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Mass composition of the escaping plasma at Mars

✍ Scribed by E. Carlsson; A. Fedorov; S. Barabash; E. Budnik; A. Grigoriev; H. Gunell; H. Nilsson; J.-A. Sauvaud; R. Lundin; Y. Futaana; M. Holmström; H. Andersson; M. Yamauchi; J.D. Winningham; R.A. Frahm; J.R. Sharber; J. Scherrer; A.J. Coates; D.R. Linder; D.O. Kataria; E. Kallio; H. Koskinen; T. Säles; P. Riihelä; W. Schmidt; J. Kozyra; J. Luhmann; E. Roelof; D. Williams; S. Livi; C.C. Curtis; K.C. Hsieh; B.R. Sandel; M. Grande; M. Carter; J.-J. Thocaven; S. McKenna-Lawler; S. Orsini; R. Cerulli-Irelli; M. Maggi; P. Wurz; P. Bochsler; N. Krupp; J. Woch; M. Fränz; K. Asamura; C. Dierker


Book ID
108138635
Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
571 KB
Volume
182
Category
Article
ISSN
0019-1035

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✍ Catherine Fenselau; Richard Caprioli; A. O. Nier; W. B. Hanson; A. Seiff; M. B. 📂 Article 📅 2003 🏛 John Wiley and Sons 🌐 English ⚖ 323 KB

Two surface samples collected from the Chryse Planitia region of Mars were heated to temperatures up to 500 °C, and the volatiles that they evolved were analyzed with a gas chromatograph-mass spectrometer. Only water and carbon dioxide were detected. This implies that organic compounds have not accu