2022
DOI: 10.1039/d2cp02044k
|View full text |Cite
|
Sign up to set email alerts
|

Vacuum ultraviolet photodissociation of OCS via the 21Σ+ state: the S(1D2) elimination channel

Abstract: The photodissociation of OCS is necessary to model the primary photochemical processes of OCS in the global cycling of sulfur and interstellar photochemistry. Here, by combining the time-sliced velocity-map ion...

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
5
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
6

Relationship

2
4

Authors

Journals

citations
Cited by 6 publications
(5 citation statements)
references
References 54 publications
0
5
0
Order By: Relevance
“…The vibronic origin of the absorption is associated with bending excitations in the 2 1 A′ and 1 1 A″ states (the 1 Δ u state splits into Renner–Teller pairs of A′ and A″ symmetry in the bent C s geometry). Based on previous studies, , the comparison between the absorption spectrum and the photofragment excitation (PHOFEX) spectrum reveals subtle differences. Therefore, in this work, the PHOFEX spectrum was obtained by measuring the total O­( 1 D 2 ) atomic photofragment yield while scanning the VUV photolysis laser from 143.00 to 155.00 nm in this work.…”
Section: Results and Discussionmentioning
confidence: 97%
See 1 more Smart Citation
“…The vibronic origin of the absorption is associated with bending excitations in the 2 1 A′ and 1 1 A″ states (the 1 Δ u state splits into Renner–Teller pairs of A′ and A″ symmetry in the bent C s geometry). Based on previous studies, , the comparison between the absorption spectrum and the photofragment excitation (PHOFEX) spectrum reveals subtle differences. Therefore, in this work, the PHOFEX spectrum was obtained by measuring the total O­( 1 D 2 ) atomic photofragment yield while scanning the VUV photolysis laser from 143.00 to 155.00 nm in this work.…”
Section: Results and Discussionmentioning
confidence: 97%
“…The experiment employed the time-sliced velocity-mapped ion imaging apparatus combined with two independent laser sources (a tunable VUV source for photolysis and a fixed UV source for (2 + 1) REMPI detection) for CO 2 molecular photodissociation. The detailed configuration of the experimental setup has been introduced in our previous studies, and thus only a brief description is presented here. The CO 2 molecular beam (the rotational temperature was ∼10 K) was formed in a pulsed supersonic expansion of 10% CO 2 in Ar at a 1 bar backing pressure.…”
Section: Methodsmentioning
confidence: 99%
“…Carbonyl sulfide (OCS) is the most abundant, long-lived S-containing gas in Earth's atmosphere and a major supplier of sulfur to the stratospheric sulfate aerosol layer. OCS has been observed in the deep atmosphere of Venus, in dense molecular clouds and in Jupiter's atmosphere following the impact of comets [ 75 ]. Carbon disulfide (CS 2 ) is also ubiquitous in the ISM and has been proposed as a likely precursor for CS and S 2 radicals observed in cometary coma [ 76 ].…”
Section: Experimental Methodsmentioning
confidence: 99%
“…The photodissociation of OCS at near UV wavelengths λ >200 nm is dominated by the spin-allowed channel yielding S( 1 D) + CO(X) products; the latter are formed vibrationally ‘cold’ but rotationally ‘hot’, in at least qualitative accord with that expected given the forces introduced by a bent ← linear excitation process [ 84 ]. The same product channel has been investigated using TSVMI methods following excitation in the range 142.98 ≤ λ ≤ 154.37 nm [ 75 ] and other single-bond fission channels yielding S( 1 S) + CO(X) [ 85 ] and S( 3 P) + CO(A) [ 86 ] products have also been reported when exciting at similar VUV wavelengths.…”
Section: Experimental Methodsmentioning
confidence: 99%
“…An example of a small but important sulfur-bearing species is carbonyl sulfide (OCS). , For example, OCS is the most abundant sulfur-containing molecule in Earth’s atmosphere, with a mixing ratio of ∼500 ppt . Moreover, OCS contributes to stratospheric sulfate aerosol formation, due to the long tropospheric lifetime of OCS (τ > 2 years) allowing transportation to the stratosphere. In the Venusian atmosphere, a rapid reduction in the OCS mixing ratio from 10 to 20 ppm at an altitude of 30 km, to 0.35 ppm at 38 km, is observed, with reasons for this decline still unknown. , Furthermore, OCS was found to exist in several Jupiter family comets and, more recently, in the L1455-IRS1 and L1551-IRS5 class I protostars …”
Section: Introductionmentioning
confidence: 99%