Processing math: 100%

Labels

Thursday, May 9, 2019

A simple derivation for parker transport equation

The continuity equation in differential form
ft=S.

In a given volume, the rate of change of the number of particles,ft, is given by the numer of particles that across the surface enclosing the volume, assuming no source of particle is present.
S is the streaming crrent density of particles across the surface.

S = Vf Kf pSp=1p2p(p2˙pf) , Sp=˙pf

ft+(VfKf)+(1p2p(p2˙pf))=0

note. The streaming is included in S.
adiabatic cooling resulting the average change in momentum is ˙p=p3V.
ft+fV+Vf(V)3p2(3p2f+p3fp)=ft+fV+Vf(V)(f+p3fp)=ft+Vf(V)p3fp


note. dTdt=dpdtdTdp=V3(ppT+m)=(V)3T(T+2mT+m).dEdt=dpdtdEdp=(V)3(pv)


When differential energy density, Up=4πp2f, is convected with velocity V, the flux observed is not VUp, but rather Sp=CVUp, where C=13lnflnp=13pffp is called the Compton-Getting coefficien.
For f=Apγ, C is γ3. if γ is 4.7, then the C is 4.7/31.57.

The adiabatic rate of change of momentum ˙p=(1/3)pV referred to above, is actually the rate of change in the non-inertial frame. The rate in the stationary frame is ˙p=(1/3)pV(f/f).


Reference
Radiation Environments and Damage in Silicon Semiconductors Silicon chapter4
Cosmic-Ray Modulation Equations

No comments:

Post a Comment