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首页> 外文期刊>International Journal of Scientific & Technology Research >Mining Of Geophysical Data To Predict Groundwater Prospect In A Basement Complex Terrain Of Southwestern Nigeria
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Mining Of Geophysical Data To Predict Groundwater Prospect In A Basement Complex Terrain Of Southwestern Nigeria

机译:尼日利亚西南部地下复杂地形的地球物理数据挖掘以预测地下水前景

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摘要

This study applied the multi criteria decision analysis to geophysical data acquired to achieve an unbiased integration of geoelectric parameters obtained from the results of the interpretation of the geophysical data in the order of their hydrogeologic importance to consequently produce a groundwater prediction model. The geoelectric parameters which were the coefficient of anisotropy, aquifer resistivity, aquifer thickness, overburden thickness and overburden resistivity were the main subsurface factors controlling the flow and accumulation of groundwater resources in the study area. Each parameter was assigned appropriate weight based on Saaty's nine-point scale and the weights were normalized through the Analytic Hierarchy Process (AHP). The assigned weights were adjudged to be consistent and unbiased through the attainment of consistency ratio of less than 10%. The groundwater prediction model of the area was produced from the application of the Groundwater Potential Index (GWPI) model equation developed. The prediction model classified the groundwater potential of the study area into very low; very low ' low; low ' moderate; moderate - high and high - very high classes. The results obtained from this study established that the groundwater prediction model produced from the GWPI obtained from the application of multi criteria decision analysis to subsurface factors is accurate and reliable. It has also proven the ability of the methodology adopted as a good decision making tool in the presence of two or more conflicting criteria. This ability makes it a useful tool that can be adopted in the groundwater prediction domain.
机译:这项研究对获取的地球物理数据应用了多准则决策分析,以实现从地球物理数据解释结果中获得的地电参数的无偏积分(按其水文地质重要性排序),从而生成地下水预测模型。地电参数是各向异性系数,含水层电阻率,含水层厚度,覆盖层厚度和覆盖层电阻率,是控制研究区地下水流动和聚集的主要地下因素。根据Saaty的九点量表为每个参数分配适当的权重,并通过层次分析法(AHP)对权重进行归一化。通过达到小于10%的一致性比率,可以确定分配的权重是一致且无偏的。该地区的地下水预测模型是根据开发的地下水潜力指数(GWPI)模型方程生成的。预测模型将研究区域的地下水潜力分类为非常低;很低低中中等-高和高-非常高的阶层。从这项研究中获得的结果证明,通过将多准则决策分析应用于地下因素而获得的GWPI所生成的地下水预测模型是准确可靠的。它也证明了在两个或多个冲突标准存在的情况下,采用该方法作为良好决策工具的能力。这种能力使其成为可用于地下水预测领域的有用工具。

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