Rate constant of the gas phase reaction of dimethyl sulfide (CH3SCH3)with ozone

被引:42
作者
Du, Lin
Xu, Yongfu [1 ]
Ge, Maofa
Jia, Long
Yao, Li
Wang, Weigang
机构
[1] Chinese Acad Sci, Inst Chem, Beijing Natl Lab Mol Sci, State Key Lab Struct Chem Unstable & Stable Speci, Beijing 100080, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China
[3] Chinese Acad Sci, Grad Univ, Beijing 100039, Peoples R China
[4] Beijing Normal Univ, Res Ctr Atmospher Environm, Beijing 100875, Peoples R China
基金
中国国家自然科学基金;
关键词
D O I
10.1016/j.cplett.2007.01.025
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
The gas phase reaction of ozone with dimethyl sulfide (DMS) has been studied in our self-made chamber. Experiments were conducted under supposedly pseudo-first-order decay conditions, keeping [DMS](0) > 10[O-3](0), but having different combinations of [DMS](0) and [O-3](0), Cyclohexane was added into the reactor to eliminate the effect of OH radicals. A value of (1.04 +/- 0.21) X 10(-19) cm(3) molecule(-1) s(-1) for rate constant was obtained under room temperature of about 301 K. The wall effects and the role of cyclohexane are discussed. Our results enrich the kinetics data of atmospheric chemistry, and further confirm that the gas phase reaction of DMS with ozone is not important for the loss of DMS in the atmosphere. (c) 2007 Elsevier B.V. All rights reserved.
引用
收藏
页码:36 / 40
页数:5
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