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Preliminary Groundwater Assessment using Electrical Method at Quaternary Deposits Area

机译:初步地下水评估在第四季沉积区

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Alternative water sources using groundwater has increasingly demand in recent years. In the past, proper and systematic study of groundwater potential was varies due to several constraints. Conventionally, tube well point was drilled based on subjective judgment of several parties which may lead to the uncertainties of the project success. Hence, this study performed an electrical method to investigate the groundwater potential at quaternary deposits area particularly using resistivity and induced polarization technique. Electrical method was performed using ABEM SAS4000 equipment based on pole dipole array and 2.5 m electrode spacing. Resistivity raw data was analyzed using RES2DINV software. It was found that groundwater was able to be detected based on resistivity and chargeability values which varied at 10 - 100 Qm and 0-lms respectively. Moreover, suitable location of tube well was able to be proposed which located at 80 m from the first survey electrode in west direction. Verification of both electrical results with established references has shown some good agreement thus able to convince the result reliability. Hence, the establishment of electrical method in preliminary groundwater assessment was able to assist several parties in term groundwater prospective at study area which efficient in term of cost, time, data coverage and sustainability.
机译:近年来,使用地下水的替代水源越来越多。过去,由于若干约束,对地下水潜力的适当和系统的研究变化。传统上,基于若干各方的主观判断,钻探管阱点,这可能导致项目成功的不确定性。因此,该研究进行了一种电气方法,以研究季沉积区域的地下水电位,特别是使用电阻率和诱导的极化技术。使用基于极偶极阵列和2.5M电极间距的ABEM SAS4000设备进行电气方法。使用Res2dinv软件分析电阻率原始数据。发现可以基于在10-100 QM和0-LMS在10-100 QM和0-LMS中变化的电阻率和带电值来检测地下水。而且,能够提出管孔的合适位置,该位置位于西方方向的第一测量电极的80米处。通过建立的参考的电气结果验证已经显示出一些良好的协议,从而能够说服结果可靠性。因此,在初步地下水评估中建立电气方法,能够在学习区域提供若干方面的地下水预期,其成本,时间,数据覆盖率和可持续性有效。

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