Department of Applied Environmental Science and Bert Bolin Centre for Climate Research, Stockholm University, SE-10691 Stockholm, Sweden.
J Phys Chem A. 2013 Jan 17;117(2):410-20. doi: 10.1021/jp310594e. Epub 2013 Jan 9.
The condensational growth of submicrometer aerosol particles to climate relevant sizes is sensitive to their ability to accommodate vapor molecules, which is described by the mass accommodation coefficient. However, the underlying processes are not yet fully understood. We have simulated the mass accommodation and evaporation processes of water using molecular dynamics, and the results are compared to the condensation equations derived from the kinetic gas theory to shed light on the compatibility of the two. Molecular dynamics simulations were performed for a planar TIP4P-Ew water surface at four temperatures in the range 268-300 K as well as two droplets, with radii of 1.92 and 4.14 nm at T = 273.15 K. The evaporation flux from molecular dynamics was found to be in good qualitative agreement with that predicted by the simple kinetic condensation equations. Water droplet growth was also modeled with the kinetic multilayer model KM-GAP of Shiraiwa et al. [Atmos. Chem. Phys. 2012, 12, 2777]. It was found that, due to the fast transport across the interface, the growth of a pure water droplet is controlled by gas phase diffusion. These facts indicate that the simple kinetic treatment is sufficient in describing pure water condensation and evaporation. The droplet size was found to have minimal effect on the value of the mass accommodation coefficient. The mass accommodation coefficient was found to be unity (within 0.004) for all studied surfaces, which is in agreement with previous simulation work. Additionally, the simulated evaporation fluxes imply that the evaporation coefficient is also unity. Comparing the evaporation rates of the mass accommodation and evaporation simulations indicated that the high collision flux, corresponding to high supersaturation, present in typical molecular dynamics mass accommodation simulations can under certain conditions lead to an increase in the evaporation rate. Consequently, in such situations the mass accommodation coefficient can be overestimated, but in the present cases the corrected values were still close to unity with the lowest value at ≈0.99.
亚微米气溶胶颗粒凝结增长到与气候相关的尺寸对其容纳蒸汽分子的能力很敏感,这由质量吸收系数来描述。然而,其潜在过程尚未完全了解。我们使用分子动力学模拟了水的质量吸收和蒸发过程,并将结果与从动力学气体理论推导出的凝结方程进行了比较,以阐明两者的兼容性。在 268-300 K 的范围内的四个温度以及在 T = 273.15 K 时的两个半径为 1.92 和 4.14nm 的液滴上,对平面 TIP4P-Ew 水表面进行了分子动力学模拟。从分子动力学得到的蒸发通量与简单的动力学凝结方程预测的结果具有很好的定性一致性。还使用 Shiraiwa 等人的动力学多层模型 KM-GAP 对水滴生长进行了建模。[Atmos. Chem. Phys. 2012, 12, 2777]。结果发现,由于界面快速传输,纯水液滴的生长受气相扩散控制。这些事实表明,简单的动力学处理足以描述纯水的凝结和蒸发。发现液滴尺寸对质量吸收系数的值影响最小。对于所有研究的表面,质量吸收系数均为 1(在 0.004 以内),这与先前的模拟工作一致。此外,模拟的蒸发通量表明蒸发系数也为 1。比较质量吸收和蒸发模拟的蒸发速率表明,在典型的分子动力学质量吸收模拟中存在的高碰撞通量(对应于高过饱和度)在某些条件下可能导致蒸发速率增加。因此,在这种情况下,质量吸收系数可能会被高估,但在目前情况下,校正值仍接近 1,最低值约为 0.99。