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摘要:
The onset of thermal convection, due to heating from below in a system consisting of a fluid layer overlying a porous layer with anisotropic permeability and thermal diffusivity, is investigated analytically. The porous medium is both anisotropic in permeability whose principal axes are oriented in a direction that is oblique to the gravity vector and in thermal conductivity with principal directions coincident with the coordinate axes. The Beavers-Joseph condition is applied at the interface between the two layers. Based on parallel flow approximation theory, a linear stability analysis is conducted to study the geothermal river beds system and documented the effects of the physical parameters describing the problem. The critical Rayleigh numbers for both the fluid and porous layers corresponding, to the onset of convection arising from sudden heating and cooling at the boundaries are also predicted. The results obtained are in agreement with those found in the past for particular isotropic and anisotropic cases and for limiting cases concerning pure porous media and for pure fluid layer. It has demonstrated that the effects of anisotropic parameters are highly significant.
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篇名 Stability of Geothermal Convection in Anisotropic River Beds
来源期刊 工程(英文)(1947-3931) 学科 数学
关键词 River BEDS Critical RAYLEIGH NUMBERS ISOTROPIC ANISOTROPIC
年,卷(期) 2019,(7) 所属期刊栏目
研究方向 页码范围 343-365
页数 23页 分类号 O1
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River
BEDS
Critical
RAYLEIGH
NUMBERS
ISOTROPIC
ANISOTROPIC
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期刊影响力
工程(英文)(1947-3931)
月刊
1947-3931
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
367
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1
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0
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