Published March 1, 2017 | Version v1
Journal article

Recalibration of the Mars Science Laboratory ChemCam instrument with an expanded geochemical database

  • 1. Los Alamos National Laboratory (United States)
  • 2. USGS Flagstaff (United States)
  • 3. L'Institut de Recherche en Astrophysique et Planétologie (France)
  • 4. Universite de Lorraine (France)
  • 5. University of Massachusetts (United States)
  • 6. Mt. Holyoke College (United States)
  • 7. SUNY Stony Brook (United States)
  • 8. Johnson Space Center (United States)
  • 9. Franklin & Marshall College (United States)
  • 10. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109 (United States)
  • 11. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 (United States)
  • 12. University of New Mexico (United States)
  • 13. Space Science Institute (United States)
  • 14. University of Massachusetts Lowell (United States)
  • 15. The College of New Jersey (United States)

Description

The ChemCam Laser-Induced Breakdown Spectroscopy (LIBS) instrument onboard the Mars Science Laboratory (MSL) rover Curiosity has obtained > 300,000 spectra of rock and soil analysis targets since landing at Gale Crater in 2012, and the spectra represent perhaps the largest publicly-available LIBS datasets. The compositions of the major elements, reported as oxides (SiO2, TiO2, Al2O3, FeOT, MgO, CaO, Na2O, K2O), have been re-calibrated using a laboratory LIBS instrument, Mars-like atmospheric conditions, and a much larger set of standards (408) that span a wider compositional range than previously employed. The new calibration uses a combination of partial least squares (PLS1) and Independent Component Analysis (ICA) algorithms, together with a calibration transfer matrix to minimize differences between the conditions under which the standards were analyzed in the laboratory and the conditions on Mars. While the previous model provided good results in the compositional range near the average Mars surface composition, the new model fits the extreme compositions far better. Examples are given for plagioclase feldspars, where silicon was significantly over-estimated by the previous model, and for calcium-sulfate veins, where silicon compositions near zero were inaccurate. The uncertainties of major element abundances are described as a function of the abundances, and are overall significantly lower than the previous model, enabling important new geochemical interpretations of the data. - Highlights: • A LIBS spectral database from 408 geochemical standards has been compiled. • This database was used to generate new ChemCam multivariate calibration models for the major elements. • The results of this model produce more accurate geochemical results for the ChemCam Mars observations. • The ChemCam accuracies and precisions have been improved.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.sab.2016.12.003

Additional details

Identifiers

DOI
10.1016/j.sab.2016.12.003;
PII
S0584-8547(16)30391-3;

Publishing Information

Journal Title
Spectrochimica Acta. Part B, Atomic Spectroscopy
Journal Volume
129
Journal Page Range
p. 64-85
ISSN
0584-8547
CODEN
SAASBH

Optional Information

Copyright
Copyright (c) 2017 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.