1990
DOI: 10.1002/kin.550220605
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Rate constants for the reactions of OH radicals and Cl atoms with diethyl sulfide, Di‐n‐propyl sulfide, and Di‐n‐butyl sulfide

Abstract: Rate constants for the reactions of OH radicals and C1 atoms with diethyl sulfide (DES), din-propyl sulfide (DPS), and di-n-butyl sulfide (DBS) have been determined at 295 ? 3 K and a total pressure of 1 atm. Hydroxyl radical rate data was obtained using the absolute technique of pulse radiolysis combined with kinetic spectroscopy. The chlorine atom rate constants were measured using a conventional photolytic relative rate method. The rate constant for the reaction of C1 atoms with dimethyl sulfide (DMS) was a… Show more

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Cited by 36 publications
(26 citation statements)
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“…All of the rate coefficient values determined at high pressure (700-760 Torr) [9,11,12] are in reasonable agreement. However, in the relative kinetic investigation of Kinnison et al [12], a small consistent enhancement of the rate coefficient measured in synthetic air over that measured in pure N 2 was found.…”
Section: Introductionsupporting
confidence: 67%
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“…All of the rate coefficient values determined at high pressure (700-760 Torr) [9,11,12] are in reasonable agreement. However, in the relative kinetic investigation of Kinnison et al [12], a small consistent enhancement of the rate coefficient measured in synthetic air over that measured in pure N 2 was found.…”
Section: Introductionsupporting
confidence: 67%
“…A low-pressure limit rate coefficient of ∼1.8 × 10 −10 cm 3 molecule −1 s was found by these authors for the reaction at 3 Torr of N 2 that increased to a value of (3.3 ± 0.5) × 10 −10 cm 3 molecule −1 s −1 at 700 Torr of N 2 . The highpressure value was in agreement with the first determination of the rate coefficient by Nielsen et al [11] at a total pressure of 760 Torr N 2 using a relative kinetic technique. The work of Stickel et al [9] also established that the reaction proceeds via two channels: a pressure-dependent adduct-forming channel and a pressure-independent channel producing HCl:…”
Section: Introductionsupporting
confidence: 61%
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“…C1+ CH,SCH, -HC1+ CH,SCH, (la) C1, + CH,SCH, -CH,SCH,Cl + C1 (6) C1+ wall -products(9) C1+ CH,SCH, -products(10) CH,SCH2 + CH,SCH, -products (1 1) CH,SCH, -t-wall -Kinetic dependencies for reagents and product in the Cl/ C12DMS system: [C12]/[C12]0 (A), [DMS]/[DMS]o (O), [CH3SCH2Cl]/ [Clz]~ (0). Initial conditions: (a) [DMS] = 2.1 x [Clz] = 2.4 x (b) [DMS] = 1.5 x [Clz] = 2.3 x lOI4 molecules ~m -~.…”
mentioning
confidence: 99%
“…The vast majority of DMS released into the atmosphere are removed by chemical reaction with OH (Cox and Sandalls, 1974;Kurylo, 1978;Niki et al, 1983); Cl (Stickel et al, 1986;Tyndall et al, 1986;Nielsen et al, 1990;Kinnison et al, 1996) and NO 3 (Atkinson et al, 1984;Tyndall et al, 1986;Wallington et al, 1986) radicals. Ozone is also an important oxidant in the atmosphere and responsible for consuming varieties of gas species.…”
mentioning
confidence: 99%