Department of Chemistry and Biochemistry, University of Maryland, College Park, College Park, Maryland 20742, United States.
Department of Chemical and Biomolecular Engineering, University of Maryland, College Park, College Park, Maryland 20742, United States.
Environ Sci Technol. 2024 Sep 3;58(35):15551-15561. doi: 10.1021/acs.est.4c02356. Epub 2024 Aug 19.
Water vapor condensation on hygroscopic aerosol particles plays an important role in cloud formation, climate change, secondary aerosol formation, and aerosol aging. Conventional understanding considers deliquescence of nanosized hygroscopic aerosol particles a nearly instantaneous solid to liquid phase transition. However, the nanoscale dynamics of water condensation and aerosol particle dissolution prior to and during deliquescence remain obscure due to a lack of high spatial and temporal resolution single particle measurements. Here we use real time transmission electron microscopy (TEM) imaging of individual sodium chloride (NaCl) nanoparticles to demonstrate that water adsorption and aerosol particle dissolution prior to and during deliquescence is a multistep dynamic process. Water condensation and aerosol particle dissolution was investigated for lab generated NaCl aerosols and found to occur in three distinct stages as a function of increasing relative humidity (RH). First, a < 100 nm water layer adsorbed on the NaCl cubes and caused sharp corners to dissolve and truncate. The water layer grew to several hundred nanometers with increasing RH and was rapidly saturated with solute, as evidenced by halting of particle dissolution. Adjacent cube corners displayed second-scale curvature fluctuations with no net particle dissolution or water layer thickness change. We propose that droplet solute concentration fluctuations drove NaCl transport from regions of high local curvature to regions of low curvature. Finally, we observed coexistence of a liquid water droplet and aerosol particle immediately prior to deliquescence. Particles dissolved discretely along single crystallographic directions, separated by few second lag times with no dissolution. This work demonstrates that deliquescence of simple pure salt particles with sizes in the range of 100 nm to several microns is not an instantaneous phase transition and instead involves a range of complex dissolution and water condensation dynamics.
水汽在吸湿性气溶胶颗粒上的凝结在云形成、气候变化、二次气溶胶形成和气溶胶老化中起着重要作用。传统的认识认为纳米级吸湿性气溶胶颗粒的潮解是一个几乎瞬间的固-液相转变。然而,由于缺乏高时空分辨率的单颗粒测量,在潮解之前和期间,水凝结和气溶胶颗粒溶解的纳米级动力学仍然不清楚。在这里,我们使用实时透射电子显微镜(TEM)对单个氯化钠(NaCl)纳米颗粒的成像,证明了在潮解之前和期间,水的吸附和气溶胶颗粒的溶解是一个多步骤的动态过程。我们研究了实验室生成的 NaCl 气溶胶的水凝结和气溶胶颗粒溶解,发现它们作为相对湿度(RH)增加的函数,发生在三个不同的阶段。首先,<100nm 的水层吸附在 NaCl 立方体上,导致尖锐的角溶解和截断。随着 RH 的增加,水层生长到几百纳米,并迅速被溶质饱和,这可以从颗粒溶解的停止中得到证明。相邻立方体角显示出第二尺度的曲率波动,没有净颗粒溶解或水层厚度变化。我们提出,液滴溶质浓度波动驱动 NaCl 从高局部曲率区域向低曲率区域迁移。最后,我们观察到在潮解之前,存在一个液态水滴和一个气溶胶颗粒共存。颗粒沿着单一的晶面方向离散溶解,间隔几秒钟的滞后时间,没有溶解。这项工作表明,在 100nm 到几微米范围内的简单纯盐颗粒的潮解不是一个瞬间的相变,而是涉及一系列复杂的溶解和水凝结动力学。