| 双重介质含水层中井水位潮汐相位滞后现象的理论分析 |
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| 引用本文： | 王六桥 李善因. 2001: 双重介质含水层中井水位潮汐相位滞后现象的理论分析. 地震学报, 23(5): 530-535. |
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| 作者姓名： | 王六桥 李善因 |
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| 作者单位： | （中国乌鲁木齐830011新疆维吾尔自治区地震局） |
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| 摘 要： | 简略地介绍了双重介质含水层模型；推导出引潮力作用下双重介质含水层中渗流运动的偏微分方程；将此泛定的方程与潜水的Boulton方程进行数学类比，从而得出一个新的迟后给水项，为解释固体潮致井水位振荡相位滞后现象奠定了物理基础；通过对该泛定方程的分析，还发现该迟后给水项与深部含水层中存在的一种潮汐液流振荡现象有关．
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| 关 键 词： | 双重介质 水位潮汐 相位滞后 |
| 文章编号： | 0253-3782(2001)05-0530-06 |
| 修稿时间： | 2000-12-08 |
THEORETIC ANALYSIS ON PHASE DELAY PHENOMENA OF WELL WATER LEVEL TIDE IN THE DOUBLE MEDIUM AQUIFER MODEL |
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| Wang Liuqiao Li Shanyin. THEORETIC ANALYSIS ON PHASE DELAY PHENOMENA OF WELL WATER LEVEL TIDE IN THE DOUBLE MEDIUM AQUIFER MODEL[J]. Acta Seismologica Sinica, 2001, 23(5): 530-535 |
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| Authors: | Wang Liuqiao Li Shanyin |
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| Abstract: | A model of double medium aquifer is briefly introduced in this paper, a partial differential equation about seepage motion derived by the tidal stress i n the model layer is deduced. Compared this equation with Boulton equation used in the unconfined aquifer, a new lagging supply water term is obtained, which establish the physical basis for interpreting the phase delay phenomena of well water level caused by the solid tide. By analyzing the partial diffe rential equation, it is found that this lagging supply term is rela ted with the fluctuation of tide occurred in the deep aquifer. |
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| Keywords: | double medium aquifer water level tide phase lag |
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