Torque Reversals in Disc Accreting Pulsars

Jianke Li \& Dayal T. Wickramasinghe, PASA, 15 (2), 250
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Idea of disc-induced magnetospheric instability

The proposition of our semi-quantitative model is based on the recent result that the funnel does not spin up the star (Li, Wickramasinghe & Rüdiger 1996). The implication of this result is that the accreting matter will not directly exert a torque tex2html_wrap_inline149, as assumed in the standard model, though the magnetospheric spin-up torque may yield such an effective term (Li & Wickramasinghe 1997). However, the later cannot be easily justified.

To explain the torque reversal with similar magnitude of spin-up and spin-down torques, we assumed that the magnetosphere can abruptly change its extent which determines the total magnetic torque. In general, we expect two state of magnetosphere as it yields two distinct torques. One corresponds to a smallest outer magnetosphere so roughly only the inner magnetosphere is significant, and the other corresponds to a largest outer magnetosphere which extends far beyond the corotation radius as normally envisioned in a standard star-disc interaction so the outer magnetosphere is the largest (Fig. 1). The ad hoc assumptions are that these two magnetosphere states are linearly stable since otherwise we could not be able to observe the stable torques, and it is non-linearly unstable because otherwise no torque reversal would occur. We attempted to explain why the system can alternate from one state to another. The basic question is the stability of the magnetosphere in a disc-star interacting system.

However, an insufficient knowledge of the stability of a magnetosphere and lack of a model addressing the disc-star interaction are combined to impede a complete analysis of the problem. At the present time, one thus could only expect a semi-quantitative description for the specific observation for a given system. Though torque variation is certainly affected by an accretion rate change, it is clear that modelling this aspect is not our objective. In fact, the observations suggest a different mechanism which might be in operation. We do not know whether the accretion rate variation must be intimately involved when other mechanisms play important roles, the simplest approach so far is nevertheless to assume a constant tex2html_wrap_inline145. It is our intention to see whether other causes other than the accretion rate will lead to dramatical torque reversal.

It has been discussed that assuming a constant mass accretion rate inevitably leads to the conclusion that the disc viscosity and resistivity are not constants, as the the disc-star interaction affects them. This is probably a more physical picture, as star and disc belong to a whole. This concept is not totally new. Popham & Narayan (1991) argued that the stellar inner boundary condition may drastically affect the angular momentum flux, and thus given a accretion rate one is forced to expect change in viscosity.

The stability of a magnetosphere (force-free) is an unresolved problem (e.g. Aly 1985; Low 1987). However, the currently accepted criterion for stability is that the toroidal magnetic field cannot be significantly larger than the poloidal field. In our context, the toroidal fields are generated by the winding between the star and the disc, and one may thus argue that the outer magnetosphere cannot be extended to infinity, where the poloidal field is the weakest (so the magnetosphere is not stable). The extent of the magnetosphere is determined by the condition at its edge and therefore must depend on the resistivity of the disc, given the assumption of quasi-steady state. If the resistivity has two values, the stable outer magnetosphere must have two states. As the outer magnetosphere is bounded at the corotation radius, where the toroidal field is zero, one would expect that any variation in the outer magnetosphere will stop at the corotation radius.

Problems exist for the nature of the viscosity in the presence of strong magnetic field. Assuming a normal disc when no stellar magnetic connection is present, the presence of star-disc magnetic interaction must alter the nature of the viscosity. As we know, the magnetospheric interaction in the inner accretion disc (inside of the corotation radius) tends to spin up the star so the viscosity is not important (accretion may proceed even without viscous stress). The situation is just opposite outside the corotation radius, as the magnetospheric interaction tends to spin up the disc and so the viscosity must be larger enough to carry away more angular momentum. In this sense, the stellar magnetic connection adds a component to the normal viscosity in a normal disc. By the argument above for the outer magnetosphere, we have to conclude that the part associated with magnetospheric interaction opposes the normal part. The conductivity relates to the normal viscosity part , which depends on the strength of the turbulence. The turbulence of the disc matter determines the dissipation of the mean magnetic flux or resistivity, and the overall star-disc interaction affects the strength of turbulence. In this picture, a reduction of the outer magnetosphere would result in an increase of the conductivity, making the magnetosphere less stable.

It is thus argued that a large amplitude perturbation, either a reconnection for the smaller magnetosphere or a blow-up in the larger magnetosphere, will lead to a turn-over from one state to another. Once the outer magnetosphere increases, the spin-down torque increases, and as a result, more angular momentum must be carried outwards. This can be archived simply by increasing the normal viscosity. As the resistivity is proportional to the normal part of the viscosity, the resistivity becomes larger and the magnetosphere becomes more stable. Thus more reconnection will occur and eventually the magnetosphere reaches the second state and the star spins down. The reverse process is that an opening-up a certain flux tube in the larger magnetosphere leads to a smaller spin-down torque and therefore smaller resistivity. Thus the magnetosphere becomes less stable and this leads to an opposite chain effect until the magnetosphere reduces to near the corotation radius where the magnetosphere is supposed to be stable again because of smaller toroidal magnetic fields.

The observed changes of the sign of the torque in Cen X-3 indicates that instantaneous rotational equilibrium is not achieved. Since the instantaneous torques are large, the system is expected to evolve to the mean rotational equilibrium rather quickly. The much smaller mean torque in Cen X-3 may indeed be a signature of closer to the mean rotational equilibrium.

The observed quick transition between two torque states implies that the transit time scale must be significantly smaller than 1 days, which is comparable to the viscous time scale. In contrast, the time scale of Alfvén waves in the magnetosphere is much shorter. Thus in a viscous time scale, the magnetic processes can be regarded to be steady state. Since the observed one-torque state can last up to tex2html_wrap_inline155 10 days, the disc accretion can be regarded to be in steady states. We have adopted a quasi-steady approach regardless the details of the transition, and this means that the system manages to adjust to a steady angular momentum flux in a time scale comparable to the viscous time scale.

The previous discussion relates to the nonlinear process and the mechanism might work only when perturbations are large enough to change the star-disc interaction. This is consistent with the observations. The disc sets the boundary condition for the magnetosphere and the magnetospheric interaction reacts back on the disc. This basic disc-star interaction argues for the existence of the so-called Disc-induced Magnetospheric instability which leads to alteration between two magnetospheric states. Since the stability of magnetosphere is still not fully resolved, so our current investigation is limited only in a semi-quantitative level. It has been estimated that a 10% of flux reconfiguration might be sufficient in leading to a transition between two magnetospheric states. This suggests that intermediate magnetospheric states are inadmissible, therefore explains why torque reversal is similar in amplitude.


Next Section: Summary and problems ahead
Title/Abstract Page: Torque Reversals in Disc
Previous Section: Introduction
Contents Page: Volume 15, Number 2

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