The first Keplerian disk simulation, CK5, considers a disk with an inner edge at R=10, set back from rms. This will investigate disk accretion removed from the dynamical forces associated with the pseudo-Newtonian potential's innermost circular orbit. The simulation follows the global development of the MRI, turbulent angular momentum transport, and the resulting gradual accretion of matter and inward drift of the disk edge.
The initial conditions consist of an isothermal gas at constant
density,
,
and a sound speed
cs = 0.03054 which gives a Mach number
at R=10. With the decrease in velocity
the Mach number declines to 4.3 by the
outer radial boundary. The azimuthal angle
runs from 0 to
in 58 grid zones, and in the vertical direction z runs from 0
to 2 in 24 grid zones. The vertical scale height at R=10 corresponds
to 0.87. Of course in the cylindrical disk approximation the absence
of a vertical gravitational force means that the scale height has no
hydrodynamical significance in z; it is merely a convenient
expression of the temperature of the disk in terms of the ratio of the
sound speed to orbital frequency.
With a magnetic field, the vertical domain size retains significance
even in the cylindrical disk limit in relation to the most unstable
wavelength of the MRI. The magnetic field strength determines this
wavelength, and the initial pressure determines the value of
to which this field strength corresponds. For CK5 the
initial magnetic field is purely toroidal with
.
For this
strength of field the ratio of the Alfvén speed to the orbital
frequency,
,
ranges from 0.6 at the inner disk boundary to
10.2 at R=60. The critical azimuthal wavenumber for the MRI,
,
ranges from 16 at the inner disk to 6 at the outer
boundary. Since the azimuthal direction spans
with 58 grid
zones, only wavenumbers
will be realizable. With the
chosen magnetic field strength, however, the unstable azimuthal
wavenumbers of the MRI should be well resolved throughout the disk.
The simulation is run out to time t=3972 which is 22 orbits
at the disk's initial inner boundary, and 180 orbits at
rms. As the simulation proceeds the MRI
develops, first at the inner disk edge and spreading outward through
the disk as time advances. Small wavelength perturbations (large
m) grow most rapidly, but the largest azimuthal scales dominate
in the end. The exponential growth of the poloidal field at a given
radius ends after approximately five orbits, as measured locally. The
Maxwell stress in the resulting MHD turbulence transports angular
momentum and the disk evolves. Figure 1 shows a spacetime
(R,t) plot of the Maxwell stress,
, in terms of a Shakura & Sunyaev (1973)
using the initial pressure as a normalization,
. This plot illustrates the
rapid local buildup of magnetic stress to significant levels, as well
as the large fluctuations in time and space.
Figure 1: Spacetime diagram of the Maxwell stress in run CK5 normalized by the initial pressure
. The stress develops first at R=10 and then spreads out through the disk as the MRI grows at a rate proportional to the local orbital frequency. At the end of the simulation the stress rises rapidly from near zero at R=5, reaches the highest levels between R=15 and 30, then declines rapidly with radius. Within the disk the stress varies strongly in both time and space.
Overall, the disk never attains a steady state; its inner edge
slowly moves inward and fluid in the outer disk moves outward. Through
the course of the simulation the disk inner edge moves from R=10
down to R=5. This is illustrated in Figure 2 which shows
at several times during the run. At
the end time, the disk has not quite reached
rms and there is no significant mass flux
through the marginally stable orbit and into the central hole.
Magnetic field has been carried inward along with the mass. The
regions with the strongest fields lie between the peaks in the density
distribution. The average
value varies between 8 at the density peaks and 2 in
between.
Figure 2: Radial profile of density
at times t=0 (solid bold line), 890 (short dashed line), 1835 (dash-dotted line), 2734 (thick dashed line), 3848 (solid thin line) in simulation CK5. These times correspond to 0, 4.9, 10.2, 15.2, and 21.5 orbits at R=10. Angular momentum transport produced by MHD turbulence causes the inner edge of the disk to drift gradually inward.
Averaged properties of the accretion flow within the disk can be
derived from a region between R=13 and 22 which comes into an
approximate time-averaged steady state after t=2800. The
time-averaged accretion rate within this region is roughly constant
with radius, with
,
and
.
The
instantaneous fluctuations in radial velocity,
typically range between 0.01 and -0.02. Within
the turbulent disk the toroidal field energy dominates over that of the
poloidal field, with the ratio
.
The radial field
energy is, in turn, a factor of 6 greater than the that of the vertical
field. The toroidal field energy is essentially unchanged in the mean
from its initial value, although there are spatial variations in
strength by a factor of two within the disk. At the end of the run the
region of significant Maxwell stress has moved out to around R=40
with the largest values lying between R=7 and 30 (Fig. 1). The
time-averaged Maxwell stress over this range is about
5.5 x
10-5, corresponding to an average value of
.
The
relatively low level of the radial field compared to the toroidal is
reflected in the value of
,
the ratio of the Maxwell
stress to the total magnetic pressure (
).
In the inner disk this value ranges between 0.2 and 0.3. The toroidal
field simulation of ARC obtained an
slightly below 0.01, and
an
.
(Note that there are differences in
terminology between this paper and ARC.)
The averaged magnetic properties of the turbulence are consistent with
the results of toroidal field local shearing box simulations (cf. Table
3 of HGB95). For those simulations
was typically
a few times 0.01, and
for simulations that
began with weak toroidal fields and
for those that
began, like this simulation, with stronger toroidal fields.
Title Page
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2. Problem
Setup
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3.2 Disk with initial vertical field