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地下井体建设对地磁观测场地的干扰 被引量:1
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作者 王晓睿 王淑辉 +2 位作者 刘允 张帅 代青沁 《地震地磁观测与研究》 2023年第2期112-118,共7页
以大连地震监测中心地震前兆观测新建地下井体为例,基于场地梯度测量方法,定量分析井体建设对地磁观测场地的干扰。基于观测井设计数据,计算其理论干扰距离,发现最大干扰距离s=456.6 m>270 m(二者的实际间距),推测此地下井体会对地... 以大连地震监测中心地震前兆观测新建地下井体为例,基于场地梯度测量方法,定量分析井体建设对地磁观测场地的干扰。基于观测井设计数据,计算其理论干扰距离,发现最大干扰距离s=456.6 m>270 m(二者的实际间距),推测此地下井体会对地磁观测产生干扰。以井体与地磁观测仪器室之间50 m×160 m的范围为测量区域,以10 m×10 m的网格进行测线及测点的布设,计算并对比分析井体建设前后各测线地磁总场强度F的梯度值,结果发现,除个别临近办公区的测点梯度值不稳定,其他测点梯度值基本处于重合状态,排除测量区域葡萄架和接线井的干扰后,磁场梯度整体符合规范,即ΔF_(b)≤1 nT/m。分析认为,地下井体对地磁场的最大干扰距离为160 m,表明该中心地下井体建设不会对地磁观测场地造成干扰。 展开更多
关键词 地磁观测场 地梯度 井体干扰 干扰距离
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Analysis and Study on the Change of the Observed Geo-electric Field Data at Lhasa Geomagnetic Station before and after the Nepal MS8.1 Earthquake
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作者 Xi Jilou Guan Huaping +7 位作者 Liu Chao Zhuang Nan Guan Xinying Yang Xiaoming Zhang Zhiguo Ci Zhuoga Kelsang Drolma Ma Aiming 《Earthquake Research in China》 CSCD 2016年第4期526-541,共16页
In this paper,the main purpose is to analyze and research the characteristics of the geoelectric field observed data with a long time span and large amplitude abnormal change,at the Lhasa geomagnetic station( hereafte... In this paper,the main purpose is to analyze and research the characteristics of the geoelectric field observed data with a long time span and large amplitude abnormal change,at the Lhasa geomagnetic station( hereafter referred to as "Lhasa station "),before and after the Nepal M_S8. 1 strong earthquake,which occurred on April 25,2015. Based on the observation conditions,the observation system,and the observed data of Lhasa station preliminary discussed,the main characteristics of the abnormal change and evolution process are analyzed and studied,using the following two methods; the "synthesis energy accumulation"and the "power as MSA spectrum"analysis,from the two aspects of the"Time Domain"and"Frequency Domain. "The results show that the abnormal change of the geo-electric field observation of Lhasa station experienced a development stage following the process of "trend change- disturbance change- earthquake period-recovery period",and an evolution process of "low frequency change- high frequency change- smooth change- high frequency change ",before and after the Nepal M_S8. 1strong earthquake. Comprehensive analysis shows that the variation characteristics and evolution process of the geo-electric field at Lhasa station are basically consistent with the results of the relevant mechanism and phenomenon research. So far,this is valuable information with certain objectivity,which is typical and representative to reflect the whole process of the gestation, occurrence and complete development of such strongearthquakes. 展开更多
关键词 Geo-electric field Nepal Ms8. 1 earthquake Lhasa geomagnetic station Abnormal change Synthesis energy accumulation Power as MSA spectrum
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