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Different heating of Maxwellian and kappa distributions at shocks

Published online by Cambridge University Press:  13 September 2022

Michael Gedalin*
Affiliation:
Department of Physics, Ben-Gurion University of the Negev, Beer-Sheva, Israel
Natalia Ganushkina
Affiliation:
Finnish Meteorological Institute, Helsinki, Finland
*
Email address for correspondence: gedalin@bgu.ac.il
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Abstract

Ion heating in collisionless shocks is non-adiabatic and efficient. The amount of heating and the downstream distributions depend on the shock parameters and on the incident ion distribution. The number of reflected ions and their distribution depend on the detailed shape of the tail of the distribution. In supercritical shocks the reflected ion contribution is significant. Kappa distributed ions are heated more strongly and have a larger fraction of reflected ions than Maxwellian distributed ions with the same upstream temperature and the same shock parameters. For kappa distributions the phase space dips are shallower.

Type
Research Article
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Copyright
Copyright © The Author(s), 2022. Published by Cambridge University Press

1 Introduction

Shocks efficiently convert the energy of the directed flow into thermal energy (de Hoffmann & Teller Reference de Hoffmann and Teller1950). In collisionless shocks different plasma species are heated differently (Feldman et al. Reference Feldman, Bame, Gary, Gosling, McComas, Thomsen, Paschmann, Sckopke, Hoppe and Russell1982; Sckopke et al. Reference Sckopke, Paschmann, Bame, Gosling and Russell1983; Thomsen et al. Reference Thomsen, Gosling, Bame and Mellott1985Reference Thomsen, Stansberry, Bame and Gosling1987; Schwartz et al. Reference Schwartz, Thomsen, Bame and Stansberry1988; Sckopke et al. Reference Sckopke, Paschmann, Brinca, Carlson and Luehr1990). In an electron–proton plasma, heating occurs at the expense of the energy of the incident ions. The incident ions cross the shock against the cross-shock potential (Morse Reference Morse1973; Formisano Reference Formisano1982; Schwartz et al. Reference Schwartz, Thomsen, Bame and Stansberry1988; Gedalin Reference Gedalin1997b,Reference Gedalina; Dimmock et al. Reference Dimmock, Balikhin, Krasnoselskikh, Walker, Bale and Hobara2012; Hanson et al. Reference Hanson, Agapitov, Mozer, Krasnoselskikh, Bale, Avanov, Khotyaintsev and Giles2019) and begin to gyrate. Ion distributions in the vicinity of the main magnetic field jump (ramp) are non-gyrotropic (Sckopke et al. Reference Sckopke, Paschmann, Bame, Gosling and Russell1983; Burgess, Wilkinson & Schwartz Reference Burgess, Wilkinson and Schwartz1989; Li et al. Reference Li, Lewis, LaBelle, Phan and Treumann1995; Gedalin Reference Gedalin1997a). Farther downstream, gyrophase mixing gyrotropizes the distributions and the gyration speeds become the dispersion in the velocity space, thus the contribution to the ion temperature (see Gedalin (Reference Gedalin2021) and references therein). In supercritical shocks, ion reflection comes to play a progressively more important role in ion heating with the increase of the Mach number (Burgess et al. Reference Burgess, Wilkinson and Schwartz1989; Sckopke et al. Reference Sckopke, Paschmann, Brinca, Carlson and Luehr1990; Zimbardo Reference Zimbardo2011; Gedalin Reference Gedalin2019). Reflected ions have larger gyration speeds than the ions of the bulk of the flow and their contribution to the downstream temperature exceeds their contribution to the downstream density. Simply put, ions may be reflected in two ways (Gedalin Reference Gedalin2016). Ions, which enter the ramp with sufficiently low velocities along the shock normal, are unable to overcome the cross-shock potential and return back to the upstream region where they gyrate back to the ramp and cross it again. This mode of reflection depends mainly on the cross-shock potential and is not sensitive to the magnetic compression. Ions with sufficiently high initial velocities along the shock normal overcome the potential and cross the ramp towards the downstream region. Such ions may retain sufficiently large gyration speeds to gyrate back to the ramp. If this happens, they cross the ramp towards upstream, gyrate in the upstream region, and cross the ramp once again towards downstream. This mode requires sufficient magnetic compression to ensure that the gyration speed is larger than the drift which causes ions to proceed farther downstream. In both reflection modes magnetic deflection within the ramp affects the velocity along the shock normal, so that the above description is somewhat simplified. Ions which are reflected in both modes come from the tail of the distribution function and not from the core. Thus, the shape of the upstream distribution function may affect the downstream ion distributions and heating in supercritical shocks. Most of heating analyses, including numerical simulation, performed so far, assumed Maxwellian distribution for incident ions. However, the actual distribution of ions in the solar wind may differ and is often found to be better described as a kappa ($\kappa$) distribution (see, e.g. Nicolaou et al. (Reference Nicolaou, Livadiotis, Owen, Verscharen and Wicks2018), and references therein). Since the Maxwellian and $\kappa$ distributions have different tails, one may expect to observe differences in the ion distributions formed at the shock crossing, even if the velocity dispersion is the same. The objective of the present paper is to analyse the effects of the shape of the tails of these two distributions on the ion heating at a slightly supercritical shock.

2 Approach: numerical ion tracing

Since we are interested in separating the effects of the distribution from all other effects, it is reasonable to control all other shock parameters. It is most efficiently done by tracing ions as test particles across a model shock. A slightly supercritical shock is expected to be a nearly planar and stationary low-Mach number shock, with a weak overshoot. Let subscripts $u$ and $d$ denote upstream and downstream, respectively. We choose the coordinates so that $x$ is along the shock normal, pointing towards downstream, and $x$$z$ is the coplanarity plane. The magnetic field profile is described as follows:

(2.1)\begin{equation} B_z=B_u\sin\theta\left(\frac{R-1}{2}+\frac{R+1}{2}\tanh\frac{3x}{D}\right), \end{equation}

where $B_u$ is the upstream magnetic field magnitude, $\theta$ is the angle between the shock normal and the upstream magnetic field vector, and the magnetic compression is

(2.2)\begin{equation} \frac{B_d}{B_u}=\sqrt{R^2\sin^2\theta+\cos^2\theta}. \end{equation}

The parameter $D$ gives the shock width. We do not include any overshoot in this analysis, since its influence is expected to be minor. The upstream proton gyrofrequency is $\varOmega _u=eB_u/m_pc$. The upstream proton plasma frequency is $\omega _{p}=\sqrt {4{\rm \pi} e^2n_u/m_p}$, where $n_u$ is the upstream proton number density. The ion inertial length is $c/\omega _{p}$ and the Alfvén speed is $v_A=c\varOmega _u/\omega _{p}$. Let the upstream plasma velocity along the shock normal in the shock frame be $V_u$, then the Alfvénic Mach number is $M=V_u/v_A$. The upstream convective proton gyroradius is $\rho _p=V_u/\varOmega _{u}=M(c/\omega _{p})$. In what follows we shall use dimensional parameters and variables as follows:

(2.3a–d)\begin{equation} \frac{x}{\rho_p}\rightarrow x,\quad \varOmega_u t\rightarrow t, \quad \frac{\boldsymbol{v}}{V_u}\rightarrow \boldsymbol{v}, \quad \frac{\boldsymbol{B}}{B_u}\rightarrow \boldsymbol{B}. \end{equation}

The two most convenient shock frames and the de Hoffman–Teller frame (HT), in which the upstream and downstream plasma velocities are along the upstream and downstream magnetic field vectors, respectively, and the normal incidence frame (NIF), in which the upstream plasma velocity is along the shock normal. In HT the motional electric field $E_y{({\rm HT})}=0$ vanishes identically, while in NIF it is constant $E_y^{({\rm NIF})}=V_uB_u\sin \theta /c$ throughout the shock. In both frames $E_z=0$. The shape of the cross-shock electric field $E_x^{({\rm HT})}$ is chosen as follows:

(2.4)\begin{equation} E_x^{({\rm HT})}={-}K_E\frac{{\rm d}B_z}{{\rm d} x}, \end{equation}

where the coefficient $K_E$ is determined from the cross-shock potential

(2.5)\begin{equation} \phi_{{\rm HT}}={-}\int_{-\infty}^\infty E_x\,{\rm d}x\end{equation}

and is one of the model parameters. In the dimensionless form we have

(2.6)\begin{equation} s_{{\rm HT}}=e\phi_{{\rm HT}}/(m_pV_u^2/2). \end{equation}

The non-coplanar magnetic field is chosen in a similar form,

(2.7)\begin{equation} B_y=K_B\frac{{\rm d}B_z}{{\rm d} x}, \end{equation}

while

(2.8)\begin{equation} \phi_{{\rm NIF}}-\phi_{{\rm HT}}=\frac{V_u\tan\theta}{c}\int_{-\infty}^\infty B_y\,{\rm d}x. \end{equation}

For $V_u/\cos \theta \ll c$ the transformation between the two frames is non-relativistic which means that the magnetic field can be considered the same. The parameter

(2.9)\begin{equation} s_{{\rm NIF}}=e\phi_{{\rm NIF}}/(m_pV_u^2/2) \end{equation}

is also the model parameter which determines the coefficient $K_B$. In the present analysis $s_{{\rm NIF}}=0.4$, $s_{{\rm HT}}=0.1$ and $D=(c/\omega _{p})$. The chosen magnetic compression is $B_d/B_u=2.6$ and $\theta =70^\circ$. The Mach number $M=2.9$ is derived from isotropic Rankine–Hugoniot relations (Kennel Reference Kennel1988) with $\beta _p=8{\rm \pi} n_uT_u/B_u^2=0.2$. Here $T_u$ is the upstream ion temperature.

The initial upstream distributions of ions are taken either Maxwellian

(2.10)\begin{equation} f^{(M)}_u(\boldsymbol{v})=\frac{n_u}{(2{\rm \pi})^{3/2}v_T^3} \exp \left(-\frac{(\boldsymbol{v}-\boldsymbol{V})^2}{2v_T^2}\right)\end{equation}

or a $\kappa$ distribution

(2.11)\begin{equation} f^{(K)}_u(\boldsymbol{v})=\frac{n_u}{{\rm \pi}^{3/2}v_T^3} \left(\kappa-\frac{3}{2}\right)^{{-}3/2}\frac{\varGamma(\kappa+1)}{\varGamma(\kappa-1/2)} \left(1+\frac{(\boldsymbol{v}-\boldsymbol{V})^2}{(2\kappa-3)v_T^2}\right)^{-\kappa-1}, \end{equation}

where in both cases

(2.12)\begin{gather} n_u\boldsymbol{V}=\int f_u(\boldsymbol{v})\,{\rm d}^3\boldsymbol{v}, \end{gather}
(2.13)\begin{gather}n_uv_T^2=\int (\boldsymbol{v}-\boldsymbol{V})^2f_u(\boldsymbol{v})\,{\rm d}^3\boldsymbol{v} \end{gather}

and $\varGamma$ is the $\varGamma$-function. In the present analysis $\kappa =4$ (Smith et al. Reference Smith, Renfroe, Pogorelov, Zhang, Gedalin and Kim2022).

3 Downstream distributions and heating parameters

Figure 1 shows the distributions functions $f_u(v_\parallel,v_\perp )$ and $f_d(v_\parallel,v_\perp )$ for the Maxwellian distributed incident ions. Here

(3.1)\begin{gather} v_\parallel{=}\frac{\boldsymbol{v}\boldsymbol{\cdot} \boldsymbol{B}}{|\boldsymbol{B}|}, \end{gather}
(3.2)\begin{gather}v_\perp{=}\frac{|(\boldsymbol{v}-\boldsymbol{V})\times \boldsymbol{B}|}{|\boldsymbol{B}|}, \end{gather}

where $\boldsymbol {B}$ is the local magnetic field. The upstream distributions are gyrotropic by choice. The downstream distributions become gyrotropic well beyond the shock transition. The distributions are in HT. The maximum of the downstream distribution is not at $v_\perp =0$ which shows that initially the whole distribution gyrates around the magnetic field. After gyrotropization, this gyration is the main contribution to the velocity dispersion, that is, to the temperature. There is a distinct population of reflected ions. Their density is low and there is a clear gap between the directly transmitted ions and reflected ions. The figure uses a logarithmic scale with $f_{\min }/f_{\max }>10^{-6}$. The upstream temperature of the ions is $T_u/m_pV_u^2=0.0118$. The downstream parallel temperature is $T_{d,l}=T_u$, while the downstream perpendicular temperature is $T_{d,p}/m_pV_u^2=0.0973$.

Figure 1. The upstream (left-hand side) and downstream (right-hand side) gyrotropic distributions for initially Maxwellian distributed ions, on a log scale.

Figure 2 shows the distributions functions $f_u(v_\parallel,v_\perp )$ and $f_d(v_\parallel,v_\perp )$in the same format as in figure 1. The population of the reflected ions is substantially larger, and there is no gap between the directly transmitted and reflected ions. The upstream temperature of the ions is $T_u/m_pV_u^2=0.0118$, as for the Maxwellian ions. The downstream parallel temperature is $T_{d,l}/m_pV_u^2=0.0126$, while the downstream perpendicular temperature is $T_{d,p}/m_pV_u^2= 0.1004$. The 10 % difference in the downstream perpendicular temperature is due to the reflected ions. The difference in the downstream density is negligible.

Figure 2. The upstream (left-hand side) and downstream (right-hand side) gyrotropic distributions for initially $\kappa$-distributed ions, on a log scale.

Figure 3 shows the downstream reduced distribution

(3.3)\begin{equation} f_d(v_\perp)=\int_{-\infty}^\infty f_d(v_\parallel,v_\perp)\,{\rm d}v_\parallel, \end{equation}

for the initially Maxwellian ions (blue) and initially $\kappa$ ions (red). The left-hand vertical black line stands at the maximum of the distribution of the directly transmitted population. The right-hand line marks the maximum of the reflected ions. The middle line is for the minimum of the distribution. There are no noticeable differences in the positions of the three points in both cases. For $\kappa$ ions the maximum of the reflected ions and the integral under the curve part, corresponding to these ions, are substantially larger. In the minimum the distribution function does not drop as strongly as for the Maxwellian ions.

Figure 3. The downstream reduced distribution for the initially Maxwellian ions (blue) and initially $\kappa$ ions (red). The left-hand vertical black line stands at the maximum of the distribution of the directly transmitted population. The right-hand line marks the maximum of the reflected ions. The middle line is for the minimum of the distribution.

Figure 4 shows the reduced distribution function

(3.4)\begin{equation} f(x,v_x)=\int f(x,\boldsymbol{v})\,{\rm d}v_y\,{\rm d}v_z \end{equation}

throughout the shock for initially Maxwellian ions. The gyration and relaxation of directly transmitted ions is clearly seen, as well as the gyrating reflected ions. There is a phase space hole separating the two populations. Reflected ions are seen in the upstream region up to the distance $\approx 0.5(V_u/\varOmega _u)$.

Figure 4. The reduced distribution function $f(x,v_x)$ throughout the shock for initially Maxwellian ions.

Figure 5 throughout the shock for initially $\kappa$ ions. Now the two populations, albeit clearly seen, are not separated by phase space holes. Reflected ions are seen in the upstream region up to the distance $\approx (V_u/\varOmega _u)$. However, their density there is hardly detectable in reality. The sharp drop of the distribution at $0.5(V_u/\varOmega _u)$ for Maxwellian ions versus the smooth decrease over $-(V_u/\varOmega _u)< x<-0.5(V_u/\varOmega _u)$ is because of the much faster drop of the tail for Maxwellian ions. The slower decreasing tail of $\kappa$ is also responsible for filling the phase space holes.

Figure 5. The reduced distribution function $f(x,v_x)$ throughout the shock for initially $\kappa$ ions.

4 Conclusions

Longer tails of the distribution function of incident ions result in stronger heating and smaller anisotropy of the downstream distribution. Both effects are due to stronger ion reflection, since the reflected ions come from the tail of the distribution. Longer tails may be also responsible for filling the ion phase space holes. The distribution of reflected ions is much more diffuse for $\kappa$-distributed ions than for Maxwellian-distributed ions.

Acknowledgements

Editor Antoine C. Bret thanks the referees for their advice in evaluating this article.

Funding

The work was partially supported by the European Union's Horizon 2020 research and innovation programme under grant agreement no. 101004131 (SHARP).

Declaration of interests

The authors report no conflict of interest.

References

REFERENCES

Burgess, D., Wilkinson, W.P. & Schwartz, S.J. 1989 Ion distributions and thermalization at perpendicular and quasi-perpendicular supercritical collisionless shocks. J. Geophys. Res. 94, 8783.CrossRefGoogle Scholar
de Hoffmann, F. & Teller, E. 1950 Magneto-hydrodynamic shocks. Phys. Rev. 80 (4), 692703.CrossRefGoogle Scholar
Dimmock, A.P., Balikhin, M.A., Krasnoselskikh, V.V., Walker, S.N., Bale, S.D. & Hobara, Y. 2012 A statistical study of the cross-shock electric potential at low Mach number, quasi-perpendicular bow shock crossings using Cluster data. J. Geophys. Res. 117 (A), 02210.Google Scholar
Feldman, W., Bame, S., Gary, S., Gosling, J., McComas, D., Thomsen, M., Paschmann, G., Sckopke, N., Hoppe, M. & Russell, C. 1982 Electron heating within the Earth's bow shock. Phys. Rev. Lett. 49 (3), 199201.CrossRefGoogle Scholar
Formisano, V. 1982 Measurement of the potential drop across the Earth's collisionless bow shock. Geophys. Res. Lett. 9, 1033.CrossRefGoogle Scholar
Gedalin, M. 1997 a Ion dynamics and distribution at the quasiperpendicular collisionless shock front. Surv. Geophys. 18 (6), 541566.CrossRefGoogle Scholar
Gedalin, M. 1997 b Ion heating in oblique low-Mach number shocks. Geophys. Res. Lett. 24 (2), 25112514.CrossRefGoogle Scholar
Gedalin, M. 2016 Transmitted, reflected, quasi-reflected, and multiply reflected ions in low-Mach number shocks. J. Geophys. Res. 121 (1), 10.CrossRefGoogle Scholar
Gedalin, M. 2019 Kinematic collisionless relaxation of ions in supercritical shocks. Front. Phys. 7, 692.CrossRefGoogle Scholar
Gedalin, M. 2021 Shock heating of directly transmitted ions. Astrophys. J. 912 (2), 82.CrossRefGoogle Scholar
Hanson, E.L.M., Agapitov, O.V., Mozer, F.S., Krasnoselskikh, V., Bale, S.D., Avanov, L., Khotyaintsev, Y. & Giles, B. 2019 Cross-shock potential in rippled versus planar quasi-perpendicular shocks observed by MMS. Geophys. Res. Lett. 46 (5), 23812389.CrossRefGoogle Scholar
Kennel, C.F. 1988 Shock structure in classical magnetohydrodynamics. J. Geophys. Res. 93 (A8), 85458557.CrossRefGoogle Scholar
Li, X., Lewis, H.R., LaBelle, J., Phan, T.D. & Treumann, R.A. 1995 Characteristics of the ion pressure tensor in the Earth's magnetosheath. Geophys. Res. Lett. 22 (6), 667670.CrossRefGoogle Scholar
Morse, D.L. 1973 Electrostatic potential rise across perpendicular shocks. Plasma Phys. 15 (1), 12621264.CrossRefGoogle Scholar
Nicolaou, G., Livadiotis, G., Owen, C.J., Verscharen, D. & Wicks, R.T. 2018 Determining the kappa distributions of space plasmas from observations in a limited energy range. Astrophys. J. 864 (1), 3.CrossRefGoogle Scholar
Schwartz, S.J., Thomsen, M.F., Bame, S.J. & Stansberry, J. 1988 Electron heating and the potential jump across fast mode shocks. J. Geophys. Res. 93 (A11), 1292312931.CrossRefGoogle Scholar
Sckopke, N., Paschmann, G., Bame, S.J., Gosling, J.T. & Russell, C.T. 1983 Evolution of ion distributions across the nearly perpendicular bow shock – specularly and non-specularly reflected-gyrating ions. J. Geophys. Res. 88 (A8), 61216136.CrossRefGoogle Scholar
Sckopke, N., Paschmann, G., Brinca, A.L., Carlson, C.W. & Luehr, H. 1990 Ion thermalization in quasi-perpendicular shocks involving reflected ions. J. Geophys. Res. 95, 6337.CrossRefGoogle Scholar
Smith, W.P., Renfroe, K., Pogorelov, N.V., Zhang, M., Gedalin, M. & Kim, T. 2022 Bulk properties of pickup ions derived from the ulysses solar wind ion composition spectrometer data. Astrophys. J. 933, 124.CrossRefGoogle Scholar
Thomsen, M.F., Gosling, J.T., Bame, S.J. & Mellott, M.M. 1985 Ion and electron heating at collisionless shocks near the critical Mach number. J. Geophys. Res. 90 (A1), 137.CrossRefGoogle Scholar
Thomsen, M., Stansberry, J., Bame, S. & Gosling, J. 1987 Strong electron heating at the Earth's bow shock. J. Geophys. Res. 92, 1011910124.CrossRefGoogle Scholar
Zimbardo, G. 2011 Heavy ion reflection and heating by collisionless shocks in polar solar corona. Planet. Space Sci. 59 (7), 468474.CrossRefGoogle Scholar
Figure 0

Figure 1. The upstream (left-hand side) and downstream (right-hand side) gyrotropic distributions for initially Maxwellian distributed ions, on a log scale.

Figure 1

Figure 2. The upstream (left-hand side) and downstream (right-hand side) gyrotropic distributions for initially $\kappa$-distributed ions, on a log scale.

Figure 2

Figure 3. The downstream reduced distribution for the initially Maxwellian ions (blue) and initially $\kappa$ ions (red). The left-hand vertical black line stands at the maximum of the distribution of the directly transmitted population. The right-hand line marks the maximum of the reflected ions. The middle line is for the minimum of the distribution.

Figure 3

Figure 4. The reduced distribution function $f(x,v_x)$ throughout the shock for initially Maxwellian ions.

Figure 4

Figure 5. The reduced distribution function $f(x,v_x)$ throughout the shock for initially $\kappa$ ions.