Grain Formation in Nova Envelopes

Physics

Scientific paper

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Scientific paper

Grain formation in ejected envelopes of novae is investigated. To solar abundance is assumed as one of the typical examples that C/O is smaller than unity. The magnesium silicate is proved to be the firstmain condensate. We estimate the monomer concentration c1(t1) at the onset of condensation to be about 105 cm-3 for Δ M =3 × 10-4 M&sun; and Vexp = 1000 km sec-1. (Δ M is the ejected mass and Vexp is the expansion velocity.) Then we calculate the time variation of the concentrations of magnesium-silicate grains on the basis of thenonsteady nucleation theory. The size distributions are found to be flat or diffuse and have no conspicuous peak. The boundary whether grains are formed or not is determined mainly by the amount of the ejected mass. The lower limit of the ejected mass for about 10-4Modot. The maximum radius of grains is estimated to be about 50 Å for c1(t1) = 5 × 105 cm-3.

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