首页|基于非结构有限元电各向异性介质井-地激发极化法响应特征研究

基于非结构有限元电各向异性介质井-地激发极化法响应特征研究

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井中激发极化法因其具备工作效率高、勘探效果好,在深部找矿、油气资源勘查和水资源勘查中得到了广泛应用.目前井-地激发极化法的相关研究均是将地下介质假设为各向同性,但是实际地球介质的电性特征表现为各向异性,此时基于各向同性模型的传统成像及反演成像技术就不再适用于各向异性数据的处理解释.为分析各向异性特征对井-地激发极化法的影响规律,本文基于有限单元法开展不同主轴方向的电导率、极化率各向异性正演算法研究,从点源场满足的偏微分方程和边界条件得出异常电位法下的稳定电流场的边值问题和变分问题,实现各向异性介质的井地激发极化法的三维正演模拟.通过对复杂三维各向同性模型和三维各向异性模型的测试与对比,验证了算法的有效性与正确性.构建典型各向异性地质模型分析了不同主轴方向的电导率、极化率各向异性异常体对井-地激发极化响应的影响.结果表明x主轴电导率各向异性导致视电阻率响应值增大其视极化率响应增强,y轴和z轴电导率各向异性时视极化率均表现出较强敏感度;x轴极化率各向异性导致异常体的视极化率响应减弱而y轴和z轴方向极化率各向异性变化不敏感;y轴方向和z轴方向电导率、极化率各向异性时,视极化率响应变化敏感度低,x轴方向的响应变化比较敏感.该研究不仅有利于理解各向异性对井中激电的影响规律,而且可以为考虑各向异性的井中激电资料的数据解释提供理论支撑.
Study on response characteristics of well ground induced polarization method in electrical anisotropic media based on unstructured finite element method
The method of stimulated polarization in wells has been widely used in deep-searching,oil and gas resources exploration and water resources exploration because it possesses high working efficiency and good exploration effect.At present,the well-ground excitation polarization method of the relevant studies are the subsurface medium is assumed to be isotropic,but the actual electrical characteristics of the earth medium is anisotropic is the existence of anisotropy,this time based on the isotropic model of the traditional imaging and inverse imaging technology is no longer applicable to the anisotropic data processing and interpretation.In order to analyze the influence law of anisotropic features on the well-surface excited polarization method,In this paper,we carry out the research on the anisotropic orthogonal algorithm of conductivity and polarizability in different main axis directions based on the finite cell method.Marginal and variational problems for the steady current field under the anomalous potential method are derived from the partial differential equations and boundary conditions satisfied by the point-source field to realize three-dimensional orthogonal simulations of the well ground excitation polarization method for anisotropic media.The effectiveness and correctness of the algorithm is verified by testing and comparing the complex 3D isotropic model and 3D anisotropic model.A typical anisotropic geological model was constructed to analyze the effect of anisotropic anomalies of conductivity and polarizability in different principal axis directions on the polarization response of well-surface excitation.The results show that x-spindle conductivity anisotropy leads to an increase in the apparent resistivity response and an enhancement of its apparent polarizability response.Both y-and z-axis conductivity anisotropy show strong sensitivity in visual polarizability,x-axis polarizability anisotropy results in a diminished apparent polarizability response of the anomaly while polarizability anisotropy changes in the y-and z-axis directions are insensitive.When the conductivity and polarizability are anisotropic in the y-axis and z-axis directions,the sensitivity of the response change in the apparent polarizability is low,and the response change in the x-axis direction is more sensitive.This study not only facilitates the understanding of the law of the influence of anisotropy on the excitation in wells,but also can provide theoretical support for the data interpretation of the excitation data in wells considering anisotropy.

Well ground induced polarization methodAnisotropyFinite element analysisAbnormal potential method3D forward modeling

张俊可、周磊、王新宇、谢兴兵、毛玉蓉、严良俊

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长江大学地球物理与石油资源学院,武汉 430100

长江大学油气资源与勘探技术教育部重点实验室,武汉 430100

中国地质大学(武汉)地球物理与空间信息学院,武汉 430100

井-地激发极化法 各向异性 有限元 异常电位法 三维正演

国家自然科学基金面上项目国家自然科学基金重点项目

4227410342030805

2024

地球物理学进展
中国科学院地质与地球物理研究所 中国地球物理学会

地球物理学进展

CSTPCD北大核心
影响因子:1.761
ISSN:1004-2903
年,卷(期):2024.39(3)