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ICE Mantle Formation in the Envelopes of OH/IR Stars

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Planetary Nebulae

Part of the book series: International Astronomical Union / Union Astronomique Internationale ((IAUS,volume 155))

Abstract

We have computed ice column densities for a sample of O-rich late-type stars.

Water ice is observed in the outflows from several late-type stars (e.g. Smith et al. 1988) and it is of some observational and theoretical importance to understand how common ice mantles may be and how their formation depends upon the physical conditions in the envelope such as the radial distributions of density and temperature. We have developed a simple theory of the gas-grain interaction in circumstellar shells (Jura & Morris 1985; Charnley et al. 1992) and used it to compute ice column densities (N ice ) and mantle thicknesses (d) for a sample of well-studied OH/IR stars (Herman & Habing 1985). The models are most sensitive to the dust and gas mass loss rates, as well as to the inner radius of the envelope, R i , which is poorly determined. Representative results are presented in the Table below where R i was estimated according to the prescription of Herman et al. (1986).

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© 1993 Springer Science+Business Media Dordrecht

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Charnley, S.B., Smith, R.G. (1993). ICE Mantle Formation in the Envelopes of OH/IR Stars. In: Weinberger, R., Acker, A. (eds) Planetary Nebulae. International Astronomical Union / Union Astronomique Internationale, vol 155. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-2088-3_128

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  • DOI: https://doi.org/10.1007/978-94-011-2088-3_128

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-7923-2440-9

  • Online ISBN: 978-94-011-2088-3

  • eBook Packages: Springer Book Archive

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