|
Read Full Article (file size: 1097020 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 108, NO. E12,
8070,
doi:10.1029/2002JE002041,
2003
Physical properties and localization investigations associated with the 2003 Mars Exploration rovers
R. E. Arvidson
McDonnell Center for the Space Sciences, Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri,
USA
R. C. Anderson
Jet Propulsion Laboratory, Pasadena, California, USA
A. F. C. Haldemann
Jet Propulsion Laboratory, Pasadena, California, USA
G. A. Landis
NASA Glenn Research Center, Cleveland, Ohio, USA
R. Li
Department of Civil and Environmental Engineering and Geodetic Science, Ohio State University, Columbus, Ohio, USA
R. A. Lindemann
Jet Propulsion Laboratory, Pasadena, California, USA
J. R. Matijevic
Jet Propulsion Laboratory, Pasadena, California, USA
R. V. Morris
NASA Johnson Space Center, Houston, Texas, USA
L. Richter
DLR Institut für Raumsimulation, Köln, Germany
S. W. Squyres
Center for Radiophysics and Space Research, Cornell University, Ithaca, New York, USA
R. J. Sullivan
Center for Radiophysics and Space Research, Cornell University, Ithaca, New York, USA
N. O. Snider
McDonnell Center for the Space Sciences, Department of Earth and Planetary Sciences, Washington University, St. Louis, Missouri,
USA
Abstract
A number of physical properties experiments will be conducted during the NASA 2003 Mars Exploration Rover Mission as the two
vehicles explore Meridiani Planum and the floor of Gusev Crater. The investigations will include quantifying dust accumulation
and dispersal dynamics by periodically monitoring the rover decks with the Athena Pancam and Mini-TES instruments. Properties
of soil-like materials will be inferred from analyses of wheel track patterns, depths, and wheel slippage dynamics during
traverses. The rovers will be modeled as dynamic mechanical systems to extract along-track terrain topography and physical
properties from times series of rover tilt vectors, wheel encoder counts, azimuths, motor currents, and rocker and bogie angles.
Trenches will be excavated using rover wheels to characterize mechanical properties of soil-like materials with depth and
to expose subsurface materials for remote and in situ observations using the Athena Payload. The Rock Abrasion Tools will
be used to expose rock subsurfaces for detailed analyses. Motor currents and penetration magnitudes will be compared to a
database of rocks excavated by an engineering model of the Rock Abrasion Tool to understand Martian rock mechanical properties.
Image-based localization analyses will be pursued to better understand rover traverse directions and magnitudes and thus rover
locations as a function of time. The physical properties and localization investigations, when combined with analyses of the
full ensemble of Athena observations, will greatly improve our understanding of Martian surface properties and provide significant
technology lessons for future landed missions.
Received 31
December
2002;
accepted 17
June
2003;
published 24
October
2003.
Index Terms: 5494 Planetology: Solid Surface Planets: Instruments and techniques; 5470 Planetology: Solid Surface Planets: Surface materials and properties; 5464 Planetology: Solid Surface Planets: Remote sensing; 5460 Planetology: Solid Surface Planets: Physical properties of materials.
Read Full Article (file size: 1097020 bytes) Cited by
Citation: Arvidson, R. E., et al.
(2003),
Physical properties and localization investigations associated with the 2003 Mars Exploration rovers,
J. Geophys. Res.,
108(E12),
8070,
doi:10.1029/2002JE002041.
Copyright 2003 by the American Geophysical Union.
|