New Particle Formation from Methanesulfonic Acid and Amines/Ammonia as a Function of Temperature

被引:77
作者
Chen, Haihan [1 ]
Finlayson-Pitts, Barbara J. [1 ]
机构
[1] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA
基金
美国国家科学基金会;
关键词
METHANE SULFONIC-ACID; SULFURIC-ACID; VERTICAL-DISTRIBUTION; BINARY NUCLEATION; ATMOSPHERIC NUCLEATION; ORGANIC-COMPOUNDS; DIMETHYL SULFIDE; BOUNDARY-LAYER; WATER-SYSTEMS; AEROSOL IONS;
D O I
10.1021/acs.est.6b04173
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Previous studies have shown that methanesulfonic acid (MSA) reacts with amines and ammonia to form particles, which is expected to be particularly important in coastal and agricultural areas. We present the first systematic study of temperature dependence of particle formation from the reactions of MSA with trimethylamine (TMA), dimethylamine (DMA), methylamine (MA), and ammonia over the range of 21-28 degrees C and 0.4-5.9 s in a flow reactor under dry conditions and in the presence of 3 X 10(17) cm(-3) water vapor. Overall activation energies (E-overall) for particle formation calculated from the dependence of rates of particle formation on temperature for all of these bases are negative. The negative E-overall is interpreted in terms of reverse reactions that decompose intermediate clusters in competition with the forward reactions that grow the clusters into particles. The average values of E-overall for the formation of detectable particles are: TMA,-(168 +/- 19) kcal mol(-1) DMA, -(134 +/- 30) kcal mol(-1); MA,-(68 +/- 23) kcal mol(-1); NH3,-(110 +/- 16) kcal mol(-1) (+/- 1 sigma). The strong inverse dependence of particle formation with temperature suggests that particle formation may not decline proportionally with concentrations of MSA and amines if temperature also decreases, for example at higher altitudes or in winter.
引用
收藏
页码:243 / 252
页数:10
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