First-principles Fermi acceleration in magnetized turbulence Martin Lemoine Institut dAstrophysique de Paris

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First-principles Fermi acceleration in magnetized turbulence
Martin Lemoine
Institut d’Astrophysique de Paris,
CNRS – Sorbonne Universit´e,
98 bis boulevard Arago, F-75014 Paris, France
(Dated: October 4, 2022)
This work provides a concrete implementation of E. Fermi’s model of particle acceleration in
magnetohydrodynamic (MHD) turbulence, connecting the rate of energization to the gradients of
the velocity of magnetic field lines, which it characterizes within a multifractal picture of turbulence
intermittency. It then derives a transport equation in momentum space for the distribution function.
This description is shown to be substantiated by a large-scale numerical simulation of strong MHD
turbulence. The present, general framework can be used to model particle acceleration in a variety
of environments.
Introduction– Particle energization through scatterings
off inhomogeneous, random moving structures is a uni-
versal process [1,2], which has stirred considerable in-
terest in various branches of physics: primarily astro-
physics, with applications ranging from solar flares [3] to
more remote phenomena involving plasmas in extreme
conditions, e.g. [4], but also statistical plasma physics [5]
or high energy density physics [6]. Remarkably, the two
papers of E. Fermi [1,2] represent the first concrete sce-
narios for the origin of non-thermal particles in the Uni-
verse. While the literature has placed significant empha-
sis on acceleration at shock fronts, numerical experiments
have demonstrated that stochastic acceleration can be ef-
ficient [79], notably so at large turbulent Alfv´en veloc-
ity [1014], in the sense that it produces extended, hard
powerlaw distributions of suprathermal particles. Be-
sides, the stochastic Fermi process assuredly plays a role
in the vicinity of shock fronts [1517], just as it seemingly
controls part of the energization in reconnection environ-
ments [18,19].
While the overall scenario is commonly pictured as
originally formulated by E. Fermi – a sequence of discrete,
point-like interactions between a particle and infinitely
massive, perfectly conducting plasma clouds – its imple-
mentation in a realistic turbulent context has remained
a challenge [2022], to the extent that phenomenological
applications rely on a Fokker-Planck model parameter-
ized by a momentum diffusion coefficient.
The present Letter proposes a novel approach to this
problem and formulates a transport equation to describe
the evolution of the distribution function in momentum
space. It is first shown that particle momenta obey a
continuous-time random walk (CTRW), whose random
force scales as the gradients of the velocity of magnetic
field lines, coarse-grained on a scale comparable to the
particle gyroradius rgpc/eB (pmomentum, B=|B|
with Bmagnetic field). A key observation is that those
gradients are subject to intermittency on small length
scales. Hence, the random forces are neither Gaussian,
nor white noise in time and consequently, the random
walk deviates from Brownian motion, just as the trans-
port equation, which is derived here from known prop-
erties of CTRW, differs from Fokker-Planck. This equa-
tion is characterized by the statistics of velocity gradi-
ents, which are captured via a multifractal description of
turbulence intermittency. This framework is eventually
shown to reproduce the time- and momentum-dependent
Green functions obtained by tracking a large number
of test particles in a large-scale MHD simulation. The
present formalism thus provides a successful implemen-
tation of stochastic Fermi acceleration in realistic, colli-
sionless MHD turbulence.
A (continuous-time) random walk picture– To evalu-
ate energy gains/losses in the original Fermi model, it
proves convenient to boost to the scattering center frame
where the motional electric field Evanishes. The gen-
eralization of that model to a continuous random flow
similarly tracks the particle momentum in the instan-
taneous (here, non-inertial) frame R/
Ein which Evan-
ishes [23,24], which, in ideal MHD, moves at velocity
vE=cE×B/B2. In that frame, momentum gains or
losses scale in direct proportion to the (lab frame) spatio-
temporal gradients of the velocity field vE, as expressed
by Γacc, Γkand Γbelow. In detail, the momentum pof
particles with gyroradius rg`c(`ccoherence length of
the turbulence) evolves as
˙p=pΓacc + Γk+ Γ,(1)
with Γacc =v1µb·tvE(vparticle velocity; µ=
p·b/p pitch-angle cosine with respect to the magnetic
field direction b=B/B); Γk=µ2b·(b·)vEand
Γ=1µ2[·vEb·(b·)vE]/2. For sim-
plicity, the present work focuses on the sub-relativistic
limit vEc. Equation (1) – more precisely, its rela-
tivistic limit – has been shown to account for the bulk of
acceleration in numerical simulations of collisionless tur-
bulence [25], putting the present model on solid footing.
It generalizes the two contributions originally identified
by E. Fermi: interactions with moving magnetic mirrors
are captured by Γ, while orbits in dynamic, curved mag-
netic field lines are represented by Γk; the remaining term
Γacc describes the effective gravity force associated to ac-
celeration/deceleration of the field lines; of second order
in vE/c, it is subdominant in the sub-relativistic limit,
unless vvA.
arXiv:2210.01038v1 [astro-ph.HE] 3 Oct 2022
2
All quantities in Eq. (1) are understood to be coarse-
grained on wavenumber scale kgr1
g(length scales lg
2π rg), where rg=pc/eB denotes the particle gyroradius
in the lab frame. This procedure filters out wavenumbers
k > kg, whose contribution averages out over a gyro-
orbit, to retain the larger scales that shape the velocity
structures responsible for acceleration (in accord with the
original Fermi picture).
Henceforth, Eq. (1) is simplified to the symbolic ˙p=
pΓlg, Γlgrepresenting an aggregate (random) force ex-
erted by electromagnetic fields, coarse-grained on scale
lg; order of unity factors related to µare thus omitted;
we also consider relativistic particles (vc) to ease the
discussion. For technical details concerning the model-
ing of this random process, see [Supp. Mat. A]. Sepa-
rate now fluctuations from the mean, Γl=hΓli+δΓl,
the average carrying over the statistical realizations of
the turbulent flow: hΓlicharacterizes systematic heat-
ing, while the random δΓlrepresents the diffusive part.
If δΓlwere Gaussian distributed, and its time correlation
function that of white noise, the process would describe
Brownian motion, in one-to-one correspondence with a
Fokker-Planck equation for the distribution function [26].
As anticipated above, however, those random forces are
neither Gaussian in amplitude, nor white noise in time:
at small scales, they develop large powerlaw tails as a re-
sult of intermittency, while at large scales, the coherence
time of the random force &lg/c cannot be regarded as
infinitesimal.
To obtain the transport equation, we first observe that
the process ˙p=pΓlgcan be described as a CTRW: unlike
discretized Brownian motion, which operates at a fixed
and uniform time step, the random walk is here defined
by the joint probability φ(p|p0;tt0) to jump from p0to
pin time ∆t=tt0, with both ∆p=pp0and ∆t
regarded as random variables. Expectations are ∆t
lg(p0)/c – thus, a function of p0 and ∆ ln pΓlgt.
We will assume ∆tto be exponentially distributed with
mean waiting time tplg(p0)/c and ∆ ln pdistributed as
Γlglg/c [lg=lg(p0)], see [Supp. Mat. A] for methodology.
The random walk is then entirely defined by the statistics
of the velocity gradients Γlg.
Statistics of momentum jumps– In turbulence theories,
such statistics are conveniently described within a mul-
tifractal analysis [2729], which ascribes to each position
xa local scaling exponent h(x) for gradients on coarse-
graining scale l,viz.
Γl(x)Γ`c(x) (l/`c)h(x),(2)
and which describes the set of locations xwith index
h(x) as a fractal of dimension d(h). The statistics of Γl
are thus entirely captured by the probability distribution
function (p.d.f.) pΓ`cof Γ`cand by the spectrum d(h),
since the probability of being at xin a set with exponent
hon scale levolves as the volume filling fraction lDd(h)
(Dnumber of spatial dimensions). The gradient Γ`c(x)
on the coherence scale `cis naturally modeled as a Gaus-
sian variable with standard deviation σcvA/`c, where
vAdenotes the Alfv´en velocity of the turbulent compo-
nent. The spectrum d(h) can take different forms, the
simplest being log-normal [30], modern descriptions of
the statistics of Els¨asser fields in MHD turbulence rather
relying on log-Poisson models [3134]. We use the former
log-normal form, as it provides a simple and satisfactory
description of the statistics of the gradients of vE; see
[Supp. Mat. B], which includes Refs. [3538]. We thus
derive the p.d.f. pΓlof Γlas (using D= 3) [29]
pΓlZ`cpΓ`cZdh l3d(h)δhΓlΓ`c(l/`c)hi.
(3)
This p.d.f. remains to be properly normalized. In this
formulation, the gradient statistics pΓlon all scales re-
duce to a function of the main quantities vA,`cand the
few parameters characterizing d(h), which themselves de-
pend on the physical properties of the turbulence. This
offers a first-principles connection between the funda-
mental statistics of turbulence intermittency and the
physics of particle energization.
The transport equation– The CTRW is exactly equivalent
to the following kinetic equation for the volume averaged
distribution np(t)=4πp2f(p, t), where f(p, t) represents
the angle-averaged distribution function [39,40]:
tnp(t) = Z+
0
dp0Zt
0
dt0ψ(p|p0;tt0)np0(t0)
ψ(p0|p;tt0)np(t0).
(4)
The kernel ψ(p|p0;tt0) differs from the CTRW jump
distribution probability φ(p|p0;tt0) introduced earlier,
yet the two are related as follows. Denoting with a tilde
symbol the Laplace transform in time, and νthe Laplace
variable conjugate to tt0,
˜
ψ(p|p0;ν) = ν˜
φ(p|p0;ν)
1˜
φp0(ν),(5)
with the short-hand notation ˜
φp0(ν)
R+
0dp˜
φ(p|p0;ν), the subscript p0emphasizing the
dependence on p0. As discussed above, we characterize
the CTRW with a joint probability distribution of the
form:
φ(p|p0;tt0) = ϕ(p|p0)e(tt0)/tp0
tp0
,(6)
recalling that tp0lg(p0)/c. Then,
˜
ψ(p|p0;ν) = ϕ(p|p0)
tp0
,(7)
in which case the transport equation becomes local in
time [40],
tnp(t) = Z+
0
dp0ϕ(p|p0)
tp0
np0(t)ϕ(p0|p)
tp
np(t).
(8)
摘要:

First-principlesFermiaccelerationinmagnetizedturbulenceMartinLemoineInstitutd'AstrophysiquedeParis,CNRS{SorbonneUniversite,98bisboulevardArago,F-75014Paris,France(Dated:October4,2022)ThisworkprovidesaconcreteimplementationofE.Fermi'smodelofparticleaccelerationinmagnetohydrodynamic(MHD)turbulence,co...

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