During the Ðrst 20 s of its life, the enormous neutrino luminosity of a neutron star drives appreciable mass loss from its surface.This neutrino-driven wind has been previously identiÐed as a likely site for the r-process.Qian & Woosley have derived, both analytically and numerically, the physical conditions relevant for heavy element synthesis in the wind.These conditions include the entropy (S), the electron fraction the dynamic timescale, and the mass loss rate.Here we explore the implications of these (Y e), conditions for nucleosynthesis.We Ðnd that the standard wind models derived in that paper are inadequate to make the r-process, though they do produce some rare species above the iron group.We further determine the general restrictions on the entropy, the electron fraction, and the dynamic timescale that are required to make the r-process.In particular, we derive from nuclear reaction network calculations the conditions required to give a sufficient neutron-to-seed ratio for production of the platinum peak.These conditions range from and baryon~1 for reasonable dynamic time-Y e B 0.2 S [ 100 scales of D0.001È0.1 s, to and baryon~1 for a dynamic timescale of D0.1 s.Y e B 0.4È0.495S Z 400 These conditions are also derived analytically to illustrate the physics determining the neutron-to-seed ratio.
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Hoffman et al. (1997) studied this question.
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