A&A 471, 7-15 (2007)
DOI: 10.1051/0004-6361:20077413
M. Siewert - H.-J. Fahr
Argelander Institut für Astronomie der Universität Bonn, Abteilung f. Astrophysik und Extraterrestrische Forschung, Auf dem Huegel 71, 53121 Bonn, Germany
Received 5 March 2007 / Accepted 24 May 2007
Abstract
Aims. We attempt to describe kinetic properties of the solar wind termination shock (and similar MHD shocks in general) using the appropriate form of the kinetic Boltzmann equation, for arbitrary inclinations
between the magnetic field and the shock normal.
Methods. In order to understand the deviations from the perpendicular shock, for which we have already derived an exact solution in an earlier publication, we first prove that our current Boltzmann equation is unable to describe a stationary quasiparallel shock. To ease and open up further research, we derive conditions for the specific form of the relevant Boltzmann equation.
Results. We demonstrate that the simplest Boltzmann equation aiming to describe a parallel MHD shock is in conflict with the predictions from pure MHD. We identify several possible reasons for this, and likewise derive conditions based on the mass flow conservation which must be fulfilled for the shock to be stationary. Assuming that a model for (quasi-)stationary shocks does exist, we are able to explain the unchanged power law index at the passage of the solar wind termination shock observed by the Voyager 1 spacecraft in 2004. We also show that different dissipation mechanisms lead to different transition scales for perpendicular and parallel MHD shocks, and that these differences in the dissipation process also need to be included in the case-competent Boltzmann equation.
Key words: plasmas - shock waves - magnetohydrodynamics (MHD) - solar wind
Magnetohydrodynamics (MHD) is the most successful theory so far capable of describing astrophysical shocks, such as the solar wind termination shock, planetary bowshocks, or supernova shock waves. The shocks are usually described in the form of jump conditions, which are based on the conservation of certain flows of physical quantities, such as the mass flow, the momentum, and the energy flows (for more recent different model approaches concerning the multifluid properties of the solar wind termination shock see Zank et al. 1993; Chalov & Fahr 1995; Fahr & Scherer 2005; Chalov & Fahr 1994; Zank 1999; Chalov & Fahr 1996). For a magnetized plasma, the jump conditions are usually used in the form given by Serrin (1959), Zel'dovich & Raizer (1966), Landau & Lifshitz (1977) or Diver (2001). However, there are several problems with the MHD treatment of the shock. First and foremost, this approach only works for collision-dominated shocks, guaranteeing an effective equilibrium of the distribution functions. But there are many kind of shocks where this condition is not fulfilled, such as solar wind bowshocks found near astrophysical objects (comets or planets), shocks forming in corotating interaction regions, traveling interplanetary shocks, or the heliospheric termination shock.
Another, less popular problem related to the MHD treatment of astrophysical
shocks is the fact that the jump conditions for the lower moments
of the distribution function are underdetermined,
which means that there remains one variable that cannot be determined
by the set of jump conditions alone. Usually, this
variable is selected to be the downstream pressure anisotropy,
,
since in most physical situations,
the dependence of the system on this parameter is very weak
(see, e.g. Erkaev et al. 2000). Nevertheless, the MHD description of a shock
transition is not complete; in particular the dissipation mechanisms
producing entropy are not specified. Even without going into
too much detail, it is well known that a full understanding of
such processes requires the knowledge of the full upstream
and downstream distribution functions, including its dependence
upon time and position, which is clearly not provided by a simple set of MHD jump
conditions (or, for that part, MHD itself, where the distribution function
is reduced to a few low-order velocity moments, while only the knowledge
of all these moments is equivalent to a distribution function.
In addition, recently, several spacecraft missions have provided us with directly measured data of the immediate upstream and downstream distribution functions around several astrophysical shocks. The Voyager 1 spacecraft took data on the solar wind termination shock (Stone et al. 2005; Burlaga et al. 2005; Gurnett & Kurth 2005; Decker et al. 2005), observing power law spectra with identical power law indices on both sides of the transition region (Cummings et al. 2006). The Cluster mission consists of four identical spacecrafts able to observe the dynamics of the terrestrial bowshock on a much larger scale (Escoubet et al. 1997); observations from these satellites hint that the shock is highly nonstationary (see e.g. Lobzin et al. 2007).
While numerical simulations are, in principle, able to model such systems with rather high accuracy using shock simulation calculations within hybrid or full particle codes (e.g., see Hada et al. 2003; Scholer et al. 2003), these simulations are, nevertheless, numerical, which makes understanding the physics beyond the results somewhat difficult. In many situations, these simulations, especially in case of quasiparallel shocks, do not show a regular shock shape, but a highly irregular profile. This is, in principle, in good agreement with Cluster observations; however, there are no theoretical, physical explanations for these results yet (Lobzin et al. 2007).
Recently Krasnoselskikh et al. (2002) have investigated the non-stationarity
of strong collisionless quasiperpendicular shocks and thereby have compared
available theoretical results with full particle numerical simulations. They
have proposed an analysis of the shock stationarity based on the theory of
nonlinear waves. As it turns out, for those shocks with supercritical Mach
numbers the region, where an abrupt increase of the magnetic field occurs, can
be treated as a nonlinear whistler wave of large amplitude. They show that
beyond some linear whistler Mach number MA,w no stationary linear wave
trains can survive in the shock precursor, i.e. stand still ahead of
the field ramp, but are swept into the ramp and pile up there to form a
strongly nonlinear whistler wave. This critical Mach number is found by the expression
![]() |
(1) |
In face of these difficulties, we have recently developed a completely different approach, based on kinetic equations (Fahr & Siewert 2006), aiming to describe the solar wind termination shock, although our results should offer considerably more application opportunities. Especially, our approach should be able to cross the gap between a numerical treatment of many particles in a box, where one is always in danger of overemphasizing numerics over physics, and the MHD treatment, which may be insufficient in face of highly nonstationary processes, as hinted in numerical simulations (Hada et al. 2003; Scholer et al. 2003).
So far, we have successfully applied our model to close the set of anisotropic jump conditions for the purely perpendicular shock, suggesting that our approach leads to physical results. In addition, our approach should prove useful as a test case for numerical codes aiming to simulate the creation and behavior of astrophysical shocks. (Of course, these simulations do likewise present a possibility to test our kinetic approaches.)
While the perpendicular shock leads to a simple and analytic relation between the upstream plasma and the downstream plasma (see Eq. (6)), up to now, for an arbitrary inclination between the magnetic field and the plasma flow, we were unable to arrive at a physical downstream distribution function. In this paper, we greatly expand our previous analysis of the parallel shock, and obtain an improved description of the physics which one has to respect when aiming to understand quasiparallel shocks in astrophysical plasmas.
In a recent paper (Fahr & Siewert 2006) we have derived the Boltzmann equation
for the distribution function
of a
collisionless magnetized plasma crossing an MHD shock,
where
are the velocity components of the individual
plasma particles parallel and perpendicular to the magnetic field.
The equation is written in the accelerated reference
frame co-moving with the bulk velocity
,
and s is
the streamline coordinate in the direction of the shock normal.
In the most simple configuration, when only the deceleration of
the ions across the shock is considered, the Boltzmann equation takes the form
An alternate approach is to multiply this equation by parallel and
perpendicular velocities, integrate over velocity space, and obtain
differential equations for the change of a few selected velocity
moments, which corresponds to the pure MHD treatment. However, in this
situation, as in common MHD, one is again faced with a hierarchy of
momentum equations which need to be closed. In addition, nonlinear
terms such as
introduce terms
which may no longer be identified with the usual MHD moments, complicating
the situation even further. For these reasons,
we now attempt to solve this equation analytically.
For a purely perpendicular shock (
),
where the subscripts 1 and 2 denote the upstream and downstream sides
of the shock, the Boltzmann equation reduces to
| aij,2 = x(1+i/2) aij,1, | (7) |
Unfortunately,
for the purely parallel shock, we encountered several technical problems
(Fahr & Siewert 2006), mainly
related to a singularity at
in
Eqs. (3) and (4),
which need to be interpreted and treated in a physical way.
For a purely parallel shock, the Boltzmann equation reduces to
Aiming to understand the parallel shock better, we now estimate
whether this configuration is the exception where our equation fails,
or if, perhaps, the perpendicular shock is the only configuration
where our equation works. In order to do this, we investigate the
quasi-perpendicular shock (
),
and develop the Boltzmann equation around
,
leading to
The second term on the RHS of Eq. (10) may be evaluated starting from the
general form of the Boltzmann equation (Eq. (2)), leading to
![]() |
(12) |
![]() |
(13) |
![]() |
(14) | ||
| (15) |
![]() |
(16) |
![]() |
(17) |
Taking these results together, we may write Eq. (10) in the form
In this analysis, we now also consider the Boltzmann equation in the non-accelerated rest frame of the standing transition region, which we derive now. This approach may be useful to estimate which terms in Eq. (2) are more "problematic'' than others. We would also like to note that, as we are working in the non-relativistic limit, the Boltzmann equation derived in the co-moving accelerated rest frame of the plasma stream should be qualitatively identical with the equation one would derive in the inertial rest frame of the shock transition region. In fact, most of the terms in the Boltzmann equation may be derived exactly in the same way as in Fahr & Siewert (2006), which means we only need to emphasize the changes.
In a more general form, the Boltzmann equation is written as
| (21) |
The electric field E(s) may be derived from the MHD equation of ion motion, which is given for a one-dimensional system in the form
![]() |
(23) |
![]() |
(24) |
![]() |
(25) |
![]() |
(26) |
![]() |
(27) |
![]() |
(28) |
![]() |
(29) |
To solve the Boltzmann equation for an arbitrary angle
,
we use the representation
![]() |
(31) |
| (34) |
To verify that the ansatz presented in Eq. (30) does not contradict earlier results,
we first demonstrate that the exact solution for the perpendicular shock
(Siewert & Fahr 2007),
![]() |
(35) |
![]() |
(37) |
Next, we investigate the purely parallel shock (
), where
the Boltzmann equation reduces to Eq. (9), which automatically leads to
| (38) |
Since our Boltzmann equation has been explicitly derived in the
co-moving accelerated MHD reference frame, the parallel velocity
moment,
![]() |
(40) |
| |
= | ||
| = | ![]() |
(41) |
| (42) |
![]() |
(43) |
Finally, we consider the almost perpendicular shock, i.e. just an infinitesimal step from the situation where our approach works. In this case, it automatically follows from Eqs. (19) and (32) that this Boltzmann coefficient describes a systematic deceleration of the upstream velocity distribution function away from the co-moving reference frame, on top of the implicit MHD deceleration at the shock.
To improve our analysis, we now repeat the arguments presented in
Sect. 3.2, taking the parallel Boltzmann equation
in the rest frame of the shock,
![]() |
(46) |
![]() |
(47) |
![]() |
(48) |
Is it at all possible, for a solution of an equation of the form (2), to find a combination of functions
and
which is not in conflict with MHD?
We now attempt to answer this
question by going deeper into the underlying mathematical
structures.
We begin with the most simple MHD jump condition, the mass flow
conservation,
| (49) |
Making the ansatz given by Eq. (30), we may write Eq. (50) in integral form,
We now need to estimate which coordinate transformations
are compatible with these relations. Considering that only the
upstream parallel velocity moment,
,
identically vanishes on account of the initial assumptions,
we require a linear relation between the parallel components,
![]() |
(56) |
This result already allows us to write the most general,
particle number conserving downstream ion distribution function as
Using the formalism developed in the previous sections, we
may now explain why
our Boltzmann equations seemingly conflicts with basic MHD. Inserting
Eq. (58) into Eq. (2), we obtain
| |
= | ![]() |
|
| = | |||
| = | ![]() |
||
| = | ![]() |
(60) |
![]() |
(61) | ||
![]() |
(62) |
Since
and
must not depend on
,
we automatically see that our Boltzmann coefficients given by Eqs. (54) and (57)
are only able to describe a simple
(i.e. not explicitly time-dependent, not turbulent, etc.)
MHD shock for
,
when the derived
coefficients ai do not depend upon w. For all other
magnetic field orientations, the singular factor clearly rules
out the required w-dependence.
Using the requirements derived in Sect. 3 for a
stationary MHD shock, we may now derive relations between the
upstream and downstrem MHD moments; repeating the
calculations done by Siewert & Fahr (2007), we obtain
![]() |
(67) |
Next, we would like to point out an interesting fact.
Taking Eq. (58),
and applying this to a power law distribution function,
![]() |
(70) |
![]() |
(71) |
In the last sections, we have demonstrated that two simple
physical principles, stationarity and mass flow conservation,
strongly restrict the Boltzmann coefficients in Eq. (2).
We now attempt to understand what kind of physical processes might
be compatible with these conditions. In order to do this, we first
note that, during the initial derivation of our Boltzmann equation
(Fahr & Siewert 2006), we obtained an equation of the form
![]() |
(72) |
![]() |
(73) |
Obviously, we need to understand the physical meaning behind the
LHS. Considering that Un is the normal bulk velocity of the plasma
flow, it is straightforward to interpret the entire term as
a differential bulk velocity, i.e. the entire "slice'' of
individual particles moving at
identical
(and arbitrary
)
is crossing the
shock with a differential velocity of
![]() |
(74) |
Furthermore, this analysis points towards another problem, namely the question of charge-neutrality. In MHD, this assumption is usually a requirement, although in many situations, electrons are left out of the analysis because of their small rest masses. This hints that the remedy for that situation must be to include electrons as a separate dynamical population. This is because only in case of the perpendicular MHD shock the system of the plasma bulk velocity is a preferred system, since here the perpendicular magnetic field controlling both the bulk motion of the ions and the electrons is just convected with this bulk velocity system. This causes bulk velocities of ions to be identical with that of electrons, which is no longer the case for non-perpendicular shocks. In the latter case, electrons react completely differently compared to ions to the electric fields inside the transition region. While these fields do decelerate the ions, leading to a very similar term in the Boltzmann equation than the pseudo forces appearing in the co-moving accelerated reference frame, electrons will be accelerated instead; considering the much smaller electron mass compared to the heavier ions, this acceleration should be much larger than the proton deceleration, perhaps even leading into the relativistic regime. This, however, enforces the need to also consider an independent Boltzmann equation for the electrons and, in addition, to couple the two Boltzmann equations for ions and electrons, by addition of adequate friction force terms.
Some general control on this two-population system for the parallel shock
(z-direction parallel to
)
is given by standard electrodynamic
requirements for this shock. From Maxwells
equation
,
we may conclude for the
1-dimensional shock that
![]() |
|||
| (75) |
| jz=e(neUe-npUp)=0, | (76) |
![]() |
(77) |
So far, we have made no specific assumptions on the fine structure of the shock transition region, partially on account of the fact that we have never truly required such assumptions yet. However, the nonstationarity of the shock clearly suggests that this simplification is no longer valid, and that we need to allow for an explicitly extended shock. In this section, as a preparation for further work, we present estimations on how thick the shock might be in the perpendicular and parallel situations.
Roughly spoken the extent of the collision-less shock transition is defined by the length needed in a shock-generated gradient structure to create enough entropy, and dissipate enough kinetic energy of the upstream flow into thermal energy of the downstream flow. The rate of entropy generation, however, strongly depends on the available mechanisms which can effectively work for such dissipations, with the available mechanisms in turn depending on the distribution function of the plasma.
Lee et al. (1986) have considered single ion trajectories through a planar
MHD structure in a test particle approach, by parameterizing
the planar perpendicular MHD shock by a shock scale
measured
in natural ion length units
(where U1 is
the upstream plasma bulk velocity, and
is the
ion gyrofrequency related to the upstream tangential field component
Bt1). They have found that, for a strong shock (i.e.
), the gyrophase average of the
downstream gyrational ion energy first increases with increase of
up
to a maximum value
at
and then decreases at further
increase of
.
This downstream gyrational energy
,
however, is in a low-entropic form and by no means
fulfills the dissipation requirements of Rankine-Hugoniot relations with a
conversion rate
of
upstream kinetic into downstream thermal energy. Nevertheless from their study
it becomes evident that the parameter
can be optimized such that the
resulting dissipation attains a maximum. For very small values of
,
pure ion overshoot will happen, while for large
,
pure conservation of
the magnetic ion moment will occur. Maximum dissipation, however, appears to
be in between these two extreme cases. This intermediate case is perhaps
realized when an unstationary shock structure eventually becomes stationary
just when meeting the right steepness conditions. Though not based on a
rigorous theoretical treatment, one may nevertheless draw the qualitative
conclusion from it, that the strong perpendicular MHD shock may have a
transition scale of
.
In contrast to the above, a corresponding scale estimate
for the parallel shock has to be elaborated on completely different physical
grounds. In this particular case, where
Bn1=Bn2 is valid, no
dissipation can be achieved by conversion into gyrational energy modes. The
only way to realize dissipation is through dynamical coupling between ions and
overshooting electrons either by electrostatic or by Whistler wave turbulences
which culminates in the requirement (see Quest 1986) that the upstream
electron resistive diffusion length
be of the order of the ion
inertial length
(where
is the ion plasma frequency). This criterion has been proven to
be fairly correctly fulfilled based on corresponding investigations of data
obtained with ISEE at several Earth bowshock crossings (Scudder et al. 1986).
More recently it has been shown in measurements of the Cluster satellites
(Lobzin et al. 2007)
that the required anomalous electron
resistivity most probably in case of the Earth`s bowshock is enforced by large
amplitude Whistler waves which are driven unstable towards some saturation
level in the bowshock transition region. These authors are also
able to demonstrate that the bowshock structure is unstationary,
as long as Whistler
wave turbulence amplitudes stay low, and only becomes stationary, if the
turbulence amplitudes have reached a supercritical level.
We thus can estimate the transition scale
of the
parallel MHD shock looking for the dimension over which overshooting electrons
can couple their kinetic energy via Whistler waves to the shocked ions.
Whistler waves in the electron frame have frequencies
which in the
ion bulk frame are seen with a frequency
with the following
relation valid
| (78) |
where k is the wave vector of the Whistler wave and
is the
difference in the bulk velocities of protons and electrons. The latter can
easily be estimated by the expression
![]() |
(79) |
Only the left-handed Whistler wave can be absorbed by ions when the Whistler
wave frequency is seen in the ion frame as ion cyclotron frequency
,
thus requiring as resonance condition a Whistler frequency of
![]() |
(80) |
which can be expressed as a pure function of frequency when using the Whistler
wave dispersion relation
and thus yields
![]() |
(81) |
where
is the phase velocity of the resonant
Whistler wave. When entering with the above frequency
into the
Whistler wave dispersion relation one finds with
for
the absorption of the resonant Whistler wave a typical extinction length of
![]() |
(82) |
is then obtained.
Reminding now that the following relation is valid
![]() |
(83) |
we finally find
![]() |
(84) |
demonstrating that, depending on the specific shock conditions, the transition scale of the parallel shock is larger than that of the associated perpendicular shock by about
| (85) |
To summarize, the different transition scales at different magnetic field orientations supports our initial idea that the parallel and perpendicular shocks require a significant amount of additional physical processes included into our model.
We have analyzed the simplest form of the Boltzmann equation for an ion-only MHD plasma crossing a shock, where no additional physical processes besides the deceleration itself are present. Our results clearly prove that this equation is unable to describe the situation, since both the plasma is decelerated more strongly than predicted by the MHD jump conditions, and the mass flow is not conserved either. We have clearly identified one point where our current approach may be oversimplified, an inadequate (or even missing) treatment of electrons, and it is highly possible that even more such points do emerge in a more in-depth analysis, which is currently in progress.
However, despite all complications, we are already able to give one interesting result. Assuming that a Boltzmann equation compatible with stationary shock conditions does exist (which may be valid, perhaps, after sufficient time-averaging), we are able to explain the observations of the passage of the Voyager 1 spacecraft across the solar wind termination shock in 2004 (Stone et al. 2005; Burlaga et al. 2005; Gurnett & Kurth 2005; Decker et al. 2005), where the power law index of the solar wind does not seem to change (Cummings et al. 2006). This connection supports our results and encourages further research, including, but not limited to modeling of situations where even, after averaging over time, the shock front is not stationary, as found e.g. in supernova shock waves.
Acknowledgements
We are grateful for financial support to the DFG within the frame of the DFG-Project Fa 97/31-1.