Lithologic characterization of Iguosa erosion site using geoelectrical techniques

D. Egbo, O. J. Airen
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Abstract

Considering the devastating menace of gully erosion for which lithology is one amongst several other agents that drives soil loss and gully erosion, Vertical Electrical Sounding (VES) and Electrical Resistivity (ERT) techniques were adopted to investigate subsurface lithology in Iguosa gully erosion site. PASI 16GL model resistivity meter was used in acquiring data for VES and ERT in the area under investigation. VES data acquired were processed both qualitatively and quantitatively, and geoelectric sections were generated using AUTOCAD software by combination of two or more interpreted VES results along a profile. ERT data were processed using Res2dinv software to an inverse model resistivity section. The geoelectric image generated were interpreted to obtain lithology of the subsurface. The analysis and interpretation of the subsurface image reveals presence of topsoil, sand, dry sand, clayey sand and coarse sand. The subsurface lithology within the study location is predominantly sandy. The result obtained from the resistivity of all profiles shows that erodibility increases with depth within this study area with corresponding high resistivity values. Due to the fact that sand within the study area is loose coarse and silty, which can give rise to high resistivity and causes erosion.
利用地电技术对Iguosa侵蚀场地进行岩性表征
考虑到沟槽侵蚀的破坏性威胁,岩性是导致土壤流失和沟槽侵蚀的其他因素之一,采用垂直电测深(VES)和电阻率(ERT)技术对Iguosa沟槽侵蚀场地的地下岩性进行了研究。利用PASI 16GL模型电阻率仪在调查区采集了地震电磁法和ERT数据。对采集的VES数据进行定性和定量处理,并利用AUTOCAD软件将两条或多条解释的VES结果结合在一起生成地电剖面。利用Res2dinv软件对ERT数据进行处理,得到电阻率反演模型剖面。对生成的地电图像进行解译,得到地下岩性。对地下图像的分析和解释揭示了表土、砂、干砂、粘土砂和粗砂的存在。研究区内地下岩性以砂质为主。所有剖面的电阻率结果表明,在研究区内,可蚀性随深度增加而增加,相应的电阻率值较高。由于研究区内砂质疏松、粗、粉质,易产生高电阻率,易造成侵蚀。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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