The Rosseland mean opacity of interstellar grains

The opacity of interstellar grains in the temperature range 10-1500 K is calculated. Two composite grain models have been considered. One of them consists of silicate coated with an ice mantle and the second has a graphite core coated also with an ice mantle. These models are compared with isolated...

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Bibliographic Details
Published in:Astrophysics and space science Vol. 188; no. 1; pp. 109 - 116
Main Authors: ALI, A, EL-NAWAWY, M. S, EL SHALABY, M. A
Format: Journal Article
Language:English
Published: Dordrecht Kluwer 01-02-1992
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Summary:The opacity of interstellar grains in the temperature range 10-1500 K is calculated. Two composite grain models have been considered. One of them consists of silicate coated with an ice mantle and the second has a graphite core coated also with an ice mantle. These models are compared with isolated grain models. An exact analytical and computational development of Guttler's formulas for composite grain models has been used to calculate the extinction coefficient. It has been found that the thickness of the mantle affects the opacity of the interstellar grains. The opacity of composite models differs from that of the isolated models. The effect of the different species (ice, silicate, and graphite) is also clear. (Author)
Bibliography:ObjectType-Article-2
SourceType-Scholarly Journals-1
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content type line 23
ISSN:0004-640X
1572-946X
DOI:10.1007/BF00642927