摘要
对柯坪地电阻率台整点观测数据进行FFT变换,计算出其年变周期约为305.5 d;分析了观测区地下水位、气温的变化以及下伏地层的影响系数与年变间的关系,最终明确柯坪地电阻率台观测数据的反常年变形态是由测区特殊的电性结构引起的。
FFT is performed to the hourly sampled earth resistivity observations at the Keping Seismic Station,and its annual variation period is determined to be about 305.5 d.The relationship between the variation of groundwater level,air temperature,and the influence coefficient of underlying strata and the annual variation is analyzed.Finally,it is concluded that the abnormal annual variation of earth resistivity observations at the Keping Seismic Station is caused by the special electrical structure of the survey area.
作者
饶文
刘海洋
张治广
赖爱京
冯英
RAO Wen;LIU Haiyang;ZHANG Zhiguang;LAI Aijing;FENG Ying(Aksu Seismic Station,Earthquake Agency of Xinjiang Uygur Autonomous Region,Xinjiang 843000,China;Earthquake Agency of Xinjiang Uygur Autonomous Region,Urumqi 830011 China)
出处
《地震地磁观测与研究》
2021年第1期61-68,共8页
Seismological and Geomagnetic Observation and Research
基金
新疆维吾尔自治区地震局科研项目(项目编号:201916)。
关键词
地电阻率
FFT
年变
地下水位
气温
影响系数
earth resistivity
FFT
annual variation
underground water level
air temperature
sensitivity coefficient