Kinetics and Branching for the Reactions of N2+with C3H4Isomers atLow Temperatures and Implications for Titan?s Atmosphere

被引:3
作者
Mortada, Ahmad [1 ]
Carles, Sophie [1 ]
Demes, Sandor [1 ]
Joalland, Baptiste [1 ]
Lique, Francois [1 ]
Benidar, Abdessamad [1 ]
Lavvas, Panayotis [2 ]
Biennier, Ludovic [1 ]
机构
[1] Univ Rennes, IPR Inst Phys Rennes UMR 6251, CNRS, F-35000 Rennes, France
[2] Univ Reims, Grp Spectrometrie Mol & Atmospher, UMR CNRS 7331, F-51687 Reims, France
来源
ACS EARTH AND SPACE CHEMISTRY | 2022年 / 6卷 / 05期
关键词
reactive collisions; uniform supersonicflows; temperature-dependent reactivity; planetary sciences; astrochemistry; PHOTO-ION COINCIDENCE; PHOTOIONIZATION; HYDROCARBONS; CHEMISTRY; C3H3+; REACTIVITY; COLLISIONS; PROPYNE; GROWTH; CH3CN;
D O I
10.1021/acsearthspacechem.1c00347
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The photoionization of N2plays a key role ininitiating the formation of complex organic molecules in thenitrogen-rich atmosphere of Saturn's largest moon, Titan. To date,only a handful of laboratory studies have explored the reactivity ofN2+ions with hydrocarbons???limited to methane, acetylene, andethylene???at the low temperatures relevant to Titan. Here, the ratecoefficients, product identity, and branching ratios of the ion-molecule reactions of N2+with C3H4isomers, namely, propyneCH3CCH and allene CH2CCH2, were measured between 24 and72 K in uniform supersonicflows. The rate coefficients arecollisional and their temperature dependence is in remarkableagreement with capture models. The outcomes of both reactionsare similar: they proceed primarily via dissociative charge transfer,leading to the formation of C3H3+(main product, >70%) and C3H2+(between 9 and 17%), whereas a second, nondissociativecharge-transfer mechanism leading to C3H4+becomes slightly more prominent as the temperature decreases (from 3 to 12%). C3H3+is plausibly formed predominantly as the smallest aromatic cation, cyclopropenylc-C3H3+, by following the lowest-energy pathwayfor the decomposition of allene and propyne cations. The measured rate coefficients and branching ratios were included in aphotochemical model of Titan's atmosphere. The results point toward a secondary role of N2++C3H4reactive pathways in theproduction ofc-C3H3+.
引用
收藏
页码:1227 / 1238
页数:12
相关论文
共 64 条
[51]   Herschel/PACS spectroscopy of trace gases of the stratosphere of Titan [J].
Rengel, M. ;
Sagawa, H. ;
Hartogh, P. ;
Lellouch, E. ;
Feuchtgruber, H. ;
Moreno, R. ;
Jarchow, C. ;
Courtin, R. ;
Cernicharo, J. ;
Lara, L. M. .
ASTRONOMY & ASTROPHYSICS, 2014, 561
[52]   CYCLIC AND LINEAR ISOMERS OF C3H2+ AND C3H3+ - THE C3H+ + H-2 REACTION [J].
SMITH, D ;
ADAMS, NG .
INTERNATIONAL JOURNAL OF MASS SPECTROMETRY AND ION PROCESSES, 1987, 76 (03) :307-317
[53]   THE ION-MOLECULE CHEMISTRY OF C3H3+ AND THE IMPLICATIONS FOR SOOT FORMATION [J].
SMYTH, KC ;
LIAS, SG ;
AUSLOOS, P .
COMBUSTION SCIENCE AND TECHNOLOGY, 1982, 28 (3-4) :147-154
[54]   PARAMETRIZATION OF THE ION-POLAR MOLECULE COLLISION RATE-CONSTANT BY TRAJECTORY CALCULATIONS [J].
SU, T ;
CHESNAVICH, WJ .
JOURNAL OF CHEMICAL PHYSICS, 1982, 76 (10) :5183-5185
[55]   Abundance measurements of Titan's stratospheric HCN, HC3N, C3H4, and CH3CN from ALMA observations [J].
Thelen, Alexander E. ;
Nixon, C. A. ;
Chanover, N. J. ;
Cordiner, M. A. ;
Molter, E. M. ;
Teanby, N. A. ;
Irwin, G. J. ;
Serigano, J. ;
Charnley, S. B. .
ICARUS, 2019, 319 :417-432
[56]   DISSOCIATIVE CHARGE-TRANSFER REACTIONS OF AR+ WITH SIMPLE ALIPHATIC-HYDROCARBONS AT THERMAL-ENERGY [J].
TSUJI, M ;
KOUNO, H ;
MATSUMURA, K ;
FUNATSU, T ;
NISHIMURA, Y ;
OBASE, H ;
KUGISHIMA, H ;
YOSHIDA, K .
JOURNAL OF CHEMICAL PHYSICS, 1993, 98 (03) :2011-2022
[57]   Analysis of Cassini/CIRS limb spectra of Titan acquired during the nominal mission I. Hydrocarbons, nitriles and CO2 vertical mixing ratio profiles [J].
Vinatier, Sandrine ;
Bezard, Bruno ;
Nixon, Conor A. ;
Mamoutkine, Andrei ;
Carlson, Ronald C. ;
Jennings, Donald E. ;
Guandique, Ever A. ;
Teanby, Nick A. ;
Bjoraker, Gordon L. ;
Flasar, F. Michael ;
Kunde, Virgil G. .
ICARUS, 2010, 205 (02) :559-570
[58]   Simulating the density of organic species in the atmosphere of Titan with a coupled ion-neutral photochemical model [J].
Vuitton, V. ;
Yelle, R. V. ;
Klippenstein, S. J. ;
Horst, S. M. ;
Lavvas, P. .
ICARUS, 2019, 324 :120-197
[59]   The process of tholin formation in Titan's upper atmosphere [J].
Waite, J. H., Jr. ;
Young, D. T. ;
Cravens, T. E. ;
Coates, A. J. ;
Crary, F. J. ;
Magee, B. ;
Westlake, J. .
SCIENCE, 2007, 316 (5826) :870-875
[60]   Ion Neutral Mass Spectrometer results from the first flyby of Titan [J].
Waite, JH ;
Niemann, H ;
Yelle, RV ;
Kasprzak, WT ;
Cravens, TE ;
Luhmann, JG ;
McNutt, RL ;
Ip, WH ;
Gell, D ;
De La Haye, V ;
Müller-Wordag, I ;
Magee, B ;
Borggren, N ;
Ledvina, S ;
Fletcher, G ;
Walter, E ;
Miller, R ;
Scherer, S ;
Thorpe, R ;
Xu, J ;
Block, B ;
Arnett, K .
SCIENCE, 2005, 308 (5724) :982-986