School of Engineering and Applied Sciences & Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts, USA.
Phys Chem Chem Phys. 2009 Nov 21;11(43):10095-107. doi: 10.1039/b910432a. Epub 2009 Sep 15.
The deliquescence phase transitions of populations of internally mixed particles of solid ammonium bisulfate and letovicite, having overall extents of neutralization between 0.60 and 0.75 and diameters between 15 and 60 nm, were studied using a hygroscopic tandem nano-differential mobility analyzer (HTnDMA). Populations having particles sufficiently small or large, as well as particles sufficiently acidic or neutralized, behaved as expected, with prompt transitions of all particles at a single relative humidity. Populations having particles of simultaneously intermediate diameter and acidity, however, behaved differently and unexpectedly. Subpopulations of individual particles did exhibit prompt deliquescence but did so over a broad range of relative humidity (RH) for the entire population. For example, some particles of 20-nm diameter and an extent of neutralization of 0.65 deliquesced promptly at as low as 38% RH, whereas some particles in the same experiment deliquesced promptly at as high as 59% RH. Across this 21% RH span, prompt deliquescence of particle subpopulations was observed, which resulted in the continuous deliquescence of the population as the aerosol progressed from dominantly solid to dominantly aqueous particles for increasing RH. Morphological differences among particles in different subpopulations that drive variable rates of water uptake, such as coatings of letovicite of varying thickness, porosity, and hence water permeability on cores of ammonium bisulfate, are hypothesized to explain these observations.
采用吸湿串联纳米差分迁移率分析仪(HTnDMA)研究了中和度在 0.60 到 0.75 之间、直径在 15 到 60nm 之间的内混合固体硫酸氢铵和 letovicite 颗粒的复相混合物的潮解相转变。对于足够小或足够大的颗粒,以及足够酸性或中和的颗粒,其行为符合预期,所有颗粒在单一相对湿度下迅速转变。然而,对于具有同时处于中间直径和酸度的颗粒的颗粒混合物,其行为则不同且出乎意料。个别颗粒的亚群确实表现出迅速的潮解,但对于整个颗粒混合物而言,潮解发生在很宽的相对湿度(RH)范围内。例如,一些直径为 20nm 且中和度为 0.65 的颗粒在低至 38%RH 时迅速潮解,而在同一实验中,一些颗粒在高达 59%RH 时迅速潮解。在这个 21%RH 跨度内,观察到颗粒亚群的迅速潮解,这导致气溶胶从主要为固态颗粒向主要为水相颗粒的转变,随着 RH 的增加,颗粒混合物连续潮解。假设不同亚群中颗粒之间的形态差异导致了不同的吸水速率,例如 letovicite 的厚度、孔隙率和因此的硫酸氢铵核心的水渗透性存在差异,这些差异可以解释这些观察结果。