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金沙江水网各观测井温度梯度的精细测量结果及其分析
引用本文:车用太,何案华,鱼金子,刘成龙,李万明.金沙江水网各观测井温度梯度的精细测量结果及其分析[J].中国地震研究,2012,26(1):59-72.
作者姓名:车用太  何案华  鱼金子  刘成龙  李万明
基金项目:supported by the Jinsha River Development Corporation Limited,China Yangtze Three Gorge Engineering Development Group(JSJ(06)-007)
摘    要:Fine measurements have been conducted to temperatures and their gradients of six wells of the Jinsha River Groundwater Observational Network.The results show that the influence depths of sun radiation heat are 50m to 125m,average temperature gradients in the wells range from 0.11 to 2.81℃/hm and most are 1~2℃/hm,and the temperature gradients on varied depth sections of one well are highly changeable.Lithology of strata and their integrity,particularly high-angle crashed fault zones,have imposed major effects on the influence depths of sun radiation heat and temperature gradients of the wells.The micro dynamic characteristics of water temperature,such as coseismic effects,tidal effects and anomalies of the wells prior to earthquakes,probably depend,to a large degree,on the temperature gradients of the depths at which the water temperature sensors are settled.

关 键 词:Temperature  Temperature  gradient  Observational  well  Jinsha  River  Groundwater  Observational  Network
收稿时间:2011/4/11 0:00:00
修稿时间:8/2/2011 12:00:00 AM

Fine Measurements and Analysis of Temperature Gradients in the Wells of the Jinsha River Groundwater Observational Network
Che Yongtai,He Anhu,Yu Jiizi,Liu Chenglong and Li Wanming.Fine Measurements and Analysis of Temperature Gradients in the Wells of the Jinsha River Groundwater Observational Network[J].Earthquake Research in China,2012,26(1):59-72.
Authors:Che Yongtai  He Anhu  Yu Jiizi  Liu Chenglong and Li Wanming
Institution:1) Institute of Geology, China Earthquake Administration, Beijing 100029, China;2) Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085 , China;1) Institute of Geology, China Earthquake Administration, Beijing 100029, China;1) Institute of Geology, China Earthquake Administration, Beijing 100029, China;3) Institute of Engineering Mechanics, China Earthquake Administration, Harbin 150080, China
Abstract:Fine measurements have been conducted to temperatures and their gradients of six wells of the Jinsha River Groundwater Observational Network.The results show that the influence depths of sun radiation heat are 50m to 125m,average temperature gradients in the wells range from 0.11 to 2.81℃/hm and most are 1~2℃/hm,and the temperature gradients on varied depth sections of one well are highly changeable.Lithology of strata and their integrity,particularly high-angle crashed fault zones,have imposed major effects on the influence depths of sun radiation heat and temperature gradients of the wells.The micro dynamic characteristics of water temperature,such as coseismic effects,tidal effects and anomalies of the wells prior to earthquakes,probably depend,to a large degree,on the temperature gradients of the depths at which the water temperature sensors are settled.
Keywords:Temperature  Temperature gradient  Observational well  Jinsha River Groundwater Observational Network
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