刘滔, 林文贤. 低Pr数流体非稳态自然对流流动的标度分析[J]. 力学与实践, 2007, 29(1): 23-28. DOI: 10.6052/1000-0992-2005-505
引用本文: 刘滔, 林文贤. 低Pr数流体非稳态自然对流流动的标度分析[J]. 力学与实践, 2007, 29(1): 23-28. DOI: 10.6052/1000-0992-2005-505
SCALING ANALYSIS OF UNSTEADY NATURAL CONVECTION FLOW OF A FLUID WITH LOW PRANDTL NUMBER[J]. MECHANICS IN ENGINEERING, 2007, 29(1): 23-28. DOI: 10.6052/1000-0992-2005-505
Citation: SCALING ANALYSIS OF UNSTEADY NATURAL CONVECTION FLOW OF A FLUID WITH LOW PRANDTL NUMBER[J]. MECHANICS IN ENGINEERING, 2007, 29(1): 23-28. DOI: 10.6052/1000-0992-2005-505

低Pr数流体非稳态自然对流流动的标度分析

SCALING ANALYSIS OF UNSTEADY NATURAL CONVECTION FLOW OF A FLUID WITH LOW PRANDTL NUMBER

  • 摘要: 施加了恒定热通量的竖直平板置于静止的均匀或线性分层流体中会在板壁上形成自然对流流 动. 它在达到稳态前将先历经起始和过渡两个阶段. 而表征其瞬时流动特征的主要参数是壁温、热边界层厚度、内层和外层速度边界层厚度、边界层内竖直方向的最大速度、以及层流边界层发展达到稳态所需的时间. 利用标度分析得到了均匀和线性分层低普郎特数(Pr<1)流体沿恒定热通量竖直平板的非稳态自然对流流动在各个发展阶段的标度关系.

     

    Abstract: A natural convection flow will be formed adjacent to a verticalplane immersed in a quiescent homogeneous or linearly-stratified fluid afterthe plate is heated with a uniform thermal flux. The flow will undergo astart-up stage, followed by a transitional stage, before reaching a steadystate. The transient behavior of the flow is parameterized by the platetemperature, the thermal boundary-layer thickness, the inner and outervelocity boundary-layer thicknesses, the maximum vertical velocity withinthe boundary layer, and the time for the boundary layer to reach the steadystate. In this paper, a scaling analysis is used to obtain scaling laws for all the parameters at various development stages of unsteady natural convection boundary-layer flow in homogeneous and linearly-stratified fluidswith low Prandtl number (Pr<1) along a vertical plate heated with a uniform thermal flux.

     

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