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摘要:
In this article, the model of a non-Newtonian fluid (Thixotropic) flow past a vertical surface in the presence of exponential space and temperature dependent heat source in a thermally stratified medium is studied. It is assumed that free convection is induced by buoyancy and exponentially decaying internal heat source across the space. The dynamic viscosity is taken to be constant and thermal conductivity of this particular fluid model is assumed to vary linearly with temperature. Thermal stratification has been properly incorporated into the governing equation so that its effect can be revealed and properly reported. The governing partial differential equations describing the model are transformed and parameterized to a system of non-linear ordinary differential equation using similarity transformations. Approximate analytic solutions were obtained by adopting Optimal Homotopy Analysis Method (OHAM). The results show that for both cases of non-Newtonian parameters (Thixotropic) (K1=K2=0?& K1=K2=1.0), increasing stratification parameters, relate to decreasing in the heat energy entering into the fluid region and thus reducing the temperature of the Thixotropic fluid as it flows.
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篇名 Optimal Homotopy Analysis of MHD Natural Convection Flow of Thixotropic Fluid under Subjection of Thermal Stratification: Boundary Layer Analysis
来源期刊 美国计算数学期刊(英文) 学科 数学
关键词 Thixotropic FLUID NATURAL Convection Thermal Stratification OPTIMAL Homotopy ANALYSIS Method and BOUNDARY Layer ANALYSIS
年,卷(期) 2019,(2) 所属期刊栏目
研究方向 页码范围 116-131
页数 16页 分类号 O1
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Thixotropic
FLUID
NATURAL
Convection
Thermal
Stratification
OPTIMAL
Homotopy
ANALYSIS
Method
and
BOUNDARY
Layer
ANALYSIS
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美国计算数学期刊(英文)
季刊
2161-1203
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)
355
总下载数(次)
1
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0
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