2009
DOI: 10.1088/0963-0252/18/3/034016
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Corona discharge experiments in admixtures of N2and CH4: a laboratory simulation of Titan's atmosphere

Abstract: Corona discharge experiments in admixtures of N2 and CH4: a laboratory simulation of Titan's atmosphere. Plasma Sources Science and Technology, 18(3) For guidance on citations see FAQs.

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Cited by 27 publications
(27 citation statements)
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“…In contrast to our earlier measurements made in a coaxial corona discharge [23], NH 3 was observed as a new product in the abnormal glow discharge identified by its strong peak at 966 cm −1 , surrounded by dense rotational in range 800-1200. Bands at around 3300 cm…”
Section: Experimental Set-upcontrasting
confidence: 99%
See 1 more Smart Citation
“…In contrast to our earlier measurements made in a coaxial corona discharge [23], NH 3 was observed as a new product in the abnormal glow discharge identified by its strong peak at 966 cm −1 , surrounded by dense rotational in range 800-1200. Bands at around 3300 cm…”
Section: Experimental Set-upcontrasting
confidence: 99%
“…The most likely primary processes leading to the polymer formation is a transport of active CN and C/C 2 radicals onto the electrode surfaces where they are neutralized before undergoing a series of homogeneous reactions with other radicals leading to deposit formation. Moreover, it is postulated that negative ions may play a key role in the formation of such deposits [23].…”
Section: -P7mentioning
confidence: 99%
“…Thus the C 2 H 2 neutral -detected in our earlier measurements made in coaxial corona discharge [12]-leads to the formation of CN − , C 3 N − and C 5 N − anions rather than C 2 H − production. The formation of cluster anions in low-power discharges has been reported by several authors.…”
Section: Resultsmentioning
confidence: 62%
“…The energy sources used in the laboratory are proxies for the solar irradiation and the precipitation of magnetospheric electrons. Those natural sources are reproduced in the laboratory by UV photon fluxes Imanaka and Smith 2010;Trainer et al 2012;Tran et al 2008;Trainer et al 2006) and/or by plasma discharges (Somogyi et al 2005;Coll et al 1999;Horvath et al 2009;Imanaka et al 2004;Hörst and Tolbert 2013). Pressure and temperature are strongly dependent on the experiments, and can hardly reproduce the whole range and extreme conditions occurring in real atmospheres.…”
Section: Simulation Facilities For Organic Aerosols In Planetary Atmomentioning
confidence: 99%