Magnetorotational instability driven dynamos at low magnetic Prandtl numbers
Numerical simulations of the magnetorotational instability (MRI) with zero initial net flux in a non-stratified isothermal cubic domain are used to demonstrate the importance of magnetic boundary conditions.In fully periodic systems the level of turbulence generated by the MRI strongly decreases as the magnetic Prandtl number (), which is the ratio of kinematic viscosity and magnetic diffusion, is decreased. No MRI or dynamo action below is found, agreeing with earlier investigations. Using vertical field conditions, which allow the generation of a net toroidal flux and magnetic helicity fluxes out of the system, the MRI is found to be excited in the range , and that the saturation level is independent of . In the vertical field runs strong mean-field dynamo develops and helps to sustain the MRI.
keywords:magnetic fields — MHD — turbulence — accretion, accretion discs
The realization of the astrophysical signifigance of the magnetorotational instability (Balbus & Hawley, 1991), first discovered in the context of Couette flow (Velikhov, 1959; Chandrasekhar, 1960), seemed to resolve the long-standing problem of the mechanism driving turbulence in accretion disks. Early numerical simulations produced sustained turbulence, large-scale magnetic fields and outward angular momentum transport (e.g. Brandenburg et al., 1995; Hawley et al., 1995). These results also showed that a significant qualitative difference exists between models where an imposed uniform magnetic field is present as opposed to the situations where such field is absent: the saturation level of turbulence and angular momentum transport are substantially higher when a non-zero vertical net flux is present (e.g. Brandenburg et al., 1995; Stone et al., 1996). Also the presence of an imposed net toroidal field seemed to enhance the transport (Stone et al., 1996).
In the meantime, a lot of numerical work has been done with zero net flux setups that omit stratification and adopt fully periodic or perfectly conducting boundaries in order to study the saturation behaviour of the MRI in the simplest possible setting (e.g. Fromang & Papaloizou, 2007; Fromang et al., 2007; Liljeström et al., 2009; Korpi et al., 2010). Due to the boundary conditions, the initial net flux in conserved and no magnetic helicity fluxes out of the system are allowed. The results of these investigations have shown that as the numerical resolution of the simulations increases, or equivalently as the explicit diffusion decreases, the level of turbulence and angular momentum transport transport decrease, constituting a convergence problem for zero net flux MRI (Fromang et al., 2007). Runs with explicit diffusion show that sustaining turbulence becomes increasingly difficult as the magnetic Prandtl number, , where is the viscosity and the magnetic diffusivity, is decreased (Fromang et al., 2007). Currently the convergence problem is without a definite solution. It has been suggested that this issue could be related to the -dependence of the fluctuation dynamo (e.g. Schekochihin et al., 2007). It has even been argued that the MRI in periodic zero net flux systems would vanish in the limit of large Reynolds numbers and that a large-scale dynamo would be needed to sustain the MRI and turbulence (Vishniac, 2009). Notably, large-scale dynamos have no problems operating at low magnetic Prandtl numbers as long as the relevant Reynolds and dynamo numbers exceed critical values (Brandenburg, 2009).
From the point of view of mean-field dynamo theory (Brandenburg & Subramanian, 2005), systems with fully periodic or perfectly conducting boundaries are rather special. In such closed setups magnetic helicity, defined as a volume integral of , where is the vector potential and is the magnetic field, is a conserved quantity in ideal MHD. In the presence of magnetic diffusion, magnetic helicity can change only on a timescale based on microscopic diffusivity, which is usually a very long in any astrophysical setting. Such a behaviour, which has been captured in numerical simulations (Brandenburg, 2001), is well described by simple mean-field models taking into account magnetic helicity conservation (e.g. Blackman & Brandenburg, 2002). This would mean that generating appreciable large-scale magnetic fields, which are possibly vital for sustaining the MRI, can take a very long time. Furthermore, the saturation value of the mean magnetic field decreases inversely proportional to the magnetic Reynolds number (e.g. Cattaneo & Hughes, 1996; Brandenburg, 2001). In dynamo theory this detrimental effect to the large-scale dynamo is known as the catastrophic quenching (Vainshtein & Cattaneo, 1992).
The situation, however, changes dramatically if magnetic helicity flux out of the system is allowed. In particular, the Vishniac & Cho (2001) flux, which requires large-scale velocity shear to be present and flows along the isocontours of shear, is a potential mechanism that can drive a magnetic helicity flux out of the system and alleviate catastrophic quenching. Indirect evidence for its importance exists from convection simulations in a shearing box setup (Käpylä et al., 2008, 2010b), where dynamo excitation is easier in systems with boundaries that allow a net magnetic helicity flux. However, these results can be explained by a somewhat higher critical dynamo number in the perfect conductor case (Käpylä et al., 2010b), which is a purely kinematic effect. More dramatic differences between different boundary conditions are seen in the nonlinear saturation regime, with strong quenching of large-scale magnetic fields in the perfect conductor case (Käpylä et al., 2010b). The reason for this behaviour is not yet clear, especially in light of recent results of Hubbard & Brandenburg (2010) who failed to find evidence of the Vishniac–Cho flux in a numerical setup similar to ours.
In the present paper we demonstrate that the boundary conditions play a crucial role for the excitation of the MRI and the associated large-scale dynamo. Following previous work that has shown that open boundary conditions allow more efficient dynamo action (Käpylä et al., 2008, 2010b), we model a system that is isothermal, non-stratified, and the magnetic field has a zero net flux initially. We then apply vertical field boundary conditions which allow a magnetic helicity flux through the vertical boundaries by letting the magnetic field cross them. We show that if the MRI is excited, a large-scale dynamo is also excited and that the saturation level of the turbulence, large-scale magnetic field, and angular momentum transport are essentially independent of . This is contrasted by periodic simulations where we find a strong -dependence in accordance with earlier studies. Our results also suggest that for a given the results (level of turbulence and angular momentun transport) are independent of the magnetic Reynolds number (see also Fromang, 2010).
2 The model
In an effort to keep the system as simple as possible, we assume that the fluid is non-stratified and isothermal. The diffusion processes are modeled with explicit Laplacian diffusion operators with constant coefficients. A similar model was used by Liljeström et al. (2009) and Korpi et al. (2010), although in these models higher order hyperdiffusive operators were used instead of the Laplacian ones. The computational domain is a cube with volume . We solve the usual set of hydromagnetic equations in this geometry
where is the advective time derivative, is the magnetic vector potential, is the magnetic field, and is the current density, is the vacuum permeability, and are the magnetic diffusivity and kinematic viscosity, respectively, is the density, is the velocity, and is the rotation vector. The large-scale shear is given by , with , corresponding to Keplerian rotation, in all runs. We use isothermal equation of state , characterised by a constant speed of sound, . In the present models we choose the sound speed so that the Mach number remains of the order of 0.1 or smaller in order to minimize the effects of compressibility. The rate of strain tensor is given by
where the commas denote spatial derivatives. The initial magnetic field can be written in terms of the vector potential as
where the amplitude of the resulting magnetic field that contains and –components is given by . We use , , and in all models.
The values of , and are selected so that both the wavenumber with the largest growth rate, , where is the Alfvn velocity, and the largest unstable wavenumber, , are well resolved by the grid. The other condition for the onset of MRI, namely , where is the ratio of thermal to magnetic pressure, is also satisfied as for the maximum values of the initial magnetic field.
We use the Pencil Code111http://pencil-code.googlecode.com which is a high-order explicit finite difference method for solving the equations of compressible magnetohydrodynamics. Resolutions of up to are used, see Figure 1 for a snapshot of a high resolution run.
2.1 Boundary conditions
In all models the -direction is periodic and shearing-periodic boundary conditions are used for the -direction (Wisdom & Tremaine, 1988). On the -boundaries we use two sets of conditions. Firstly, we apply periodic boundaries (denoted as PER).
Secondly, we apply a vertical field (VF) condition for the magnetic field, which is fulfilled when
at the -boundaries. In this case we use impenetrable, stress-free conditions for the velocity according to
The novel property of the VF conditions is that they allow a net toroidal flux to develop and allow magnetic helicity fluxes out of the domain.
2.2 Units, nondimensional quantities, and parameters
Dimensionless quantities are obtained by setting
where is the mean density. The units of length, time, velocity, density, and magnetic field are then
The simulations are controlled by the following dimensionless parameters: the magnetic diffusion in comparison to viscosity is measured by the magnetic Prandtl number
The effects of viscosity and magnetic diffusion are quantified respectively by the parameters
We also define the fluid and magnetic Reynolds numbers
where is the root-mean-square (rms) value of the velocity, better decribing the nonlinear outcome of the simulations. Furthermore, we often measure the magnetic field in terms of the equipartition field which is defined via
where the brackets denote volume averaging. A convenient measure of the turbulent velocity is the Mach number
We define the mean quantites as horizontal averages
Often an additional time average over the statically saturated state is also taken. The size of error bars is estimated by dividing the time series into three equally long parts. The largest deviation of the average for each of the three parts from that over the full time series is taken to represent the error.
We perform two sets of simulations listed in Table LABEL:Runs where we use either periodic (Set A) or vertical field (Set B) boundary conditions. In Set A, Runs A0–A3 were started with the initial conditions described in Section 2 whereas Runs A4–A6 were continued from a snapshot of Run A3 in the saturated state, see Fig. 2. Run A7 was continued from a snapshot of Run A6 with a two times lower diffusivities at roughly where is the orbital period. The minimum duration of the runs in Set A is . Runs in Set B were all started from scratch and typically ran a significantly shorter time than those in Set A, e.g. in the low– cases (see Fig. 2), because final saturation occurs much faster.
3.1 Saturation level of the MRI
3.1.1 Periodic case
Earlier studies have shown that exciting the MRI in a periodic zero net flux system becomes increasingly harder as the magnetic Prandtl number is decreased (Fromang et al., 2007). Furthermore, the saturation level of turbulence has been reported to decrease as a function of . This has been conjectured to be associated with the difficulties of exciting a small-scale or fluctuation dynamo at low (e.g. Schekochihin et al., 2007). It is, however, unclear how the saturation level of the small-scale dynamo is affected by this. It is conceivable that at magnetic Reynolds numbers close to marginal it takes a long time to reach saturation and that the current simulations have not been run long enough. On the other hand, if catastrophic quenching is to blame, the mean magnetic field should decrease as (e.g. Brandenburg & Subramanian, 2005, and references therein). A further possibility is the scenario suggested by Vishniac (2009): in the absence of an outer scale for the magnetic field, the microscopic diffusivities determine the minimum lenght scale of MRI, which leads to turbulence intensity decreasing proportional to .
We study this issue by performing runs keeping fixed and increasing the Reynolds numbers. We find that the saturation level of turbulence, measured by the Mach number and root mean square value of magnetic field, are unaffected when is increased by a factor of three for the case (Runs A1–A3) and by a factor of two for the cases (Runs A4–A5) and (Runs A6–A7), see Table LABEL:Runs and Fig. 3. Furthermore, the Mach number and rms magnetic field, normalised with the rms value of the initial field, increase roughly linearly with . The -dependence of rms magnetic field normalised to the equipartition field strength, listed in Table LABEL:Runs, shows a much weaker trend. This is to be expected as is proportional to the rms velocity which, on the other hand, is a produced by the magnetic field itself. Since the parameter range of our simulations is rather limited, no definite conclusions can be drawn. However, taking the results at face value, it appears that , not , is the parameter that determines the saturation level in the periodic zero net flux case. Recently, Fromang (2010) reached the same conclusion independently for the case of . According to our results, the catastrophic quenching and the diffusivity-limited MRI length scale scenarios would be ruled out. Although there is the possibility that our calculations have not been run long enough, the results seem to suggest the small-scale dynamo being harder to excite as decreases.
3.1.2 Vertical field case
We find that the saturation behaviour is markedly different when vertical field boundary conditions are applied (Table LABEL:Runs and Fig. 3). The saturation level of turbulence depends only weakly on the magnetic Prandtl number: the difference of the values of between and cases is roughly 50 per cent. Furthermore, the Mach number decreases as function of , the trend being weaker but opposite to the periodic case. This is likely caused by the increase of viscosity by two orders of magnitude rather than the intrinsic dependence of the MRI on . This conjecture is supported by the saturation values of the magnetic fields which are independent of (lower panel of Fig. 3). The runs in Set B, however, seem to fall into two distinct regimes of magnetic field strength, where the magnetic energy differs by roughly a factor of two. The reason for this apparent discrepancy is that a different mode of the large-scale magnetic field is excited in the different branches (see below). Similar behaviour of the large-scale dynamo has previously been seen in isotropically forced turbulece (Brandenburg & Dobler, 2002).
3.2 Large-scale magnetic fields
In the runs with periodic boundaries we occasionally see the emergence of large-scale magnetic fields with a sinusoidal dependence on (see Fig. 4), i.e. , in accordance with earlier investigations (Lesur & Ogilvie, 2008). Similar large-scale dynamos have recently been reported from nonhelically forced turbulence with shear where the MRI is absent (e.g. Yousef et al., 2008; Brandenburg et al., 2008). As in the forced turbulence case a strong large-scale field is not present at all times and the fields undergo apparently random sign changes that are not fully understood (see, however, Lesur & Ogilvie, 2008; Brandenburg et al., 2008). The intermittent nature of the large-scale fields could also explain the apparent lack of catastrophical quenching of the time averaged mean magnetic field (see Table LABEL:Runs).
In the vertical field runs a strong large-scale dynamo is always excited continuously. The two branches of solutions that are visible in the total magnetic energy (Fig. 3) are due to different modes of the large-scale field. This is illustrated in Fig. 5 where the horizontally averaged horizontal magnetic field components are shown as functions of time for Run B1. As is common for dynamos with strong shear, the streamwise component of the magnetic field is much stronger than the cross-stream one. Although the initial condition of the magnetic field is the same in all runs, the large-scale field which develops in the non-linear stage can choose any of the available wavenumbers consistent with the vertical boundary condition . In practice, the dominant large-scale component is or in our simulations. The large-scale dynamo tends to accumulate energy at the smallest possible wavenumber (Brandenburg, 2001), i.e. the largest spatial scale. However, if the dominant mode is on some intermediate scale initially, those modes can also be long-lived (Brandenburg & Dobler, 2002). Ultimately the large-scale field evolves towards final saturation where the largest possible scale dominates which was seen in Brandenburg & Dobler (2002) and in some of our runs (cf. Fig. 5). The fact that the magnetic energy in Runs B2, B6, B7, and B8 is smaller is due to the fact that the large-scale field is predominantly of the flavour, and that final saturation of the large-scale magnetic field has not yet occured. Lesur & Ogilvie (2008) found that the toroidal large-scale magnetic field generated in their simulations is close to that yielding the maximum growth rate for an non-axisymmetric instability. Using their notation we find a similar result so that for and for , using for the mode. However, the full signifigance of this result is as of yet unclear.
Although the source of the turbulence and the nature of the dynamos (kinematic vs. nonlinear) is different between the nonhelically forced turbulence simulations (e.g. Yousef et al., 2008; Brandenburg et al., 2008) and the non-stratified MRI runs such as those presented here, it is conceivable that the large-scale field generation mechanism is the same. Since the periodic system is homogeneous, the cause of the large-scale fields cannot be the -effect of mean-field dynamo theory (Moffatt, 1978; Krause & Rädler, 1980), which is in simple systems proportional to the density gradient or the turbulence inhomogeneity due to boundaries (e.g. Giesecke et al., 2005; Käpylä et al., 2010a). However, a fluctuating with zero mean can also drive a large-scale dynamo when shear is present (e.g. Vishniac & Brandenburg, 1997; Sokolov, 1997; Silant’ev, 2000; Proctor, 2007). This is the most likely source of the large-scale magnetic fields in the present case. Furthermore, it is possible that the shear–current and –effects can drive a large-scale dynamo (Rädler, 1969; Rogachevskii & Kleeorin, 2003, 2004), although present evidence from numerical models does not support this (Brandenburg et al., 2008).
In the VF runs the impenetrable stress-free -boundaries make the turbulence inhomogeneous near the boundary. This leads to the generation of mean kinetic helicity , where is the vorticity. The quantity is important, because the mean-field -effect is, in simple settings, proportional to it (e.g. Krause & Rädler, 1980). Such contributions, however, will not show up in volume averages because the sign of the helicity, and thus of the -effect, are different near the different boundaries. Figure 6 shows the horizontally averaged kinetic helicity for Run B7. Here we average also in time over the saturated state of the run. In most of the volume the kinetic helicity is consistent with zero, although there are regions close to the boundaries where non-zero mean values are present. The rms-value of , however, is at least five times greater than its mean (see the inset of Fig. 6). Note also that the normalization factor contains the integral scale . A more proper definition would be to use the wavenumber where turbulent energy peaks which is likely at least a factor of few greater than . Thus our estimates for the normalised helicity can be considered as upper limits. The rather small values of mean helicity and the dominance of fluctuations suggest that the generation mechanism of the large-scale fields could indeed be the incoherent –shear dynamo. However, a conclusive answer can only be obtained by extracting the turbulent transport coefficients and by performing mean-field modeling of the same system (see e.g. Gressel, 2010).
3.3 Angular momentum transport
The main effect of turbulence in astrophysical disks is to enhance diffusion which enables efficient accretion. In accretion disk theory it is customary to parametrise the turbulent viscosity in terms of the Shakura–Sunyaev viscosity parameter , which relates with the local gas pressure (Shakura & Sunyaev, 1973).
We define the Shakura–Sunyaev viscosity parameter as (Brandenburg et al., 2004)
is the Reynolds stress and
the Maxwell stress, and where the angular brackets denote volume averaging. Here we decompose the velocity and magnetic field into their mean (), taken here as the horizontal average, and fluctuating () parts. The mean velocities show no systematic large-scale pattern and the remaining signal is likely a residual of averaging over a finite number of cells. The contribution of mean flows to the angular momentum transport and the dynamo process is thus likely to be negligible.
For the runs in Set A we find essentially the same scaling, consistent with , with magnetic Prandtl number as in the case of the turbulent kinetic and magnetic energies, see Fig. 7. This is consistent with the mixing length estimate of turbulent viscosity which is proportional to the turbulence intensity (e.g. Snellman et al., 2009). The numerical values of decrease from for , to for . In Set B, on the other hand, is essentially independent of magnetic Prandtl number. The value of is consistently of the order of , which is significantly greater than that found in runs with periodic boundaries. Here the qualitative behaviour of resembles that of the turbulent kinetic energy, whereas the two different dynamo modes seen in magnetic energy are not visible in the angular momentum transport.
A possible clue to understanding the convergence problem in zero net flux simulations comes from MRI models with density stratification: in them the level of turbulence does converge when the Reynolds numbers are increased (Davis et al., 2010), even with perfect conductor of periodic boundaries. Furthermore, such setups exhibit a large-scale dynamo (e.g. Brandenburg et al., 1995; Stone et al., 1996; Gressel, 2010) where the magnetic helicity changes sign at the midplane (Gressel, 2010).
Recent numerical results from a different setting suggest that a diffusive flux of magnetic helicity also exists (Mitra et al., 2010). Such a flux can alleviate catastrophic quenching by transporting oppositely signed magnetic helicity to the midplane where annihilation occurs. This could explain the successful convergence of the stratified MRI runs. In the non-stratified case with periodic or perfectly conducting boundaries, however, no net flux of magnetic helicity occurs and the large-scale dynamo can be catastrophically quenched, shutting off the MRI. When a flux is allowed by changing to vertical field boundary conditions, this limitation is removed and the large-scale dynamo can operate without hindrance. However, this hypothesis requires further study and more careful analysis of the helicity fluxes that we postpone to a future publication.
We present three-dimensional numerical simulations of the magnetorotational instability in an isothermal non-stratified setup with zero net flux initially. Using fully periodic boundaries, that do not allow the generation of a mean toroidal flux or magnetic helicity fluxes out of the system, we encounter the convergence problem (Fromang et al., 2007) of the MRI: turbulent kinetic and magnetic energies, and the angular momentum transport increase approximately proportional to the magnetic Prandtl number. Intermittent large-scale magnetic fields are observed in the periodic runs. Increasing the Reynolds numbers moderately at a given does not appear to markedly change the results in the saturated state.
When vertical field boundary conditions, allowing the generation of a mean flux and a magnetic helicity flux, are used, the MRI is excited at least in the range for our standard value of . We find that the saturation level of the turbulence and the angular momentum transport are only weakly dependent on the Prandtl number and that strong large-scale fields are generated in all cases. The Shakura–Sunyaev viscosity parameter has consistently a value of in the vertical field case. Exploring even lower values of is infeasible at the moment due to prohibitive computational requirements but there are no compelling arguments against a large-scale dynamo operating at low (Brandenburg, 2009). We conjecture that the operation of the MRI at low is due to the efficient large-scale dynamo in the system. It is conceivable that the dynamo only works if magnetic helicity is allowed to escape (see also Vishniac, 2009) or annihilate at the disk midplane due to an internal diffusive flux (Mitra et al., 2010). However, measuring the magnetic helicity fluxes in the presence of boundaries is difficult due to the fact that they are in general gauge dependent (e.g. Brandenburg et al., 2002; Hubbard & Brandenburg, 2010).
The current results highlight the close connection between dynamo theory and the theory of magnetised accretion disks (see also Blackman, 2010) and the importance of studying the results in a common framework (e.g. Gressel, 2010). Clearly, a more thorough study is needed in order to substantiate the possible role of magnetic helicity fluxes for the excitation and saturation of the MRI. We plan to address these issues in future publications.
The authors acknowledge Axel Brandenburg for his helpful comments on the manuscript. The numerical simulations were performed with the supercomputers hosted by CSC – IT Center for Science in Espoo, Finland, who are administered by the Finnish Ministry of Education. Financial support from the Academy of Finland grant Nos. 121431 (PJK) and 112020 (MJK), are acknowledged. The authors acknowledge the hospitality of NORDITA during the program “Solar and Stellar Dynamos and Cycles”.
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