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小颗粒的潮解和升华。

Deliquescence and efflorescence of small particles.

机构信息

Department of Environmental Sciences, Atmospheric Sciences Division, Brookhaven National Laboratory, Upton, New York 11973, USA.

出版信息

J Chem Phys. 2009 Nov 21;131(19):194705. doi: 10.1063/1.3251056.

Abstract

We examine size-dependent deliquescence/efflorescence phase transformation for particles down to several nanometers in size. Thermodynamic properties of inorganic salt particles, coated with aqueous solution layers of varying thickness and surrounded by vapor, are analyzed. A thin layer criterion (TLC) is introduced to define a limiting deliquescence relative humidity (RH(D)) for small particles. This requires: (1) equality of chemical potentials between salt in an undissolved core, and thin adsorbed solution layer, and (2) equality of chemical potentials between water in the thin layer and vapor phase. The usual bulk deliquescence conditions are recovered in the limit of large dry particle size. Nanosize particles are found to deliquesce at relative humidity just below the RH(D) on crossing a nucleation barrier, located at a critical solution layer thickness. This barrier vanishes precisely at the RH(D) defined by the TLC. Concepts and methods from nucleation theory including the kinetic potential, self-consistent nucleation theory, nucleation theorems, and the Gibbs dividing surface provide theoretical foundation and point to unifying features of small particle deliquescence/efflorescence processes. These include common thermodynamic area constructions, useful for interpretation of small particle water uptake measurements, and a common free-energy surface, with constant RH cross sections describing deliquescence and efflorescence related through the nucleation theorem.

摘要

我们研究了小至数纳米大小的颗粒的尺寸依赖性潮解/反潮相变。分析了涂有不同厚度水溶液层并被蒸汽包围的无机盐颗粒的热力学性质。引入了薄层准则(TLC)来定义小颗粒的限定潮解相对湿度(RH(D))。这需要:(1) 未溶解核中盐和薄吸附溶液层之间的化学势相等,以及 (2) 薄层中的水和蒸汽相之间的化学势相等。在大干燥颗粒尺寸的极限下,恢复了通常的批量潮解条件。纳米尺寸的颗粒在穿过位于临界溶液层厚度的成核势垒时,在相对湿度略低于 RH(D)的情况下潮解。该势垒恰好消失在 TLC 定义的 RH(D)处。成核理论的概念和方法,包括动力学势、自洽成核理论、成核定理和 Gibbs 分割面,为小颗粒潮解/反潮过程提供了理论基础,并指出了它们的统一特征。这些特征包括用于解释小颗粒水吸收测量的共同热力学面积构造,以及具有恒定 RH 截面的共同自由能表面,描述了潮解和反潮,它们通过成核定理相关联。

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