HYDROGEOLOGIC INVESTIGATION USING VERTICAL ELECTRICAL SOUNDING METHOD IN AGBARHA OTOR, DELTA STATE NIGERIA

E. Atakpo, Merrious Oviri Ofomola
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Abstract

Vertical resistivity sounding measurements were conducted at fifteen(15) locations in Agbarha-otor in Ughelli North Local Government Area in Delta State using Schlumberger electrode configuration. The field data where interpreted qualitatively as well as quantitatively. Five basic geoelectric layers were delineated in the area such as topsoil, laterite, fine sand and medium-coarse grain sand with resistivity ranging from 257- 3873!m, 479-3022!m, 519-3071!m and 1137-3735!m and a depth ranging from 0.6-1.5m, 3.8-9.5m, 11.6-51.6m respectively. The result of the study shows that, at a depth of 5.1-51.6m lies the aquifer in the area with resistivity ranging from 990-3071!m and the thickness of the aquifer in the area was observed to be between 9.1-47m. The NE part of the region is prone to contamination from human activity such as landfill as a result of the shallow depth to the top of the aquifer. Portable water can be obtained from VES8 and VES9 in NE-SW direction of the study area due to aquifer thickness of 47m and 43m respectively.
垂直电测深法在尼日利亚三角洲州agbarha otor的水文地质调查
利用斯伦贝谢的电极配置,在三角洲州Ughelli北部地方政府区的Agbarha-otor的15个地点进行了垂直电阻率测深测量。现场数据进行了定性和定量解释。在该地区圈定了表层土、红土、细砂、中粗粒砂等5个基本地电层,电阻率范围为257 ~ 3873!米,479 - 3022 !米,519 - 3071 !M和1137-3735!M,深度分别为0.6-1.5m、3.8-9.5m、11.6-51.6m。研究结果表明,在5.1 ~ 51.6m深度处存在含水层,其电阻率范围为990 ~ 3071!M,观测到该地区含水层厚度在9.1 ~ 47m之间。该地区的东北部容易受到人类活动的污染,例如填埋,这是由于含水层顶部的深度较浅。由于含水层厚度分别为47m和43m, VES8和VES9在研究区NE-SW方向可获得可采水。
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