基于微量元素统计方法的土壤导电路径研究

Zude Lu, Yaozheng Ji, Xiaobin Cao, Qiheng Ma, Tao Li, Ruifang Li
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摘要

土壤电导率将直接决定接地系统的稳定性,在相同的接地电阻下,由于不同地区土壤电阻率的差异,接地系统的成本将相差高达100倍。土壤作为多孔介质,固体矿物颗粒之间存在大量孔隙,离子可以通过孔隙水形成的通道迁移,从而形成电流。已有研究发现,土壤的电阻率会随着含水量的变化而不断变化,并且存在突变现象,但考虑到土壤水电导率最高,因此只能猜测突变原因是水分分布的连通性造成的。本文利用MATLAB软件编写程序建立土壤分形模型,然后利用ANSYS仿真软件进行求解,从而分析土壤的电导率模型,并统计分析土壤中水分微量元素的表观电导率,研究其在土壤模型中的分布。进一步研究突变前后不同时间土壤电阻率的连通性,统计土壤传导路径中所含细胞数。通过控制土壤含水量参数的变化,研究了土壤模型各柱土壤传导路径中细胞数的分布。结果发现,随着土壤含水量的增加,各柱细胞数分布范围增大,数值波动幅度明显减小。因此,引入均值和方差来分析数据的变化规律。在此基础上,可以通过改变孔隙度的大小来研究孔隙度对土壤导电路径的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study on soil conductive path based on micro-element statistical method
Soil conductivity will directly determine the stability of grounding system, and the cost of grounding system will vary up to 100 times due to the difference of soil resistivity in different areas under the same grounding resistance. Soil, as a porous medium, has a large number of pores between solid mineral particles, and ions can migrate through the channels formed by pore water, thus forming electric currents. Existing studies have found that the resistivity of the soil will change constantly with the change of water content, and there is a mutation phenomenon, but considering the soil water conductivity is highest, so can only guess at mutation reason is caused by the connectivity of water distribution. In this paper, MATLAB software was used to write a program to establish a soil fractal model, and then ANSYS simulation software was used to solve the problem, so as to analyze the conductivity of the soil model, and statistical analysis of the apparent conductivity of water micro-element in the soil and study its distribution in the soil model. In addition, the connectivity of soil resistivity at different times before and after the mutation was further studied and the number of cells contained in the conduction path of soil was counted. By controlling the variation of soil water content parameter, the distribution of cell number in soil conduction path in each column of soil model was studied. It was found that with the increase of soil water content, the distribution range of cell number in each column increased, and the fluctuation of numerical value decreased significantly. Therefore, the mean value and variance were introduced to analyze the variation rule of data. On the basis of this study, the influence of porosity on soil conductive path can be studied by changing the size of porosity.
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