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Analysis of the effect of water activity on ice formation using a new thermodynamic framework

机译:使用新的热力学框架分析水分活度对冰形成的影响

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In this work a new thermodynamic framework is developed and used to investigate the effect of water activity on the formation of ice within supercooled droplets. The new framework is based on a novel concept where the interface is assumed to be made of liquid molecules “trapped” by the solid matrix. It also accounts for the change in the composition of the liquid phase upon nucleation. Using this framework, new expressions are developed for the critical ice germ size and the nucleation work with explicit dependencies on temperature and water activity. However unlike previous approaches, the new model does not depend on the interfacial tension between liquid and ice. The thermodynamic framework is introduced within classical nucleation theory to study the effect of water activity on the ice nucleation rate. Comparison against experimental results shows that the new approach is able to reproduce the observed effect of water activity on the nucleation rate and the freezing temperature. It allows for the first time a phenomenological derivation of the constant shift in water activity between melting and nucleation. The new framework offers a consistent thermodynamic view of ice nucleation, simple enough to be applied in atmospheric models of cloud formation.
机译:在这项工作中,开发了一种新的热力学框架,并用于研究水活度对过冷液滴中冰的形成的影响。新框架基于一个新颖的概念,其中假定界面由固体基质“捕获”的液体分子组成。它也解释了成核后液相组成的变化。使用此框架,针对临界冰胚大小和核化工作开发了新的表达式,并且显着依赖于温度和水分活度。但是,与以前的方法不同,新模型不依赖于液体和冰之间的界面张力。在经典形核理论中引入了热力学框架,以研究水活度对冰形核速率的影响。与实验结果的比较表明,新方法能够重现观察到的水分活度对成核速率和冻结温度的影响。它首次实现了融化和成核之间水活度恒定变化的现象学推导。新框架提供了一致的冰核热力学视图,其足够简单,可以应用于云层形成的大气模型中。

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