Effect of Particle Morphology on Cloud Condensation Nuclei Activity

被引:45
作者
Altaft, Muhammad Bilal [1 ]
Dutcher, Dabrina D. [2 ,3 ]
Raymond, Timothy M. [3 ]
Freedman, Miriam Arak [1 ]
机构
[1] Penn State Univ, Dept Chem, University Pk, PA 16802 USA
[2] Bucknell Univ, Dept Chem, Lewisburg, PA 17837 USA
[3] Bucknell Univ, Dept Chem Engn, Lewisburg, PA 17837 USA
来源
ACS EARTH AND SPACE CHEMISTRY | 2018年 / 2卷 / 06期
基金
美国国家科学基金会;
关键词
liquid-liquid phase separation; organic aerosol; droplet activation; cloud microphysics; climate; LIQUID PHASE-SEPARATION; OPTICAL-PROPERTIES; ORGANIC AEROSOL; HYGROSCOPIC GROWTH; SODIUM-CHLORIDE; SIZE-DEPENDENCE; SURFACE-TENSION; SUCCINIC ACID; WATER; REPRESENTATION;
D O I
10.1021/acsearthspacechem.7b00146
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Cloud condensation nuclei (CCN) activation is sensitive to the size, composition, and morphology of aerosol particles of <200 nm. By controlling the particle morphology of internally mixed samples (i.e., homogeneous versus phase separated), we have probed the effect of morphology on CCN activity using model organic aerosol systems, where ammonium sulfate was mixed with either pimelic acid or succinic acid in a 50:50 mixture by weight. Surprisingly, for systems of the same composition but distinct morphology, we observe a noticeable impact on CCN activity. Specifically, a phase separated morphology results in activation diameters close to that of ammonium sulfate, while a homogeneous morphology yields an activation diameter in between the pure inorganic and organic components. Our results suggest that morphology-resolved CCN data may be an important parameter to consider in cloud microphysics models to improve predictions of CCN activity of complex organic aerosols. For laboratory CCN studies, it is important to control or account for atomized solution drying rates, which have been shown to affect morphology and ultimately CCN activity.
引用
收藏
页码:634 / 639
页数:6
相关论文
共 34 条
[1]   Effect of Drying Rate on Aerosol Particle Morphology [J].
Altaf, Muhammad Bilal ;
Freedman, Miriam Arak .
JOURNAL OF PHYSICAL CHEMISTRY LETTERS, 2017, 8 (15) :3613-3618
[2]   Role of nucleation mechanism on the size dependent morphology of organic aerosol [J].
Altaf, Muhammad Bilal ;
Zuend, Andreas ;
Freedman, Miriam Arak .
CHEMICAL COMMUNICATIONS, 2016, 52 (59) :9220-9223
[3]  
[Anonymous], 1988, THESIS
[4]   Sink or Surf: Atmospheric Implications for Succinic Acid at Aqueous Surfaces [J].
Blower, Patrick G. ;
Ota, Stephanie T. ;
Valley, Nicholas A. ;
Wood, Suzannah R. ;
Richmond, Geraldine L. .
JOURNAL OF PHYSICAL CHEMISTRY A, 2013, 117 (33) :7887-7903
[5]   CCN activity and droplet growth kinetics of fresh and aged monoterpene secondary organic aerosol [J].
Engelhart, G. J. ;
Asa-Awuku, A. ;
Nenes, A. ;
Pandis, S. N. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (14) :3937-3949
[6]   Atmospheric Processes and Their Controlling Influence on Cloud Condensation Nuclei Activity [J].
Farmer, Delphine K. ;
Cappa, Christopher D. ;
Kreidenweis, Sonia M. .
CHEMICAL REVIEWS, 2015, 115 (10) :4199-4217
[7]   Discontinuities in hygroscopic growth below and above water saturation for laboratory surrogates of oligomers in organic atmospheric aerosols [J].
Hodas, Natasha ;
Zuend, Andreas ;
Schilling, Katherine ;
Berkemeier, Thomas ;
Shiraiwa, Manabu ;
Flagan, Richard C. ;
Seinfeld, John H. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2016, 16 (19) :12767-12792
[8]  
Lamb D., 2011, Physics and Chemistry of Clouds
[9]  
McNeill VF, 2014, TOP CURR CHEM, V339, P1, DOI 10.1007/978-3-642-41215-8
[10]   Surface tension prevails over solute effect in organic-influenced cloud droplet activation [J].
Ovadnevaite, Jurgita ;
Zuend, Andreas ;
Laaksonen, Ari ;
Sanchez, Kevin J. ;
Roberts, Greg ;
Ceburnis, Darius ;
Decesari, Stefano ;
Rinaldi, Matteo ;
Hodas, Natasha ;
Facchini, Maria Cristina ;
Seinfeld, John H. ;
O'Dowd, Colin .
NATURE, 2017, 546 (7660) :637-641