用温纳-斯伦贝谢构造地电法估算坡卡冲积平原物质的电阻率

Andrias Izaac Latupapua, Fahrul Dadan Tahapary, Rudy Soplanit
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摘要

本研究采用温纳-斯伦贝谢配置电极,确定了Poka冲积平原上材料电阻率值的横向和垂直分布。测绘在2条线上进行,每条线长120米,最小间距为10米。结果表明:材料的电阻率范围为48.8 Ωm ~ 2.247 Ωm,横向分布深度达26.2 m;上层为松散砂质层,中层为冲积层和砂层,下层为无承压含水层砂层和水层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Estimation of Resistivity of Poka Alluvial Plain Material by Geoelectric Method with Wenner-Schlumberger Configuration
This study was conducted to determine the lateral and vertical distribution of material resistivity values on Poka alluvial plain using electrodes with Wenner-Schlumberger configuration. Mapping is carried out on 2 lines each 120 m long with the smallest space of 10 m. The results showed that the resistivity of the material ranged from 48.8 Ωm to 2.247 Ωm spread laterally with a depth of up to 26.2 m. Loose Sand material occupies the upper layer, followed by the Alluvium and Sand layers in the middle, and Sand and Water which are unconfined aquifers in the lower layer.
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