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The Interaction Between the Substrate and Frost Layer Through Condensate Distribution

机译:凝析物分布对基质与霜层的相互作用

摘要

Microscopic observations of frost deposition on a variety of substrates havingdifferent contact angles, (polytetrafluoroethylene PTFE, kapton, glass and others) allowthe quantification of substrate effects on frost structure during inception and growth. Thedeposition of water vapor at the beginning of the frosting process on a clean glasssubstrate is found to be as condensate (condensation frosting) rather than as ice(ablimation frosting) for a substrate temperatures above -33??C and an absolute humidityabove 0.15 g/kg. The inception of "condensation frosting" (the condensation period andearly frost growth period) is further examined microscopically as a function of air andsubstrate temperatures, absolute humidity, and substrate contact angle. The waterdistribution on the substrate at the end of the condensation period is found to be stronglydependent on substrate temperature, humidity ratio, and substrate contact angle. Coldersubstrates result in smaller more uniform droplets and substrates with lower contactangles result in shorter, larger diameter droplets with a larger percentage of the substratecovered. The effective density of the condensate on hydrophobic substrates is found tobe lower than that on hydrophilic substrates. The structure and form of the iceimmediately after freezing is substrate dependent. High-speed imaging of the freezingprocess is used to study the propagation of the freezing front in a droplet. The imagesshow that a protrusion is formed at the top of the droplets during freezing. Fromobservations, this protrusion is hypothesized to result from the convective condition atthe droplet surface and the difference in specific volume between liquid and solid water.Additionally, the apparent ejection of water vapor during freezing of a droplet on a hydrophobic substrate was observed. This ejection of water vapor is thought to be causedby the wanning of the droplet caused by the release of latent heat. In contrast to trendsobserved during the early growth period, the growth rate of mature frost is found todecrease with substrate contact angle while frost density is found to increase. Thisbehavior is explained in terms of the effect of substrate contact angle on the structure andform of the incipient frost, which constitutes the initial condition for further (mature)frost growth. A higher conductivity layer is formed on the hydrophilic than on thehydrophobic substrate. A model relating crystal orientation to conductivity is used tosimulate the frost growth rate and density on the two different substrates and match theexperimental data. Using similar reasoning, the higher conductivity frost formed oncolder substrates is also explained.
机译:在各种具有不同接触角的基材(聚四氟乙烯PTFE,聚醚砜,玻璃等)上的霜沉积物的显微观察可以量化基材在开始和生长过程中对霜冻结构的影响。发现在结霜过程开始时,在干净的玻璃基板上沉积的水蒸气是冷凝物(冷凝结霜),而不是冰(融化结霜)(对于基板温度高于-33?C和绝对湿度高于0.15 g /)。公斤。根据空气和基材温度,绝对湿度和基材接触角的函数,进一步从微观上检查“凝结霜”的开始(凝结期和早期霜生期)。发现在冷凝时间结束时在基板上的水分布强烈地取决于基板温度,湿度比和基板接触角。较冷的基材会导致较小,更均匀的液滴,而具有较小接触角的基材会导致较短,较大​​直径的液滴,并且覆盖的基材比例较大。发现在疏水性基材上的冷凝物的有效密度低于在亲水性基材上的冷凝物的有效密度。冷冻后立即制冰的结构和形式取决于底物。冷冻过程的高速成像用于研究液滴中冷冻前沿的传播。图像显示在冷冻过程中,液滴顶部形成了突起。根据观察,推测该突起是由于液滴表面的对流条件和液态水与固态水之间的比容差异引起的。此外,观察到液滴在疏水性基质上冻结过程中水蒸气的表观喷射。水蒸气的这种喷射被认为是由于潜热释放引起的液滴的减少而引起的。与生长初期观察到的趋势相反,发现成熟霜的生长速率随基质接触角而降低,而霜密度却升高。用基底接触角对初期霜冻的结构和形式的影响来解释这种行为,这构成了进一步(成熟)霜冻生长的初始条件。在亲水性上比在疏水性基底上形成更高的电导率层。将晶体取向与电导率相关的模型用于模拟两种不同基质上的霜冻生长速率和密度,并匹配实验数据。使用类似的推理,还解释了在较冷的基底上形成的较高电导率的霜。

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