| 延寿井水温资料的远场效应研究 |
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| 引用本文： | 吴海波,李希文,柴红泽,朱家明,李婧,孙鹏宇,王海涛,武晓军.延寿井水温资料的远场效应研究[J].东北地震研究,2011,27(4):26-29. |
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| 作者姓名： | 吴海波 李希文 柴红泽 朱家明 李婧 孙鹏宇 王海涛 武晓军 |
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| 作者单位： | 1. 延寿地震台,黑龙江哈尔滨,150700
2. 通河地震台,黑龙江哈尔滨,150900 |
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| 摘 要： | 本文简单介绍了延寿台水温井的观测条件与环境，分析了该井观测到的多次同震水位变化以及伴随的深层水温变化，并且水温多是上升，震后一至数小时后又恢复。由于井水振荡使水受到扰动，导致不同深度不同温度水的混合，从而造成同震水温变化的弥散模型，而后由于水的热传导作用又恢复正常。
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| 关 键 词： | 地震 井水位 井水温 同震效应 弥散模型 |
BRIEFNESS ANALYSIS OF YANSHOU COSEISMIC WELL TEMPERATURE CHANGES PHENOMENA |
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| WU Hai-bo,LI Xi-wen,CHAI Hong-ze,ZHU Jia-ming,LI Jing,SUN Peng-yu,WANG Hai-tao,WU Xiao-jun.BRIEFNESS ANALYSIS OF YANSHOU COSEISMIC WELL TEMPERATURE CHANGES PHENOMENA[J].Seismological Research of Northeast China,2011,27(4):26-29. |
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| Authors: | WU Hai-bo LI Xi-wen CHAI Hong-ze ZHU Jia-ming LI Jing SUN Peng-yu WANG Hai-tao WU Xiao-jun |
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| Institution: | 1.Yanshou Seismic Station, Heilongjiang Harbin 150700, China; 2.Tonghe Seismic Station, Heilongjiang Harbin 150900, China) |
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| Abstract: | This paper briefly introduced the condition and environment of observation on the water temperature of Yanshou well. The coseismic water level oscillation and correlated deep water temperature changes have been observed in this well. And the water temperature usually rises and recovers after one to several hours. It suggested that the temperature drop is produced by dispersive transfer of heat as the water oscillates, and follow-up thermal conduction makes temperature recovery. |
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| Keywords: | earthquake water level water temperature coseismal effect smeared model |
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