๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

Identification of the D3h Isomer of Carbon Trioxide (CO3) and Its Implications for Atmospheric Chemistry

โœ Scribed by Corey S. Jamieson; Alexander M. Mebel; Ralf I. Kaiser


Publisher
John Wiley and Sons
Year
2006
Tongue
English
Weight
176 KB
Volume
7
Category
Article
ISSN
1439-4235

No coin nor oath required. For personal study only.

โœฆ Synopsis


Abstract

The CO~3~ molecule is considered an important reaction intermediate in the atmospheres of Earth and Mars for quenching electronically excited oxygen atoms and in contributing to the anomalous ^18^O isotope enrichment. The geometry of the CO~3~ intermediate plays an important role in explaining these effects; however, only the cyclic (C~2__v__~) isomer has been experimentally confirmed so far. Here, we report on the first spectroscopic detection of the acyclic (D~3h~) isomer of carbon trioxide (^12^C^16^O~3~) via its ฮฝ~1~ and ฮฝ~2~ vibrational modes centered around 1165 cm^โˆ’1^ under matrix isolation conditions; the identification of the ^12^C^18^O~3~, ^13^C^16^O~3~, ^13^C^18^O~3~, ^16^O^12^C^18^O~2~, and ^18^O^12^C^16^O~2~ isotopomers of the acyclic isomer confirms the assignments.


๐Ÿ“œ SIMILAR VOLUMES


Upper limits for the gas-phase reaction
โœ T. J. Wallington; K. W. Jucks; G. S. Tyndall ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 114 KB ๐Ÿ‘ 2 views

Upper limits of and were established for 4 ฯซ 10 7 ฯซ 10 cm molecule s the gas-phase reactions of H 2 O 2 with O 3 and NO, respectively. These reactions are too slow to explain features observed in the atmospheric vertical profile of H 2 O 2 .

Kinetics of O(1D) interactions with the
โœ P.H. Wine; A.R. Ravishankara ๐Ÿ“‚ Article ๐Ÿ“… 1981 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 763 KB

lL11c coefficrents for coll1s1on~1 removal of Ott D) by SLY atnlosplrertc gases have been measured by momtormg the appearance of O(3P) followng photolvtlc productlon of O(' D) The measured values, x"hI 2 SJ, m units of IO-" cm3 molccule-' s-l arc k-0, = ?? 8 5 :! 3, k~~ = 2 52 ? 0.25, k-co, = 10 4 +