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首页> 外文期刊>Hydrology and Earth System Sciences >Determination of fluid transmissivity and electric transverse resistance for shallow aquifers and deep reservoirs from surface and well-log electric measurements
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Determination of fluid transmissivity and electric transverse resistance for shallow aquifers and deep reservoirs from surface and well-log electric measurements

机译:通过地表和测井电学测量确定浅层含水层和深层储层的流体透​​过率和横向电阻

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Fluid transmissivity (layer thickness times permeability) and electrictransverse resistance (layer thickness time resistivity) are important parameterin groundwater and hydrocarbon exploration. Determination of these parametersprovides a good knowledge of the potential of porous media, because they relatefluid flow to electric-current conduction, in terms of layer thickness,permeability and resistivity. In this study, both parameters were determined forshallow aquifers (Schleswig-Holstein, northern Germany) and deep reservoirs(Jeanne d'Arc Basin, offshore of eastern Canada), utilizing surface and well-logelectric measurements. Direct relationships between both parameters, withcoefficients of correlation of 0.99 (for the aquifers) and 0.94 (for thereservoirs), were obtained. The relationships suggest that an increase in bothparameters indicate presence of zones of high fluid potential within theaquifers and the reservoirs.
机译:流体的渗透率(层厚度乘以渗透率)和横向电阻(层厚度乘以电阻率)是地下水和油气勘探的重要参数。确定这些参数可以很好地了解多孔介质的潜力,因为就层厚度,磁导率和电阻率而言,它们将流体流与电流传导相关联。在这项研究中,利用地表和测井电学测量,确定了浅层含水层(石勒苏益格-荷尔斯泰因州,德国北部)和深层储层(Jeanne d'Arc盆地,加拿大东部沿海地区)的两个参数。得到两个参数之间的直接关系,相关系数为0.99(对于含水层)和0.94(对于储层)。这些关系表明,两个参数的增加表明在含水层和储层内存在着高流体潜能的区域。

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