首页> 外文期刊>Journal of Geoscience and Environment Protection >Comparison of Thickness and Depth Resolution Power of Wenner and Schlumberger Arrays: A Case Study of Temidire Quarters, Akure, Nigeria
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Comparison of Thickness and Depth Resolution Power of Wenner and Schlumberger Arrays: A Case Study of Temidire Quarters, Akure, Nigeria

机译:Wenner和Schlumberger阵列厚度和深度分辨率的比较 - 以尼日利亚策略季度,Akure

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摘要

An electrical resistivity sounding investigation was carried out within the vicinity of some hand dug wells at Temidire Quarters in Akure, Ondo State, Nigeria. The aim of this study was to compare depth and thickness resolution power of Schlumberger and Wenner arrays. The investigation involved twenty-four vertical electrical soundings (VES) which consisted of twelve Schlumberger array VES and twelve Wenner array VES. The VES results delineated geoelectric layers beneath each VES locations, their layer resistivities, layer thicknesses and depth to aquifer layer(s). Depth to aquifer layer was also determined from static water level measurement and this aided the aquifer layer delineation from VES results. The geoelectric sounding results showed that the study area is dominated by a KH-curve type which consists of top soil, clay/weathered layer, fractured basement and fresh basement. Results from both Schlumberger and Wenner array data were correlated with the static water level measurement; Schlumberger array was found to have higher correlation value than Wenner array.
机译:在尼日利亚的Akure,尼日利亚州伊达尔州的牡丹宿煤附近,在尼日利亚州的一些手挖井附近进行电阻率调查调查。本研究的目的是比较Schlumberger和Wenner阵列的深度和厚度分辨率。调查涉及二十四个垂直电气探测(VES),它由十二个钢板阵列VES和12个Wenner阵列Ves组成。 VES结果将每个VES位置,其层电阻,层厚度和深度描绘出电气电层,其层厚度和深度至含水层。对含水层层的深度也从静态水位测量确定,并且这辅助从VES结果中描绘含水层层。电气发声结果表明,研究区由KH曲线型占主导地位,该曲线型由顶部土壤,粘土/风化层,裂缝地下室和新鲜地下室组成。 Schlumberger和Wenner阵列数据的结果与静态水位测量相关;发现舒尔伯达阵列与Wenner阵列具有更高的相关值。

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