吉林大学学报(地球科学版) ›› 2026, Vol. 56 ›› Issue (4): 1397-1408.doi: 10.13278/j.cnki.jjuese.20240322

• 地球探测与信息技术 • 上一篇    下一篇

2022年天水井下地电阻率异常核实实例

姚赛赛1,2,高曙德1,2,狄国荣2,张丽琼1,2,刘天兵3,缑亚江2,周建华2   

  1. 1.中国地震局兰州地震研究所,兰州 730000
    2.兰州地球物理国家野外科学观测研究站,兰州 730000
    3.国家电网天水供电公司,甘肃 天水 741000
  • 收稿日期:2024-12-06 出版日期:2026-07-26 发布日期:2026-08-11
  • 作者简介:姚赛赛(1993— ),男,工程师,主要从事地震监测工作,E-mail: yaosaisai23@mails.ucas.ac.cn
  • 基金资助:
    甘肃省地震局地震科学发展基金野外站项目(2022Y-03);国家自然科学基金重点项目地震联合基金(U2039206);中国地震局监测、预报、科研三结合课题(3JH-202301005)

A Case Study  on the Virification  of Borehole Apparent Resistivity Anomaly in Tianshui, 2022

Yao Saisai1,2, Gao Shude1,2, Di Guorong2, Zhang Liqiong1,2, Liu Tianbing3, Gou Yajiang2, Zhou Jianhua2   

  1. 1. Lanzhou Institute of Seismology, CEA, Lanzhou 730000, China
    2. Gansu Lanzhou Geophysics National Observation and Research Station, CEA, Lanzhou 730000, China
    3. Tianshui Electric Power Supply Company, State Grid Corporation of China, Tianshui 741000, Gansu, China
  • Received:2024-12-06 Online:2026-07-26 Published:2026-08-11
  • Supported by:
    the Science and Technology Development Foundation of Gansu Earthquake Agency (2022Y-03), the National Natural Science Foundation Key Project on Earthquake Joint Fund (U2039206) and the Combination Project with Monitoring, Prediction and Scientific Research of Earthquake Technology CEA (3JH-202301005)

摘要: 2022-06-16,天水井下地电阻率三向数据出现高频扰动,变化形态和幅度与2013-04-20芦山MS 7.0、2013-07-22岷县—漳县MS 6.6、2017-08-08九寨沟MS 7.0地震前相似。通过资料收集整理、异常调查分析、干扰核实处理等工作,主要包括自然环境和场地环境调查、观测系统检定、工频干扰测试、干扰源确定、线路检修和运行监测等,发现此次天水井下地电阻率异常并非震前地球物理异常,而是变压器接地漏电电流与地电阻率测量供电电流耦合造成的高频扰动。此次异常核实案例可以为井下地电阻率台站供电线路规划、观测系统运维及漏电异常排查提供参考。

关键词: 地电阻率, 高频扰动, 异常核实, 漏电干扰

Abstract: On 16 June 2022, high-frequency disturbances were observed in the three-orientation borehole apparent resistivity data in Tianshui. Their change pattern and amplitude were similar to those observed before the 20 April 2013 Lushan MS 7.0, 22 July 2013 Minxian-Zhangxian MS 6.6, and 8 August 2017 Jiuzhaigou MS 7.0 earthquakes. Data collection and organization, anomaly investigation and analysis, and interference verification and treatment were conducted through a series of procedures, primarily including natural environment and site environment investigations, observational system verification, power frequency interference testing, identification of interference sources, line maintenance, and operational monitoring. It is found that Tianshui borehole apparent resistivity anomaly is not a pre-earthquake geophysical anomaly, but a high-frequency disturbance caused by the coupling of transformer grounding leakage current and the supply current during the instrumental measurement. This anomaly verification case provides a reference for power supply circuit planning, observation system maintenance and wire leakage anomaly investigation of borehole apparent resistivity stations.

Key words: apparent resistivity, high frequency disturbance, anomaly verification, leakage interference

中图分类号: 

  • P319
[1] 叶青, 王晓, 杜学彬, 解滔, 范晔, 周振贵, 刘高川.

中国地震井下地电阻率研究进展 [J]. 吉林大学学报(地球科学版), 2022, 52(3): 669-683.

[2] 宁亚灵, 许家姝, 解滔, 张国苓, 卢军. 大柏舍深井地电阻率观测布极方式分析[J]. 吉林大学学报(地球科学版), 2018, 48(2): 525-533.
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