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首页> 外文期刊>International Journal of Thermal Sciences >Buoyancy driven heat and species transports inside an energy storage enclosure partially saturated with thermal generating porous layers
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Buoyancy driven heat and species transports inside an energy storage enclosure partially saturated with thermal generating porous layers

机译:浮力驱动的热量和物种内部的储能箱内部,部分地饱和热产生多孔层

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AbstractCombined thermal and moisture convections in an enclosure partially filled with porous medium are numerically and analytically investigated, aiming to enhance moisture transport in the thermal energy storage unit. Two representative configurations of porous layers were taken into considerations, being placed centrally in the space or attached to the vertical walls. Moist air motions are simultaneously driven by the internal heat generation and external concentration difference imposed across the enclosure. Effects of Darcy number, mass diffusion coefficient, thermal Rayleigh number and buoyancy ratio on the heat and moisture transfer across the enclosure are discussed. Heat and mass transfer of the fluid/porous interface is analyzed as a function of the permeability of the porous layer. In the extreme case of high permeability and solutal-driven flow, a scale analysis is applied to predict the order of magnitudes involved in the boundary layer regime. Also, correlations for the average Nusselt and Sherwood numbers based on discrete numerical results are proposed. There is an agreement between the analytical and numerical results of moisture transfer rate, while a slight difference of heat transfer rate is observed due to different configurations of porous layers were imposed. Present research could benefit future development of sustainable building energy storage.Highlights?Heat and mass natural convection in an energy storage enclosure.?Flow boundary layer scale analysis is conducted to predict Nu and Sh.?NuApeaks around at Da?=?10?4, while NuBmonotonically increases with Da.?NuBis generally higher than NuA, excluding intermediate permeability.?Nu and Sh are nonlinear and monotonous functions of Kc.]]>
机译:<![CDATA [ 抽象 部分填充有多孔介质的外壳中的热量和水分对流在数值上和分析上进行研究,旨在增强水分在热能储能单元中运输。考虑到两种代表性层的多孔层配置,在空间中央放置在空间中或附接到垂直壁。潮湿的空气运动通过施加在外壳上的内部发热和外部浓度差异的同时驱动。讨论了达西数,质量扩散系数,热瑞利数和浮力比在外壳上的热量和水分转移的影响。作为多孔层的渗透性分析流体/多孔界面的热量和传质。在高渗透率和跟随流动的极端情况下,施加比例分析以预测边界层制度所涉及的幅度阶数。此外,提出了基于离散数值结果的平均NUSELET和SHERWOOD数量的相关性。在湿度转移率的分析和数值结果之间存在一致性,而由于施加不同的多孔层的不同构造,观察到传热速率的轻微差异。目前的研究可以使未来的可持续建筑能量存储的发展受益。 突出显示 储能机箱中的热量和质量自然对流。 流边界层比例分析进行预测Nu和Sh。 nu a < / ce:inf>在da?= 10 ?4 ,而nu b 用da单调增加。 nu b 通常高于nu a ,不包括中间渗透性。 ?< / ce:标签> nu和sh是kc的非线性和单调功能。 ]]>

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