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In this study we refer to a non-steady state, one-dimensional (on the x-axis), unconfined and saturated flow in an aquifer, described by the Boussinesq equation, combined with accretion. In accordance with the above, the moving boundary of the saturated area (toward x → +∝) serves as a horizontal water flux source to the unsaturated area. As time advances, the horizontally saturated zone, lying on the x-axis, becomes wider. A self-similar solution is derived that, after some mathematical manipulation, it is described in terms of Hypergeometric functions. The long-time behaviors of the solution describe the situation at which the water flux, that penetrates horizontally to the non-saturated zone, is equal to the water flux entering into the saturated zone.
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篇名 A Short Note on Self-Similar Solution to Unconfined Flow in an Aquifer with Accretion
来源期刊 流体动力学(英文) 学科 数学
关键词 BOUSSINESQ Equation SELF-SIMILAR Solution HYPERGEOMETRIC Function
年,卷(期) 2015,(1) 所属期刊栏目
研究方向 页码范围 51-57
页数 7页 分类号 O1
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BOUSSINESQ
Equation
SELF-SIMILAR
Solution
HYPERGEOMETRIC
Function
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期刊影响力
流体动力学(英文)
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2165-3852
武汉市江夏区汤逊湖北路38号光谷总部空间
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