Vlasov equation

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Template:Short description In plasma physics, the Vlasov equation is a differential equation describing time evolution of the distribution function of collisionless plasma consisting of charged particles with long-range interaction, such as the Coulomb interaction. The equation was first suggested for the description of plasma by Anatoly Vlasov in 1938[1][2] and later discussed by him in detail in a monograph.[3] The Vlasov equation, combined with Landau kinetic equation describe collisional plasma.

Difficulties of the standard kinetic approach

First, Vlasov argues that the standard kinetic approach based on the Boltzmann equation has difficulties when applied to a description of the plasma with long-range Coulomb interaction. He mentions the following problems arising when applying the kinetic theory based on pair collisions to plasma dynamics:

  1. Theory of pair collisions disagrees with the discovery by Rayleigh, Irving Langmuir and Lewi Tonks of natural vibrations in electron plasma.
  2. Theory of pair collisions is formally not applicable to Coulomb interaction due to the divergence of the kinetic terms.
  3. Theory of pair collisions cannot explain experiments by Harrison Merrill and Harold Webb on anomalous electron scattering in gaseous plasma.[4]

Vlasov suggests that these difficulties originate from the long-range character of Coulomb interaction. He starts with the collisionless Boltzmann equation (sometimes called the Vlasov equation, anachronistically in this context), in generalized coordinates: ddtf(𝐫,𝐩,t)=0,

explicitly a PDE: ft+d𝐫dtf𝐫+d𝐩dtf𝐩=0, and adapted it to the case of a plasma, leading to the systems of equations shown below.[5] Here Template:Math is a general distribution function of particles with momentum Template:Math at coordinates Template:Math and given time Template:Mvar. Note that the term d𝐩dt is the force Template:Math acting on the particle.

The Vlasov–Maxwell system of equations (Gaussian units)

Instead of collision-based kinetic description for interaction of charged particles in plasma, Vlasov utilizes a self-consistent collective field created by the charged plasma particles. Such a description uses distribution functions fe(𝐫,𝐩,t) and fi(𝐫,𝐩,t) for electrons and (positive) plasma ions. The distribution function fα(𝐫,𝐩,t) for species Template:Mvar describes the number of particles of the species Template:Mvar having approximately the momentum 𝐩 near the position 𝐫 at time Template:Mvar. Instead of the Boltzmann equation, the following system of equations was proposed for description of charged components of plasma (electrons and positive ions): fet+𝐯efee(𝐄+𝐯ec×𝐁)fe𝐩=0fit+𝐯ifi+Zie(𝐄+𝐯ic×𝐁)fi𝐩=0

×𝐁=4πc𝐣+1c𝐄t,𝐁=0,×𝐄=1c𝐁t,𝐄=4πρ,

ρ=e(Zifife)d3𝐩,𝐣=e(Zifi𝐯ife𝐯e)d3𝐩,𝐯α=𝐩/mα1+p2/(mαc)2

Here Template:Mvar is the elementary charge (e>0), Template:Mvar is the speed of light, Template:Mvar is the charge of the ions, Template:Mvar is the mass of the ion, 𝐄(𝐫,t) and 𝐁(𝐫,t) represent collective self-consistent electromagnetic field created in the point 𝐫 at time moment Template:Mvar by all plasma particles. The essential difference of this system of equations from equations for particles in an external electromagnetic field is that the self-consistent electromagnetic field depends in a complex way on the distribution functions of electrons and ions fe(𝐫,𝐩,t) and fi(𝐫,𝐩,t).

The Vlasov–Poisson equation

The Vlasov–Poisson equations are an approximation of the Vlasov–Maxwell equations in the non-relativistic zero-magnetic field limit: fαt+𝐯αfα𝐱+qα𝐄mαfα𝐯=0,

and Poisson's equation for self-consistent electric field: 2ϕ+ρε=0.

Here Template:Mvar is the particle's electric charge, Template:Mvar is the particle's mass, 𝐄(𝐱,t) is the self-consistent electric field, ϕ(𝐱,t) the self-consistent electric potential, Template:Mvar is the electric charge density, and ε is the electric permitivity.

Vlasov–Poisson equations are used to describe various phenomena in plasma, in particular Landau damping and the distributions in a double layer plasma, where they are necessarily strongly non-Maxwellian, and therefore inaccessible to fluid models.

Moment equations

In fluid descriptions of plasmas (see plasma modeling and magnetohydrodynamics (MHD)) one does not consider the velocity distribution. This is achieved by replacing f(𝐫,𝐯,t) with plasma moments such as number density Template:Mvar, flow velocity Template:Math and pressure Template:Math.[6] They are named plasma moments because the Template:Mvar-th moment of f can be found by integrating vnf over velocity. These variables are only functions of position and time, which means that some information is lost. In multifluid theory, the different particle species are treated as different fluids with different pressures, densities and flow velocities. The equations governing the plasma moments are called the moment or fluid equations.

Below the two most used moment equations are presented (in SI units). Deriving the moment equations from the Vlasov equation requires no assumptions about the distribution function.

Continuity equation

The continuity equation describes how the density changes with time. It can be found by integration of the Vlasov equation over the entire velocity space. dfdtd3v=(ft+(𝐯r)f+(𝐚v)f)d3v=0

After some calculations, one ends up with nt+(n𝐮)=0.

The number density Template:Mvar, and the momentum density Template:Math, are zeroth and first order moments: n=fd3v n𝐮=𝐯fd3v

Momentum equation

The rate of change of momentum of a particle is given by the Lorentz equation: md𝐯dt=q(𝐄+𝐯×𝐁)

By using this equation and the Vlasov Equation, the momentum equation for each fluid becomes mnDDt𝐮=𝒫+qn𝐄+qn𝐮×𝐁, where 𝒫 is the pressure tensor. The material derivative is DDt=t+𝐮.

The pressure tensor is defined as the particle mass times the covariance matrix of the velocity: pij=m(viui)(vjuj)fd3v.

The frozen-in approximation

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We introduce the scales Template:Mvar, Template:Mvar, and Template:Mvar for time, distance and speed respectively. They represent magnitudes of the different parameters which give large changes in f. By large we mean that ftTf|f𝐫|Lf|f𝐯|Vf.

We then write t=tT,𝐫=𝐫L,𝐯=𝐯V.

Vlasov equation can now be written 1Tft+VL𝐯f𝐫+qmV(𝐄+V𝐯×𝐁)f𝐯=0.

So far no approximations have been done. To be able to proceed we set V=Rωg, where ωg=qB/m is the gyro frequency and Template:Mvar is the gyroradius. By dividing by Template:Mvar, we get 1ωgTft+RL𝐯f𝐫+(𝐄VB+𝐯×𝐁B)f𝐯=0

If 1/ωgT and RL, the two first terms will be much less than f since f/tf,v1 and f/𝐫f due to the definitions of Template:Mvar, Template:Mvar, and Template:Mvar above. Since the last term is of the order of f, we can neglect the two first terms and write (𝐄VB+𝐯×𝐁B)f𝐯0(𝐄+𝐯×𝐁)f𝐯0

This equation can be decomposed into a field aligned and a perpendicular part: 𝐄f𝐯+(𝐄+𝐯×𝐁)f𝐯0

The next step is to write 𝐯=𝐯0+Δ𝐯, where 𝐯0×𝐁=𝐄

It will soon be clear why this is done. With this substitution, we get 𝐄f𝐯+(Δ𝐯×𝐁)f𝐯0

If the parallel electric field is small, (Δ𝐯×𝐁)f𝐯0

This equation means that the distribution is gyrotropic.[7] The mean velocity of a gyrotropic distribution is zero. Hence, 𝐯0 is identical with the mean velocity, Template:Math, and we have 𝐄+𝐮×𝐁0

To summarize, the gyro period and the gyro radius must be much smaller than the typical times and lengths which give large changes in the distribution function. The gyro radius is often estimated by replacing Template:Mvar with the thermal velocity or the Alfvén velocity. In the latter case Template:Mvar is often called the inertial length. The frozen-in conditions must be evaluated for each particle species separately. Because electrons have much smaller gyro period and gyro radius than ions, the frozen-in conditions will more often be satisfied.

See also

References

Template:Reflist

Further reading

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