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Transient natural ventilation of a room with a distributed heat source

机译:具有分布式热源的房间的瞬时自然通风

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摘要

We report on an experimental and theoretical study of the transient flows which develop as a naturally ventilated room adjusts from one temperature to another. We focus on a room heated from below by a uniform heat source, with both high-and low-level ventilation openings. Depending on the initial temperature of the room relative to (i) the final equilibrium temperature and (ii) the exterior temperature, three different modes of ventilation may develop. First, if the room temperature lies between the exterior and the equilibrium temperature, the interior remains well-mixed and gradually heats up to the equilibrium temperature. Secondly, if the room is initially warmer than the equilibrium temperature, then a thermal stratification develops in which the upper layer of originally hot air is displaced upwards by a lower layer of relatively cool inflowing air. At the interface, some mixing occurs owing to the effects of penetrative convection. Thirdly, if the room is initially cooler than the exterior, then on opening the vents, the original air is displaced downwards and a layer of ambient air deepens from above. As this lower layer drains, it is eventually heated to the ambient temperature, and is then able to mix into the overlying layer of external air, and the room becomes well-mixed. For each case, we present new laboratory experiments and compare these with some new quantitative models of the transient flows. We conclude by considering the implications of our work for natural ventilation of large auditoria.
机译:我们报告了对瞬态流量的实验和理论研究,这些瞬态流量随着自然通风的房间从一个温度调整到另一个温度而发展。我们关注的是一个由均匀热源从下方加热的房间,该房间同时设有高低通风口。根据相对于(i)最终平衡温度和(ii)外部温度的房间初始温度,可能会形成三种不同的通风方式。首先,如果室温介于外部和平衡温度之间,则内部保持充分混合并逐渐加热到平衡温度。其次,如果房间最初比平衡温度更热,则会形成热分层,其中原始热空气的上层被相对较冷的流入空气的下层向上移位。在界面处,由于穿透对流的作用,发生了一些混合。第三,如果房间最初比外部凉爽,则在打开通风孔时,原始空气会向下移位,并且周围的空气层会从上方加深。随着下层的排干,最终将其加热到环境温度,然后能够混入上层外部空气中,从而使房间充分混合。对于每种情况,我们都会提供新的实验室实验,并将其与瞬态流量的一些新定量模型进行比较。最后,我们考虑了我们的工作对大礼堂自然通风的影响。

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