Deliquescence, efflorescence, and water activity in ammonium nitrate and mixed ammonium nitrate/succinic acid microparticles

被引:177
作者
Lightstone, JM
Onasch, TB
Imre, D [1 ]
Oatis, S
机构
[1] Brookhaven Natl Lab, Dept Environm Sci, Div Atmospher Sci, Upton, NY 11973 USA
[2] Long Isl Univ, Southampton Coll, Div Nat Sci, Southampton, NY 11968 USA
关键词
D O I
10.1021/jp002137h
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
We have investigated the thermodynamics and kinetics of ammonium nitrate/water and mixed ammonium nitrate/succinic acid/water microparticles. The water activity of ammonium nitrate microparticles is determined as a function of composition down to 12% relative humidity by accounting for the rapid evaporation of ammonia and nitric acid. Both the observed deliquescence and water activities for ammonium nitrate/water microparticles are found to be in good agreement with predicted values. Supermicron ammonium nitrate particles generated from high-purity methanol are found not to effloresce, but form an anhydrous liquid state observed only in particle form. We also present data on the hydroscopicity and phase transitions of internally mixed ammonium nitrate/succinic acid particles. A pronounced reduction in the particle growth factor at deliquescence is reported, indicating that the succinic acid does not take up a significant amount of water. Additionally, the deliquescence relative humidity is found to decrease slightly as the mass percent of succinic acid is increased from 12.5 to 50%. Solid succinic acid in ammonium nitrate drops acts to catalyze efflorescence of ammonium nitrate at high relative humidity. However, when the relative humidity is increased sufficiently to completely dissolve the succinic acid, no efflorescence is observed. The resulting data are analyzed using classical nucleation theory to derive the free energy barrier to nucleation, the critical supersaturation, the size of the critical nucleus, and the contact parameter between ammonium nitrate crystal and the solid succinic acid.
引用
收藏
页码:9337 / 9346
页数:10
相关论文
共 61 条
[31]   WATER ACTIVITY IN SUPERSATURATED AQUEOUS-SOLUTIONS OF ORGANIC SOLUTES [J].
NA, HS ;
ARNOLD, S ;
MYERSON, AS .
JOURNAL OF CRYSTAL GROWTH, 1995, 149 (3-4) :229-235
[32]   LARGE CONTRIBUTION OF ORGANIC AEROSOLS TO CLOUD-CONDENSATION-NUCLEI CONCENTRATIONS [J].
NOVAKOV, T ;
PENNER, JE .
NATURE, 1993, 365 (6449) :823-826
[33]  
Orr C., 1958, J. Colloid Sci, V13, P472, DOI [DOI 10.1016/0095-8522(58)90055-2, 10.1016/0095-8522(58)90055-2]
[34]   SECONDARY ORGANIC AEROSOL FORMATION AND TRANSPORT [J].
PANDIS, SN ;
HARLEY, RA ;
CASS, GR ;
SEINFELD, JH .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1992, 26 (13) :2269-2282
[35]   RELATIONSHIP BETWEEN MEASURED WATER-VAPOR GROWTH AND CHEMISTRY OF ATMOSPHERIC AEROSOL FOR GRAND-CANYON, ARIZONA, IN WINTER 1990 [J].
PITCHFORD, ML ;
MCMURRY, PH .
ATMOSPHERIC ENVIRONMENT, 1994, 28 (05) :827-839
[36]   EVAPORATION OF AMMONIUM-NITRATE PARTICLES [J].
RICHARDSON, CB ;
HIGHTOWER, RL .
ATMOSPHERIC ENVIRONMENT, 1987, 21 (04) :971-975
[37]   A STUDY OF HETEROGENEOUS NUCLEATION IN AQUEOUS-SOLUTIONS [J].
RICHARDSON, CB ;
SNYDER, TD .
LANGMUIR, 1994, 10 (07) :2462-2465
[38]   Sources of fine organic aerosol. 9. Pine, oak and synthetic log combustion in residential fireplaces [J].
Rogge, WF ;
Hildemann, LM ;
Mazurek, MA ;
Cass, GR ;
Simoneit, BRT .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1998, 32 (01) :13-22
[39]   Water-soluble organics in atmospheric particles: A critical review of the literature and application of thermodynamics to identify candidate compounds [J].
Saxena, P ;
Hildemann, LM .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1996, 24 (01) :57-109
[40]   ORGANICS ALTER HYGROSCOPIC BEHAVIOR OF ATMOSPHERIC PARTICLES [J].
SAXENA, P ;
HILDEMANN, LM ;
MCMURRY, PH ;
SEINFELD, JH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D9) :18755-18770