A&A 483, 815-830 (2008)
DOI: 10.1051/0004-6361:20079307
M. Ilgner - R. P. Nelson
Astronomy Unit, Queen Mary, University of London, Mile End Road, London E1 4NS, UK
Received 21 December 2007 / Accepted 13 February 2008
Abstract
Context. Protostellar accretion discs have cool, dense midplanes where externally originating ionisation sources such as X-rays or cosmic rays are unable to penetrate. This suggests that for a wide range of radii, MHD turbulence can only be sustained in the surface layers where the ionisation fraction is sufficiently high. A dead zone is expected to exist near the midplane, such that active accretion only occurs near the upper and lower disc surfaces. Recent work, however, suggests that under suitable conditions the dead zone may be enlivened by turbulent transport of ions from the surface layers into the dense interior.
Aims. In this paper we present a suite of simulations that examine where, and under which conditions, a dead zone can be enlivened by turbulent mixing.
Methods. We use three-dimensional, multifluid shearing box MHD simulations, which include vertical stratification, ionisation chemistry, ohmic resistivity, and ionisation due to X-rays from the central protostar. We compare the results of the MHD simulations with a simple reaction-diffusion model.
Results. The simulations show that in the absence of gas-phase heavy metals, such as magnesium, turbulent mixing has essentially no effect on the dead zone. The addition of a relatively low abundance of magnesium, however, increases the recombination time and allows turbulent mixing of ions to enliven the dead zone completely beyond a distance of 5 AU from the central star, for our particular disc model.
Conclusions. During the late stages of protoplanetary disc evolution, when small grains have been depleted and the disc surface density has decreased below its high initial value, the structure of the dead zone may be significantly altered by the action of turbulent transport. This may have important consequences for ongoing planet formation in these discs.
Key words: accretion, accretion disks - magnetohydornamics (MHD) - stars: planetary systems: protoplanetary disks - stars: planetary systems: formation
There are continuing questions, however, about the applicability of the MRI to cool, dense protostellar discs, as the ionisation fraction is expected to be low (Blaes & Balbus 1994). A protostellar disc model has been presented by Gammie (1996) in which the main source of ionisation is Galactic cosmic rays. Such a disc is predicted to have magnetically ``active zones'' near the disc surface in which turbulence is sustained by the MRI due to cosmic ray ionisation, but with a ``dead zone'' near the disc midplane where cosmic rays are unable to penetrate. Sano et al. (2000) have examined the effects of a more complex chemical reaction network and the influence of small dust grains. Glassgold et al. (1997) and Igea & Glassgold (1999) examined X-rays emitted by the protostellar corona as a possible source of disc ionisation, since it is doubtful that cosmic rays can penetrate the inner disc regions because of the attenuating effect of the T Tauri wind. Fromang et al. (2002) demonstrated the potential importance of gas phase heavy metals such as magnesium, whose presence in trace quantities can significantly increase the recombination time and decrease the size of the dead zone (at least in a dust free disc). Semenov et al. (2004) examined the disc chemistry and ionisation fraction using a reaction network drawn from the UMIST database, and analysed results using a reduced reaction network.
Nonlinear numerical studies of the effects of ohmic resistivity on
MRI-driven MHD turbulence have also been presented. Fleming et al. (2000)
performed MHD simulations of resistive discs, and showed that
turbulence is not sustained in discs with a magnetic Reynolds number
which is below a critical value
.
Fleming & Stone (2003) performed simulations where resistivity decreased
as a function of height in the disc, as predicted by the Gammie (1996) model,
and showed that active zones could indeed coexist with dead zones in the disc.
They also showed that a low Reynolds stress can be maintained in the dead zone,
such that low levels of accretion are sustained there. A recent study of
resistive discs has also been presented by Turner et al. (2007), who presented
stratified shearing box simulations of discs in which resistivity varied with height,
and a multifluid simulation in which disc chemistry was evolved along with the
dynamics. This latter run showed that turbulent mixing can potentially have
an important effect in generating stresses in the dead zone.
Fromang & Papaloizou (2007) have recently performed a resolution study
of shearing box simulations, and showed that the level of turbulent
activity reduces as the resolution increases. An analysis of
existing shearing box simulations in the literature by Pessah et al. (2007)
led to a similar conclusion. In a companion paper to
Fromang & Papaloizou (2007),
Fromang et al. (2007) also examined how turbulent activity scales with
magnetic Prandtl number (defined by
where Re is the Reynolds
number and
is the magnetic Reynolds number). They showed that
both the Reynolds number and magnetic Prandtl number are the parameters that
control the level of turbulent activity in a disc, with
flows
showing no sustained turbulent activity for zero net flux magnetic fields.
Clearly there is much work to be done in understanding the nature of MHD turbulence
in discs.
In a recent set of publications, we have undertaken an extensive study of
the chemistry and ionisation
fraction in protoplanetary discs. In Ilgner & Nelson (2006a, hereafter Paper I) we examined the
dead zone structure in standard
-disc models as predicted by a
number of different chemical reaction networks, and showed that the
simple model of Oppenheimer & Dalgarno (1974) gives good agreement with
more complex models based on the UMIST database (Le Teuff et al. 2000).
We also demonstrated that grain depletion by factors even lower than
10-6 are required to reduce significantly the sizes of dead zones.
In Ilgner & Nelson (2006b, hereafter Paper II) we constructed
a reaction-diffusion model to examine the role of turbulent mixing on
dead zone structure. The results showed that turbulent mixing has
essentially no effect throughout the disc in the absence of gas phase
heavy metals such as magnesium. In the presence of trace quantities
of magnesium, however, turbulent mixing was able to enliven the
dead zone out beyond a few AU, where the mixing time becomes shorter
than the recombination time (see also Inutsuka & Sano 2005). In a third paper of the series (Ilgner & Nelson 2006c),
we examined the effect of X-ray flares on dead zone structure.
In this paper we present a suite of shearing box simulations of stratified local disc models in which we evolve the disc chemistry along with the magnetohydrodynamic equations. The primary aim is to re-examine the results of Paper II using multifluid MHD simulations, and determine whether, and under what conditions, turbulent mixing can enliven a dead zone by mixing ions from the surface layers down toward the midplane. We use the simple reaction scheme of Oppenheimer & Dalgarno (1974), which we incorporate into a multifluid MHD code, and assume that dust grains are absent and ionisation is caused primarily by X-rays from the central star. We examine the effects of mixing as a function of gas phase magnesium abundance and distance from the central star. Our results are in very good agreement with the predictions of Paper II. Disc models which contain no gas phase magnesium show that the dead zone structure is essentially unmodified by turbulent mixing. In the presence of magnesium, however, our simulations show that the dead zone can be enlivened completely beyond a distance of 5 AU from the central star.
The paper is organised as follows. In Sect. 2 we present the basic equations and the chemical reaction network that we solve. In Sect. 3 we discuss the reaction-diffusion model, which we use to compare with the MHD simulations. In Sect. 4 we discuss the method used for calculating the X-ray ionisation rate, and in Sect. 5 we discuss previous simulations that have examined dead zone structure. In Sect. 6 we present our simulation results, and finally in Sect. 7 we draw our conclusions.
In this section we give a detailed description of the chemical model used in our simulations, and present the multifluid MHD equations that we solve.
For the purposes of simplicity and computational tractability,
we have applied the simple kinetic model of Oppenheimer & Dalgarno
(1974) to evolve the gas-phase chemistry within the simulations.
This reaction network has been described
in Ilgner & Nelson (2006a), where it was compared with more complex reaction
networks and found to predict electron fractions that were slightly higher
on average, due to the lower number of molecular ion species present in
the simpler model. The Oppenheimer & Dalgarno reaction network may be written:
Equations (1)-(4) form a set of stiff coupled ordinary differential equations, and we use the Gear method for their solution at each point in the simulation domain and for each simulation time step. The major source of ionisation that we consider is X-rays from the central protostar, and our approach to calculating the ionisation rate is described below in Sect. 4.
Table 1: Rate coefficients for the Oppenheimer & Dalgarno model.
As the mean-free path for collisions, and the ion gyro-radii, are very much
smaller than the length scales we consider in our calculations, we adopt
a multifluid MHD approach to incorporating chemical evolution of the gas
during the dynamical evolution of our disc models. We use the shearing
box representation of a local patch of the protostellar disc
(Goldreich & Lynden-Bell 1965),
in which the fluid is described using Cartesian coordinates (x, y, z).
The origin of this coordinate system rotates with the local Keplerian
angular velocity,
,
and the x coordinate represents the radial
direction, the y coordinate the azimuthal direction, and z the vertical
direction.
The standard shearing box equations for MHD, including ohmic
resistivity, are:
In our scheme the five species are treated
as indivdual but tightly coupled fluids which move with the bulk velocity
,
and so we must solve
a continuity equation for each of them. When combined with
the possibility that the local abundance of species may change because
of chemical evolution as well as advection, then the continuity
equation for each species i may be written:
The MHD simulations that we performed
were calculated using a system of dimensionless variables, as is
convenient when performing shearing box simulations.
In order to evolve the chemistry, however, whose reaction rates depend on
local temperature and density, we need to ascribe physical units
to these simulated quantities. We assume that the central star is
of solar mass, and we adopt a disc model for which
the surface density varies according to
,
and where the volume density varies with disc height
as a Gaussian:
The basic disc model used is described in Sect. 2.3.
The initial velocities of the gas in the simulations were taken
to be the shearing box equilibrium values
,
but with random fluctuations imposed
with maximum amplitude equal to 10-3 of the sound speed.
The initial magnetic field is a zero net flux vertical field given by
,
where B0 is
defined by the requirement for the volume averaged plasma parameter
.
At the beginning of each shearing box simulation,
the equilibrium particle concentrations
of species
are
taken as initial abundances. Note that we use different concentrations
of magnesium for our models, and we simulate local patches
of the disc at different radii from the central star. In each case
we calculate the local equilibrium chemistry prior to initiating
the MHD simulations.
We use the same computational set-up as
Fromang & Papaloizou (2006). The computational
domain is given by
[-H/2, H/2],
,
and
[-3H, 3H] in x, y, and z. We use a grid resolution of
.
Standard periodic boundary
conditions apply in y and z,
while periodic boundary conditions in shearing coordinates are used
for x. For a detailed description of the shearing box set up and
boundary conditions see Hawley et al. (1995).
Following Fromang & Papaloizou (2006)
we introduced a vertical length scale
which is used to prevent unphysical fluctuations due to the
non vanishing vertical component
of the gravitational force at the z boundary. By applying
Eq. (30) of Fromang &
Papaloizou (2006) we ensure that the vertical gravity acts on
vertical length scales
L < H0 only.
In Paper II we calculated the ionisation fraction for
conventional
-disc models and examined the
effect of turbulent mixing by
modelling the diffusion of chemical species vertically
through the disc. To recap: applying
a one dimensional reaction-diffusion model, we assumed
that vertical mixing arises
because of turbulent diffusion, and adopted the approximation
using the
prescription to calculate
.
Here
is the (turbulent) kinematic
viscosity that drives the radial diffusion of mass through the
protostellar disc, and
denotes the vertical diffusion coefficient.
Instead of just mimicking the effects of turbulent mixing in this way, we now model the turbulent transport of chemical species by solving the corresponding non-ideal MHD equations in a three dimensional shearing box as discussed above. The mixing now is a direct outcome of the MHD turbulence.
One purpose of this paper, however, is to examine
whether or not the effects of turbulent
mixing on the ionisation fraction described
in Paper II,
can also be observed in shearing box simulations when MHD turbulence
operates. Hence, we calculated the ionistion fraction
obtained for the kinetic model
of Oppenheimer & Dalgarno by applying the reaction-diffusion
model at the corresponding cylindrical
radius R, in order to aid a direct comparison between
the results obtained for the
reaction-diffusion and the shearing box model.
We have
good reason to make this comparison because
Balbus & Papaloizou (1999) have shown
that the mean flow dynamics of the MHD turbulence follows
the
prescription.
For the reaction-diffusion model we assume the same vertical density profile
we use for the shearing box simulation at
t = 0. The same applies for
the gas temperature. We further adopt the approximation
with
Since we expect the largest gradients in the electron fraction to be in
vertical (z) direction, we consider only vertical diffusion in the
reaction-diffusion model. The rate of change of the molar density of the ith
component of the fluid within a given volume due to chemical reactions and diffusion
caused by concentration gradients is
The numerical method applied to solve the reaction-diffusion
model is described in
Paper II, and the same boundary conditions apply.
The boundaries are
at [0,+3H] such that the computational domain has size
Lz = 3 H;
the number of grid cells is
,
ensuring that the elements and
charge are conserved to high accuracy.
For a given metal elemental abundance,
the reaction-diffusion models are initiated with
the equilibrium composition obtained for
,
exactly as they are for the
shearing box simulations.
As in Paper I, we assumed that the ionisation of the disc
material arises because of incident X-rays that originate in the corona of the
central T Tauri star. We neglect contributions from Galactic cosmic rays as it
remains uncertain whether they can penetrate into the inner disc regions we
consider due to the stellar wind. The details for determining the
effective ionisation
rate
have been described in Paper I.
However, here we do not consider standard
-disc models as we did
in that paper. Instead, we adopted a locally
isothermal disc with the
same Gaussian vertical profile for the mass density used for the local shearing
box model at t = 0. When calculating the X-ray ionisation rate we assumed
that this density profile did not vary with time, an assumption that
is confirmed by the shearing box
simulations which show that the density profile closely follows its initial
Gaussian profile throughout the nonlinear evolution of the MRI,
(see top right panel of Fig. 3).
We adopted values
and
for the total
X-ray luminosity
and the plasma temperature
,
respectively. Compared with the values
applied in Ilgner & Nelson (2006a,b),
(i.e.
and
), the X-ray source considered here is
more both harder and more luminous in order to increase the ionisation
fraction above a theshold which makes the shearing box simulations feasible
(a low ionisation fraction leads to a small time step size).
However,
the new values are still consistent with the observational constraints
(e.g. Favata et al. 2005; Wolk et al. 2005).
The effective ionisation rate (per hydrogen nucleus)
is approximated
by Eq. (3) in Paper I.
Calculating the X-ray optical depth
along
the line of sight between the X-ray source and the point in
question, we derived the
effective ionisation rate shown in Fig. 1.
In particular, we applied the same
data range in order to aid direct comparison with the ionisation rates
of our previous
-disc models (e.g. compare with Fig. 6 of Paper I).
The effective
ionisation rate shown in Fig. 1 is higher because of the
brighter (by one order of magnitude) and harder (more penetrating) X-ray source applied.
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Figure 1:
The effective X-ray ionisation rate
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Figure 2:
Vertical profiles of the magnetic Reynolds numbers
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As has been well documented in the literature, there remain questions about the
applicability of the MRI to protostellar discs because of their high densities and low
temperatures, which lead to low levels of ionisation (e.g. Blaes & Balbus 1994;
Gammie 1996). The first fully non linear study of the MRI including the effects
of resistivity were performed by Fleming et al. (2000), who employed shearing
box simulations to examine the conditions under which fully developed turbulence could be
sustained. They showed that the important quantity that determines the outcome is the
magnetic Reynolds number,
,
defined by:
Shearing box simulations of stratified protostellar discs, with resistivity
varying with height, were presented by Fleming & Stone (2003). Calculations
were presented with different vertical resistivity and magnetic Reynolds number profiles,
and it was shown that layered accretion resulted when the magnetic Reynolds number
satisfied
in the surface layers, with
in the midplane regions. Their results also showed that a low Reynolds stress could be sustained
in the dead zones due to the penetration of sound waves excited in the overlying active regions.
The magnetic Reynolds number profile assumed in the simulation for a ``small dead zone'' from
Fleming & Stone (2003) is shown by the solid line in Fig. 2.
The magnetic Reynolds number varies from 1000 at the midplane, to
,
,
and
at z/H = 1,
z/H = 2, and z/H = 3, respectively, resulting in a simulated disc with a dead zone
whose vertical height is
H.
In a recent paper, Turner et al. (2007) have presented a study of dead zones which
included shearing box simulations of vertically stratified discs with
resistivity varying as a function of height, and also a multifluid
simulation in which the resistivity was able to change locally because
of chemical evolution of the gas. In this study, Turner et al. (2007)
employed the reactionnetwork given by Eqs. (1)-(4)
in order to calculate the ionisation fraction and resistivity. For those
runs in which the resistivity was kept constant in time, the initial
resistivity profile was obtained from the equilibrium solutions
to Eqs. (1)-(4). The run in which
resistivity varied in time and space employed a multifluid approach,
similar to that described in Sect. 2.
Ionisation was assumed to be due to cosmic rays, and the underlying
disc model was the minimum mass solar nebula model of Hayashi (1981).
In Fig. 2 we present two of the resistivity profiles
employed by Turner et al. (2007) corresponding to their runs F1 and F56.
In run F1 the resistivity was a fixed function of height and
corresponded to a radial location R=1 AU with the gas-phase abundance of
magnesium equal to the solar abundance (
magnesium atoms
per hydrogen nucleus, corresponding to
in our units). This run led to a layered accretion flow with active surface
layers and midplane dead zone, as expected from the steep resistivity profile.
It was shown that the boundary between dead and active zones is well described
by the criterion that MHD turbulence is sustained by the MRI if the
Lundquist number
,
where
is the
Alfvén speed.
Run F56 had a resistivity profile corresponding to a disc at 5 AU with
gas phase magnesium abundance equal to 10-6 below solar abundance (corresponding
closely to our model with
).
This model led to a fully turbulent disc, as expected from the flat resistivity
profile obtained because the disc provides less shielding of cosmic rays
at 5 AU.
The multifluid model presented by Turner et al. (2007), in which the chemistry was evolved simultaneously with the dynamics, led to an interesting and somewhat unexpected result. This disc model corresponded to the radial position R=1 AU in the disc, and assumed a gas-phase magnesium abundance equal to the solar value. During the early phase of the model, the disc showed the expected layered structure with dead zone near the midplane, and active zone near the disc surface. After about 60 orbits the situation changed after a period of more intense mixing caused by enhanced turbulent activity. The recombination time then exceeded the mixing time, allowing free electrons to mix toward the midplane, where net radial and azimuthal fields had built up due to field of the opposite polarity advecting through the vertical boundaries. The presence of these net magnetic fields leads to an enhance magnetic stress that partially enlivens the dead zone during periods when the ionisation fraction has been increased.
In this paper, we assume that the ionisation of the disc material arises because of X-rays that originate in the corona of the central T Tauri star. We neglect contributions from Galactic cosmic rays, as it remains an open question whether or not they can to penetrate into disc regions we consider. The X-ray ionisation rate decreases with cylindrical radius R, because the X-ray optical depth along the line of sight increases as one moves out into the disc.
Our use of strictly periodic boundary conditions in the vertical direction,
along with an initial magnetic field that has zero net flux,
means that the net flux remains zero throughout the simulations.
The expectation then is that turbulence will be sustained
only in those regions where the magnetic Reynolds number
,
and we do not expect that large scale net-flux magnetic fields will be able to
accumulate in the dead zones of our simulations. As such we do not expect to observe
the behaviour shown by simulation V1 of Turner et al. (2007).
We now present the results from a series of systematic experiments which
examine the effects of chemical evolution and turbulent mixing
on the evolution of the MRI.
In this section we present the results of our multifluid MHD simulations which examine the role of turbulent mixing on the structure of dead zones. The primary aim of these simulations is to demonstrate that there exists a region of parameter space in which turbulent mixing can enliven a dead zone which is otherwise predicted to exist in models that neglect turbulent transport. A further aim is to demonstrate good agreement between MHD simulations and the predictions of a simple reaction-diffusion scheme. This latter issue is addressed in Sect. 6.3.
When discussing the results of our simulations we will often refer to
certain averaged quantities.
We use
the same averaging procedures presented in recent publications studying
vertically stratified disc models (e.g. Stone et al. 1996; Fleming & Stone 2003;
Fromang & Papaloizou 2006). The azimuthal and radial average of quantity
f(r, t) at a given time t is defined by
Table 2: List of models considered. Note that the column ``recombination process included'' specifies whether or not recombination of free electrons occurs along with dynamical evolution.
A measure of the effective shear stress generated by the turbulence is given by the parameter
1) model1: This model assumes a static resistivity profile which
varies with height. The resistivity profile at t = 0 is obtained using
the equilibrium solution of the kinetic model presented in
Eqs. (1)-(4).
During the simulations the local resistivity values are kept fixed.
This model corresponds to the single fluid
models of Fleming & Stone (2003), and the runs F1, F52, F56, F58
of Turner et al. (2007).
2) model2: This is a multifluid model in which the
resistivity varies in both time and space.
The chemical reaction network given by Eqs. (1)-(4) is
solved simultaneously with the dynamical evolution. The resistivity
profile at t = 0 is obtained from the equilibrium solution of the
kinetic model.
3) model3: This is a multifluid model which has
a resistivity profile which varies in time and space.
The resistivity profile at t = 0 is obtained using the
equilibrium solution of the kinetic model presented in
Eqs. (1)-(4).
For t > 0, however, the recombination
of free electrons with ions is switched off, as is further ionisation
of neutral species by X-rays.
Local changes in the resistivity are due only to the turbulent mixing
of ions. This model is equivalent to one in which the initial values
of resistivity are conserved on fluid elements by being advected with the flow.
We now present our simulation results in detail. We begin by highlighting simulations which show that turbulent mixing can remove the dead zone, before examining disc evolution at different radii and with different magnesium abundances.
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Figure 3:
model1/model2: Time averaged vertical profiles of the horizontally
averaged density, normalised Maxwell and Reynolds stresses
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Figure 4:
model1/model2: Time averaged vertical profiles of the horizontally
averaged kinetic energy,
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Figure 5:
model3: Time averaged vertical profiles of the horizontally averaged value of
normalised Maxwell and Reynolds stresses
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In this subsection we present a suite of models which demonstrate that
turbulent mixing and continuing chemical evolution
of the gas are able to enliven a dead zone.
All three models presented in this subsection correspond to a radial
location in the disc R=10 AU, and have a gas-phase magnesium
abundance
.
Because of the identical initial conditions used for these three models,
we can identify the specific effects of the chemistry on the evolution
of the MRI.
model1
The resistivity in this model is calculated from the equilibrium
electron abundance predicted by the chemical model presented
in Sect. 2, and is held constant throughout the simulation.
The variation of magnetic Reynolds number with height is
shown in Fig. 2, which shows that the
resistivity profile is intermediate between that applied
by Fleming & Stone (2003) in their ``small dead zone'' model,
and the model F56 presented by Turner et al. (2007).
Specifically
takes the following
values:
at the disc midplane;
at z/H=1;
at z/H=2;
at z/H=3.
In agreeement with our expectations, this simulation resulted in
a disc with well-defined dead and active zones, with the boundary
between these occuring at
where
and
.
This dead zone is larger than that obtained by Fleming & Stone (2003)
in their model whose resistivity profile is shown in
Fig. 2, for which the dead zone was confined to
.
The time and volume averaged sum of the Maxwell and Reynolds stresses was found to
be
when the time average was taken over the interval [20, 100] orbits.
When taken over an interval [100, 200] orbits, the stresses were
found to decrease to
.
This occurs
because the stresses are higher during the development of the
non linear stage of evolution early on in the simulation.
We note that a fully active disc is expected to have a value
(see later).
The vertical profiles for the horizontally averaged density
,
the
values
associated with the Maxwell and Reynolds stresses,
the plasma parameter
,
the kinetic
and magnetic energy are shown in the left hand panels of
Figs. 3 and 4.
The time averages are taken over 10 orbit intervals,
starting from t =0 (dashed line) towards
[140,150] (solid line). The dotted lines refer to profiles averaged over
.
For each of the profiles,
the same qualitative behaviour reported in Fleming & Stone (2003) is observed:
model2
In this model the initial free electron abundance and resistivity profile
is calculated from the equilibrium solution to Eqs. (1)-(4).
The full set of multifluid equations, and the chemical
network, are evolved together so that the local resistivity can change
through turbulent transport of ions and
and chemical evolution (recombination/ionisation) of the gas.
For this model we estimate that the turbulent mixing time
corresponding to
is shorter than the recombination
time, such that chemical mixing should enliven the dead zone.
This is indeed what we find, as the
simulation results in a turbulent flow which fills the entire volume
of the disc,
with
,
where the time average was performed in the interval [20, 100] orbits.
We plot the vertical profiles of the various physical quantities
that we have already described for model1 in
Figs. 3 and 4. Comparing the figures
for model1 and model2 we can make the
following observations:
model3
At t = 0 the initial resistivity profile is set up in the same way
as described for model1 and model2.
For t > 0, the local resistivity is updated after every MHD time step because
of the transport of free electrons and ions only. Due to the inhibition of recombination and
ionisation in this model, free electrons
diffuse and cause the resistivity to become homogeneous on long time scales.
In the presence of sufficient numbers of free
electrons in the initial ionisation state of the disc, we expect
that mixing will lead to a fully active disc, and indeed this
is what we find. Instead of the two-layer structure obtained using
model1 above,
with dead and active zones, the MHD turbulence now fills the full
vertical extent of the disc.
For t > 40 orbits, we observe a quasi
steady state characterised by small fluctuations around the mean value
,
where the time average
was taken in the interval [20,100] orbits. The vertical profiles of various quantities
are shown in Fig. 5. Compared with the results obtained for
model1, we see that the volume averaged turbulent stresses in each case
are very similar, even though model1
had a dead zone. The reason for this is that the resistivity in
model3 is higher near the disc surface because of mixing, and so reduces the
strength of the turbulence there. The subsequent enlivening of the midplane
in model3 does not lead to a substantial increase in the overall stress because
the now-uniform resistivity is sufficient to damp the strength of the
turbulence compared to its state in an ideal MHD calculation.
Comparing model3 with model2 we see that
higher stresses and more vigorous turbulence are generated by model2.
This is because model3
generates a disc without a dead zone, but in which the
resisivity is higher than for model2, such that the
strength of the resulting turbulence is suppressed somewhat.
The results for model3 show that mixing the initial
free electron population
throughout the disc can cause the dead zone to disappear, but
that allowing the chemical evolution of the disc to continue
during the turbulent mixing leads to a more active disc. This
is because the continuing ionisation of species near the disc
surface, followed by mixing toward the midplane, produces
a higher ionisation fraction overall.
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Figure 6:
model2: Space-time plots of the horizontally averaged value of |
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Figure 7:
model2: Space-time plots of the horizontally averaged value of |
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A primary motivation for this paper was the indication in Paper II
that dead zones could be
enlivened by a combination of turbulent mixing and sufficient abundance of
gas-phase magnesium atoms.
In that paper we presented calculations of the ionisation fraction in standard
-discs using reaction-diffusion models. The main results were that
turbulent mixing could only change the structure of a dead zone if:
(i) the abundance of magnesium was sufficient (so as to increase the recombination time);
(ii) one was considering locations further out in the disc where the
lower temperatures and densities increase the recombination time relative to the
local turbulent transport time.
The purpose of the simulations presented in the following subsections are to examine
how turbulent mixing affects dead zone structure as a function of magnesium
abundance and radial position in the disc, as a test of the predictions contained
in Paper II. We also perform a detailed comparison between some
of our MHD simulations and the predictions of the reaction-diffusion model.
These simulations solve the full set of multifluid equations in combination
with the chemical model described in Sect. 2.
We first present shearing box simulations of discs at various locations between 1 and 10 AU
with gas-phase magnesium abundance equal to zero, before considering a similar set of models
with gas-phase magnesium abundance
,
which is about
10-6 of the solar value.
We begin our discussion by first examining the dead zone structure after saturation obtained
for model2 with
.
We examine the disc evolution at
radii R= 1, 3, 5, 7 and 10 AU. In basic agreement with the
results obtained in Paper II, the dead zone structures obtained when
magnesium is absent
are very similar for all radii considered. In Fig. 6 we present space-time
plots of the horizontally averaged value of
,
and it is clear that the disc
sustains a two-zone structure for all radii and all time, which consists of a large
dead zone which extends from the midplane to
where the magnetic Reynolds
number
and the Lundquist number
(shown by the solid lines in Fig. 6).
Across the region bounded by
we
find that the horizontally averaged
varies by more than two orders of magnitude,
and this is maintained for the duration of the simulation (100 orbits).
We now consider the dead zone structures obtained for a magnesium abundance of
at radii R= 1, 3, 5, 7, and 10 AU.
Space-time plots of the horizontally averaged value of
are
shown in Fig. 7. At
and
,
the location of the boundary separating the dead from the active layer
matches very well the structure obtained for
,
since the
height at which
begins to exceed 4000 is
(which is also the height at which the Lundquist number Lu > 1,
shown by the solid lines in Fig. 7).
Significant changes in the dead zone
structure start to become evident at
.
At this radius the recombination time is similar to the turbulent mixing
time, allowing the resistivity to be reduced there through the transport of
free electrons into the dead zone. Over longer time scales we see that the dead zone
that is established early on in the simulation starts to diminish, and between 80-100
orbits there is evidence that the dead zone size has decreased significantly.
Nonetheless, at 100 orbits we find that there remains a region in the vicinity of
the midplane that retains an average values of
.
By contrast,
the space-time plots of the horizontally averaged value of
at R = 7
and
show that the two-layer structure has completely disappeared, because
mixing reduces the resistivity, and hence increases the magnetic Reynolds number to
values
4000.
Turbulence now fills the entire computational domain which is confirmed
by the time and volume averaged values of
:
for
and
for
.
Our results indicate that dead zones can be reduced or removed altogether through turbulent mixing. The criteria for sustaining MHD turbulence have already been discussed in the context of reaction-diffusion models in Paper II, and also apply to the shearing box models considered here. These criteria are:
Encouraged by the good qualitative agreement obtained between the MHD simulations and
the results presented in Paper II, we now examine in detail the
level of agreement between the simulations and the reaction-diffusion model.
As mentioned in Sect. 3, we assume
that the diffusion coefficient,
,
which governs the rate at which chemical
species mix vertically in the disc, is equal to an effective kinematic
viscosity generated by the turbulence
,
where
refers to a dimensionless parameter that measures the rate
of vertical mixing (not to be confused with the value of
associated
with the radial transport of angular momentum).
When solving the reaction-diffusion equations we use a range of
values to obtain different solutions, which we then
compare with the results of the MHD simulations. Previous work on
the vertical mixing of dust grains and molecules (Carballido et al. 2005;
Johansen & Klahr 2005; Turner et al. 2006; Fromang & Papaloizou 2006) suggests
that the ratio of the rate of angular momentum transport to the rate of
transport of chemical species by the turbulence should lie in the
range
,
and we examine how well our best-fit value of
agrees with this expectation.
Furthermore, the results of Turner et al. (2006) and Fromang & Papaloizou (2006)
show that the diffusion coefficient is not constant with height above the
midplane, but increases with height because the turbulent velocities
increase in proportion to the Alfvén speed. Although we consider only a
constant value of
for
each reaction-diffusion model that we run, we examine the quality of
the best-fit that we obtain, and quantify this by stating the error
obtained in predicting the magnetic
Reynolds number (which is a proxy for the free-electron abundance)
at the disc midplane and surface. In general we find that using a uniform
diffusion coefficient leads to a slight overestimate of the mixing rate near the
midplane, and a slight underestimate near the surface.
Overall we find
good agreement between the reaction-diffusion model and the MHD simulation
when the value of
adopted in the former is between a factor
of 1-2 times lowerer than the
time and volume averaged value of
obtained in the latter.
The
values corresponding to each MHD simulation are
listed in Table 3.
The best-fit values of
are listed in Table 4, along with the Schmidt number which
measures
.
![]() |
Figure 8:
model2: Comparison between vertical profiles of the magnetic
Reynolds number obtained for
|
| Open with DEXTER | |
Table 3:
Time and volume averaged values of
obtained for the models described in the paper. The first column gives the
model label and the cylindrical radius considered. The values of
are listed in the 2nd and
3rd column assuming a elemental metal abundance
of 0
and
,
respectively. Apart from the value denoted with
the symbol , the time average was taken over [20, 100] orbits, while
()
refers to the time average taken over [100, 200] orbits.
We have compared the results of models located at disc radii
R=5, 7 and 10 AU, and with magnesium abundances
and
.
In each case we examine
how the vertical profile of the magnetic Reynolds number
evolves with time, and in the case of the reaction-diffusion model
we calculate the equilibrium value of
from the underlying
ionisation fraction. In each case we initiate the calculation
assuming that the initial chemical abundance profile is equal
to the equilibrium state in the absence of mixing.
For each disc radius, we plot the profile of
the evolving
below. In the left panels we present
the results from the MHD simulations,
and in the right panels the equilibrium profile from
the corresponding reaction-diffusion model assuming different values of
.
The values of
plotted for shearing box simulations are horizontal
and time averages, where each time average was performed over 10 orbit
intervals. We plot the initial value of
using the dashed line,
and subsequent values are plotted using dotted lines starting at
t=[0,10] and moving up to t=[80,90]. The final values at
t=[90,100]are shown using the solid line.
![]() |
Figure 9:
model2: Comparison between vertical profiles of the magnetic
Reynolds number obtained for
|
| Open with DEXTER | |
Table 4:
Values of the diffusion coefficients applied to the
reaction-diffusion
model which best matches the corresponding MHD results for model2 with
.
The Schmidt number
is listed in
the 3rd column refering to time and volume averaged values of
between [20, 100] orbits.
![]() |
Figure 10:
model2: Comparison between vertical profiles of the magnetic
Reynolds number obtained for
|
| Open with DEXTER | |
We first discuss the results for
which are
shown in Fig. 8. Note that in the upper left panel of
Fig. 8, the magnetic Reynolds number shows a well defined
minimum, and this arises because this MHD simulation was performed
with a ceiling being adopted for the resistivity in the induction equation,
corresponding to
a minimum value of
.
This was done to ensure that
the time step constraint arising from the diffusive term in
the induction equation was not too severe. The minimum
value of
that we calculated from the electron fraction during this
simulation was
.
The upper left panel of Fig. 8 simply shows that
the model at 5 AU with
maintains a significant
dead zone with
(where
)
throughout, and the magnetic
Reynolds number does not change from its initial value.
The upper right hand panel shows that the reaction-diffusion
equation agrees with this, as the single line plotted is
actually three lines overplotted corresponding to
,
10-3 and 10-2. In the absence of magnesium, the recombination
rate is simply too high to allow mixing to modify the dead zone for
values in this range.
The lower left panel shows the evolution of
with
.
It is clear that the
profile in this case is non stationary near the
midplane, even after 100 orbits, and this appears to be
because this particular model is one which maintains
a dead zone throughout the run, but whose parameters
are close to those which would allow mixing to remove the dead zone.
Episodic increases and decreases in turbulent activity modify
the ionisation state near the midplane, causing the
values
to oscillate about a value close to 1000.
The lower right panel shows the results from the reaction-diffusion
model agree quite well with the mean
profile from the MHD run,
in particular when
.
Inspection of table 3
shows that mean value of
obtained from the MHD run was
.
Table 4 shows
that the best fit reaction-diffusion model
has a value of
(such
that the Schmidt number equals 1.88). The error in the predicted value
of
at the midplane was 3%, while the error at the disc surface was ![]()
,
showing good overall agreement even when a uniform
diffusion coefficient is adopted in the reaction-diffusion models.
The lower left and right panels show models for which
.
Here we see that there is very
significant change in the magnetic Reynolds number profile as
turbulent mixing ensues. In the MHD simulation we see that
the minimum value of
changes from 1000 to
4000,
which is high enough for the disc midplane to become active.
The lower right panel shows good agreement with the MHD simulation
when
.
We see from Table 3
that the average value of
from the MHD run is
.
Table 4 shows
that the best fit reaction-diffusion model
has a value of
(such
that the Schmidt number equals 1.23). The error in the predicted value
of
at the midplane was 2%, while the error at the disc surface was ![]()
.
![]() |
Figure 11:
model3: Comparison between vertical profiles
of the magnetic Reynolds number obtained for
|
| Open with DEXTER | |
The profiles obtained at
are shown in
Fig. 10. The upper panels are again in good
agreement when
,
showing that mixing has
no effect on the dead zone structure.
The lower panels show that the
profile
is changed significantly by mixing when
,
such that the dead zone
is enlivened completely. In the MHD simulation the minimum value of
changes from
1000 to
6000, allowing the
dead zone to become MRI-active and the disc to be turbulent
throughout its height. Good agreement in the
profile is obtained using the reaction-diffusion
model when
,
which as expected is slightly
lower than the value
listed in Table 3
as arising from the MHD simulation.
Table 4 shows
that the actual best fit reaction-diffusion model
has a value of
(such
that the Schmidt number equals 1.41). The error in the predicted value
of
at the midplane was <1 %,
while the error at the disc surface was
![]()
,
which again illustrates the fact that reasonable
agreement can be obtained when using a uniform diffusion coefficient.
We finally present a comparison between the MHD simulation
for model3 and a corresponding reaction-diffusion
model. To recap: model3 allows the free electrons and
ions to diffuse, but does not include recombination or on-going
ionisation. The MHD simulation and reaction-diffusion model
were initiated with the equilibrium chemical abundance for
the case
at R=10 AU.
The expectation is that turbulent mixing will cause the
profiles to change from their initial values
to become uniform. Inspection of Fig. 11 confirms
that our models agree with this expectation.
We have presented the results from a series of shearing box multifluid MHD simulations aimed at examining the evolution and structure of dead zones in protoplanetary discs, in the presence of turbulent transport of ions, on-going chemical evolution of the gas, and ionisation due to X-rays emitted by the central star. We have adopted a number of simplifying assumptions, including the absence of small grains whose presence in even modest numbers would lead to rapid removal of free electrons (Sano et al. 2000; Ilgner & Nelson 2006a). As such, our results are likely to be most applicable to protostellar discs at a fairly late stage of evolution after grains have accumulated to form larger bodies.
A primary objective of this work was to use MHD simulations to re-examine the results
of Ilgner & Nelson (2006b),
who used a simple reaction-diffusion model to calculate the effects of turbulent
mixing on dead zone structure. The simple model predicted that turbulent transport
can be effective at enlivening a dead zone provided that: (i) the abundance of gas-phase
magnesium is sufficient; (ii) one considers regions of the disc beyond radii
5 AU
where turbulent mixing occurs on a shorter time scale than recombination.
The main conclusions of this paper are that full multifluid MHD simulations
are in good agreement with these predictions. Models simulated at radii
between 1-10 AU, and with no magnesium
in the gas-phase, showed a two-layer structure consisting of
an actively accreting zone near the disc surface, and a magnetically
inactive region near the midplane. The addition of gas-phase magnesium
with fractional abundance
led to significant
dead zones persisting for radii
AU, but models at 7 and 10 AU
resulted in fully active discs without dead zones. The implications for
protoplanetary discs is that at late times, when most of the small submicron sized
dust grains have grown to much larger sizes, the dead zone beyond 5 AU may be
enlivened because of turbulent transport of ions toward the midplane.
Regions interior to 5 AU will, however, retain their dead zones.
A further conclusion of our work is that detailed comparison between the simple reaction-diffusion model and the MHD simulations leads to very good agreement in the vertical profiles of resistivity and magnetic Reynolds number when an appropriate diffusion coefficient is chosen. Typically we find that the best-fit vertical diffusion coefficient corresponds to a ratio in the range 1-2 between the rate at which angular momentum in transported radially and the rate at which diffusion of chemical species occurs vertically. This result is consistent with those presented by Carballido et al. (2005), Johansen & Klahr (2005), Turner et al. (2006) and Fromang & Papaloizou (2006) who showed that turbulent diffusion of dust (and chemical tracers) occurs on a slightly slower time scale than the transport of angular momentum, since it is driven through correlations in the perturbed flow velocities only.
It has traditionally been assumed that MRI-driven MHD turbulence in discs
can be sustained against the damping effects provided by ohmic resistivity
if magnetic field diffusion over the characteristic wavelength of the
instability occurs on a time scale longer than the growth time.
Indeed Turner et al. (2007) showed that such a condition provides
a good indicator of where the transition between active and dead zones
in a disc will occur. They showed that the transition zone occurs
where the Lunquist number
,
and our simulation results are in good agreement with this.
Recent work by Fromang & Papaloizou (2007) and Fromang et al. (2007), however,
has shown that in the case of non stratified shearing box simulations, turbulence
is only sustained in discs where the magnetic Prandtl number
(where
is the physical (molecular) viscosity),
even when Lu > 1 in the initial state.
The interpretation is that MRI-driven turbulence
cascades the magnetic field down to the smallest scales available, by virtue
of the turbulent velocity field twisting the field up. If the characteristic
scale on which velocity fluctuations are damped is smaller than the resistive scale,
then a zero net flux field will be dissipated and turbulence will die.
Interestingly, the magnetic Prandtl number in protostellar discs is expected to be
,
since resistivity is high and viscosity is low. Fromang & Papaloizou (2007)
also show that the intrinsic numerical magnetic Prandtl number of the ZEUS code is >1,
at least for simulations with resolutions feasible on current computers.
This suggests that the results in this paper, and those in other papers that
have looked at dead zones, are modelling discs which only fullfil one of the
necessary criteria for MHD turbulence to be sustained in a physical way, namely that
Lu > 1. The condition for
is satisfied because of the nature
of numerical dissipation in the code. We note that the effects
observed by Fromang & Papaloizou (2007) and Fromang et al. (2007) occur
for the particular case of non stratified shearing box simulations, and
that a mechanism for maintaining active MRI turbulence may be the generation
of large scale magnetic field through magnetic buoyancy effects and
field stretching in vertically
stratified discs, such as those we consider in this paper. Nonetheless,
it is clearly necessary to examine these issues by including the
appropriate viscous as well as resistive transport coefficients in simulations,
and we will do this in a future publication.
There are two additional issues that we have not addressed in this paper.
The first is that scattering of X-rays toward the disc midplane
may increase the ionisation rate in the disc by up to an order of
magnitude (Igea & Glassgold 1999), and this can have an obvious effect
on the structure of the dead zone. Although we have not undertaken
an extensive analysis of the effect of this, we have run a model at 1 AU
with
with the X-ray luminosity increased
by two orders of magnitude. We find only a small change in the dead zone
structure in this case. We would expect in general that increases
in the X-ray luminosity due to scattering will move the radial boundary of the
dead zone inward slightly, but will not completely remove the dead zone.
A final issue that we have not addressed in this paper in that of X-ray flares.
Observations of T Tauri stars by CHANDRA have shown that they emit regular
outbursts of X-rays which may increase the X-ray luminosity by a few orders
of magnitude, and also harden the X-ray spectrum (Favata et al. 2005; Wolk et al. 2005).
This issue was examined by Ilgner & Nelson (2006c), who showed that
the flaring could significantly modify dead zones in protoplanetary discs.
We will address this issue in a future paper using multifluid MHD simulations
with chemistry, so that both the effects of X-ray flaring and chemical mixing
on dead zone structure can be examined.
Acknowledgements
We would like to thank Sébastien Fromang, who very kindly made his version of the ZEUS code available to us. The referee, Neal Turner, provided numerous comments which improved this paper. The simulations presented here paper were performed on the QMUL High Performance Computing Facility purchased under the SRIF initiative.