Statistics – Computation
Scientific paper
Dec 2011
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011agufm.p41a1583r&link_type=abstract
American Geophysical Union, Fall Meeting 2011, abstract #P41A-1583
Statistics
Computation
[1060] Geochemistry / Planetary Geochemistry, [6235] Planetary Sciences: Solar System Objects / Mercury
Scientific paper
The MESSENGER Gamma-Ray Spectrometer (GRS) measures energy spectra of gamma rays emanating from the surface of Mercury. Analysis of these spectra provides elemental abundances of surface material. The MESSENGER mission necessarily provides some data normalization challenges for GRS analysis. So as to keep the spacecraft cool while orbiting the dayside of the planet, the orbits are highly eccentric, with altitudes varying from 200-500 km to ~ 15,000 km. A small fraction of time is spent at the low altitudes where gamma-ray signals are largest, requiring a large number of orbits to yield sufficient counting statistics for elemental analysis. Also, the sunshade must always shield the spacecraft from the Sun, which causes the orientation of the GRS often to be far from nadir-pointing, so the detector efficiency and attenuation of gamma rays from the planet must be known for a wide range of off-nadir orientations. An efficiency/attenuation map for the expected ranges of orientations and energies was constructed in a ground calibration experiment for a limited range of orientations using a nuclear reactor and radioisotope sources, and those results were extended to other orientations by radiation transport computations using as input a computer-aided design model of the spacecraft and its composition. This normalization has allowed abundance determinations of elements K, Th, and U from radioisotopes of these elements in the Mercury regolith during the first quarter of the year-long mission. These results provide constraints on models of Mercury's chemical and thermal evolution. The normalization of gamma-ray spectra for surface elements not having radioisotopes is considerably more complex; these gamma rays come from neutron inelastic-scatter and capture reactions in the regolith, where the neutrons are generated by cosmic ray impact onto the planet. A radiation transport computation was performed to generate the expected count rates in the neutron-generated gamma-ray peaks, for a fixed cosmic ray flux and a regolith composition approximating that expected. These peak count rates must be matched to the corresponding GRS peak count rates to determine abundances and normalized to a proxy for the cosmic ray flux (such as the charge-reset rate of the GRS shield). The background subtraction for neutron-generated gamma-ray peaks for elements that are also present in the spacecraft, such as Fe, Ti, Al, and Mg, is complicated by a background increase due to neutrons from the planet interacting with the spacecraft at low altitude. We are presently using simple formulas involving planet-subtended solid angle and proxies for neutron flux at the spacecraft to correct for this background increase. There is no background subtraction for elements not present at significant levels in the spacecraft, such as Ca, S, and Cl. Improvements in normalization and count statistics will enable determination of abundances for more elements.
Boynton Willam V.
Evans Larry G.
Hamara David K.
Peplowski Patrick N.
Rhodes Edgar A.
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