Variations on solar condensation: Sources of interstellar dust nuclei

Astronomy and Astrophysics – Astrophysics

Scientific paper

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Solar Physics, Astrophysics, And Astronomy

Scientific paper

Some portion of the interstellar dust entering the heliosphere is a refractory (Ca-Al-Ti-Mg-Si-Fe-Ni-Cr-Co-rich) component either condensed at high temperature from stellar outflows or formed in the interstellar medium (ISM). Condensation sequences for T>1100K, assuming chemical equilibrium, are calculated for stellar outflow gas having (1) solar composition at various Ptot; (2) compositions approaching C/O=0.9, otherwise solar; (3) metallicities reduced by Z/Z0=0.10; and (4) metallicities enhanced by added dust components. Calculated depletions are relatively insensitive to these excursions from the canonical ``cosmic'' abundances. The intragroup similarities of depletions observed for the element groups (Ca-Ti), (Fe-Ni-Cr-Co), and (Mg-Si) reflect the dominant mineralogy calculated for stardust: Ti- and Ca-aluminate phases, metal alloy, and Mg2SiO4 (Mg-olivine). This result suggests that the bulk of the refractory component of ISM dust was condensed in stellar environments.

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