垂直电测深测定尼日利亚西南部奥尼耶Adumasun地区裂缝分布

T. Adagunodo, L. Sunmonu, O. Oladejo, I. A. Ojoawo
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引用次数: 16

摘要

居住在尼日利亚西南部伊巴丹的人们已经开始将他们的重点转移到靠近大都市的村庄建造房屋。因此,必须进行这项研究,以便在时机成熟时建议在尼日利亚西南部奥尼耶Adumasun地区建立的结构类型,以避免此后可能发生的灾难性失败。本研究的目的是在尼日利亚西南部奥尼耶的Adumasun地区进行垂直电测深地球物理测量,以确定研究区内的裂缝分布。研究区位于北纬070 37′55.37″~ 070 38′00″,东经0030 11′10.2″~ 0030 11′16.8″之间。采用斯伦贝谢电极阵列进行研究,采用r50电阻率仪进行数据采集。地电测量包括10次深度探测,最大电流电极间距(AB)为200m。a型曲线占40%,h型曲线占50%,kh型曲线占10%。测深曲线的地电剖面分别显示3层和4层地球模型。模型显示,次表层分为表土、第二层和第三层(它存在的地方)。研究区三分之一为新鲜基岩,三分之二为断裂基岩。建议在基岩新鲜、覆盖层厚度较薄的地区建造高层建筑,在基底断裂、覆盖层厚度较厚的地区建造低层建筑。结论是,研究区域平均胜任高层建筑和低层建筑的建设,这取决于个体建筑商所在的位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vertical Electrical Sounding to Determine Fracture Distribution At Adumasun Area, Oniye, Southwestern Nigeria.
People living in Ibadan, Southwestern Nigeria have started shifting their focus on construction of buildings towards villages that are close to the metropolis. It is therefore imperative to carry out this research in order to recommend the types of structures to be erected at Adumasun area, Oniye, Southwestern Nigeria when the time comes in order to avoid catastrophic failure that might have happened thereafter. The aim of this research is to carry out vertical electrical sounding geophysical survey at Adumasun area, Oniye, Southwestern Nigeria with a view to determining the fracture distribution within the study area. The study area is located between latitude 070 37′ 55.37″ to 070 38′ 00″ North and longitude 0030 11′ 10.2″ to 0030 11′ 16.8″ East. Schlumberger electrode array was employed for the study using R 50 Resistivity meter for the data acquisition. The geoelectric survey comprised of ten depth soundings, with maximum current electrode spacing (AB) of 200m. 40% of the modeled curves are A-type, 50% are H-type, and 10% are KH-type. The geoelectric sections obtained from the sounding curves revealed 3-layer and 4-layer earth models respectively. The models showed that the subsurface layers were categorized into the topsoil, the second layer, and the third layer (where it is present). One-third of the study area showed fresh bedrock while two-third showed fractured bedrock. Areas underlying with fresh bedrock and thin overburden thickness are recommended for the construction of high-rise buildings while areas with fractured basement and thick overburden thickness are recommended for the construction of low-rise buildings. It is concluded that the study area is averagely competent for the construction of high-rise buildings and low-rise buildings depending on where individual builders are located.
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