Probing heterogeneous chemistry of individual atmospheric particles using scanning electron microscopy and energy-dispersive X-ray analysis

被引:89
作者
Krueger, BJ
Grassian, VH [1 ]
Iedema, MJ
Cowin, JP
Laskin, A
机构
[1] Univ Iowa, Dept Chem, Iowa City, IA 52242 USA
[2] Univ Iowa, Ctr Global & Reg Environm Res, Iowa City, IA 52242 USA
[3] Pacific NW Natl Lab, William R Wiley Environm Mol Sci Lab, Richland, WA 99352 USA
关键词
D O I
10.1021/ac034455t
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
In this paper, we demonstrate the utility of single-particle analysis to investigate the chemistry of isolated, individual particles of atmospheric relevance such as NaCl, sea salt, CaCO3, and SiO2. A variety of state-of-the-art scanning electron microscopy techniques, including environmental scanning electron microscopy and computer-controlled scanning electron microscopy/energy-dispersive X-ray analysis, were utilized for monitoring and quantifying phase transitions of individual particles, morphology, and compositional changes of individual particles as they react with nitric acid. Clear differences in reaction mechanisms were observed between SiO2, CaCO3, NaCl, and sea salt particles. SiO2 particles exposed to HNO3 showed no change, indicating that the reaction of SiO2 particles is limited to the particle surface and would not involve bulk atoms in its reactivity. Calcium carbonate was seen to convert to aqueous calcium nitrate droplets while sodium chloride formed microcrystallites of sodium nitrate on top of the particle. Sea salt particles showed morphology changes that could be described as a combination of these as both spherical droplets and microcrystallites were observed. This is consistent with the multicomponent composition of sea salt. Further differences were found in the reaction rates for sea salt and sodium chloride with nitric acid. Sea salt yielded a significant increase in reactivity when compared to the NaCl particles under similar conditions. The reaction of nitric acid with calcium carbonate was found to be strongly enhanced at higher relative humidity.
引用
收藏
页码:5170 / 5179
页数:10
相关论文
共 61 条
[31]   Physical and chemical characterization of atmospheric aerosols by atomic force microscopy [J].
Lehmpuhl, DW ;
Ramirez-Aguilar, KA ;
Michel, AE ;
Rowlen, KL ;
Birks, JW .
ANALYTICAL CHEMISTRY, 1999, 71 (02) :379-383
[32]  
LIDE DR, 1983, CRC HDB CHEM PHYSICS
[33]   Cosmic rays, clouds, and climate [J].
Marsh, N ;
Svensmark, H .
SPACE SCIENCE REVIEWS, 2000, 94 (1-2) :215-230
[34]   CHLORINE LOSS FROM PUERTO-RICAN AND SAN-FRANCISCO-BAY AREA MARINE AEROSOLS [J].
MARTENS, CS ;
WESOLOWSKI, JJ ;
HARRISS, RC ;
KAIFER, R .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (36) :8778-8792
[35]   MEASUREMENTS OF CHLORIDE DEPLETION AND SULFUR ENRICHMENT IN INDIVIDUAL SEA-SALT PARTICLES COLLECTED FROM THE REMOTE MARINE BOUNDARY-LAYER [J].
MCINNES, LM ;
COVERT, DS ;
QUINN, PK ;
GERMANI, MS .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D4) :8257-8268
[36]   SHATTERING AND MODIFICATION OF SEA-SALT PARTICLES IN THE MARINE ATMOSPHERE [J].
MOURI, H ;
OKADA, K .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (01) :49-52
[37]   GASEOUS AND PARTICULATE BROMINE IN MARINE ATMOSPHERE [J].
MOYERS, JL ;
DUCE, RA .
JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 77 (27) :5330-+
[38]   Global sensitivity experiments of the radiative forcing due to mineral aerosols [J].
Myhre, G ;
Stordal, F .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D16) :18193-18204
[39]  
Noble CA, 2000, MASS SPECTROM REV, V19, P248, DOI 10.1002/1098-2787(200007)19:4<248::AID-MAS3>3.0.CO
[40]  
2-I