节点文献
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
【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.
【关键词】 汶川8.0级地震;
日本9.0级地震;
动水位;
水温;
同震响应;
【Key words】 Wenchuan M_s 8.0 earthquake; Japan M_s 9.0 earthquake; water level; water temperature; co-seismic change;
【Key words】 Wenchuan M_s 8.0 earthquake; Japan M_s 9.0 earthquake; water level; water temperature; co-seismic change;
【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