Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/17113
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Depth selective Mossbauer spectroscopy: Analysis and simulation of 6.4 keV and 14.4 keV spectra obtained from rocks at Gusev Crater, Mars, and layered laboratory samples
Authors: Fleischer, Iris
Klingelhoefer, Goestar
Schröder, Christian
Morris, Richard Van
Hahn, Matthias
Rodionov, Daniel S
Gellert, Ralf
de, Souza Jr Paulo A
Contact Email: christian.schroeder@stir.ac.uk
Keywords: depth-selective Mössbauer spectroscopy
Mars
Issue Date: 26-Jun-2008
Publisher: Wiley-Blackwell for the American Geophysical Union
Citation: Fleischer I, Klingelhoefer G, Schröder C, Morris RV, Hahn M, Rodionov DS, Gellert R & de Souza Jr PA (2008) Depth selective Mossbauer spectroscopy: Analysis and simulation of 6.4 keV and 14.4 keV spectra obtained from rocks at Gusev Crater, Mars, and layered laboratory samples, Journal of Geophysical Research: Planets, 113 (E6), Art. No.: E06S21.
Abstract: The miniaturized Mössbauer spectrometer (MIMOS) II Mössbauer spectrometers on the Mars Exploration Rovers (MER) simultaneously obtained 6.4 keV and 14.4 keV Mössbauer spectra from rock and soil targets. Because photons with lower energy have a shallower penetration depth, 6.4 keV spectra contain more mineralogical information about the near-surface region of a sample than do 14.4 keV spectra. The influence of surface layers of varying composition and thickness on Mössbauer spectra was investigated by Monte Carlo simulation and by measurement using a copy of the MER MIMOS II instrument and samples with one or two layers of known thicknesses. Thin sections of minerals or metallic Fe foil on top of a thick mineral sample were used to produce samples with thin layers of known thickness on a thick substrate. Monte Carlo simulation of MER spectra obtained on the rock Mazatzal, which displays a coating on a basaltic substrate, and other Adirondack Class rocks results in a calculated thickness of 10 micrometer for the Mazatzal surface layer. The 6.4 keV spectra obtained on Adirondack Class rocks, on laboratory samples, and in Monte Carlo calculations show an apparent olivine enrichment which is not related to any observable surface layer.
Type: Journal Article
URI: http://hdl.handle.net/1893/17113
DOI Link: http://dx.doi.org/10.1029/2007JE003022
Rights: Copyright 2008 by the American Geophysical Union. AGU allows authors to deposit their journal articles if the version is the final published citable version of record, the AGU copyright statement is clearly visible on the posting, and the posting is made 6 months after official publication by the AGU.
Affiliation: Johannes Gutenberg University of Mainz
Johannes Gutenberg University of Mainz
Biological and Environmental Sciences
National Aeronautics and Space Administration (NASA)
Johannes Gutenberg University of Mainz
Johannes Gutenberg University of Mainz
University of Guelph
University of Tasmania

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