在尼日利亚的Awka,使用垂直电测深和地磁地球物理技术检查隧道侵蚀

Chibuogwu IU, Ugwu GZ
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引用次数: 0

摘要

本研究利用垂直电测深(VES)和磁地球物理技术研究了尼日利亚Awka地区土壤管道的性质和特征。VES测量使用Pasi电阻率计进行,而地面磁测量使用质子精密磁强计进行。探测结果显示了2到5个不同的地电剖面和14条特征测深曲线,这些曲线表明了地下的垂直变化。研究结果表明,靠近研究区表面的风化土具有促进土管发育的最佳土壤结构。二维等电阻率图显示,土管沿NW-SE方向发育,与研究区应力方向、流体运移路径及泥泞地形一致。地磁测量结果是利用野外产生的日校正异常技术获得的。这一发现表明,低磁化率(-124.4 ~ -300nT)在地下积累,主要集中在西南地区,大部分土壤管道位于该地区。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Examining tunnel erosion using vertical electrical sounding and ground magnetic geophysical techniques in Awka, Nigeria
The present study investigates the nature and characteristics of soil piping using Vertical Electrical Sounding (VES) and Magnetic geophysical techniques at Awka, Nigeria. The VES survey was conducted using a Pasi resistivity meter, while the ground magnetic survey was carried out using a proton precision magnetometer. The VES survey revealed two to five distinct geo-electrical sections and fourteen characteristically sounding curves, which indicate vertical changes in the subsurface. The findings illustrate that the weathered soil in proximity to the surface of the study area has the best soil formations that encourage soil pipe development. Moreover, the iso-resistivity 2D maps demonstrate that the soil pipes describe a direction in the NW-SE, which is consistent with the stress direction, fluid migration paths, and sloppy terrains of the study area. The results of the ground magnetic survey were obtained using a diurnal corrected anomaly technique generated from the field. This finding suggests that low magnetic susceptibility, ranging from -124.4 to -300nT, has accumulated in the subsurface, primarily in the south-western region, where most of the soil pipes are located in the surveyed areas.
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