Lunar and Planetary Science XXXVI (2005) 2379.pdf AN UPDATE ON RESULTS FROM THE MAGNETIC PROPERTIES EXPERIMENTS ON THE MARS EXPLORATION ROVERS, SPIRIT AND OPPORTUNITY. M.B. Madsen1, H.M. Arneson2, P. Bertelsen1, J.F. Bell III2, C.S. Binau1, R. Gellert3, W. Goetz4, H.P. Gunnlaugsson5, K.E. Herk- enhoff6, S.F. Hviid4, J.R. Johnson6, M.J. Johnson2, K.M. Kinch5, G. Klingelhöfer7, J.M. Knudsen1, K. Leer1, D.E. Madsen1, E. McCartney2, J. Merrison5, D.W. Ming8, R.V. Morris8, M. Olsen1, J.B. Proton2, D. Rodionov7, M. Sims9, S.W. Squyres2, T. Wdowiak10, A.S. Yen11, and the Athena Science Team. 1Center for Planetary Science, DSRI and University of Copenhagen, Denmark (
[email protected]); 2Cornell University, Ithaca, USA; 3Max-Planck-Institut fűr Chemie, Mainz, Germany; 4Max Planck Institut für Sonnensystemforschung, Lindau, Germany; 5Institute for Physics and Astronomy, Aarhus University, Den- mark; 6Astrogeology Team, USGS, Flagstaff, Arizona, USA; 7Institut für Anorganische und Analytische Chemie, Johannes Gutenberg-Universität, Mainz, Germany; 8NASA Johnson Space Center, Houston, Texas, USA; 9NASA Ames Research Center; 10Birmingham University, Alabama, USA; 11Jet Propulsion Laboratory, Pasadena, USA. Introduction: The Magnetic Properties Experi- ceptibility (hence the “filtering”). Both magnets are ments were designed to investigate the properties of tilted an angle of 45 degrees with respect to horizontal the airborne dust in the Martian atmosphere. A pre- enabling them to sample airborne dust settling out of ferred interpretation of previous experiments (Viking the atmosphere – and to some degree enabling less and Pathfinder) was that the airborne dust is primarily magnetic or non-magnetic particles to escape capture 3 composed by composite silicate particles containing as by the magnets .