|
|
The application of Cole-Cole model parameters to the time domain induced polarization prospecting |
Wei PENG1,2, Yi-Qiang LIANG1,2, Chun ZHANG2, Peng-Peng LIU2 |
1. Chengdu University of Technology, Chengdu 610072, China 2. Geophysical Exploration Party of Sichuan Bureau of Exploration and Development of Geology and Minerals Resources, Chengdu 610072, China |
|
|
Abstract the routine time domain induced polarization can only obtain two parameters, i.e., resistivity and polarizability, which often makes it difficult to accurately interpret induced polarization anomaly and thus causes less information for orebody interpretation and poor detection resolution. Such a phenomenon is especially prominent in the exploration of some ore resources characterized by associated or accompanying minerals like carbonaceous limestone, pyrite and limonite whose resistivities or polarizabilities are close to each other. In order to enrich orebody geological information, improve the understanding of orebody and reduce mistaken or incomplete judgement, the authors utilized the feature that Cole-Cole model could describe time response of induced polarization effect and employed damping least squares method to realize the best fitting of the time response with time domain Cole-Cole model so as to obtain varied kinds of Cole-Cole model parameters. Practice shows that this method is economical and effective and, through integrated interpretation of varied kinds of physical parameters, it can realize more overall understanding and correct induction and interpretation of induced polarization and also improve the resolution of the time domain induced polarization in deep prospecting.
|
Received: 01 June 2017
Published: 04 June 2018
|
|
|
|
|
|
|
组号 | 参数项 | η1 | η2 | η3 | η4 | 1 | 时间宽度/ms | 20 | 40 | 80 | 160 | 视极化率/% | 0.4646 | 0.4411 | 0.4076 | 0.3642 | 2 | 时间宽度/ms | 40 | 80 | 160 | 320 | 视极化率/% | 0.4563 | 0.4177 | 0.3706 | 0.3169 | 3 | 时间宽度/ms | 80 | 160 | 320 | 640 | 视极化率/% | 0.4423 | 0.3841 | 0.3242 | 0.1677 | 4 | 时间宽度/ms | 160 | 320 | 640 | 1280 | 视极化率/% | 0.4202 | 0.3407 | 0.2718 | 0.1427 |
|
|
组号 | 参数项 | m/% | τ/ms | c | 1 | 理论值 | 0.6 | 1 | 0.5 | 拟合值 | 0.5986 | 0.9979 | 0.5027 | 精度/% | 0.23 | 0.21 | 0.54 | 2 | 理论值 | 0.6 | 1 | 0.5 | 拟合值 | 0.6011 | 0.9948 | 0.4968 | 精度/% | 0.18 | 0.52 | 0.64 | 3 | 理论值 | 0.6 | 1 | 0.5 | 拟合值 | 0.6017 | 0.9897 | 0.4966 | 精度/% | 0.28 | 1.03 | 0.68 | 4 | 理论值 | 0.6 | 1 | 0.5 | 拟合值 | 0.6015 | 0.9929 | 0.4976 | 精度/% | 0.25 | 0.71 | 0.48 |
|
|
|
|
|
|
[1] |
昌彦君 . 时间谱电阻率法研究[D]. 武汉:中国地质大学(武汉), 2000.
|
[2] |
刘春明 . 伪随机激电多参数谱法研究[D]. 长沙:中南大学, 2006.
|
[3] |
张赛珍, 王庆乙, 罗延钟 . 中国电法勘探发展概况[J]. 地球物理学报, 1994,37(1):408-424.
|
[4] |
傅良魁 . 电法勘探教程[M]. 北京: 地质出版社, 1983.
|
[5] |
李金铭 . 激发极化法方法技术指南[M]. 北京: 地质出版社, 2004.
|
[6] |
Guptasarma D . Computation of the time-domain response of a polarizable groud[J]. Geophysics, 1982,47(11):1574-1576.
|
[7] |
Pelton W H , et al. Mineral discrimination and removal of inductive coupling with multifrequency IP[J]. Geophysics, 1978,3(43):588-609.
|
[8] |
罗延钟, 张桂青 . 频率域激电法原理[M]. 北京: 地质出版社, 1988.
|
[9] |
吴孝国 . 柯尔-柯尔模型激电时间谱的正反演方法及应用[J]. 地质与勘探, 1989,25(9):37-41.
|
[10] |
曹平华, 罗润林 . 时域激电数据进行频谱参数反演方法及应用[J]. 物探与化探, 2014,38(5):1008-1011.
|
[11] |
徐士良 . Fortran常用算法程序集[M]. 北京: 清华大学出版社, 1995.
|
[12] |
罗延钟, 吴之训 . 谱激电法频率相关系数的应用[J]. 地球物理学报, 1992,35(4):490-500.
|
[13] |
傅良魁, 李金铭, 陈兆洪 . 埋藏极化体激电时间谱视参数的实验研究结果[J]. 地质与勘探, 1985,21(12):38-43.
|
[14] |
庄明商, 尚世贵 . 用激电时间谱视参数评价激电异常的应用效果[J]. 物探与化探, 1995,19(3):218-223.
|
[1] |
Ke HE, Jian-Hua LI, Yuan-Cheng ZHAO, Wen-Bo WEI, Gao-Feng YE, Gang WANG. Comprehensive geophysical monitoring of solute transport in leaching solution of the sandstone type uranium deposit[J]. Geophysical and Geochemical Exploration, 2018, 42(3): 442-452. |
[2] |
CAO Ping-Hua, LUO Run-Lin. Spectral parameters inversion method based on TDIP and its application[J]. Geophysical and Geochemical Exploration, 2014, 38(5): 1008-1011. |
|
|
|
|