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大同地电阻率NS测向异常分析
引用本文:刘素珍,李自红,宁亚灵.大同地电阻率NS测向异常分析[J].地震地磁观测与研究,2017,38(4):105-109.
作者姓名:刘素珍  李自红  宁亚灵
作者单位:1. 中国太原 030021 山西省地震局;2. 中国山西 030025 太原大陆裂谷动力学国家野外科学观测研究站
基金项目:震情跟踪定向工作任务(项目编号:2015010412),中国地震局地质研究所基本科研业务专项(IGCEA1416),山西省自然科学基金(2015011084)
摘    要:2014年大同地震台地电阻率NS测向出现年变畸变现象,经现场调查,发现测区有铁丝网干扰。利用NS测向电测深曲线,以水平层状模型反演测区电性结构,计算各层介质影响系数,结果发现,浅层介质影响系数为正,合理解释了大同地电阻率NS测向"夏低冬高"的年变现象。在此基础上,应用有限元数值分析和三维影响系数分布,判定测区内铁丝网对地电阻率观测的影响,分析认为,当前存在的趋势异常变化为地电阻率干扰。

关 键 词:地电阻率  异常分析  影响系数  层状介质

Anomaly analysis of earth resistivity in NS direction at Datong Seismic Station
Liu Suzhen,Li Zihong,Ning Yaling.Anomaly analysis of earth resistivity in NS direction at Datong Seismic Station[J].Seismological and Geomagnetic Observation and Research,2017,38(4):105-109.
Authors:Liu Suzhen  Li Zihong  Ning Yaling
Affiliation:1. Shanxi Earthquake Agency, Taiyuan 030021, China;2. National Continental Rift Valley Dynamics Observatory of Taiyuan, Shanxi Province 030025, China
Abstract:The annual aberration of resistivity from Datong Seismic Station in NS direction is detected since 2014. After investigation, we found that the surrounding environment changes with barbed wire. Based on the electrical sounding data of earth resistivity of NS direction, the electrical structure of the measuring region are inversed on horizontal layered model. The sensitivity coefficient of each layer medium in under NS direction is calculated. Annual variation of "Low in summer and high in winter" of each resistivity is interpreted. On the base, we qualitatively analyze the disturbing effects caused by the barbed wire using numerical analysis three dimensional sensitivity coefficient. The result show that the change isn't anomaly.
Keywords:resistivity  anomaly analysis  sensitivity coefficient  layered model
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