Transport properties of the Azimuthal Magnetorotational Instability
Anna Guseva, Ashley P. Willis, Rainer Hollerbach, Marc Avila

TL;DR
This study investigates the transport properties of the azimuthal magnetorotational instability (MRI) in conducting fluids, revealing how instability onset and angular momentum transport depend on magnetic Reynolds number, magnetic Prandtl number, and flow profiles.
Contribution
It provides the first detailed numerical analysis of MRI driven by azimuthal magnetic fields across various flow profiles and parameter regimes, including low magnetic Prandtl numbers.
Findings
Instability onset depends on magnetic Reynolds number in quasi-Keplerian flows.
Angular momentum transport scales as √Pm Re^2 in turbulent regimes.
Reynolds stress can become negative at high Rm.
Abstract
The magnetorotational instability (MRI) is thought to be a powerful source of turbulence in Keplerian accretion disks. Motivated by recent laboratory experiments, we study the MRI driven by an azimuthal magnetic field in an electrically conducting fluid sheared between two concentric rotating cylinders. By adjusting the rotation rates of the cylinders, we approximate angular velocity profiles . We perform direct numerical simulations of a steep profile close to the Rayleigh line and a quasi-Keplerian profile and cover wide ranges of Reynolds () and magnetic Prandtl numbers (). In the quasi-Keplerian case, the onset of instability depends on the magnetic Reynolds number, with , and angular momentum transport scales as in the turbulent regime. The ratio of Maxwell to…
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Transport Properties of the Azimuthal Magnetorotational Instability
Anna Guseva
University of Bremen, Center of Applied Space Technology and Microgravity (ZARM), Bremen 28259, Germany
Friedrich-Alexander University Erlangen-Nürnberg, Institute of Fluid Mechanics, Erlangen 91058, Germany
Ashley P. Willis
University of Sheffield, School of Mathematics and Statistics, Sheffield S3 7RH, UK
Rainer Hollerbach
University of Leeds, School of Mathematics, Leeds LS2 9JT, UK
Marc Avila
University of Bremen, Center of Applied Space Technology and Microgravity (ZARM), Bremen 28259, Germany
Friedrich-Alexander University Erlangen-Nürnberg, Institute of Fluid Mechanics, Erlangen 91058, Germany
Abstract
The magnetorotational instability (MRI) is thought to be a powerful source of turbulence in Keplerian accretion disks. Motivated by recent laboratory experiments, we study the MRI driven by an azimuthal magnetic field in an electrically conducting fluid sheared between two concentric rotating cylinders. By adjusting the rotation rates of the cylinders, we approximate angular velocity profiles . We perform direct numerical simulations of a steep profile close to the Rayleigh line and a quasi-Keplerian profile and cover wide ranges of Reynolds () and magnetic Prandtl numbers (). In the quasi-Keplerian case, the onset of instability depends on the magnetic Reynolds number, with , and angular momentum transport scales as in the turbulent regime. The ratio of Maxwell to Reynolds stresses is set by . At the onset of instability both stresses have similar magnitude, whereas the Reynolds stress vanishes or becomes even negative as increases. For the profile close to the Rayleigh line, the instability shares these properties as long as , but exhibits a markedly different character if , where the onset of instability is governed by the Reynolds number, with , transport is via Reynolds stresses and scales as . At intermediate we observe a continuous transition from one regime to the other, with a crossover at . Our results give a comprehensive picture of angular momentum transport of the MRI with an imposed azimuthal field.
magnetohydrodynamics, instabilities, turbulence
††journal: ApJ
1 Introduction
The source of angular momentum transport remained the main question of accretion disk theory for years. Keplerian flows in accretion disks have radially decreasing angular velocity and are linearly stable according to the hydrodynamic Rayleigh criterion. However, the motion of gas in accretion disks cannot be laminar because viscous (molecular) outward transport is too slow for accretion to occur at the observed rates. Shakura & Sunyaev suggested the presence of turbulent motion and parameterized momentum transport by an effective turbulent eddy-viscosity in their early -model (Shakura & Sunyaev, 1973). The origin of turbulence was unclear until Balbus & Hawley noted in 1991 that Keplerian flows of ionized gas can be destabilized by magnetic fields by the so-called magnetorotational instability (Balbus & Hawley, 1991, 1998). The MRI was first described by Velikhov (1959) and Chandrasekhar (1961), who investigated the stability of electrically conducting fluids sheared between two concentric cylinders (Taylor-Couette flow) and subjected to an axial (poloidal) magnetic field. The MRI operates if the angular velocity decreases outwards and angular momentum increases, which is the case in Keplerian flows.
Since the seminal work of Balbus & Hawley (1991) there has been considerable interest in the MRI from the theoretical, numerical and experimental points of view. The action of poloidal fields, which can be generated by the accreting object in the center of the disk or advected from outside, is well-studied. Weak poloidal magnetic fields lead to the amplification of axisymmetric disturbances and give rise to self-sustained turbulence in nonlinear simulations (Balbus & Hawley, 1991; Hawley et al., 1995; Stone et al., 1996). This MRI turbulence was found to significantly enhance angular momentum transport via Maxwell stresses, which were several times larger than Reynolds stresses. However, these early works did not take account of viscosity and magnetic resistivity (ideal MHD). Lesur & Longaretti (2007) considered non-ideal fluids and showed a power-law dependence of the transport coefficient of the form , with , for the explored range of magnetic Prandtl numbers and Reynolds numbers .
It is important to note that most nonlinear simulations of the MRI have been performed using the shearing sheet approximation, which consists of a local model of an accretion disk (Hawley et al., 1995). In this approximation, the equations are solved in a rotating frame in Cartesian geometry, with the rotation given by the linearization of the Keplerian law at a radial point in the disk. Periodic boundary conditions are assumed in all three directions, and radial shear is introduced by means of a coordinate transformation. These boundary conditions determine the geometry of the modes observed in the simulations and their saturation in the nonlinear regime (Regev & Umurhan, 2008). In addition, most simulations of shearing boxes neither resolve all flow scales nor implement subgrid models that capture the impact of small flow scales on the larger scales.
Ji et al. (2001) and Rüdiger & Zhang (2001) suggested the study of the MRI in an electrically conducting fluid sheared between two concentric cylinders, exactly as considered originally by Velikhov (1959) and Chandrasekhar (1961). By appropriately choosing the rotation-ratio of the cylinders, velocity profiles of the general form , including for Keplerian rotation, can be well approximated experimentally at very large Reynolds numbers (Edlund & Ji, 2015; Lopez & Avila, 2017). For an imposed axial magnetic field, Gellert et al. (2012) found the transport coefficient to be independent of magnetic Reynolds and magnetic Prandtl numbers, only scaling linearly with the Lundquist number of the axial magnetic field. However, the critical parameter values , are challenging to achieve experimentally because of the low values of for liquid metals and therefore extremely high critical Reynolds numbers . While signatures of this standard MRI were detected experimentally in the form of damped magnetocoriolis waves (Nornberg et al., 2010), unstable magnetocoriolis waves (giving rise to the MRI) have not been reported in the literature so far.
The MRI can also be triggered by toroidal magnetic fields provided that these are neither too weak nor too strong (Balbus & Hawley, 1992; Ogilvie & Pringle, 1996). Interest in this “azimuthal” MRI (AMRI) increased further following the linear stability analysis of Hollerbach et al. (2010), who found that for steep velocity profiles close to the Rayleigh line () the AMRI is governed by the Reynolds and Hartmann numbers, instead of and . The two sets of parameters are related by and . For this inductionless version of MRI continues to exist even for , , as long as and . It takes the form of an inertial wave destabilized by the magnetic field via the Lorentz force, and hence is a magnetohydrodynamic rather than hydrodynamic instability (see Kirillov & Stefani, 2010, for an extended discussion and connection to the standard MRI via helical fields).
Seilmayer et al. (2014) reported the experimental observation of the predicted non-axisymmetric AMRI modes in Taylor–Couette flow with . Because of the strong currents of nearly 20kA needed to generate the required azimuthal field, measurements could only be conducted close to the stability boundary. Using direct numerical simulations Guseva et al. (2015) probed deep into the nonlinear regime and computed the angular momentum transport of the AMRI. Despite the highly turbulent nature of the flow, for (InGaSn alloy) the angular momentum transport was found to be barely faster than in laminar flow. Recently, Rüdiger et al. (2015) examined the effective viscosity for the three relevant rotation rates: close to the Rayleigh line (), quasi-Keplerian () and galactic (), in the range of and . They suggested a scaling of the dimensionless effective viscosity as , with Maxwell stresses dominating for large . However, in the range of parameters investigated in Rüdiger et al. (2015), AMRI turbulence does not yet clearly exhibit asymptotic scaling and the transition between low- and high- instability and transport properties at low and moderate remain unclear.
In this paper, we first revisit the linear stability analysis of the AMRI by considering various rotation laws, over a range of magnetic Prandtl, Hartman and Reynolds numbers. We show the scalings determining the existence of the instability as a function of these parameters. Second, using direct numerical simulations, we compute angular momentum transport in the system for up to and . Our results give a comprehensive picture of turbulent transport via the AMRI.
2 Model
2.1 Governing equations and parameters
We consider an incompressible viscous electrically conducting fluid sheared between two rotating cylinders of inner and outer radii and . The velocity and magnetic field are determined by the coupled Navier–Stokes and induction equations:
[TABLE]
[TABLE]
together with . Here is the fluid pressure, , , and are the constant density, kinematic viscosity and magnetic diffusivity of the fluid, respectively. The Navier–Stokes and induction equations (1)–(2) are formulated in cylindrical coordinates with periodic boundary conditions in the axial and azimuthal directions. Insulating boundary conditions are imposed for . No-slip boundary conditions are imposed for , which for the azimuthal velocity read , , where () is the angular speed of the inner (outer) cylinder. The laminar angular velocity profile is
[TABLE]
In this work we take the radius ratio to be , and the rotation ratio is varied to approximate different rotation laws. Close to the Rayleigh line we focus on , and for quasi-Keplerian rotation we take , which yield and respectively, based on the average shear. The remaining dimensionless parameters of the problem are the Hartmann , Reynolds and magnetic Reynolds numbers, where is the gap between cylinders. and are connected through the magnetic Prandtl number .
2.2 Numerical methods
For the linear stability analysis of the laminar flow in §3.1, the spectral eigenvalue solver of Hollerbach et al. (2010) was employed. The fully coupled nonlinear Navier–Stokes and induction equations (1)–(2) were discretized with high-order finite-differences in the radial direction and the Fourier pseudospectral method in the axial and azimuthal directions. The time discretization is based on the implicit Crank–Nicolson method and is of second order. Details of our numerical method, implementation and tests can be found in Guseva et al. (2015). The numerical resolution was chosen so that our simulations were fully resolved; it reached finite-difference points in the radial direction and () and () Fourier modes in the axial and azimuthal directions. The aspect-ratio in the axial direction was fixed to (high ) or (low ), where is the length of the cylinders.
2.3 Angular velocity current
Frequently a net loss (gain) of angular momentum on the inner (outer) cylinder is measured in experiments as torque (Paoletti & Lathrop, 2011; Wendt, 1933). Dimensionless laminar torque can be explicitly calculated from the radial derivative of azimuthal velocity profile (3),
[TABLE]
or equivalently,
[TABLE]
In a statistically steady state, the time-averaged torques on the inner and outer cylinders are equal in magnitude.
Eckhardt et al. (2007) derived a conservation equation for the current of the angular velocity in hydrodynamic Taylor–Couette flow. In this work we extend this to the magnetohydrodynamic case as follows. Defining
[TABLE]
the -component of the Navier–Stokes equation becomes (7). Averaging over time and a co-axial cylindrical surface of area yields (8). Using the divergence-free condition for and , and multiplying by , we finally obtain equation (9). \onecolumngrid
[TABLE]
[TABLE]
[TABLE]
\twocolumngrid
The first term in equation (9) represents a Reynolds stress, whereas the second and third terms represent viscous and Maxwell stresses, respectively. For the steady rotation is conserved [, see equation (9)]. The constant can be interpreted as the conserved transverse current of azimuthal motion transporting in the radial direction. Its unit is [] = m4 s*-2* = []2. The angular velocity current is closely related to the dimensionless torque on the cylinders (Eckhardt et al., 2007):
[TABLE]
In the case of laminar flow the first and the third term in Equation (9) are zero and the laminar angular velocity current is defined by
[TABLE]
so that (10) and (4) coincide.
2.4 Effective viscosity
For the case of turbulent flow, in analogy to (11) we model angular velocity current with the mean angular velocity:
[TABLE]
where the effective viscosity is parameterized with the mean angular velocity and the size of the gap between cylinders
[TABLE]
Substituting (13) into (12) results in the following for the parameter :
[TABLE]
Here and is a Reynolds number based on the average angular velocity. Estimation of based on and the midgap radius gives . Recalling (10) we finally obtain:
[TABLE]
Protostellar-disk accretion rates indicate (Hartmann et al., 1998).
3 Stability analysis
3.1 Linear stability analysis
We begin by studying stability of the laminar flow to infinitesimal disturbances. For the curvature considered here, , the dominant AMRI mode is non-axisymmetric with azimuthal wavenumber . At fixed parameters , the axial wavenumber was varied to determine the maximum perturbation growth rate. The flow becomes unstable only after exceeds a critical threshold and remains unstable thereafter only in a certain range of , i.e. for neither too weak nor too strong magnetic fields (Hollerbach et al., 2010). The black solid curve in Fig. 1a shows the neutral stability curve of the AMRI for and . In the region enclosed by this curve the laminar flow is linearly unstable. The growth rate of the instability is maximized (for =const) along the black dashed-dotted line. The curve starts at and , which is the minimum Reynolds number at which the instability occurs. Figure 1b shows the dependence of as a function of for and . At large the two curves collapse, indicating that the AMRI becomes insensitive to rotation profile. In fact for the AMRI occurs at lower than the Rayleigh (centrifugal) instability at all . As decreases the two curves gradually depart from each other. For quasi-Keplerian rotation () and , grows inversely proportional to , and so the onset of instability occurs at a constant magnetic Reynolds number . By contrast, for the onset of instability occurs at a constant hydrodynamic Reynolds number .
To shed more light on the difference in behavior in the limit, we analyzed Maxwell and Reynolds stresses for the critical eigenmodes. The radial distributions of stresses for and at low are shown in the first and second row of Fig. 2, respectively. The ratio of Maxwell to Reynolds stresses, each integrated over the radius , for is about for both and , whereas for it decreases from to as is reduced from to . This suggests that the relative importance of stresses is essentially set by the magnetic Reynolds number.
Overall, the linear analysis of this section highlights the markedly different character of the instability at low for rotation near the Rayleigh line, with (magnetically destabilized inertial wave with transport via Reynolds stresses), and quasi-Keplerian rotation, with (unstable magnetocoriolis wave with transport via Maxwell and Reynolds stresses).
3.2 Nonlinear stability analysis
Close to the onset of instability the AMRI is a rotating wave in the azimuthal direction (Hollerbach et al., 2010), whereas in the axial direction it can be a standing wave (SW) or a traveling wave (TW) (Knobloch, 1996). For a SW is realized (Guseva et al., 2015), whereas at the AMRI manifests itself as a TW, thereby breaking the axial reflection symmetry (Guseva et al., 2017a). Close to the bifurcation is found to be supercritical in all cases. However, at large and the nonlinear AMRI pattern survives outside the left stability border (magenta diamonds in Fig. 1a), indicating a subcritical bifurcation for both and . As a result, for the left stability border widens faster than expected from the linear estimate.
4 Angular momentum transport
We performed DNS spanning a wide range in and up to and computed the torque in order to quantify the scaling of angular momentum transport via the AMRI. Each filled symbol in Fig. 3 marks a simulation in the parameter space , with . The simulations with follow the same path as for and are shown as empty symbols of the same color. Because of the cost of varying both and , we followed one-dimensional paths in parameter space (dashed-dotted lines connecting the symbols) that correspond to the maximum growth rate lines of the linear analysis (depicted by the dashed-dotted line in Fig. 1a for and ). Note that Guseva et al. (2015, 2017a) showed that the maximum growth rate of the linear analysis correlates very well with the maximum of the transport for at low and high . Mamatsashvili et al. (2017) have observed the same correlation for the helical MRI. Hence the results presented in the following can be seen as an upper bound on the angular momentum transport.
The value of depends strongly on and as shown in Fig. 1b. Hence comparing the scaling of with at different and is not straightforward. Moreover, Guseva et al. (2015, 2017a) found that at low , close to the Rayleigh line, the turbulence arising from the AMRI is not efficient in transporting momentum. At and , molecular viscosity is responsible for a significant portion of the momentum transport. As a consequence, the laminar contribution to the torque can obscure the scaling of the turbulent contribution, which will obviously dominate at the asymptotically large of interest. To enable a representation more useful for extrapolations toward large , in this section we quantify transport by showing the reduced torque (), which is proportional to the turbulent viscosity, as a function of the relative Reynolds number .
4.1 Close to the Rayleigh line
Figure 4a shows that for the reduced torque scales linearly with , whereas the dependence on is not straightforward. Lines of , where the pre-factor is a function of , provide good fits to all data sets. The pre-factors and respective errors were calculated based on the average of local fits to the data using stencils of 3 up to 5 points. The dependence of the pre-factor on is shown in Fig 4c. For , , supporting the scaling proposed by Rüdiger et al. (2015), whereas for , saturates to a small but constant value independent of . We verified this by performing DNS in the inductionless limit (, violet empty circles in 4a) and the results are in fact indistinguishable from (). This supports the hypothesis that in the limit of very small magnetic Prandtl numbers the turbulent angular momentum transport triggered by AMRI turbulence depends only on , and this dependence is linear.
The case of requires special attention. Close to the onset of instability the scaling factor tends to the low- values and the -scaling is approached only at high . This is most likely connected to the change in the dominant mode at (), illustrated by the change of slope of the maximum growth rate in Fig. 3. Thus, the quality of the linear fit for is not very good, and the error bar for on Figure 4 is the largest. Still the average value of the pre-factor approximates well the local fits of the high- part of the curve, and can be taken as an estimate.
4.2 Quasi-Keplerian rotation
Although the case of allows us to span a broad range of relevant , the astrophysically most relevant profile is the quasi-Keplerian one (). To compare the torque of the two rotation rates, we performed simulations at and , and where is low enough for DNS to be feasible (Fig. 1b). The results of this comparison are presented in Fig. 4b. Unlike in Rüdiger et al. (2015), we do not observe that the torque is lower for the profile. The lower values of torque at low are because of the later onset of instability at and converge toward the values for the case as the turbulence develops further. Hence, once the dependence of on is taken into account, the torque scales identically for both rotation profiles, as demonstrated in Figure 4c. Because for the onset of instability occurs at , studying becomes numerically unfeasible. Hence it cannot be directly tested whether a transition from the -scaling to the pure -scaling, as observed close to the Rayleigh line, occurs also in the quasi-Keplerian case.
5 Analysis of transport mechanisms
The analysis of the Maxwell and Reynolds stresses of the linear eigenmodes at low shown in §3.1 suggests that for Reynolds and Maxwell stresses are relevant, whereas for only Reynolds stresses play a role. In this section we analyze the dependence of the stress contributions for the data from the nonlinear simulations shown in Fig. 4. In nonlinear simulations of the fully coupled Navier–Stokes and induction equations, the total transport of momentum expressed by the conserved angular velocity current is the sum of the contribution of Reynolds, Maxwell and viscous stresses (9). At sufficiently large , the viscous contribution is confined to thin boundary layers attached to the cylinders. Because of the no-slip and insulating boundary conditions, at the cylinders there is only viscous transport (quantified by the torque ). As we are interested in the high limit, in this section we analyze only the Maxwell and Reynolds contributions, which is consistent with the analysis of presented in the previous section, and the characterization of the linear eigenmodes shown in Fig. 2.
Figure 5 presents the Reynolds stresses (solid) and Maxwell stresses (dashed) as functions of radius for three representative points in the parameter space. The stresses were normalized with the full azimuthal motion current , which does not depend on according to (9). Because of conservation of , the viscous part can be obtained by subtracting the Maxwell and Reynolds contributions from 1. At (, cyan) Maxwell stresses are negligible and up to 40% of the angular momentum is transported by Reynolds stresses. Despite the large , viscous transport is still prevalent and amounts to 60% of the total. At (, red) the Maxwell stresses amount to 20% of the total transport in the middle of the gap, and Reynolds stresses contribute 40%. For (, black) the Maxwell stresses dominate the transport in the center part of the domain, while Reynolds and viscous stresses are very small. Interestingly, the Reynolds stresses are negative in the center of the domain, corresponding to inward momentum transport due to velocity fluctuations. Here Maxwell stresses are larger than the total current in the middle part of the gap so that remains conserved at each radial position. Note that the negative contribution of the Reynolds stress is also present in the linear eigenmode at and shown in Fig. 2d.
The magnetic Reynolds number increases in passing through the described points: , suggesting that the relative contribution of the stresses to the total current depends strongly on magnetic Reynolds number. This is again in line with the behavior of the linear eigenmodes discussed in section §3.1. Figure 6a shows the contributions of Maxwell and Reynolds stresses, normalized by their sum, at the mid-gap as a function of magnetic Reynolds number. At low the contribution of Maxwell stresses is marginal, but thereafter it begins to noticeably grow until it becomes equal to the Reynolds-stress contribution at . If is increased further, Maxwell stresses dominate the turbulent angular momentum transport, and for Reynolds stresses become negative and act as to counteract the outward transport by Maxwell stresses. Thus, marks the border between inertial-wave turbulence (excited by the imposed magnetic field) and turbulence arising from magnetocoriolis waves, i.e. the usual MRI for which magnetic stresses prevail. This result is in agreement with our eigenmode analysis and the work of Gellert et al. (2016), who compared magnetic and kinetic energies and found them equal at . They considered so-called Chandrasekhar states, where magnetic and velocity fields have the same radial profiles (unlike here) in the similar range of .
The evolution of stresses with for the quasi-Keplerian case () is shown in Fig. 6b. Because the flow is only unstable for , here Maxwell stresses dominate directly from onset. Thereafter, the behavior is identical to that for rotation close to the Rayleigh line. Returning to the torque scaling of the form shown in Fig. 4c, one observation can be made. All data with pre-factor is for (magnetocoriolis wave), whereas the scaling with constant pre-factor is in the regime (magnetically excited inertial wave). Further, the data for and , spanning , appears to feature a transition from one type of scaling to the other as increases (see Fig. 4a), which also corresponds to the change in dominant eigenmode (see Fig. 3). Hence we conclude the crossover in transport scaling occurs at .
6 Estimation of from torque
In Taylor–Couette flow, angular momentum transport is exactly quantified by the torque, yet in the context of accretion-disk theory it is customary to use the -parameter to quantify transport. In this section, we estimate from our torque data. Our simulations show that the turbulent part of the torque is proportional to modified Reynolds number:
[TABLE]
where
[TABLE]
After inserting (16) in equation (15) the expression for reads as
[TABLE]
Considering from (5) and we find that scales as:
[TABLE]
and when :
[TABLE]
Thus, effective viscosity is independent of for and scales as for .
For near Rayleigh-line rotation at the turbulent torque scales with . Inserting , and from (5) into (18) we get a lower bound for in the limit of :
[TABLE]
corresponding to the inductionless case. At the highest value for is attained. In the case of quasi-Keplerian rotation, , equation (5) gives and increases by a factor of when compared to near Rayleigh-line rotation.
Here we must caution that in Taylor–Couette flow, because of the presence of the solid cylinders bounding the fluid, turbulence modifies the mean velocity profile. Thus, the parameter in equation (18), estimated from the mean turbulent velocity, will depart from ideal values and at first will typically grow with . In our simulations, calculated in the middle of the gap between cylinders changes, but always remains negative. As turbulence becomes fully developed, appears to saturate at around , which is a (more) hydrodynamically stable velocity profile, unstable to MRI. This saturation implies independence of in regime. The key feature of the flow here is the proportionality to of the outward turbulent transport of momentum; using the turbulent estimate simply results in values of a factor of higher, as seen from equation (15). Finally, we speculate that even if the mean flow profile were forced to remain unchanged (quasi-Keplerian), this scaling may remain unaffected, as recently observed in DNS of self-sustained quasi-Keplerian dynamos in Taylor–Couette flow (Guseva et al., 2017b).
7 Discussion
We have performed a comprehensive study of the azimuthal MRI in Taylor–Couette flow for wide range of parameters and up to . Two distinct velocity profiles were considered, namely quasi-Keplerian () and almost-constant specific angular momentum (). Our linear stability analysis and direct numerical simulations highlight the relevance of the magnetic Reynolds number in determining the radial transport of angular momentum. For , regardless of rotation profile, the flow is unstable to the usual MRI. Transport is governed by Maxwell stresses and scales as , so that , consistent with Rüdiger et al. (2015). At we found at . Hence in highly ionized disks or disk regions, the AMRI may be a vigorous source of angular momentum transport. At low , instability is found only for steep profiles very close to the Rayleigh-line. Here the flow is unstable to the inductionless MRI for hydrodynamic Reynolds number , transport is governed by Reynolds stresses, scales as and is weak with .
The ratio of Maxwell to Reynolds stresses is solely determined by and increases from zero to one as is increased. This is in agreement with Meheut et al. (2015), who performed shearing-box simulations of MRI turbulence at two magnetic Reynolds numbers and , while varying either . At each they found a constant, but different, ratio of Maxwell to Reynolds stress both for azimuthal and axial magnetic fields, with Maxwell stresses growing with .
Our results are in line with the linear analysis of Kirillov & Stefani (2010) for the MRI with imposed helical magnetic fields. They identified the inductionless instability close to the Rayleigh line as a magnetically destabilized inertial wave, whereas the usual MRI can be interpreted as arising from an unstable magnetocoriolis wave (Nornberg et al., 2010). In addition, Kirillov & Stefani (2010) showed that the transfer of instability between the two modes was continuous. Our data support also a similar scenario for the AMRI: for and a continuous transition between the two types of turbulent flow can be observed as increases. Thus we suggest that the dependence of scaling type on shall also apply to MRI in the presence of helical magnetic fields. Future liquid metal experiments planned by Stefani et al. (2017), aiming at , should confirm the crossover between the two flavors of MRI and transport scalings shown here.
This research was supported in part by the National Science Foundation under Grant No. NSF PHY-1125915. Support from the Deutsche Forschungsgemeinschaft (grant number AV 120/1-1) and computing time from the Regional Computing Center of Erlangen (RRZE) and the North-German Supercomputing Alliance (HLRN) are greatfully acknowledged.
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