Radial Current and Rotation Profile Tailoring in Highly Ionized Linear Plasma Devices
E. J. Kolmes, I. E. Ochs, M. E. Mlodik, J.-M. Rax, R. Gueroult, and N., J. Fisch

TL;DR
This paper explores how to control electric field profiles in rotating magnetized plasmas by analyzing radial currents arising from inertial and viscous effects, enabling tailored plasma behavior.
Contribution
It introduces a theoretical framework for calculating the irreducible radial current in rotating plasma cylinders considering inertial and viscous mechanisms.
Findings
Radial current depends on rotation frequency and plasma profiles.
Expressions suggest new methods for electric field profile control.
Potential for improved plasma device performance.
Abstract
In a rotating magnetized plasma cylinder with shear, cross-field current can arise from inertial mechanisms and from the cross-field viscosity. Considering these mechanisms, it is possible to calculate the irreducible radial current draw in a cylindrical geometry as a function of the rotation frequency. The resulting expressions raise novel possibilities for tailoring the electric field profile by controlling the density and temperature profiles of a plasma.
| Parameter | Definition |
|---|---|
| Parameter | Definition | Interpretation |
|---|---|---|
| Particle Outflow | ||
| Current | ||
| Inertia / Viscosity |
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††thanks: Co-first author††thanks: Co-first author
Radial Current and Rotation Profile Tailoring in Highly Ionized Linear Plasma Devices
E. J. Kolmes
I. E. Ochs
Department of Astrophysical Sciences, Princeton University, Princeton, New Jersey, USA
M. E. Mlodik
Department of Astrophysical Sciences, Princeton University, Princeton, New Jersey, USA
J.-M. Rax
Université de Paris XI - École Polytechnique, LOA-ENSTA-CNRS, 91128 Palaiseau, France
R. Gueroult
LAPLACE, Université de Toulouse, CNRS, INPT, UPS, 31062 Toulouse, France
N. J. Fisch
Department of Astrophysical Sciences, Princeton University, Princeton, New Jersey, USA
Abstract
In a rotating magnetized plasma cylinder with shear, cross-field current can arise from inertial mechanisms and from the cross-field viscosity. Considering these mechanisms, it is possible to calculate the irreducible radial current draw in a cylindrical geometry as a function of the rotation frequency. The resulting expressions raise novel possibilities for tailoring the electric field profile by controlling the density and temperature profiles of a plasma.
I Introduction
In many technologies that rely on rotating plasmas,Lehnert (1971) the cross-field conductivity is of great practical concern. Usually, the rotation is produced by imposing an electrical potential difference perpendicular to a magnetic field; the resulting fields and power dissipation depend critically on the plasma conductivity. However, a large cross-field conductivity drives up the cost of maintaining rotation. For instance, the viability of mass filters based on rotating plasmas as a replacement for chemical separation techniques is partly dependent on power efficiency.Hellsten (1977); Ohkawa and Miller (2002); Fetterman and Fisch (2011); Gueroult et al. (2015, 2018); Zweben et al. (2018) Other examples include fusion schemes that rely on rotating plasmas,Bekhtenev et al. (1980); Ellis et al. (2001); Fetterman and Fisch (2008); Kolmes et al. (2018); Rax et al. (2017) where the efficiency is similarly limited by the cross-field conductivity.
In some of these applications, it is required to have very specific control over the rotation profile (i.e. the shear). Achieving this control is a nontrivial problem; past efforts in linear devices have often focused on biasable annular end electrodes.Tsushima et al. (1986); Shinohara et al. (2001); Zhou et al. (2012); Schaffner et al. (2012); Gueroult et al. (2016); Desjardins and Gilmore (2016); Jin et al. (2019); Poulos (2019) Another possibility is through waves, or stationary perturbations,Fetterman and Fisch (2010) though this has not yet been attempted experimentally.
A recent paper by Rax et al.Rax et al. (2019) analyzed the cross-field conductivity in a plasma undergoing solid-body rotation. The present paper addresses general rotation profiles, supplementing Rax et al. Rax et al. (2019) as well as previous considerations of plasma conductivity in a rotating plasma with general rotation profiles, where the effects of shear have also been addressed.Helander and Sigmar (2002); Rozhansky (2008) In particular, we find that sheared rotation modifies the form of the inertial conductivity discussed by Rax et al. and results in additional viscosity-dependent effects. Importantly, the radial current calculation presented here suggests that control over the radial temperature profile could help to control the rotation profile even without the use of end electrodes.
The paper is organized as follows: In Sec. II, we derive the basic drift equations for ions and electrons in a rotating plasma. We then proceed to order terms based on smallness parameters. The two smallness parameters rely on the ion-electron collision frequency and the plasma rotation frequency being small compared to the gyrofrequency. We also assume that radial pressure gradients are small compared to the radial electric forces. In Sec. III, we write the governing equations of the system in nondimensional form and identify the dimensionless parameters that determine their behavior. In Sec. IV, we identify the contributions to the radial current arising from plasma viscosity, inertia, and particle sources, respectively. We apply these relations in Sec. V to show how sources and sinks might be used to control the rotation profile. In Sec. VI, we compare the results derived here to previous derivations in the literature, and we discuss how alternate viscosity models, for example those used to describe rotating turbulent plasma, might be incorporated. In Appendix A, we provide two derivations of the Braginskii viscosity components in a rotating plasma.
II Classical Cross-Field Conductivity in a Rotating Plasma with Shear
Consider the two-fluid momentum equations for a plasma with a single ion species of charge and mass :
[TABLE]
Here is the electron mass, are the scalar pressures, are the viscosity tensors, and and are the ion-electron and electron-ion friction force densities. If there are sources or sinks of sinks of charged particles (corresponding e.g. to neutral ionization), their source rates are denoted by and the velocities of the particles being added or removed are denoted by . Using the density continuity equation, the LHS of Eqs. (1) and (2) can be rewritten as
[TABLE]
where is the advective derivative .
Eqs. (1) and (2) can be rearranged, after taking the cross product with on both sides, to get expressions for the components of that are perpendicular to :
[TABLE]
[TABLE]
where and . Starting from the left, these flows are the drift, the diamagnetic drift, the viscosity drift, the frictional drift, the polarization drift, and a drift due to particle injection whose physical origin is analyzed in Sec. IV.3. If , the friction force densities are:Braginskii (1965)
[TABLE]
where and are the ion-electron and electron-ion collision frequencies.
Consider an axisymmetric plasma with , , and all gradients in the direction. In steady state, the velocities in the and directions can be written as
[TABLE]
and
[TABLE]
where the prime denotes a derivative with respect to . The bracketed part of the denominator of Eq. (8) and the last two terms of Eq. (9) come from the advective part of the total derivative , and correspond to the fictitious forces in a rotating frame.
In a strongly magnetized plasma, the ion-electron collision frequency is much smaller than the ion gyrofrequency, so is a small parameter. In many rotating plasmas of interest, the ratio of the rotation frequency to the gyrofrequency is also small. Consider a double ordering in and , similar to the one used by Spitzer,Spitzer (1952) where we denote a term of order by the tuple , as in .
Assume that . This assumption is convenient, and it is reasonable in many cases,Lehnert (1971); Rax et al. (2017) but an analogous calculation can be carried out for a stronger or weaker pressure force. It will also be useful to pick an ordering for the viscous forces. This will be discussed in greater detail later on, but for now, take the component of to be and the component to be . Finally, since the continuity equation suggests for a characteristic scale length , it makes sense to order . This will end up being .
To zeroth order in and , Eq. (8) requires that and vanish and Eq. (9) gives that the azimuthal motion is determined by the drift:
[TABLE]
The next order in includes the diamagnetic drift and an drift associated with the centrifugal force and evaluated using :
[TABLE]
Eq. (11) can be used to get the leading-order nonvanishing radial velocities from the general expression in Eq. (8):
[TABLE]
and
[TABLE]
This velocity, together with the steady-state continuity equation, governs classical particle transport: At this order, there are radial drifts due to azimuthal friction, but they are ambipolar in the sense that they do not produce net radial current, only a net radial mass flow.
To the next order in , the radial motion is
[TABLE]
The first term on the RHS of Eq. (14) is the non-ambipolar radial motion resulting from the interplay between frictional and inertial effects; intuitively, it is the Coriolis drift that results from the next-lowest order radial flow. The second term is the from the azimuthal viscous force. The third is an effective due to the momentum flux from particle sources and sinks. The last — which will not produce net charge transport at this order — is an ambipolar frictional flux resulting from higher-order corrections to , including those due to . The expression is the difference between the ion and electron azimuthal flows of .
It is necessary to verify, since the relative size of and has not been specified, that the current is not sensitive to this ordering. and vanish for all since there are no radial flows that could compete with in the inertial part of Eq. (14). There could conceivably be other orders contributing to the in Eq. (14), but the resulting flows do not contribute to the leading-order current or particle flux anyway.
Moreover, no term other than will produce the leading-order current. When constructing a non-ambipolar radial flow, one factor of is needed to produce any differential azimuthal motion and a second factor of is needed to make the drift due to in Eq. (8) not be intrinsically ambipolar. Without one factor of , there is no friction force to begin with. As such, there is no need to worry about competition from, e.g., or radial flows; the leading-order current comes from the motion described by Eq. (14).
With that in mind, the current can be written as
[TABLE]
So far, the generalization of this calculation to the case of multiple ion species would largely be trivial; the friction would have to include interactions between all pairs of species, and the thermal friction takes a slightly different form for particles of general mass, but otherwise the calculation would be the same. However, it is possible to simplify in the case of a single ion species by making use of the small mass ratio. Dropping anything of , and defining , Eq. (15) is
[TABLE]
This can be separated out into several terms, with different scalings and behaviors, as we will discuss in the next section.
III Conservation Equations and Nondimensionalization
In order to relate our sources of charge and current to the density, temperature, and rotation profiles in the system, we use the particle and charge conservation equations. In a cylindrically symmetric system, in the limit where axial losses and gradients are small compared to their radial counterparts, these are given by:
[TABLE]
Integrating, we obtain
[TABLE]
where we have defined the integrated source functions
[TABLE]
In order to understand the relationships between the different current terms, it is useful to introduce a number of dimensionless parameters. To that end, let be the radial device size, be the on-axis field strength, and , , and be a characteristic density, temperature, and Braginskii perpendicular viscosity (discussed in the next section) respectively. Define the frequencies
[TABLE]
Here and are Coulomb logarithms. Note that is the only frequency here with radial dependence, as it represents a dynamical variable which will be solved for.
Finally, define the total integrated source rate for particles and charge , and . In terms of these constants, the total number of ions and charge per unit axial length added to or extracted from the system per unit time are and respectively.
This collection of parameters can be used to construct the normalized variables listed in Table 1. These variables are characteristically by construction (at least in the case of an approximately sonic flow, for ).
Substitution of these variables into the continuity Eq. (19) and charge conservation Eq. (20), using the velocity in Eq.(12) and the current in Eq. (16), as well as the Braginskii transport coefficients,Braginskii (1965) yields several dimensionless constants, listed in Table 2. These parameters determine the characteristic sizes of the relevant particle fluxes and currents in the systems, as a function of the typical gradients. They depend on the relation between the source terms (for particles) and (for currents), on the number of particles in a cylinder of area , and on the relevant collision frequencies.
In terms of these parameters, our nondimensionalized continuity equation becomes:
[TABLE]
Here, the RHS represents the charge added to the system, whereas the LHS determines the response of the system to the added charge. Because all tilde quantities (other than ) are , the dimensionless constant determines the strength of the system response. If the normalizations are chosen appropriately, if the flow is not substantially supersonic, and if the gradient scale lengths of the various parameters are not small compared to , then Eq. (28) implies that is not larger than . This means that we cannot drive fluxes that are too large through our system without creating extremely large gradients, which will likely lead to instabilities and anomalous transport. Thus, mathematically formalizes the requirement for smooth, stable solutions with device-scale gradients.
Current conservation takes a similar form:
[TABLE]
We will explore each of these terms in detail; the final result is in Eq. (43).
IV Physical Mechanisms of Cross-Field Current
The various terms in Eq. (29) describe cross-field currents that come from three distinct physical mechanisms. The following subsections discuss their physical origins and relative sizes.
IV.1 Viscous Current
The viscous current is a radial drift resulting from the azimuthal viscous force (see Figure 1):
[TABLE]
If is the Braginskii viscosity,Braginskii (1965) then keeping the contributions from the leading-order flow ,
[TABLE]
where the relevant viscosity coefficients are
[TABLE]
The mass dependence in these coefficients means that it is generally safe to set .
The azimuthal viscous force results in a radial drift, which carries ion current. This current has the behavior one would intuitively expect from a viscosity: it acts to relax shear in the flow. It is somewhat suppressed because it is a collisional finite-Larmor-radius effect. The radial viscous force comes from the gyroviscosity. Its form is very similar to that of its azimuthal counterpart, but (perhaps counterintuitively) it is substantially larger — in the case of the ions, by a factor of . Its contribution to is nonetheless small compared to the contribution of the azimuthal viscous force, since the current associated with this large azimuthal effect is ordered down by a factor of from the original azimuthal drift, as discussed in the next section. In other words, is more important for conductivity calculations because its flow is non-ambipolar to start with, whereas can only drive current indirectly through inertial effects.
In terms of dimensionless variables, the viscous current can be written as
[TABLE]
When using the Braginskii viscosity, define and . There are two classes of rotation profile that make the viscous current vanish. The first consists of any solid-body rotation profile. This is straightforward; without shear, the viscous force vanishes. The second class of profiles can be defined by
[TABLE]
for any constant . These profiles are closely related to the irrotational vortices often found in neutral fluids. The intuition behind Eq. (36) is much the same: there is viscous stress everywhere, but that stress produces no net force on any particular fluid element away from the origin, where these profiles are generally not physical (see, e.g., Kundu, Cohen, and DowlingKundu et al. (2016)).
IV.2 Inertial Current
The inertial current can be written as
[TABLE]
Physically, this current can be explained in terms of a series of drifts. Temperature gradients and differences in the centrifugal and diamagnetic drifts between species (, Eq. (11)) produce a -directed friction between species. This friction force leads to a radial drift (, Eq. (12)). This initial radial flow does not carry net current, but the motion results in an azimuthal Coriolis force, which depends on mass and therefore affects the ions far more than the electrons. The associated with this Coriolis force is the flow which carries the leading-order radial current. This sequence of effects is shown in Figure 2.
In the limit where is constant and where particle injection effects can be neglected, the inertial current is the only current. If, in addition, the densities and temperatures are constant, the current can be written as
[TABLE]
This expression is equivalent to the nonlinear Ohm’s law described by Rax et al. Rax et al. (2019)
In terms of dimensionless variables, the inertial current can be written
[TABLE]
The inertial current vanishes wherever . The Coriolis force can be understood as a mechanism that enforces the conservation of angular momentum during radial motion; these profiles have flows with uniform angular momentum, so it makes sense to find that they do not have Coriolis drifts.
IV.3 Particle Injection Current
In a region where there are particle sources or sinks, there is an additional current:
[TABLE]
term comes from the momentum injection due to sources and sinks and the term is inertial in the sense that it comes from the left-hand side of Eqs. (1) and (2).
However, this current can be explained more intuitively in terms of single-particle dynamics.Goertz (1980); Rozhanskii (1990); Rozhansky (2008) Consider a particle placed in crossed and fields with some initial velocity and position . In the limit of locally constant fields, it will gyrate about an -coordinate that is shifted from its initial position:
[TABLE]
Thus, there will be a current resulting from the fact that particles move from their initial to their average position as they are added to the system, which results in Eq. (40). When , this has been termed the “pickup current” Goertz (1980) or “mass-loading current”.Rozhanskii (1990); Rozhansky (2008)
This current can be written in terms of dimensionless parameters as
[TABLE]
The dependence on follows from the reliance of this mechanism on the local value of .
IV.4 Comparing the Currents
Substituting in the expressions for the components of , Eq. (29) becomes:
[TABLE]
is
[TABLE]
and is
[TABLE]
Eq. (45) gives some insight into the relative sizes of the different currents. Depending on, for instance, the shape of , any of the mechanisms can be dominant. However, suppose that all gradient scale lengths are on the order of . Recall that, in many cases, . When the currents are written in terms of dimensionless quantities, the inertial and particle injection currents are attached to a prefactor of , which is small compared to 1. If is also small compared to 1, then any current may dominate. If , then the viscous current likely dominates. If is large compared to 1, then the aforementioned assumption about the gradient scale lengths is probably invalid.
We can estimate the total current drawn by the machine by balancing the two sides of Eq. (45), yielding , and solving for . This gives
[TABLE]
so
[TABLE]
V Calculating Rotation Profiles from Ohm’s Law
In a system with defined sources and sinks of charged particles, the steady-state total current through the system can often be written easily in terms of those sources and sinks. That information, combined with the appropriate Ohm’s law, can be used to extract other useful information about the system.
Suppose the particle sources and sinks are known, so that and are specified. Suppose the particle sources have . Invoking Ohm’s law and the continuity equations and simplifying,
[TABLE]
This has a general solution for :
[TABLE]
for a boundary condition imposed at .
For example, suppose were constant in space and . For some , suppose and . Then
[TABLE]
The case of uniform volumetric particle injection is given by . The case in which all particles are injected at is given by . Note that
[TABLE]
consistent with the intuition from Section III.
Now consider a scenario in which , , and have arbitrary shapes but where is not much larger than . In this case, the orderings described in Section II come out slightly differently; if the ambipolar flow is not much larger than the non-ambipolar flow, then the inertial current will be small compared to the viscous current. For example, if the system has a radial flow of electrons but no net flow of ions, then (using the same boundary condition as before)
[TABLE]
and
[TABLE]
There are practical contexts in which it is important to control the rotation profile . For example, the double well mass filter concept relies on a rotating plasma with a particular shear profile.Gueroult et al. (2014) It may be possible to control shear with end electrodes, but the calculations in this section suggest an additional strategy: that the viscosity, temperature, and particle input profiles can be used to control . Viscosity depends on the density and temperature profiles as ; there may be contexts in which these are easier to manipulate than the electric field itself.
Suppose some sufficiently sophisticated heating system could be used to specify . Then Eqs. (28), (33), and (49) determine , , and . Figure 3 shows several numerical solutions in the case of uniform particle and charge injection ( and ). If a particular were desirable, it might be possible to tailor to get that profile.
However, there are limits to what can be done with alone. To see this, consider the following expression, which follows from Eq. (48):
[TABLE]
For instance, if is to change sign at without becoming singular, must be equal to . In fact, for the simple volumetric sources used in Figure 3, it is possible to show analytically that all solutions for must be monotonic. Nonetheless, even for this very simple choice of sources, an experimentalist with good control over could achieve a wide range of density and rotation profiles.
VI Discussion and Summary
We described the motion of charge across magnetic field lines in a sheared rotating system and offered physical descriptions of the key terms in our derivation. We also suggested that sufficient control over the temperature and density profiles should allow control over the rotation profile .
Note that the form of Ohm’s law presented here can be related to expressions in a number of places elsewhere in the literature. Rax et al. Rax et al. (2019) analyzes a case which does not include shear. Their expression for Ohm’s law includes an inertial current consistent with the one derived here, but because they studied solid-body rotation they do not include the viscous current. The review by Rozhansky Rozhansky (2008) includes expressions for the viscous and mass-loading currents that agree with the ones derived here. He discusses inertial currents in general, but does not derive the Coriolis-driven inertial current that appears in a rotating plasma. The current edition of the book by Helander and Sigmar Helander and Sigmar (2002) includes a nice derivation of the inertial current, but their treatment of the viscosity (in the case of an axisymmetric rotating plasma) does not agree with the one presented here, essentially because of a mismatch between Eq. (31) and their Eq. (5.12). The derivation of Eq. (31) is given in the Appendix.
Other treatments of this problem have generally not considered the gyroviscosity, which produces as per Eq. (32). In many situations, this is not a major problem. After all, for the ordering used in this paper, does not contribute to the leading-order current despite the fact that it is substantially larger than . Nonetheless, there is some value in being aware of this term. For instance, for a plasma approaching the Brillouin limit, will no longer be small and the gyroviscous will no longer necessarily be suppressed relative to (though the form of the viscosity tensor might need to be revisited in that limit).
This derivation was done for a quiescent plasma. However, some models for anomalous transport provide prescriptions for alternate forms of the viscous force density . To the extent that the rest of the bulk behavior of the plasma is unchanged, it is possible to substitute alternate viscosities into results like Eq. (16) or Eq. (49) to understand how to control current flow or rotation profiles in turbulent regimes.
A number of authors have written about models in which (in an appropriate regime) anomalous transport produces something that looks like cross-field classical transport but with a higher effective collision frequency.Artsimovich (1971); Finn et al. (1992); Rognlien and Ryutov (1999) Rognlien and Ryutov called this “pseudoclassical transport”.Rognlien and Ryutov (1999)
Finn, Guzdar, and Chernikov studied cross-field transport for the case of stochastic field lines.Finn et al. (1992) Their work suggested a viscosity coefficient
[TABLE]
Here is the magnitude of the non-axisymmetric field fluctuations, is the turbulent correlation length (often the connection length), and is the sound speed. There are laboratory observations in which this viscosity model appears to accurately describe momentum transport.Almagri et al. (1998) In such a case, Eq. (49) describes how reacts to the suppression or increase of turbulence.
There is no guarantee that an anomalous viscosity should respect the same ordering as the Braginskii viscosity, either for or . If either of these is very large, then the expression for the inertial current might need to be reconsidered.
There are a number of other contexts in which the cross-field conductivity described in this paper would have to be modified. Cross-field dynamics can turn out quite differently in plasmas with significant ion-neutral collisions, weak magnetization, or more complicated geometries.Bonnevier (1966); Lehnert (1973); Hazeltine and Meiss (1992); Rozhansky (2008); Meier and Shumlak (2012); Rax et al. (2015); Ochs et al. (2017); Zweben et al. (2018); Poulos (2019); Jin et al. (2019) In the regime where this calculation does apply, it suggests some novel techniques with which the rotation profile might be controlled. Neutral beams, pellet injection, and electron injection can help shape the rotation profile by changing and . Moreover, charge transport is substantially temperature-dependent, so heating or cooling particular regions of the plasma can change . These techniques might be used either in place of more conventional techniques for rotation control or as a supplement to them.
Acknowledgements.
This work was supported by NNSA 83228-10966 [Prime No. DOE (NNSA) DE-NA0003764], and by NSF PHY-1506122. One author (IEO) also acknowledges the support of the DOE Computational Science Graduate Fellowship (DOE grant number DE-FG02-97ER25308).
Appendix A The Braginskii Viscosity in a Rotating Plasma
This paper uses Eqs. (31) and (32) for the components of when . This appendix will present two approaches to calculating these components from Braginskii’s viscosity expression,Braginskii (1965) which was originally given in Cartesian coordinates.
A.1 Viscosity in Arbitrary Orthonormal Coordinates
When we wish to include viscous effects while working with curvilinear coordinates, we encounter a problem: Braginskii’s viscosity tensor (Eqs. (4.41) and (4.42)) is not expressed in a coordinate-invariant way, although the later, low-flow-ordered transport equations relevant to tokamak physics included more adaptable expressions.Mikhailovskii and Tsypin (1984); Catto and Simakov (2004); Simakov and Catto (2004) This part of the Appendix will express the original Braginskii viscosity in a tensorial way that is easy to adapt to many coordinate systems.
We will start by reviewing the original form of the Braginskii viscosity matrix. The proper covariant expression should then be the tensorial expression which reduces to this expression. Finally, we will explain how our results provide an easy recipe to calculate the Braginskii viscous force in an arbitrary orthonormal coordinate system.
Our notation will follow, e.g., Carroll’s book on general relativity.Carroll (2004) Thus the covariant derivative is denoted
[TABLE]
Here, is the Christoffel symbol, given by
[TABLE]
In addition, we will adopt the convention of using to refer to the conventional (orthonormal-basis) velocity, and to refer to the generalized velocity, which is a proper (contravariant) vector in the appropriate coordinate basis. This will be important in the direction in cylindrical coordinates, since
[TABLE]
Whether we write with an upper and lower index has no significance; however, an upper vs lower index on denotes a different object (vector vs. one-form). For a diagonal metric, these quantities are related by
[TABLE]
Similarly, we will adopt the convention of using to refer to the orthonormal magnetic field unit vector, and to refer to the contravariant vector.
The Braginskii viscosity matrix is given by:Braginskii (1965)
[TABLE]
where
[TABLE]
Here, is the th component of the magnetic field unit vector, is the Kronecker delta, is the Levi-Civita symbol, , and is Braginskii’s traceless rate-of-strain tensor, given by
[TABLE]
In the above definitions, repeated indices are summed over, even if they do not appear in upper-lower pairs. (Note that, in contrast to Braginskii, we have moved the matrix label for the to the left hand side of the symbol, to make it clear that this is not a tensor index, but rather a label to a specific tensor.)
Now we need to find the covariant generalizations of the various quantities that appear in Eqs. (62-67). Make the substitutions
[TABLE]
where is the Levi-Civita tensor (rather than symbol), defined by
[TABLE]
This implies that will become . It will be convenient to define a tensor (following the notation from KrommesKrommes (2018)) by
[TABLE]
Making these substitutions, and raising indices where necessary (since only an up-down pair of indices can be summed over), Eqs. (62-67) become
[TABLE]
and
[TABLE]
Eqs. (61) and (75-80) completely define the viscous stress tensor, in a manifestly covariant way.
Now that we have the stress tensor, we can calculate the viscous force. The generalization of the tensor divergence is again given by the covariant derivative. Let be the conventional force vector, and be the force vector in covariant notation. Then
[TABLE]
where
[TABLE]
Our conventional vector components are finally given by converting this back from a contravariant vector (noting that is diagonal by assumption):
[TABLE]
This gives a clear prescription for calculating the viscous force in an arbitrary coordinate system. The sums can be carried out fairly straightforwardly in a symbolic math language such as Mathematica.
Start with the metric that defines the coordinate system, and construct the inverse metric . 2. 2.
Construct the Christoffel symbols via Eq. (57). 3. 3.
Convert velocity vectors and magnetic field vectors to covariant one-forms and via . 4. 4.
Construct the viscosity tensor given by Eqs. (61) and (75-80). Indices are raised and lowered by applying the metric and inverse metric, e.g. . 5. 5.
Calculate the contravariant force according to Eq. (82). 6. 6.
Convert the force back to orthonormal coordinates via .
This method was used to calculate the viscous forces used in the text, using the metric for a cylindrical coordinate system:
[TABLE]
In the next section, we explicitly calculate the forces in an alternate way, by converting the velocity vectors to Cartesian coordinates for substitution into the original Braginskii viscosity matrix. The results agree.
A.2 Calculation in Cartesian Coordinates
A straightforward way of calculating and directly from Braginskii’s result is to first compute the Cartesian components of and then to convert the result to cylindrical coordinates. In this section we will use index notation but assume a Cartesian coordinate system. Braginskii has
[TABLE]
and
[TABLE]
If , then
[TABLE]
and , so
[TABLE]
Then we can evaluate the components of . Let . Note that is sometimes used elsewhere to denote the vorticity ; these are equivalent in the case of solid-body rotation, but not for general rotation profiles.
[TABLE]
The necessary derivatives of these components are
[TABLE]
[TABLE]
[TABLE]
[TABLE]
The components of can be written as:
[TABLE]
and
[TABLE]
All that remains is to evaluate these.
[TABLE]
[TABLE]
Then in cylindrical coordinates,
[TABLE]
[TABLE]
The azimuthal expression is the same as the radial expression, just exchanging with . It can be rewritten as
[TABLE]
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