Influence of Magnetic Polarization on Diagrams of Inductive and Electromagnetic Logs

E.I. Shtanko, D.A. Arkhipov, M. Epov
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Abstract

––We present the results of the study of the effect of induced magnetic polarization of clay beds under the influence of an external harmonic electromagnetic field (frequencies 70 and 875 kHz). A two-stage numerical modeling procedure is proposed. At the first stage we determine the effective relative magnetic permeability of a synthetic sample with inclusions of clay particles. In this case a 3D heterogeneous mesh sample is generated. Then we numerically model a spatial distribution of an electric field. The electromotive force (EMF) induced in the measuring coil is calculated from this distribution. Relative magnetic permeability is determined by comparison with EMF of homogeneous samples with different values of magnetic permeability. It has been found that during the electric field excitation by an alternating current coil, the effect of induced magnetic polarization appears in the sample with clay particles. Its manifestation is that the effective magnetic permeability becomes complex. At the second stage we calculate the EMF diagram of the three-coil logging probe in the macro-model ‘clay cap – reservoir’. Magnetic permeability of the clay cap is given by a complex value. In the generated logs, extremes appear in the vicinity of the bottom of the clay cap; they do not correspond to the distribution of electrical conductivity and magnetic permeability in the given model. They can be incorrectly interpreted when analyzing real logs into individual formations. Numerical modeling at all stages is performed by the Vector Finite Element Method on a consistent adaptive tetrahedral partition and the first-order Webb vector basis.
磁极化对电感和电磁测井曲线图的影响
--我们介绍了在外部谐波电磁场(频率为 70 和 875 kHz)影响下粘土层诱导磁极化效应的研究结果。我们提出了一个两阶段的数值建模程序。在第一阶段,我们确定了含有粘土颗粒夹杂物的合成样品的有效相对磁导率。在这种情况下,会生成一个三维异质网格样本。然后,我们对电场的空间分布进行数值建模。测量线圈中感应的电动势(EMF)就是根据这一分布计算出来的。通过与具有不同磁导率值的均质样品的 EMF 进行比较,确定相对磁导率。研究发现,在交流线圈的电场激励下,含有粘土颗粒的样品会出现感应磁极化效应。其表现为有效磁导率变得复杂。第二阶段,我们在宏观模型 "粘土帽-储层 "中计算三线圈测井探头的电磁场图。粘土盖的磁导率由一个复杂值给出。在生成的测井曲线中,粘土帽底部附近会出现极端值;这些极端值与给定模型中的导电率和磁导率分布不符。在分析各个地层的实际测井时,可能会对它们进行错误的解释。所有阶段的数值建模都是通过矢量有限元法在一致的自适应四面体分区和一阶韦伯矢量基础上进行的。
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