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汶川8.0级地震与日本9.0级地震的同震响应特征——庐江地震台动水位与水温

Analysis of co-seismic changes of dynamic water level and water temperature responding for Wenchuan M_s 8.0 earthquake and Japan M_s 9.0 earthquake in observation wells of Lujiang Seismic Station

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【作者】 金艳刘川琴汪世仙隆爱军方素贞

【Author】 Jin Yan~(1)),Liu Chuanqin~(2)),Wang Shixian~(2)),Long Aijun~(3)) and Fang Suzhen~(1)) 1) Earthquake Administration of Anhui Province,Hefei 230031,China 2) Lujiang Seismic Station,Anhui Province 231511,China 3) Hefei Seismic Station,Anhui Province 230031,China

【机构】 安徽省地震局庐江地震台合肥地震台

【摘要】 自2000年庐江地震台数字化水位、水温观测以来,在多次大地震中水位、水温均有明显的同震效应,四川汶川8.0级地震、日本本州9.0级地震引起汤池1号井水位、水温的同震特征。动水位同震效应表现为脉冲变化,震后水位逐渐升高;水温表现为阶跃下降,震后水温缓慢恢复到正常状态。

【Abstract】 The digital water level and water temperature of Lujiang Seismic Station has been observed Since 2000,there have been obviously co-seismic change on earthquake many times.In this paper,water level and water temperature changs caused by Wenchuan M_S 8.0 erathquake and Japan M_S 9.0 erathquake are analyzed.The result concluded that water level of co-seismic change was pulse change.After earthquake the water level increased gradually.The water temperature of co-seismic change is step down.After earthquake the water temperature returned to normal gradually.

【基金】 安徽省地震局合同制课题资助
  • 【文献出处】 地震地磁观测与研究 ,Seismological and Geomagnetic Observation and Research , 编辑部邮箱 ,2012年Z2期
  • 【分类号】P315
  • 【下载频次】25
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