Water uptake coefficients and deliquescence of NaCl nanoparticles at atmospheric relative humidities from molecular dynamics simulations

被引:29
作者
Bahadur, Ranjit [1 ]
Russell, Lynn M. [1 ]
机构
[1] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
基金
美国国家科学基金会;
关键词
D O I
10.1063/1.2971040
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Deliquescence properties of sodium chloride are size dependent for particles smaller than 100 nm. Molecular dynamics (MD) simulations are used to determine deliquescence relative humidity (DRH) for particles in this size range by modeling idealized particles in contact with humid air. Constant humidity conditions are simulated by inclusion of a liquid reservoir of NaCl solution in contact with the vapor phase, which acts as a source of water molecules as uptake by the nanoparticle proceeds. DRH is bounded between the minimum humidity at which sustained water accumulation is observed at the particle surface and the maximum humidity at which water accumulation is not observed. Complete formation of a liquid layer is not observed due to computational limitations. The DRH determined increases with decreasing particle diameter, rising to between 91% and 93% for a 2.2 nm particle and between 81% and 85% for an 11 nm particle, higher than the 75% expected for particles larger than 100 nm. The simulated size dependence of DRH agrees well with predictions from bulk thermodynamic models and appears to converge with measurements for sizes larger than 10 nm. Complete deliquescence of nanoparticles in the 2-11 nm size range requires between 1 and 100 mu s, exceeding the available computational resources for this study. Water uptake coefficients are near 0.1 with a negligible contribution from diffusion effects. Planar uptake coefficients decrease from 0.41 to 0.09 with increasing fractional water coverage from 0.002 to 1, showing a linear dependence on the logarithm of the coverage fraction with a slope of -0.08 +/- 0.01 (representing the effect of solvation). Particle uptake coefficients increase from 0.13 at 11 nm to 0.65 at 2.2 nm, showing a linear dependence on the logarithm of the edge fraction (which is a function of diameter) with a slope of 0.74 +/- 0.04 (representing larger edge effects in smaller particles). (C) 2008 American Institute of Physics.
引用
收藏
页数:10
相关论文
共 64 条
[11]   Nanosize effect on the deliquescence and the efflorescence of sodium chloride particles [J].
Biskos, G ;
Malinowski, A ;
Russell, LM ;
Buseck, PR ;
Martin, ST .
AEROSOL SCIENCE AND TECHNOLOGY, 2006, 40 (02) :97-106
[12]   Structure and vibrational spectroscopy of salt water/air interfaces: Predictions from classical molecular dynamics simulations [J].
Brown, EC ;
Mucha, M ;
Jungwirth, P ;
Tobias, DJ .
JOURNAL OF PHYSICAL CHEMISTRY B, 2005, 109 (16) :7934-7940
[13]  
BUCK AL, 1981, J APPL METEOROL, V20, P1527, DOI 10.1175/1520-0450(1981)020<1527:NEFCVP>2.0.CO
[14]  
2
[15]  
CHEN JP, 1994, J ATMOS SCI, V51, P3505, DOI 10.1175/1520-0469(1994)051<3505:TODAMK>2.0.CO
[16]  
2
[17]   Dislocations as sources of ions from NaCl and KCl (100) surfaces [J].
Dabringhaus, H ;
Butman, MF .
SURFACE SCIENCE, 2004, 560 (1-3) :167-182
[18]  
DEMOTT PJ, 1990, J ATMOS SCI, V47, P1056, DOI 10.1175/1520-0469(1990)047<1056:FNRODS>2.0.CO
[19]  
2
[20]   Theory of size dependent deliquescence of nanoparticles:: Relation to heterogeneous nucleation and comparison with experiments [J].
Djikaev, YS ;
Bowles, R ;
Reiss, H ;
Hämeri, K ;
Laaksonen, A ;
Väkevä, M .
JOURNAL OF PHYSICAL CHEMISTRY B, 2001, 105 (32) :7708-7722