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Use of near infrared correlation spectroscopy for quantitation of surface iron, absorbed water and stored electronic energy in a suite of Mars soil analog materialsA number of questions concerning the surface mineralogy and the history of water on Mars remain unresolved using the Viking analyses and Earth-based telescopic data. Identification and quantitation of iron-bearing clays on Mars would elucidate these outstanding issues. Near infrared correlation analysis, a method typically applied to qualitative and quantitative analysis of individual constituents of multicomponent mixtures, is adapted here to selection of distinctive features of a small, highly homologous series of Fe/Ca-exchanged montmorillonites and several kalinites. Independently determined measures of surface iron, relative humidity and stored electronic energy were used as constituent data for linear regression of the constituent vs. reflectance data throughout the spectral region 0.68 to 2.5 micrometers. High correlations were found in appropriate regions for all three constituents, though that with stored energy is still considered tenuous. Quantitation was improved using 1st and 2nd derivative spectra. High resolution data over a broad spectral range would be required to quantitatively identify iron-bearing clays by remotely sensed reflectance.
Document ID
19890016970
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Coyne, Lelia M.
(San Jose State Univ. CA., United States)
Banin, Amos
(Hebrew Univ. Jerusalem, Israel)
Carle, Glenn
(San Jose State Univ. CA., United States)
Orenberg, James
(San Jose State Univ. CA., United States)
Scattergood, Thomas
(San Jose State Univ. CA, United States)
Date Acquired
September 6, 2013
Publication Date
March 1, 1989
Publication Information
Publication: NASA, Ames Research Center, Exobiology and Future Mars Missions
Subject Category
Lunar And Planetary Exploration
Accession Number
89N26341
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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