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Dynamic Dust Accumulation and Dust Removal Observed on the Mars Exploration Rover MagnetsThe Mars Exploration Rovers each carry a set of Magnetic Properties Experiments designed to investigate the properties of the airborne dust in the Martian atmosphere. It is a preferred interpretation of previous experiments that the airborne dust in the Martian atmosphere is primarily composed by composite silicate particles containing one or more highly magnetic minerals as a minor constituent. The ultimate goal of the magnetic properties experiments on the Mars Exploration Rover mission is to provide some information/ constraints on whether the dust is formed by volcanic, meteoritic, aqueous, or other processes. The first problem is to identify the magnetic mineral(s) in the airborne dust on Mars. While the overall results of the magnetic properties experiments are presented in, this abstract will focus on dust deposition and dust removal on some of the magnets.
Document ID
20050166990
Acquisition Source
Headquarters
Document Type
Conference Paper
Authors
Bertelsen, P.
(Copenhagen Univ. Denmark)
Bell, J. F., III
(Cornell Univ. Ithaca, NY, United States)
Goetz, W.
(Max-Planck-Inst. fuer Sonnensystemforschung Lindau, Germany)
Gunnlaugsson, H. P.
(Aarhus Univ. Denmark)
Herkenhoff, K. E.
(Geological Survey Flagstaff, AZ, United States)
Hviid, S. F.
(Max-Planck-Inst. fuer Sonnensystemforschung Lindau, Germany)
Johnson, J. R.
(Geological Survey Flagstaff, AZ, United States)
Kinch, K. M.
(Aarhus Univ. Denmark)
Knudsen, J. M.
(Copenhagen Univ. Denmark)
Madsen, M. B.
(Copenhagen Univ. Denmark)
Date Acquired
September 7, 2013
Publication Date
January 1, 2005
Publication Information
Publication: Lunar and Planetary Science XXXVI, Part 2
Subject Category
Lunar And Planetary Science And Exploration
Distribution Limits
Public
Copyright
Public Use Permitted.
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