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AGU: Journal of Geophysical Research, Planets

 

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  • Planetology: Solid Surface Planets: Origin and evolution
  • Planetology: Solid Surface Planets: Volcanism
  • Planetology: Solid Surface Planets: Surface materials and properties
  • Planetology: Solid Surface Planets: Remote sensing
Abstract
Cited By (12)
 

Abstract

Lunar Prospector neutron spectrometer constraints on TiO2

R. C. Elphic

Space and Atmospheric Sciences, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

D. J. Lawrence

Space and Atmospheric Sciences, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

W. C. Feldman

Space and Atmospheric Sciences, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

B. L. Barraclough

Space and Atmospheric Sciences, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

O. M. Gasnault

Space and Atmospheric Sciences, Los Alamos National Laboratory, Los Alamos, New Mexico, USA

S. Maurice

Observatoire Midi-Pyrénées, Toulouse, France

P. G. Lucey

Hawai'i Institute of Geophysics and Planetology, University of Hawaii at Manoa, Hawaii, USA

D. T. Blewett

Hawai'i Institute of Geophysics and Planetology, University of Hawaii at Manoa, Hawaii, USA

A. B. Binder

Lunar Research Institute, Tucson, Arizona, USA

Lunar Prospector neutron spectrometer measurements of the epithermal and thermal neutron leakage fluxes are used to provide constraints on TiO2 abundances in lunar surface materials. We use FeO abundance estimates based on both Clementine spectral reflectance techniques and preliminary Lunar Prospector gamma ray spectrometer determinations to first establish a model thermal neutron absorption due to all major elements except titanium. Then we remove the additional absorbing effects due to the rare earth elements gadolinium and samarium by using Lunar Prospector gamma ray spectrometer thorium abundances as a rare earth element proxy. The result can be compared to the ratio of epithermal to thermal neutron fluxes, which point to the presence of the additional thermal neutron absorber, titanium. We can derive abundance estimates of TiO2 and compare to other estimates derived spectroscopically. Our results show a significantly lower abundance of TiO2 than has been derived using Clementine data.

Published 30 April 2002.

Citation: Elphic, R. C., D. J. Lawrence, W. C. Feldman, B. L. Barraclough, O. M. Gasnault, S. Maurice, P. G. Lucey, D. T. Blewett, and A. B. Binder (2002), Lunar Prospector neutron spectrometer constraints on TiO2, J. Geophys. Res., 107(E4), 5024, doi:10.1029/2000JE001460.

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