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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Data-domain correlation approach for joint hydrogeologic inversion of time-lapse hydrogeologic and geophysical data
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Data-domain correlation approach for joint hydrogeologic inversion of time-lapse hydrogeologic and geophysical data

机译:时移水文地质和地球物理数据联合水文地质反演的数据域相关方法

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摘要

Inverse estimations of hydrogeologic properties often are highly uncertain because of the expense of collecting hydrogeologic data and the subsequent lack of information. Geophysical data potentially can help fill this information gap because geophysical methods can survey large areas remotely and relatively inexpensively. However, geophysical data are difficult to incorporate into hydrogeologic parameter estimations primarily because of a lack of knowledge concerning the petrophysical relationships between hydrogeologic and geophysical parameters. A method can be used that allows time-lapse geophysical data to be incorporated directly into a hydrogeologic parameter estimation when a strong correlation exists between changes in geophysical and hydrogeologic properties. This approach bypasses the need for an explicit petrophysical transform by formulating the geophysical part of the hydrogeologic inversion in terms of a data-domain correlation operator. A synthetic electrical resistivity monitoring application is used to estimate the hydraulic conductivity distribution. Including time-lapse resistivity data to supplement sparse hydrologic data appears to improve greatly the resolution of hydraulic conductivity in this case. More generally, the formulation and results suggest that geophysical monitoring data can be incorporated effectively into a hydrogeologic parameter estimation using a data-domain correlation operator, assuming a strong correlation exists between changes in hydrogeologic and geophysical properties.
机译:由于收集水文地质数据的费用高以及随后缺乏信息,水文地质属性的反演估计通常是高度不确定的。地球物理数据有可能帮助填补这一信息空白,因为地球物理方法可以远程且相对便宜地进行大范围勘测。然而,主要由于缺乏关于水文地质参数与地球物理参数之间的岩石物理关系的知识,很难将地球物理数据纳入水文地质参数估计中。当地球物理和水文地质特性的变化之间存在很强的相关性时,可以使用一种方法,该方法允许将延时的地球物理数据直接合并到水文地质参数估计中。该方法通过根据数据域相关算子来表述水文地质反演的地球物理部分,从而无需进行明确的岩石物理转换。合成电阻率监控应用程序用于估算水力传导率分布。在这种情况下,包括随时间推移的电阻率数据以补充稀疏的水文数据似乎可以大大提高水力传导率的分辨率。更一般地说,假设水文地质和地球物理性质的变化之间存在很强的相关性,则该公式和结果表明可以使用数据域相关算子将地球物理监测数据有效地纳入水文地质参数估计中。

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