| タイトル | Isotopic Composition of Carbon Dioxide Released from Confidence Hills Sediment as Measured by the Sample Analysis at Mars (SAM) Quadrupole Mass Spectrometer |
| 本文（外部サイト） | http://hdl.handle.net/2060/20150001958 |
| 著者（英） | Summons, R.; Grotzinger, J. P.; Steele, A.; McAdam, A.; Archer, P., Jr.; Mahaffy, P. R.; Jones, J.; Eigenbrode, J.; Stern, J.; Sutter, B.; Freissinet, C.; Webster, C. R.; Morris, R.; Navarro-Gozalez, R.; Franz, H. B.; Glavin, D.; Conrad, P.; Owen, T.; Ming, D. |
| 著者所属（英） | NASA Johnson Space Center |
| 発行日 | 2015-03-16 |
| 言語 | eng |
| 内容記述 | In October 2014, the Mars Science Laboratory (MSL) "Curiosity" rover drilled into the sediment at the base of Mount Sharp in a location namsed Cionfidence Hills (CH). CH marked the fifth sample pocessed by the Sample Analysis at Mars (SAM) instrument suite since Curiosity arrived in Gale Crater, with previous analyses performed at Rocknest (RN), John Klein (JK), Cumberland (CB), and Windjana (WJ). Evolved gas analysis (EGA) of all samples has indicated H2O as well as O-, C- and S-bearing phases in the samples, often at abundances that would be below the detection limit of the CheMin instrument. By examining the temperatures at which gases are evolved from samples, SAM EGA data can help provide clues to the mineralogy of volatile-bearing phases when their identities are unclear to CheMin. SAM may also detect gases evolved from amorphous material in solid samples, which is not suitable for analysis by CheMin. Finally, the isotopic composition of these gases may suggest possible formation scenarios and relationships between phases. We will discuss C isotope ratios of CO2 evolved from the CH sample as measured with SAM's quadrupole mass spectrometer (QMS) and draw comparisons to samples previously analyzed by SAM. |
| NASA分類 | Geophysics |
| レポートNO | JSC-CN-32850 |
| 権利 | Copyright, Distribution as joint owner in the copyright |
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