Physics
Scientific paper
May 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agusm...p22b03k&link_type=abstract
American Geophysical Union, Spring Meeting 2001, abstract #P22B-03
Physics
5410 Composition, 5464 Remote Sensing, 5470 Surface Materials And Properties, 6225 Mars
Scientific paper
A region on Mars within Sinus Meridiani has been interpreted as a surface partially covered by coarse-grained (gray) hematite, using spectra measured by the 1996 Global Surveyor Thermal Emission Spectrometer (TES) [Lane et al., 1999; Christensen et al., 2000]. The band strengths recorded by TES of this region are consistent with either coarse-grained hematite, or cemented poorly crystalline or cemented fine-grained hematite. The band strengths are inconsistent with unconsolidated, poorly crystalline or fine-grained hematite, including nanophase hematite dust [Christensen et al., 2000]. Currently the gray hematite interpretation is based on bands centered near 22 and 33 microns. TES also records a band centered near 18 microns that was used in early hematite interpretations [Lane et al., 1999]. However, it was noted [Kirkland et al., 1999a] that the 18 micron band is too narrow in both TES and the 1971 Mariner Mars IRIS spectra to be a good match to typical spectra of well-crystalline hematite [e.g. Salisbury et al., 1991]. The 18 micron band is near the very strong 15 micron atmospheric CO2 band, but if anything the nearby CO2 band should cause the 18 micron band to appear wider, not narrower. In addition, the higher spectral resolution of IRIS allows improved separation of the bands [Kirkland et al., 1999b]. More recent publications no longer show the TES 18 micron band [e.g. Lane et al., 2000; Christensen et al., 2000], which temporarily resolved the issue. However, we feel it is important to understand why TES and IRIS spectra exhibit an 18 micron band that is too narrow to match typical spectra of coarse-grained hematite. Smooth-surfaced cemented (e.g. ferricrete) or coated materials (e.g. desert varnish) have spectral contrast that is consistent with the observed IRIS and TES band contrast. On Mars, one possible source for cemented material or coatings would be the nanophase hematite dust. Cemented materials may occur in bulk (e.g. duricrust or ferricrete), or as a thin coating (e.g. desert varnish). We have investigated the signatures of naturally occurring cemented materials that contain hematite, and found samples that exhibit 22 and 33 micron bands that are consistent with coarse-grained hematite signatures, and yet also exhibit narrower 18 micron bands. We are continuing to study the materials more in-depth to examine the variations in spectral shape, and to determine the cause of varied 18 micron band width. References. Christensen, P. R. et al., JGR 105, 9632, 2000. Kirkland, L., K. Herr, P. Forney, and J. Salisbury, LPSC XXX, abs. 1693 and oral presentation, 1999a. Kirkland, L., K. Herr, and P. Forney, 5th Internat'l Conf. on Mars, abs. 6174, 1999b. Lane, M., R. Morris, and P. Christensen, LPSC XXX, abs. 1469, 1999. Lane, M., R. Morris, and P. Christensen, LPSC XXXI, abs. 1140, 2000. Salisbury, J., L. Walter, N. Vergo, D. D'Aria, Infrared (2.1-25 micron) Spectra of Minerals, Johns Hopkins UP, 1991.
Adams Paul M.
Herr Kenneth C.
Kirkland Laurel Ellyn
No associations
LandOfFree
Searching for an Improved Spectral Match to TES and IRIS Sinus Meridiani Spectra: Coatings and Cemented Materials does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Searching for an Improved Spectral Match to TES and IRIS Sinus Meridiani Spectra: Coatings and Cemented Materials, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Searching for an Improved Spectral Match to TES and IRIS Sinus Meridiani Spectra: Coatings and Cemented Materials will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1272026