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Calcium in Mercury's Exosphere: Modeling MESSENGER DataMercury is surrounded by a surface-bounded exosphere comprised of atomic species including hydrogen, sodium, potassium, calcium, magnesium, and likely oxygen. Because it is collisionless. the exosphere's composition represents a balance of the active source and loss processes. The Mercury Atmospheric and Surface Composition Spectrometer (MASCS) on the MErcury Surface. Space ENvironment. GEochemistry. and Ranging (MESSENGER) spacecraft has made high spatial-resolution observations of sodium, calcium, and magnesium near Mercury's surface and in the extended, anti-sunward direction. The most striking feature of these data has been the substantial differences in the spatial distribution of each species, Our modeling demonstrates that these differences cannot be due to post-ejection dynamics such as differences in photo-ionization rate and radiation pressure. but instead point to differences in the source mechanisms and regions on the surface from which each is ejected. The observations of calcium have revealed a strong dawn/dusk asymmetry. with the abundance over the dawn hemisphere significantly greater than over the dusk. To understand this asymmetry, we use a Monte Carlo model of Mercury's exosphere that we developed to track the motions of exospheric neutrals under the influence of gravity and radiation pressure. Ca atoms can be ejected directly from the surface or produced in a molecular exosphere (e.g., one consisting of CaO). Particles are removed from the system if they stick to the surface or escape from the model region of interest (within 15 Mercury radii). Photoionization reduces the final weighting given to each particle when simulating the Ca radiance. Preliminary results suggest a high temperature ( I-2x 10(exp 4) K) source of atomic Ca concentrated over the dawn hemisphere. The high temperature is consistent with the dissociation of CaO in a near-surface exosphere with scale height <= 100 km, which imparts 2 eV to the freshly produced Ca atom. This source region and energy are consistent with data from the three MESSENGER flybys; whether this holds true for the data obtained in orbit is under investigation.
Document ID
20110022524
Acquisition Source
Goddard Space Flight Center
Document Type
Presentation
Authors
Burger, Matthew H.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Killen, Rosemary M.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
McClintock, William E.
(Colorado Univ. Boulder, CO, United States)
Merkel, Aimee
(Colorado Univ. Boulder, CO, United States)
Vervack, Ronald J.
(Johns Hopkins Univ. Laurel, MD, United States)
Sarantos, Menelaos
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Sprague, Ann L.
(Arizona Univ. Tucson, AZ, United States)
Date Acquired
August 25, 2013
Publication Date
September 23, 2011
Subject Category
Lunar And Planetary Science And Exploration
Report/Patent Number
GSFC.CPR.5227.2011
GSFC.CPR.00164.2012
Meeting Information
Meeting: American Geophysical Union Fall Meeting
Location: San Francisco, CA
Country: United States
Start Date: December 5, 2011
End Date: December 9, 2011
Distribution Limits
Public
Copyright
Public Use Permitted.
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