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首页> 外文期刊>Journal of African Earth Sciences >Petrophysical and aquifer parameters estimation using geophysical well logging and hydrogeological data, Wadi El-Assiuoti, Eastern Desert, Egypt
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Petrophysical and aquifer parameters estimation using geophysical well logging and hydrogeological data, Wadi El-Assiuoti, Eastern Desert, Egypt

机译:使用地球物理测井和水文地质数据估算岩石物理和含水层参数,Wadi El-Assiuoti,埃及东部沙漠

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The study of groundwater potential in Wadi El-Assiuoti is of a prime importance for both current and future development. In this paper the groundwater occurrences are investigated using integrated; 1) geophysical well logging (Self potential, Resistivity and Gamma Ray), 2) subsurface lithologic data and 3) hydraulic data (transmissivity, transmissibility, hydraulic conductivity and storativity) in addition to reviewing all studies on Wadi El-Assiuoti. Different petrophysical parameters (formation water resistivity, formation factor, porosity, permeability, salinity and shale volume) are computed. These parameters are very necessary to identify the aquifers characteristics in the surveyed area. The integration between geophysical and hydrogeological data shows the possibility of two water bearing formation (Quaternary and Plio-Pleistocene). Generally, porosity and permeability values of these aquifers decrease toward the west. The aquifers exist under unconfined to semi confined conditions. The wide range values of both well efficiency and hydraulic conductivity indicate heterogeneity in the lithology and hydraulic characteristics of the aquifer materials. The computed transmissibility values indicate that the water-bearing sediments in the area under investigation are generally of high productivity. In some localities due to the heterogeneity of sediment, the water-bearing sediments are of moderate productivity. Recently, due to the increase of drilling activities at the middle part of the studied area some problems concerning the groundwater potential and high salinity in the area are happening.
机译:瓦迪·阿修瓦蒂(Wadi El-Assiuoti)地下水潜力的研究对于当前和未来的发展都至关重要。本文采用综合方法研究了地下水的发生。 1)地球物理测井(自电势,电阻率和伽马射线),2)地下岩性数据和3)水力数据(透射率,透射率,水力传导率和磁化率),此外还审查了有关瓦迪-阿苏蒂的所有研究。计算了不同的岩石物理参数(地层水电阻率,地层因子,孔隙度,渗透率,盐度和页岩体积)。这些参数对于确定被调查区域的含水层特征非常必要。地球物理和水文地质数据之间的整合表明,可能形成两种含水层(第四纪和上新世)。通常,这些含水层的孔隙率和渗透率值向西减小。含水层存在于不受限制的半封闭条件下。井效率和水力传导率的宽范围值表明了含水层材料的岩性和水力特性的不均匀性。计算出的透射率值表明,被调查地区的含水沉积物通常具有较高的生产率。在某些地区,由于沉积物的非均质性,含水沉积物的生产率中等。最近,由于研究区域中部钻井活动的增加,该地区正在发生一些与地下水潜力和高盐度有关的问题。

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