Mapping of Water Resistivity Using Pool Water
- 作者: Shevnin V.A.1, Matveychuk D.I.1, Dernova A.S.1
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隶属关系:
- Department of Geology, Moscow State University
- 期: 卷 74, 编号 6 (2019)
- 页面: 613-615
- 栏目: Short Communications
- URL: https://journal-vniispk.ru/0145-8752/article/view/175127
- DOI: https://doi.org/10.3103/S0145875219060085
- ID: 175127
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详细
The relationship between the resistivity (conductivity) of soil and that of pore water was stated in papers by G.E. Archie and V.N. Dakhnov. This means that water resistivity should be studied at each fieldwork area. In some areas, however, the access to groundwater (boreholes, wells, and springs) as well as to the surface reservoirs (rivers, brooks, ponds, and lakes) is not possible or is restricted. Can we measure water resistivity in pools? Immediately after a rain such water has no relationship with soil resistivity. The purpose of this work was to study the pattern of ion exchange between soil and rain water over time. In (Brunet et al., 2010) the changes in resistivity of water in contact with soil over time were measured. We have verified their results.
作者简介
V. Shevnin
Department of Geology, Moscow State University
编辑信件的主要联系方式.
Email: shevninvlad@yandex.ru
俄罗斯联邦, Moscow, 119991
D. Matveychuk
Department of Geology, Moscow State University
编辑信件的主要联系方式.
Email: matiw1998@mail.ru
俄罗斯联邦, Moscow, 119991
A. Dernova
Department of Geology, Moscow State University
编辑信件的主要联系方式.
Email: azya98@yandex.ru
俄罗斯联邦, Moscow, 119991
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