A method for locating interference source by long-and-short polar distance ratio and its practical application in geoelectric field observation
-
摘要: 提出长短极距比值干扰源定位方法用来定位地电观测中出现的地表干扰源。该方法基于均匀半空间模型且地表干扰为点电源,利用地表不同位置的干扰源所引起的同测向长短极距的电场变化差异,联合多测向比值来定位干扰源位置,并应用到徐庄子台漏电干扰一例和高邮台偶极源试验中。结果表明:利用长短极距比值法,能有效定位干扰点源,且能定位偶极干扰源的其中一个电极。Abstract: The long and short pole distance ratio method in geoelectric observation is employed here to locate the near-surface disturbance sources, on the assumption of a uniform half-space model and that the near-surface disturbance is a point source. The disturbance sources of different locations can cause different increments in the long-pole-distance and short-pole-distance geoelectric field at the same direction, which is the key mind of this method. By combining multi-directional long-and-short pole distance ratios in geoelectric field, we successfully applied this method into locating the disturbance sources of the leakage at Xuzhuangzi station and the dipole source test at Gaoyou station. The results show that the point source producing the interference in geoelectric field at Xuzhuangzi station can be effectively located, and one electrode of the dipole source can be discovered in the Gaoyou station test as well.
-
-
图 2 不同的电极布设坐标示意图(左)、地电场长短极距比值分布图(中)和比值确定时的等值线图(右)
(a) 十字形东西向;(b) L形东西向;(c) L形北东向
Figure 2. Schematic diagram of different electrode layout coordinates (left),distribution of the long and short pole distance ratio for geoelectric field (middle),and contour map when the ratio is determined (right)
(a) Cross-shaped east-west direction;(b) L-shaped east-west direction; (c) L-shaped north-east direction
表 1 徐庄子台干扰电场长短极距比
Table 1 Long-and-short polar distance ratio of interference electric field at Xuzhuangzi station
表 2 偶极源试验中干扰电场长短极距比
Table 2 Long-and-short polar distance ratio of interference electric field in dipole source test
-
陈志刚,田山,徐学恭,马朝晖,陈嵩. 2012. 地电场观测漏电干扰的排查一例[J]. 华北地震科学,30(4):44–48. Chen Z G,Tian S,Xu X G,Ma Z H,Chen S. 2012. Study on electricity-leaking interference in geoelectric field observation at Xuzhuangzi seismic station[J]. North China Earthquake Sciences,30(4):44–48 (in Chinese).
蒋延林,赵卫红,王福才,张骞,朱晔. 2015. 一种地电场观测环境干扰的分析和试验研究[J]. 中国地震,31(1):158–164. Jiang Y L,Zhao W H,Wang F C,Zhang Q,Zhu Y. 2015. Analysis and experimental study of the environment interference in the geo-electric field observation[J]. Earthquake Research in China,31(1):158–164 (in Chinese).
李伟,马钦忠,王冠玥. 2014. 地电场多极距观测的异常识别和分析[J]. 中国地震,30(1):91–101. Li W,Ma Q Z,Wang G Y. 2014. Abnormal signal recognition by multi-dipole observation of geoelectric field[J]. Earthquake Research in China,30(1):91–101 (in Chinese).
马钦忠,钱家栋,李伟,赵文舟,方国庆. 2016. 源自多个大电流源的华东地区地电场空间变化特征[J]. 地球物理学报,59(7):2598–2614. Ma Q Z,Qian J D,Li W,Zhao W Z,Fang G Q. 2016. Characteristics of the spatial variation of geoelectric field signals recorded at the stations in Huadong area in China when 4 heavy currents are injected[J]. Chinese Journal of Geophysics,59(7):2598–2614 (in Chinese).
谭大诚,赵家骝,刘小凤,范莹莹,刘君,陈军营. 2014. 自然电场的区域性变化特征[J]. 地球物理学报,57(5):1588–1598. Tan D C,Zhao J L,Liu X F,Fan Y Y,Liu J,Chen J Y. 2014. Features of regional variations of the spontaneous field[J]. Chinese Journal of Geophysics,57(5):1588–1598 (in Chinese).
田山,王建国,徐学恭,董洪军,崔晓峰,马骥. 2009. 大地电场观测地震前兆异常提取技术研究[J]. 地震学报,31(4):424–431. Tian S,Wang J G,Xu X G,Dong H J,Cui X F,Ma J. 2009. Research on the technique of extracting seismic precursory anomaly from telluric electric field observation[J]. Acta Seismologica Sinica,31(4):424–431 (in Chinese).
王福才,蒋延林,张骞,赵卫红,朱晔,薛家富. 2013. 地电观测场地干扰的一种测试查找方法[J]. 西北地震学报,35(增刊):126–134. Wang F C,Jiang Y L,Zhang Q,Zhao W H,Zhu Y,Xue J F. 2013. A test and search method for the interferences in geoelectric observation field[J]. China Earthquake Engineering Journal,35(S1):126–134 (in Chinese).
卫清,颜蕊,韩秀红,温晋. 2017. 基于牛顿迭代法的地电场观测人为漏电干扰源反演及其应用[J]. 地球物理学进展,32(4):1490–1495. Wei Q,Yan R,Han X H,Wen J. 2017. Inversion for artificial electricity-leaking in geo-electric field observations based on Newton iteration and its application[J]. Progress in Geophysics,32(4):1490–1495 (in Chinese).
张宇,王兰炜,赵家骝,蒋延林,胡哲,张兴国,王福才. 2017. 地电观测中电磁干扰源定位方法研究[J]. 地震学报,39(3):367–373. Zhang Y,Wang L W,Zhao J L,Jiang Y L,Hu Z,Zhang X G,Wang F C. 2017. Location method of electromagnetic interference sources in geo-electric field observation[J]. Acta Seismologica Sinica,39(3):367–373 (in Chinese).
中国地震学会. 2007. 中国地震科技事业的发展[J]. 国际地震动态,(8):23–37. doi: 10.3969/j.issn.0253-4975.2007.08.010 Seismological Society of China. 2007. The development of the Chinese seismological science and technology[J]. Recent Developments in World Seismology,(8):23–37 (in Chinese).
Helman D S. 2020. Seismic electric signals (SES) and earthquakes:A review of an updated VAN method and competing hypotheses for SES generation and earthquake triggering[J]. Phys Earth Planet Inter,302:106484. doi: 10.1016/j.pepi.2020.106484
Miyakoshi J. 1986. Anomalous time variation of the self-potential in the fractured zone of an active fault preceding the earthquake occurrence[J]. J Geomagn Geoelectr,38(10):1015–1030. doi: 10.5636/jgg.38.1015
Varotsos P,Alexopoulos K. 1984. Physical properties of the variations of the electric field of the earth preceding earthquakes,I[J]. Tectonophysics,110(1/2):73–98.