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Chemical Composition of Dust Expected from Condensation Models

Published online by Cambridge University Press:  12 April 2016

Tetsuo Yamamoto*
Affiliation:
Institute of Space and Astronautical Science Yoshinodai 3-1-1, Sagamihara Kanagawa 229Japan

Abstract

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This review examines to what degrees the present chemical equilibrium condensation models are effective in predicting chemical composition of grains observed in a variety of cosmic environments. The composition expected from the equilibrium calculations is reviewed separately for refractory (rocky and metallic) and volatile (icy) components. Comments are given on the limitation of the equilibrium calculations in predicting the grain composition. By taking cometary ice as a typical cosmic volatile condensate, it is pointed out that its composition is far from that expected from the equilibrium models. Theories on the formation of cometary volatiles are reviewed, and an observational clue helpful to testing the theories is pointed out. Discussion is given on the advantage for formation of organic materials from volatile solids.

Type
Origin of Interplanetary Dust: from Comets and Asteroids, Back to Interstellar Dust
Copyright
Copyright © Kluwer 1991

References

Amari, S., Anders, E., Virag, A, and Zinner, E. (1990): ‘Interstellar graphite in meteorites’, Nature 345, 238240.Google Scholar
Bernatowicz, T., Fraundorf, G., Ming, T., Anders, E., Wopenka, B., Zinner, E., and Fraundorf, P. (1987): ‘Evidence for interstellar SiC in the Murray carbonaceous meteorites’, Nature 330, 728723.Google Scholar
Bradley, J.P. and Brownlee, D.E. (1986): ‘Cometary particles: Thin sectioning and electron beam analysis’, Science 231, 15421544.CrossRefGoogle ScholarPubMed
Bode, M.F. (1988): ‘Observations and modelling of circumstellar dust’, Dust in the Universe, eds. Bailey, M.E. and Williams, D.A., Cambridge University Press, Cambridge, pp. 73102.Google Scholar
d’Hendecourt, L.B., Allamandola, L.J., and Greenberg, J.M. (1985): ‘Time dependent chemistry in dense molecular clouds I. Grain surface reactions, gas/grain interactions and infrared spectroscopy’, Astron. Astrophys. 152, 130150.Google Scholar
Duley, W.W. (1988): ‘Models of interstellar grains’, Dust in the Universe, eds. Bailey, M.E. and Williams, D.A., Cambridge University Press, Cambridge, pp. 209218.Google Scholar
Engel, S., Lunine, J.I., and Lewis, J.S. (1990): ‘Solar nebula origin for volatiles in Halley’s comet’, Icarus 85, 380393.CrossRefGoogle Scholar
Fegley, B. Jr., and Prinn, R.G. (1989): ‘Solar nebula chemistry: Implications for volatiles in the solar nebula’, The Formation and Evolution of Planetary Systems, eds. Weaver, H.A., and Danley, L., Cambridge Univ. Press., Cambridge, pp. 171211.Google Scholar
Gilman, R.C. (1969): ‘On the composition of circumstellar grains’, Astrophys. J 155, L185L187.Google Scholar
Grossman, L. and Larimer, J.W. (1974): ‘Early chemical history of the solar system’, Rev. Geophys. Space Phys. 42, 71101.Google Scholar
Greenberg, J.M. (1971): ‘The chemical and physical properties of interstellar dust’, Molecules in the Galactic Environment, eds. Gordon, M.A. and Snyder, L.E., John Wiley & Sons, New York, pp. 94124.Google Scholar
Greenberg, J.M. (1982): ‘What are comets made of? A model based on interstellar dust’, Comets, ed. Wilkening, L.L., Univ. Arizona Press, Tucson, pp. 131163.Google Scholar
Greenberg, J.M. (1988): ‘The interstellar dust model of comets: post Halley’, Dust in the Universe, eds. Bailey, M.E. and Williams, D.A., Cambridge University Press, Cambridge, pp. 121143.Google Scholar
Irvine, W.M. and Hjarmarson, Å. (1983): ‘Comets, interstellar molecules, and the origin of life’, Cosmochemistry and the Origin of Life, eds. Ponnamperuma, C., D. Reidel, Dordrecht, pp. 113142.Google Scholar
Klinger, J. (1990), ‘Physical properties of frozen volatiles - Their relevance to the study of comet nuclei’, ‘Comets in the Post-Halley Era’, eds. Newburn, R. and Rahe, J., Kluwer Academic Publishers, in press.Google Scholar
Kissel, J and Krüger, F.R. (1987): ‘The organic component in dust írom Comet Halley as measured by the PUMA mass spectrometer on board VegaNature 326, 755760.Google Scholar
Kouchi, A. and Kuroda, T. (1990): ‘Amorphization of cubic ice by ultraviolet radiation’, Nature 344, 134135.Google Scholar
Larson, H.P., Weaver, H.A., Mumma, M.J., and Drapatz, S. (1988): ‘Airborne infrared spec-troscopy of Comet Wilson (19861) and comparison with Comet Halley’, Astrophys. J. 338, 11061114.Google Scholar
Lewis, J.S. (1974): ‘The temperature gradient in the solar nebula’, Science 186, 440443.Google Scholar
Lewis, J.S., and Prinn, R.G. (1980): ‘Kinetic inhibition of CO and N2 reduction in the solar nebula’, Astrophys. J. 238, 357364.CrossRefGoogle Scholar
Léger, A. and Puget, J.L. (1984): ‘Identification of the ‘unidentified’ IR emission features of interstellar dust?’, Astron. Astrophys. 137, L5 L8.Google Scholar
Lunine, J.I. (1989): ‘Primitive bodies: Molecular abundances in Comet Halley as probes of cometary formation environment’, The Formation and Evolution of Planetary Systems, eds. Weaver, H.A., Danley, L., and Paresce, F., Cambridge Univ. Press., Cambridge, pp. 213242.Google Scholar
Mumma, M.J., Weaver, H.A., and Larson, H.P. (1987): ‘The ortho-para ratio of water vapor in comet P/Halley’, Astron. Astrophys. 187, 419424.Google Scholar
Prinn, R.G., and Fegley, B. Jr. (1989): ‘Solar nebula chemistry: Origin of planetary, satellite, and cometary volatiles’, Origin and Evolution of Planetary and Satellite Atmospheres, eds. Atrea, S., Pollack, J., and Matthews, M., Univ. Arizona Press, Tucson, pp. 78136.CrossRefGoogle Scholar
Sakata, A., Wada, S., Tanabé, T., and Onaka, T. (1984): ‘Infrared spectrum of the laboratory-synthesized quenched carbonaceous composite (QCC): Comparison with the infrared unidentified emission bands’, Astrophysical J. Lett. 287, L51 L54.Google Scholar
Salpeter, E.E. (1977): ‘Formation and destruction of dust grains’, Ann. Rev. Astron. Astrophys. 15, 267293.Google Scholar
Seki, J. and Hasegawa, H. (1981): ‘Origin of amorphous interstellar ice grains’, Prog. Theor. Phys. 66, 903912.Google Scholar
Weaver, H.A. (1989): ‘The volatile composition of comets’, Highlights Astron. 8, 387393.CrossRefGoogle Scholar
Whittet, D.C.B. (1984): ‘Interstellar grain composition: A model based on elemental depletions’, Mon. Not. R. Astron. Soc. 210, 479487.Google Scholar
Woolf, N.J. (1975): ‘Circumstellar dust’, Dusty Universe, eds. Field, G.B. and Cameron, A.G.W., Neale Watson Academic Publications, Inc., New York, pp. 5987.Google Scholar
Yamamoto, T. (1985): ‘Formation environment of cometary nuclei in the primordial solar nebula’, Astron. Astrophys. 142, 3136.Google Scholar
Yamamoto, T. (1990a): ‘Chemical theories on the origin of comets’, ‘Comets in the Post-Halley Era’, eds. Newburn, R. and Rahe, J., Kluwer Academic Publishers, in press.Google Scholar
Yamamoto, (1990b): ‘The origin of comets as viewed from the gaseous composition’, Primitive Solar Nebula and Origin of the Planets, eds. Oya, H., Nakazawa, K., and Mizutani, H., Terra Publishing Company, Tokyo, in press.Google Scholar
Yamamoto, T., Nakagawa, N., and Fukui, Y. (1983): ‘The chemical composition and thermal history of the ice of a cometary nucleus’, Astron. Astrophys. 122, 171176.Google Scholar