Literature DB >> 11538099

Plasma discharge in N2 + CH4 at low pressures: experimental results and applications to Titan.

W R Thompson1, T J Henry, J M Schwartz, B N Khare, C Sagan.   

Abstract

We report the yields of gaseous hydrocarbons and nitriles produced in a continuous flow, low-dose, cold plasma discharge excited in a 10% CH4, 90% N2 atmosphere at 295 K and pressures p of 17 and 0.24 mbar, and use the results to compute expected abundances of minor constituents in Titan's atmosphere. These experiments are, by design, relevant to the atmospheric chemistry induced by cosmic rays in Titan's troposphere and (at the lower pressure) to chemistry initiated by Saturnian magnetospheric electrons and other charged particle sources which excite stratospheric aurorae. At p = 17 mbar, 59 gaseous species including 27 nitriles are detected in overall yield 4.0 (C + N) atoms incorporated into products per 100 eV (heV). At p = 0.24 mbar, 19 species are detected, including six nitriles and three other unidentified N-bearing compounds; the yield is 0.79 (C + N)/heV, a mild decrease with pressure. The types of molecules formed change more markedly, with high degrees of multiple bonding at 0.24 mbar prevailing over more H-saturated molecules at 17 mbar. The molecules and yields at 0.24 mbar bear a striking resemblance to the minor constituents found in Titan's atmosphere, all of which are abundant products in the laboratory experiment. Using the altitude-integrated flux of charged particle energy deposition at Titan, the laboratory yields at p = 0.24 mb, and a simple eddy mixing model, we compute absolute stratospheric column abundances and mole fractions. These are found to be in very good agreement with the Voyager IRIS observations. Except for the primarily photochemical products, C2H6 and C3H8, the match is much better than that obtained by photochemical-kinetic models, demonstrating that properly designed laboratory experiments are directly applicable to modeling radiation-chemical processes in planetary atmospheres. On the basis of this agreement we expect CH3-C triple bond N (ethanenitrile = acetonitrile) CH2=CH-CH=CH2 (1,3-butadiene), CH2=C=CH2 (1,2-propadiene = allene), and CH2=CH-C triple bond CH (1-buten-3-yne) to be present at mol fractions X > 10(-9), and CH2=CH-C triple bond N (propenenitrile), CH3-CH=CH2 (propene), and CH3-CH2-C triple bond N (propanenitrile) at X > 10(-10) in Titan's atmosphere.

Entities:  

Keywords:  NASA Discipline Exobiology; NASA Discipline Number 52-20; NASA Program Exobiology; Non-NASA Center

Mesh:

Substances:

Year:  1991        PMID: 11538099     DOI: 10.1016/0019-1035(91)90068-5

Source DB:  PubMed          Journal:  Icarus        ISSN: 0019-1035            Impact factor:   3.508


  8 in total

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Authors:  S Miyakawa; K Murasawa; K Kobayashi; A B Sawaoka
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Review 2.  Electrical energy sources for organic synthesis on the early Earth.

Authors:  C Chyba; C Sagan
Journal:  Orig Life Evol Biosph       Date:  1991       Impact factor: 1.950

3.  Power measurements of spark discharge experiments.

Authors:  R Navarro-Gonzalez; A Romero; Y Honda
Journal:  Orig Life Evol Biosph       Date:  1998-04       Impact factor: 1.950

Review 4.  Possible role of volcanic ash-gas clouds in the Earth's prebiotic chemistry.

Authors:  V A Basiuk; R Navarro-Gonzalez
Journal:  Orig Life Evol Biosph       Date:  1996-04       Impact factor: 1.950

5.  Organic environments on Saturn's moon, Titan: simulating chemical reactions and analyzing products by FT-ICR and ion-trap mass spectrometry.

Authors:  Arpad Somogyi; Chu-Ha Oh; Mark A Smith; Jonathan I Lunine
Journal:  J Am Soc Mass Spectrom       Date:  2005-03-29       Impact factor: 3.109

6.  Organic haze on Titan and the early Earth.

Authors:  Melissa G Trainer; Alexander A Pavlov; H Langley DeWitt; Jose L Jimenez; Christopher P McKay; Owen B Toon; Margaret A Tolbert
Journal:  Proc Natl Acad Sci U S A       Date:  2006-11-13       Impact factor: 11.205

Review 7.  Chemical evolution on Titan: comparisons to the prebiotic earth.

Authors:  D W Clarke; J P Ferris
Journal:  Orig Life Evol Biosph       Date:  1997-06       Impact factor: 1.950

8.  Archean geochemistry of formaldehyde and cyanide and the oligomerization of cyanohydrin.

Authors:  T Arrhenius; G Arrhenius; W Paplawsky
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  8 in total

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