RECOVERING OF THE RESERVOIR CONDUCTIVITY BY MEASUREMENTS ON THE SURFACE USING GPR DATA

M. Shishlenin, Aliya Shakhatova, T. Mirgalikyzy
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Abstract

In this article we consider a mathematical model of interpretation of a geoelectric section based on georadar data. One of the reasons preventing the spread of GPR technologies is the complexity of data interpretation, which requires the involvement of highly qualified specialists. In this regard, the study of the mathematical model and comparison with real georadar data expands the possibilities of interpretation of the georadar. To test the algorithm for solving the inverse problem of determining the electrical conductivity of layered media, data from exploration wells of the Karaganda coal basin field were used. We assume that the medium is horizontally layered and the electromagnetic pa- rameters of the medium depend only the depth. The problem of determining the conductivity is reduced to the problem of minimizing the cost functional by the gra- dient method. The gradient of the functional is calculated through the solution of the adjoint problem, the results of numerical calculations are given.
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利用地面探地雷达数据测量储层电导率
在本文中,我们考虑了一个基于地质雷达数据的地电剖面解释的数学模型。阻止探地雷达技术传播的原因之一是数据解释的复杂性,这需要高素质的专家参与。在这方面,对数学模型的研究以及与真实地质雷达数据的比较扩大了解释地质雷达的可能性。为了验证求解层状介质电导率反演问题的算法,使用了卡拉干达煤田探井的数据。我们假设介质是水平分层的,介质的电磁参数仅取决于深度。通过梯度法,将确定电导率的问题简化为最小化成本函数的问题。通过求解伴随问题来计算泛函的梯度,并给出了数值计算结果。
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