利用电阻率法进行地下水位的地球物理调查&以阿布扎比大学二期学生宿舍为例

F. Ogbozige, Sadiq Sani
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引用次数: 0

摘要

在尼日利亚扎里亚艾哈迈杜·贝洛大学(ABU)二期新建的两个名为丹格特(Dangote)和谢胡·伊德里斯(Shehu Idris)的宿舍(宿舍)进行了地下水地球物理调查。采用电阻率法的垂直电测深(VES)技术,对分布在两个主体内的七个VES点采用斯伦贝谢阵列。结果表明,研究区域内存在4至6个地电层,电流电极之间的间距最多为200米。所有VES点的地电层电阻率值范围为26.6Ωm–30342Ωm,厚度和深度分别为0.263 m–40.34 m和0.572 m–50.66 m。然而,四个VES点(每个宿舍两个)被确定为适合钻孔,但这四个VESs点中的三个点每个点都有一个含水层,电阻率和厚度范围为34.4Ωm–40.57Ωm和2.02 m–7.49 m。相反,第四个VES点有两个位于第三层和第五层的含水层,电阻率值范围为26.6Ωm–51.4Ωm,厚度范围为1.93 m–18.7 m。建议在确定包含含水层的四个VES点(每个宿舍两个)中,应优先考虑每个宿舍厚度较大的点。
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GEOPHYSICAL INVESTIGATION OF GROUNDWATER POTENTIALS USING RESISTIVITY METHOD: A CASE STUDY OF ABU PHASE II STUDENTS’ HOSTEL
Geophysical survey for groundwater was conducted in two newly built halls of residence (hostels) named Dangote and Shehu Idris at the second phase of Ahmadu Bello University (ABU), Zaria in Nigeria. The vertical electrical sounding (VES) technique of resistivity method was employed with Schlumberger array in seven VES points distributed within the two hostels. Results showed that 4 to 6 geoelectric layers exist within the study area for a spacing of at most 200 m between current electrodes. The resistivity values of the geoelectric layers in all the VES points ranged from 26.6 Ωm – 30342 Ωm while the thickness and depth ranged from 0.263 m – 40.34 m and 0.572 m – 50.66 m respectively. However, four VES points (two in each hostel) were identified to be suitable for borehole drilling though, three out of these four VES points have single aquifer in each with resistivity and thickness ranging from 34.4 Ωm – 40.57 Ωm and 2.02 m – 7.49 m respectively. Conversely, the fourth VES point has two aquifers positioned at the third and fifth layers with resistivity values ranging from 26.6 Ωm – 51.4 Ωm and thickness ranging from 1.93 m – 18.7 m. It was recommended that among the four VES points (two in each hostel) identified to contain aquifers, priority should be given to the ones with larger thickness in each hostel.
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