.111 ln(ρ) + 1.7605, w(L) = 109.98ρ_(-0.268), and w_(C) = 121.88ρ~(-0.363) with determination coefficients, R~2 that ranged between 0.69 – 0.89. This research therefore contributes a means of predicting these geotechnical parameters by related persons such as geophysicist, engineers and geologist who use these resistivity techniques in ground exploration.
机译:在过去,大多数土壤电阻率图表是基于独立的地质材料分类开发的,其与其与一些地岩土参数的关系贡献最小。此外,该值引用了具有有时重叠值的非常广泛的电阻率,并且对特定土壤条件具有几乎没有意义。因此,它在传统上基于专家和经验丰富的人民的定性异常判决的观察中的观察中创造了一些含糊的歧义。因此,本研究提出了基于实验室实验的土壤电阻率值,以预测松散和致密土壤的土壤含水量和密度。本研究使用了土箱和电阻率计来测试粘土淤泥土壤,基于1500克干燥的土壤增加其水的用量从1-3%。在土壤上同时观察到所有水分含量和密度数据。所使用的所有测试和配方均符合BS1377(1990)中规定的。显然,土壤电阻率值在松散(l)和紧凑型(c)条件下不同,水分含量(w)和密度(ρ_(批量))相关性如下建立; ρ_((批量)(c))=2.5991ρ〜(-0.037),ρ_(散装)(l)= -0.111 ln(ρ)+ 1.7605,w(l)=109.98ρ_( - 0.268),和w_( c)=121.88ρ〜(-0.363),测定系数,R〜2范围在0.69-0.89之间。因此,该研究贡献了通过在地面探索中使用这些电阻率技术的地球物理学家,工程师和地质学家等相关人来预测这些岩土工程学参数的方法。

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