利用点汇叠加法建立湿空气中水汽滴状凝结的数值模型

Tridibesh Chattoraj, Avishek Chatterjee, Tibin M Thomas, Pallab Sinha Mahapatra, Achintya Mukhopadhyay
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引用次数: 0

摘要

在过冷的疏水表面上,潮湿空气中的水蒸气会凝结成离散的液滴,并随着时间的推移而增长。当周围的水汽场渗透到液滴中时,液滴附近的水汽浓度场会影响每个液滴的生长。水蒸气分子在潮湿空气中的扩散及其与液-汽界面的相互作用会影响单个冷凝液滴的生长。然而,大多数现有的凝结数值模型都忽略了邻近液滴和每个液滴周围水汽浓度场的影响。本研究采用了点汇叠加法(PSSM),通过近似计算液滴间的相互作用和周围蒸汽浓度场的影响来计算冷凝液滴的增长率。此外,本研究还通过捕捉凝聚、液滴排出和再成核等凝结动态,模拟了垂直方向疏水表面上的凝结过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Numerical modelling of dropwise condensation of water vapor from humid air using point sink superposition method

On a subcooled hydrophobic surface, the water vapor from humid air condenses into discrete liquid droplets and grows over time. The water vapor concentration field of the droplets in their immediate vicinity influences the growth of each droplet as the surrounding vapor field permeates the droplets. The diffusion of water vapor molecules in the humid air and their interaction with the liquid-vapor interface govern the growth of the individual condensate droplets. Nevertheless, most existing numerical models for condensation neglect the effect of neighboring droplets and the vapor concentration field surrounding each droplet. In this study, the point sink superposition method (PSSM) is used to calculate the growth rate of condensing droplets by approximating the inter-droplet interaction and the influences of the surrounding vapor concentration field. Further, this study simulated the condensation process on a vertically oriented hydrophobic surface by capturing condensation dynamics such as coalescence, droplet drainage, and renucleation.

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