Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-18T16:39:10.542Z Has data issue: false hasContentIssue false

Optical Constants Of Kerogen From 0.15 To 40 μm: Comparison with Meteoritic Organics

Published online by Cambridge University Press:  12 April 2016

B.N. Khare
Affiliation:
Cornell UniversityIthaca, NY 14853USA
W.R. Thompson
Affiliation:
Cornell UniversityIthaca, NY 14853USA
C. Sagan
Affiliation:
Cornell UniversityIthaca, NY 14853USA
E.T. Arakawa
Affiliation:
Oak Ridge National Lab. Oak Ridge, TN 37831
C. Meisse
Affiliation:
Oak Ridge National Lab. Oak Ridge, TN 37831
I. Gilmour
Affiliation:
Oak Ridge National Lab. Oak Ridge, TN 37831

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

A vacuum evaporation technique has been used to produce thin, optical quality films of samples of Type II kerogen and of insoluble organic residue from the Murchison meteorite. Using these films, optical constants have been measured from 0.15 to 40 μm for kerogen, and from 2.5 to 40 μm for the Murchison residue. The infrared absorption properties of these materials show many similarities, although Murchison residue is more opaque throughout the infrared than is kerogen, and shows no distinct aliphatic absorptions.

Type
Interplanetary Dust: Physical and Chemical Analysis
Copyright
Copyright © Kluwer 1991

References

Bell, J.F., Cruikshank, D. P., and Gaffey, M. J. (1985) ‘The composition and origin of the Iapetus dark material’, Icarus 61, 192.Google Scholar
Gradie, J. and Veverka, J. (1980) ‘The Composition of the Trojan asteroids’, Nature 283, 840.Google Scholar