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Astron. Astrophys. 330, 1070-1076 (1998) 2. The role of tearing instabilitiesThe accretion disk of a YSO is somehow connected with the the dipole magnetic field of the central object (see Fig. 1). The interaction of the dipole field with the disk can be quite complicated (e.g. Shu et al. 1994; Lovelace et al. 1995) but the rotation of the disk should result in a significant twist of closed magnetic flux tubes anchored at the surface of the YSO thereby injecting continuously magnetic helicity into the flux tubes (cf. Hayashi et al. 1996; Li 1996). Consequently, a sheared magnetic field configuration with electric currents flowing develops.
This situation is favorable for magnetic reconnection and is very similar to the physics of rapid bursters (Aly and Kuijpers 1990; Kuijpers and Kuperus 1995), where neutron stars are interlinked magnetically with accretion disks, as well as to particle acceleration phenomena in the magnetospheres of active galactic nuclei (Lesch & Birk 1997). Moreover, it is well documented that solar flares are usually associated with sheared magnetic fields and thus, with current sheets (e.g. Sturrock 1972; Priest 1983, 1985; van Hoven 1979; Sturrock et al. 1984). A generic spontaneous type of magnetic reconnection processes in current sheets is the resistive tearing instability which is caused by the Lorentz force between parallel electric currents. It has long been recognized as a potential candidate for initiating the release and conversion of magnetic energy stored in sheared astrophysical magnetic fields. This instability process can operate at locations where a magnetic field component reverses direction. It results in a reconnection of magnetic field lines across the
plane of field reversal with a subsequent conversion of free magnetic
energy to plasma heating and particle acceleration. The acceleration
of charged particles in magnetic field-aligned electric fields is a
generic feature of reconnection processes (Schindler et al. 1991). The
formation of tearing unstable current sheets in magnetospheres of YSO
is illustrated in Fig. 2. The main idea is that a differentially
rotating disk/magnetosphere in dynamical equilibrium (cf. Li 1996)
gives rise to a toroidal magnetic field component (cf. Fig. 2a).
Since the star-disk magnetosphere is not self-similar (cf. Paatz and
Camenzind 1996) one particular flux tube among others is shown in
Fig. 2a. Different flux tubes are characterized by different
strengths of the toroidal components. The associated current sheets
form along the twisted magnetic flux tubes. Since the rotation
continuously injects magnetic helicity into the closed magnetic fields
magnetic non-equilibrium has to be expected. The unstable dynamics are
characterized by reconnection processes. As illustrated in
Fig. 2b the resulting configuration that should be examined with
respect to tearing instabilities can be approximated nicely by a
one-dimensional electric current sheet. The main component of the
magnetic field is directed along the current sheet (i.e. in the
z -direction), the shear component changes the sign at the
![]() ![]() ![]() ![]() © European Southern Observatory (ESO) 1998 Online publication: January 27, 1998 ![]() |