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SIMULATION OF HEAT TRANSFER FROM CANOPY SURFACES USING LOW-REYNOLDS NUMBER K-ε MODEL

机译:低雷诺数K-ε模型模拟冠层表面的传热

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This study focuses on the Convective Heat Transfer Coefficient (CHTC) from urban building surfaces by numerical simulation. The heat transfer effects because of various geometrical and physical properties of urban areas exhibits a differential heating and uncomfortable environment compared to rural regions called as Urban Heat Island (UHI) phenomena. Investigation of Convective heat transfer coefficient becomes more important in the study of urban heat island phenomena. Experimental simulation of urban area with various urban canopy cases in thermally stratified wind tunnel is employed for the heat transfer kind of investigations in urban area. But, it is not an easy task in wind tunnel experiments to evaluate local CHTC, which vary on individual canyon surfaces transfer such as building roof, walls and ground. Numerical simulation validated by wind tunnel experiments can be an alternative for the prediction of CHTC from building surfaces in an urban area. In our study, Water evaporation technique used in wind tunnel experiment for the evaluation of convective heat transfer coefficient and naphthalene sublimation technique conducted by other researchers are used to validate the low-Reynolds-number k-ε model which was used for the evaluation of CHTC from surfaces. The calculated CFD results showed good agreement with both water evaporation technique and naphthalene sublimation experimental results. It is found that the low-Reynolds-number k-ε model is reliable for the investigations pertaining to heat transfer from urban canopy.
机译:本研究通过数值模拟研究了城市建筑表面的对流传热系数(CHTC)。与被称为城市热岛(UHI)现象的农村地区相比,由于城市地区的各种几何和物理特性,传热效果表现出不同的供热和不舒适的环境。对流传热系数的研究在城市热岛现象的研究中变得越来越重要。在热分层风洞中,以不同城市冠层情况下的市区模拟为研究对象。但是,在风洞实验中评估本地CHTC并非易事,因为局部CHTC随个别峡谷表面转移(例如建筑物的屋顶,墙壁和地面)而变化。通过风洞实验验证的数值模拟可以替代从市区建筑表面预测CHTC的方法。在我们的研究中,使用风洞实验中使用的水蒸发技术评估对流换热系数,并使用其他研究人员进行的萘升华技术来验证用于评估CHTC的低雷诺数k-ε模型从表面。计算出的CFD结果与水蒸发技术和萘升华实验结果均具有良好的一致性。发现低雷诺数k-ε模型对于与城市雨棚传热有关的研究是可靠的。

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