时间域航空电磁数据加权横向约束反演

doi:10.13278/j.cnki.jjuese.201601302

吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (1): 254-261.doi: 10.13278/j.cnki.jjuese.201601302

时间域航空电磁数据加权横向约束反演

殷长春, 邱长凯, 刘云鹤, 蔡晶

吉林大学地球探测科学与技术学院, 长春 130026

收稿日期:2015-05-19 出版日期:2016-01-26 发布日期:2016-01-26
通讯作者: 邱长凯(1991),男,研究生,主要从事电磁法正反演和方法技术研究,E-mail:qiuck13@mails.jlu.edu.cn E-mail:qiuck13@mails.jlu.edu.cn
作者简介:殷长春(1965),男,教授,国家"千人计划"特聘专家,主要从事电磁勘探理论特别是航空和海洋电磁方面的研究,E-mail:yinchangchun@jlu.edu.cn
基金资助:
国家重大科研装备研制项目(ZDYZ2012-1-03);国家自然科学基金项目(41274121);国土资源部老矿山复核项目(中地调研合同[2013]第214号)

Weighted Laterally-Constrained Inversion of Time-Domain Airborne Electromagnetic Data

Yin Changchun, Qiu Changkai, Liu Yunhe, Cai Jing

College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China

Received:2015-05-19 Online:2016-01-26 Published:2016-01-26
Supported by:
Supported by Projects on the Development of the Key Equipment of Chinese Academy of Sciences (ZDYZ2012-1-03),China Natural Science Foundation (41274121) and Ministry of Land and Resources of the Peoples Republic of China Old Mine Review Proiect(China Geological Survey Project Agreement[2013] No.214)

摘要/Abstract

摘要：

传统的单点一维反演技术处理时间域航空电磁数据得到的电阻率和层厚度容易呈现横向不连续性,导致层界面不光滑。即使相邻测点的反演结果也会出现突变现象,与实际地质情况不符,给解释工作带来困难。笔者针对时间域航空电磁数据空间采样密集、在沉积岩地区工作时地下电性结构横向连续性较好的特点,研究了时间域航空电磁数据参数加权横向约束反演方法。反演时同时考虑数据拟合、相邻测点电阻率和层厚度横向约束以及深度横向约束,利用参数加权来调整对各层模型参数和深度横向光滑度的约束强度。通过对理论和实测数据反演并与传统的单点一维反演结果进行对比,验证了拟二维横向加权约束反演是处理时间域航空电磁数据的有效方法。横向约束反演结果电阻率和层厚度横向光滑连续,层界面清晰。引入参数加权实现对不同参数横向光滑度和连续性的制约,可进一步提高反演解的稳定性。加权因子对反演结果有较大影响,在实际应用中,应该综合考虑地质资料选择合适的加权因子。

关键词: 航空电磁, 时间域, 加权横向约束, 正演, 反演

Abstract:

The resistivity and thickness inverted by traditional single-site 1D methods for time-domain airborne electromagnetic (AEM) data frequently demonstrate sharp variations along a profile. This phenomenon occurs even between neighbor stations, resulting in non-smooth layer interfaces, which can seriously complicate the interpretation. Considering that AEM systems generally have a high spatial sampling rate, and the underground structures in areas like sedimentary formations are continuous, we use the weighted laterally-constrained inversion (WLCI) algorithm to invert the time-domain AEM data. Data fitting,lateral constraints on resistivity,thickness and depth are considered at the same time, and further the constraint strength is adjusted by using the weighting factors (chosen on geological information). Through testing the above algorithm on both synthetic and survey data, and comparing the results with those from conventional inversions, the WLCI algorithm is proved to be a very reliable and effective tool to process the time-domain AEM data. The inverted results by WLCI algorithm are smooth and continuous with clear layer interfaces. Weighting for different constrained parameters can also improve the stability of inversion. The weighting factors have an important impact on the inversion results. To choose the appropriate weighting factors, the field geological information should be taken into account.

Key words: airborne electromagnetic, time-domain, weighted laterally-constrained inversion, forward modeling, inversion

中图分类号:

P631.3

殷长春, 邱长凯, 刘云鹤, 蔡晶. 时间域航空电磁数据加权横向约束反演[J]. 吉林大学学报(地球科学版), 2016, 46(1): 254-261.

Yin Changchun, Qiu Changkai, Liu Yunhe, Cai Jing. Weighted Laterally-Constrained Inversion of Time-Domain Airborne Electromagnetic Data[J]. Journal of Jilin University(Earth Science Edition), 2016, 46(1): 254-261.

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时间域航空电磁数据加权横向约束反演

Weighted Laterally-Constrained Inversion of Time-Domain Airborne Electromagnetic Data

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