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Temperature-dependent formation of NaCl dihydrate in levitated NaCl and sea salt aerosol particles

机译:悬浮NaCl和海盐气溶胶颗粒中NaCl二水合物的温度依赖性形成

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Recent laboratory studies indicate that the hydrated form of crystalline NaCl is potentially important for atmospheric processes involving depositional ice nucleation on NaCl dihydrate particles under cirrus cloud conditions. However, recent experimental studies reported a strong discrepancy between the temperature intervals where the efflorescence of NaCl dihydrate has been observed. Here we report the measurements of the volume specific nucleation rate of crystalline NaCl in the aqueous solution droplets of pure NaCl suspended in an electrodynamic balance at constant temperature and humidity in the range from 250Kto 241 K. Based on these measurements, we derive the interfacial energy of crystalline NaCl dihydrate in a supersaturated NaCl solution and determined its temperature dependence. Taking into account both temperature and concentration dependence of nucleation rate coefficients, we explain the difference in the observed fractions of NaCl dihydrate reported in the previous studies. Applying the heterogeneous classical nucleation theory model, we have been able to reproduce the 5K shift of the NaCl dihydrate efflorescence curve observed for the sea salt aerosol particles, assuming the presence of super-micron solid inclusions (hypothetically gypsum or hemihydrate of CaSO4). These results support the notion that the phase transitions in microscopic droplets of supersaturated solution should be interpreted by accounting for the stochastic nature of homogeneous and heterogeneous nucleation and cannot be understood on the ground of bulk phase diagrams alone. (C) 2016Author(s).
机译:最近的实验室研究表明,结晶状氯化钠的水合形式对于涉及卷云条件下在二水合氯化钠颗粒上沉积冰成核的大气过程潜在重要。然而,最近的实验研究报道了在观察到二水合氯化钠的风化的温度间隔之间存在很大差异。在这里,我们报告了在250K至241K的恒定温度和湿度下,以电平衡方式悬浮在纯NaCl水溶液中的纯NaCl水溶液液滴中结晶NaCl的体积比成核率的测量结果。基于这些测量结果,我们得出了界面能饱和NaCl溶液中二水合NaCl结晶的含量,并确定其温度依赖性。考虑到成核速率系数的温度和浓度依赖性,我们解释了先前研究中报道的观察到的NaCl二水合物馏分的差异。应用异质经典成核理论模型,我们能够重现观察到的海盐气溶胶颗粒的NaCl二水合物风化曲线的5K位移,假设存在超微米固体夹杂物(假设为CaSO4的石膏或半水合物)。这些结果支持这样的观念,即过饱和溶液的微观液滴中的相变应通过解释均相和异相成核的随机性质来解释,而不能仅根据整体相图来理解。 (C)2016作者

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