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| 引用本文： | 张卫华,王秋良,李井冈,罗俊秋,郭熙枝.????????λ???????????????????о?[J].大地测量与地球动力学,2012,32(4):29-32. |
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| 作者姓名： | 张卫华 王秋良 李井冈 罗俊秋 郭熙枝 |
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| 作者单位： | 中国地震局地震研究所(地震大地测量重点实验室),武汉430071;中国地震局地壳应力研究所武汉科技创新基地,武汉430071 |
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| 基金项目： | 中国长江三峡工程开发总公司专项基金(sxsn/2377) |
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| 摘 要： | ???????????????????????????????????????????λ??????????????????????????????????????????????????????????￡????λ????仯???????????????????????????????????????????????????????????????仯??????????????????????????????????????????й??
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| 关 键 词： | ??????? ???λ ????? ????????? ????? |
RESEARCH ON RELATION BETWEEN LEVEL EARTH TIDE AND PARAMETER OF THREE-GORGE WELL AQUIFER |
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| Zhang Weihua
,
Wang Qiuliang
,
Li Jinggang
,
Luo Junqiu
,
Guo Xizhi.RESEARCH ON RELATION BETWEEN LEVEL EARTH TIDE AND PARAMETER OF THREE-GORGE WELL AQUIFER[J].Journal of Geodesy and Geodynamics,2012,32(4):29-32. |
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| Authors: | Zhang Weihua Wang Qiuliang Li Jinggang Luo Junqiu Guo Xizhi |
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| Institution: | 1,2) 1)Key Laboratory of Earthquake Geodesy,Institute of Seismology,CEA,Wuhan 4300712)Wuhan Base of Institute of Crustal Dynamics,CEA,Wuhan 430071 |
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| Abstract: | On the basis of geological tectonic background and borehole structure,the relation between the characteristic difference of earth tide of well water level and physical parameters of confined aquifers at 8 stations of the ground water monitoring well network in the Three Gorges was analysised.The following conclutions are drawn that the earth tide of well water level varies inversely as the parameters of confined aquifers,with the porosity of the aquifer being constant;The earth tide of well water level varies inversely as porosity of the aquifer,with the the parameters of confined aquifers being constant,in addition,it was related to coefficient of transmissibility of confined aquifers,fault type,distance between well point and fault. |
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| Keywords: | tide characteristic well level aquifer coefficient of volume compressibility porosity |
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