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Astron. Astrophys. 319, 515-524 (1997) 6. ConclusionIn this work, we model the angular velocity time series of OAO
1657-415 and characterize the type of accretion (wind or disk). The
noise power spectrum and the structure function analysis showed that
the angular velocity time series history of OAO 1657-415 is consistent
with a random walk model,(with steps at order of several days:
This is close to our random walk noise strength value, indicating the possible formation of episodic Keplerian disks. Note however that the mass accretion rate used here is rather uncertain, since it is based on a luminosity which is calculated indirectly using a value for the pulsed fraction from earlier observations, and a very uncertain distance of 10 kpc based mainly on a high interstellar absorption and a low galactic latitude (Kamata et al. 1990). Eq. 15 also shows that the level of noise strength increases with mass accretion rate. Our findings are strongly sugesting that OAO 1657-415 has an OB type companion. In the case of a Be type of companion, the accretion disk forms from the low velocity equatorial stellar wind. In this case the orbital velocity of the system is higher than the wind velocity. Therefore the flow has enough initial specific angular momentum, and hence the formed disk should be in the same sign with orbital motion. In this case, it is unlikely to expect disk reversals (or flip flop instabilities) and one should see positive correlations between angular accelerations and mass accretion rates (Ghosh & Lamb 1979a, b). One of the important observations to test the idea of formation of disk from the stellar wind is to obtain spectral information and examine the column density (or filaments) during the orbital phases. The distribution of ionization lines and column density during the orbital phases will give additional information about accretion process (Blondin et al., 1990).
© European Southern Observatory (ESO) 1997 Online publication: July 3, 1998 ![]() |