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Coseismic effects of water temperature based on digital observation from Tayuan well, Beijing
作者姓名:杨竹转  邓志辉  陶京玲  谷圆珠  王志敏  刘成龙
作者单位:Institute of Geology China Earthquake Administration,Institute of Geology,China Earthquake Administration,Institute of Geology,China Earthquake Administration,Institute of Geology,China Earthquake Administration,Institute of Geology,China Earthquake Administration,Institute of Geology,China Earthquake Administration,Beijing 100029,China,Beijing 100029,China,Beijing 100029,China,Beijing 100029,China,Beijing 100029,China,Beijing 100029,China
基金项目:Foundation item: National Natural Science Foundation of China (40372131) and the Key Projects Required by National 10th Five-year Plan (2004BA601B01-02-02). Acknowledgements We are deeply indebted to Professor CHE Yong-tai, Professor XU Dao-yi and GU0 Xiang-yun from Baijiatuan seismic station for their sincerely help.
摘    要:On the basis of digital records from Tayuan well,we study coseismic effects of water temperature caused by re-mote earthquakes.The records show that the water temperature changes are consistently following the process ofdrop-rise-recovery regardless of focal mechanism or epicentral directions.The step amplitude of water temperatureincreases with the increase of earthquake magnitude,and decreases with the decrease of epicentral distances.Theyhave rather well correlation.Water temperature rising after earthquake is influenced by water level variations.Fi-nally,the mechanisms of coseismic effects of water temperature have been discussed.Preliminary study shows thataccelerated convection and mixing of different temperature water in virtue of seismic wave are the main causes ofwater temperature drops.Seismic wave accelerates water convection,which causes warm water to move up fromdeeper part of the well and cold water to go down from the upper part.Temperature probe will detect water tem-perature drops at early stage.After the occurrence of earthquake,as the fluctuation of water level gradually quietsdown,water temperature near the probe begins to rise.

关 键 词:北京  塔院井  井水温度  地震  等震波圈效应
文章编号:1000-9116(2007)02-0212-12
收稿时间:2006-07-26
修稿时间:2007-01-08

Coseismic effects of water temperature based on digital observation from Tayuan well, Beijing
Yang Zhu-zhuan , Deng Zhi-hui , Tao Jing-ling , Gu Yuan-zhu , Wang Zhi-min and Liu Cheng-long.Coseismic effects of water temperature based on digital observation from Tayuan well, Beijing[J].Acta Seismologica Sinica(English Edition),2007,20(2):212-223.
Authors:Yang Zhu-zhuan  Deng Zhi-hui  Tao Jing-ling  Gu Yuan-zhu  Wang Zhi-min and Liu Cheng-long
Institution:(1) Institute of Geology, China Earthquake Administration, Beijing, 100029, China
Abstract:On the basis of digital records from Tayuan well,we study coseismic effects of water temperature caused by re-mote earthquakes.The records show that the water temperature changes are consistently following the process of drop-rise-recovery regardless of focal mechanism or epicentral directions.The step amplitude of water temperature increases with the increase of earthquake magnitude,and decreases with the decrease of epicentral distances.They have rather well correlation.Water temperature rising after earthquake is influenced by water level variations.Fi-nally,the mechanisms of coseismic effects of water temperature have been discussed.Preliminary study shows that accelerated convection and mixing of different temperature water in virtue of seismic wave are the main causes of water temperature drops.Seismic wave accelerates water convection,which causes warm water to move up from deeper part of the well and cold water to go down from the upper part.Temperature probe will detect water tem-perature drops at early stage.After the occurrence of earthquake,as the fluctuation of water level gradually quiets down,water temperature near the probe begins to rise.
Keywords:Tayuan well  water temperature  earthquake  coseismic effect
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