首页> 外文期刊>Journal of Crystallization Process and Technology >Effect of Constant Magnetic Field on Convective Heat Transfer through Anisotropic River Beds
【24h】

Effect of Constant Magnetic Field on Convective Heat Transfer through Anisotropic River Beds

机译:恒定磁场对通过各向异性河床对流换热的影响

获取原文
           

摘要

An analytical investigation is conducted to study the effect of magnetic field on convection heat transfer through packed porous beds which consists of a horizontal fluid layer (river bed) and a porous zone with anisotropic permeability and underlined by a surface heated by a constant temperature T1. The free surface of the fluid layer overlying the horizontal porous layer receives solar rays to length of day and is then considered heated isothermally at temperature T2 such as T1 < T2. Flow in porous medium is assumed to be governed by the generalized Brinkman-extended Darcy law and in the fluid layer by the Navier-Stokes model. The Beavers-Joseph condition is applied at the interface between the two layers. The influence of Hartmann number and hydrodynamic anisotropy on the convective phenomenon is investigated analytically. It is found that the magnetic field, the anisotropic permeability and the thickness of the porous lining, ε, have a strong influence of the geothermal convective flow and the heat transfer rate.
机译:进行了分析研究,以研究磁场对通过多孔多孔床的对流传热的影响,多孔多孔床由水平流体层(河床)和具有各向异性渗透性的多孔区域组成,并以加热到恒定温度 T1 。覆盖水平多孔层的流体层的自由表面接收日光直到一天,然后被认为是在温度 T2 T1 em> T2 。假定多孔介质中的流动受广义Brinkman扩展的达西定律支配,而流体层中的流动则受Navier-Stokes模型支配。 Beavers-Joseph条件应用于两层之间的界面。分析了哈特曼数和流体动力学各向异性对对流现象的影响。发现磁场,各向异性渗透率和多孔衬里的厚度ε对地热对流和传热速率有很大的影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号