Title of article
Analytical techniques for retrieval of atmospheric composition with the quadrupole mass spectrometer of the Sample Analysis at Mars instrument suite on Mars Science Laboratory
Author/Authors
B. Franz، نويسنده , , Heather and G. Trainer، نويسنده , , Melissa and H. Wong، نويسنده , , Michael and L.K. Manning، نويسنده , , Heidi and C. Stern، نويسنده , , Jennifer and R. Mahaffy، نويسنده , , Paul and K. Atreya، نويسنده , , Sushil and Benna، نويسنده , , Mehdi and G. Conrad، نويسنده , , Pamela and N. Harpold، نويسنده , , Dan and A. Leshin، نويسنده , , Laurie and A. Malespin، نويسنده , , Charles and P. McKay، نويسنده , , Christopher and Thomas Nolan، نويسنده , , J. and Raaen، نويسنده , , Eric، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2014
Pages
15
From page
99
To page
113
Abstract
The Sample Analysis at Mars (SAM) instrument suite is the largest scientific payload on the Mars Science Laboratory (MSL) Curiosity rover, which landed in Mars׳ Gale Crater in August 2012. As a miniature geochemical laboratory, SAM is well-equipped to address multiple aspects of MSL׳s primary science goal, characterizing the potential past or present habitability of Gale Crater. Atmospheric measurements support this goal through compositional investigations relevant to martian climate evolution. SAM instruments include a quadrupole mass spectrometer, a tunable laser spectrometer, and a gas chromatograph that are used to analyze martian atmospheric gases as well as volatiles released by pyrolysis of solid surface materials (Mahaffy et al., 2012). This report presents analytical methods for retrieving the chemical and isotopic composition of Mars׳ atmosphere from measurements obtained with SAM׳s quadrupole mass spectrometer. It provides empirical calibration constants for computing volume mixing ratios of the most abundant atmospheric species and analytical functions to correct for instrument artifacts and to characterize measurement uncertainties. Finally, we discuss differences in volume mixing ratios of the martian atmosphere as determined by SAM (Mahaffy et al., 2013) and Viking (Owen et al., 1977; Oyama and Berdahl, 1977) from an analytical perspective. Although the focus of this paper is atmospheric observations, much of the material concerning corrections for instrumental effects also applies to reduction of data acquired with SAM from analysis of solid samples.
Keywords
atmosphere , Mars , isotopes , Mars Science Laboratory , Sample Analysis at Mars investigation , Curiosity rover
Journal title
PLANETARY AND SPACE SCIENCE
Serial Year
2014
Journal title
PLANETARY AND SPACE SCIENCE
Record number
2316198
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