We follow the approach of HPB to study the dragging of an external
magnetic field by an MHD turbulent accretion disk. As already noted,
this results in a non-relativistic model but should be able to provide
quantitative insights on the behavior of slowly rotating black holes
(where the radius of marginal stability is in a rather low
gravitational redshift regime). We consider a thin Keplerian
accretion disk with geometric thickness
extending down to the
radius of marginal stability at
. We suppose that the
disk has an effective magnetic diffusivity (due to reconnection in the
MHD turbulence) of
which is comparable to the effective
viscosity
. In other words, the effective magnetic Prandtl
number
is of order unity (see HPB for an
explicit justification of
). Note that we employ the
standard definition of
as the ratio of the viscosity to
the magnetic diffusivity which is the reciprocal of that used in Lubow
et al. (1994) and HPB.
We now suppose that an external uniform magnetic field with strength
is present in the vertical direction (i.e., aligned with the
normal to the accretion disk). We are interested in the dragging of
this field by the accretion flow. Assuming the system remains
axisymmetric at all times, and employing cylindrical polar coordinates
, the poloidal magnetic field structure is completely
described by the flux function
via
. With such a definition, the magnetic flux
threading a ring of radius
at height
from the disk plane is
and the magnetic field components are given by
![]() |
(2) | ||
![]() |
(3) |
HPB showed that the time evolution of the flux function in the
diffusive part of the disk plane,
(
), is
given by
| (7) |
At this point, a brief discussion of our
assumption
(which leads to the potential field condition) is in order. In the
non-relativistic treatment here, we can always assume that the Alfvén
speed in the disk magnetosphere is large enough such that any twist in
the magnetic field is removed via a torsional Alfvén wave. However, our
intent is to produce a toy-model for accretion onto a black hole so we
should be wary of an assumption that so explicitly relies on
non-relativistic physics. In a fully relativistic treatment, the
force-free magnetosphere around a black hole accretion disk would be
described by the Grad-Shafranov equation (BZ; MacDonald & Thorne
1982; Uzdensky 2004, 2005). It is found that the poloidal field
structure depends on both the poloidal current distribution (which
gives rise to toroidal fields) and the field line rotation (due to the
fact that the field lines are frozen into an orbiting accretion disk,
for example). In particular, the field structure is affected by the
presence of an inner and outer light cylinder. Ultimately, a
relativistic version of our model should study the flux dragging and
the magnetization of the black hole including these physical effects.
Here, we simply note that detailed studies of non-rotating (or
slowly-rotating) black hole magnetospheres have shown that the field
line rotation associated with a Keplerian accretion disk has only a
small effect on the poloidal field as compared with the equivalent
non-rotating configuration (MacDonald 1984; Uzdensky 2004). In this
sense, Keplerian accretion disks are ``slow rotators'' (Uzdensky
2004).
For the rest of this paper, we explicitly consider the behavior of the
magnetic field in the upper half of the
-plane,
-- we
suppose the system to be symmetric in the
plane such that
and
. The tension term in
eqn. 6 can be decomposed into
![]() |
(10) |
![]() |
(11) |
As part of our model, we must specify
,
and
.
For definiteness, we define
by taking the ratio
as a
fixed parameter of our model (in principle, one could substitute a
particular form for
resulting from a detailed disk model). To
specify the radial velocity field, we follow Lubow et al. (1994) and
split our disk into two zones which we dub an ``active'' and a
``dead'' zone. In the active zone (
), we
set
where
(HRB), and
. The
magnetic Prandtl number
is a fixed and constant
parameter of the active disk. Note that we have introduced the usual
of accretion disk theory (in contrast with HPB who implicitly
employ
). In the dead zone (
), the diffusivity is still given by
, but the velocity is set to zero. For
computational necessities, we impose an outer cutoff on the system at
. We assume that the disk beyond
is a
perfect and static conductor. Hence the total magnetic flux threading
a loop (
) is constant and has the value
. The inclusion of the dead-zone makes the evolution of the
inner part of the system essentially independent of the position or
exact nature of the
boundary. In particular, the dead
zone acts as a reservoir of magnetic flux that can feed the actively
accreting part of the disk -- only in the outermost parts of the
active disk does the conservation of magnetic flux lead to a
non-negligible magnetic pressure trying to ``suck'' magnetic flux out
of the active disk. The physical nature of the dead zone will be
discussed in Section 4.
Finally, we must specify boundary conditions on
. The
implementation of the inner boundary condition must capture the fact
that the plunge region is extremely effective at sweeping in poloidal
magnetic field that crosses within
. Consider a
poloidal magnetic field line which is dragged towards the plunge
region on the viscous timescale
. Once in the
plunge region, the radial velocity of the disk material rapidly
increases with no associated increase in the effective magnetic
diffusivity (indeed, to the extent that the plunge region becomes a
laminar rather than a turbulent flow, the effective magnetic
diffusivity may well plummet to very small values). For the field
strengths under consideration here (i.e., with an energy density much
less that the kinetic energy density of the accretion flow) inward
advection of the field line on a dynamical timescale
will dominate all other
processes. Since the characteristic evolution timescale of the system
is
, flux conservation gives that the
vertical magnetic field in the
plane in the plunge region
compared with that in the disk just outside is
![]() |
(13) |
For the outer boundary condition, we set
for some
. This
amounts to bounding the entire system by a perfect and static
conductor in the disk plane (
) for all
, as
discussed above.
With these assumptions, eqns. 12 and 15
completely describe the evolution of
and
from
some initial state once we fix the magnetic Prandtl number
, the disk thickness
, the characteristic radii of the
problem (
,
,
), the external
field strength
, and the viscosity parameter
. In fact
and
are trivial parameters of the model, affecting only
the scaling of the time coordinate and the absolute normalization of
, respectively. Furthermore, the inclusion of the dead-zone makes
the evolution of the inner disk/field essentially independent of the
location of the outer boundary
. Hence, the non-trivial
parameters describing this system are
,
, and
. For our initial condition, we take
![]() |
(16) |