Mixed convective flow analysis of a Maxwell fluid with double diffusion theory on a vertically exponentially stretching surface

IF 5.7 3区 环境科学与生态学 Q1 WATER RESOURCES Applied Water Science Pub Date : 2024-07-09 DOI:10.1007/s13201-024-02235-x
Muhammad Naveed Khan, Zhentao Wang, N. Ameer Ahammad, Shahram Rezapour, Meshal Shutaywi, Naim Ben Ali, Mohamed Abdelghany Elkotb
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Abstract

It observers that an object is submerged in a liquid, more pressure is applied to its bottom surface than its top surface, as a result pressure rises within depth of fluids. A buoyancy force is generated due to the pressure difference. In the current investigation, the mathematical formulation of bio-convective stagnation point flow of a radiative Maxwell fluid with multiple slip effect on an exponentially porous stretching surface is analyzed thoroughly. The buoyancy assisting and opposing conditions with magnetic field are discussed in the current investigation. Moreover, the energy and concertation equations are formulated by the utilization of Cattaneo–Christov theory and non-uniform heat source/sink. The flow model is developed in the form of partial derivatives, then use the similarity variables to convert the physical system into nonlinear ordinary derivative. The nonlinear system is tackled numerically with the help of Bvp4c approach on the MATLAB. The graphical upshots for various emerging parameter are observed with two aspects: buoyancy assisting \(\left( {\lambda > 0} \right)\) and buoyancy opposing \(\left( {\lambda < 0} \right)\). The observation shows that the greater values of mixed convection parameter improves the fluid velocity for assisting flow \(\left( {\lambda > 0} \right)\), while declining trend is noticing for opposing flow situation \(\left( {\lambda > 0} \right)\). Further, it is worth noticing that stronger inputs of thermal and concentration relaxation parameter yield lesser thermal and concentration diffusivity, which reduces the temperature and nanoparticles concentration.

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垂直指数拉伸表面上采用双重扩散理论的麦克斯韦流体混合对流分析
它观察到物体浸没在液体中时,其底面受到的压力大于上表面,因此在液体深度内压力会上升。压力差会产生浮力。在当前的研究中,对具有多重滑移效应的辐射麦克斯韦流体在指数多孔拉伸表面上的生物对流停滞点流动的数学公式进行了深入分析。本次研究讨论了磁场的浮力辅助条件和对立条件。此外,还利用卡塔尼奥-克里斯托夫理论和非均匀热源/沉积计算了能量方程和协调方程。以偏导数的形式建立流动模型,然后利用相似变量将物理系统转换为非线性常导数。借助 Bvp4c 方法在 MATLAB 上对非线性系统进行数值处理。从两个方面观察了各种新出现参数的图示:浮力辅助(\left( {\lambda > 0} \right)\)和浮力反对(\left( {\lambda < 0} \right)\)。观察结果表明,混合对流参数值越大,助流情况下的流体速度越快,而对流情况下的流体速度呈下降趋势。此外,值得注意的是,热弛豫参数和浓度弛豫参数的输入越大,热扩散率和浓度扩散率就越小,从而降低了温度和纳米粒子浓度。
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来源期刊
Applied Water Science
Applied Water Science WATER RESOURCES-
CiteScore
9.90
自引率
3.60%
发文量
268
审稿时长
13 weeks
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