Computer Simulation of PHOBOS Spectrum: Implication to Surface Composition

Details Computer Simulation of PHOBOS Spectrum: Implication to Surface Composition Computer Simulation of PHOBOS Spectrum: Implication to Surface Composition

Mar 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996lpi....27.1263s&link_type=abstract

Lunar and Planetary Science, volume 27, page 1263

Computer Science

Phobos: Composite Spectrum, Phobos: Suface Material, Spectra: Computer Simulation

Scientific paper

Composite Phobos spectrum proposed by the authors is simulated. Calculation show that (1) modification of the carbonaceous chondrite spectra by formation of fine grains of reduced iron in the upper surface layers of particles (similar to those in lunar regolith) do not match the Phobos spectral curve; (2) a good fit for it is obtained for submicron mixtures of clay minerals and dark red organic compounds, so Phobos spectral curve can be explained by higher H content in the organic components of Phobos surface material as compared to carbonaceous chondrites.

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