Mathematical Principles of Theoretical Physics

(Rick Simeone) #1

7.1. ASTROPHYSICAL FLUID DYNAMICS 411


Then, in view of (7.1.28)-(7.1.31), the equation (7.1.76) can be expressed by


(7.1.79)


1


α

(


1


r^2


α′

)



1


r^2

=−


8 πG
c^2
ρ 0 +

1


2 α ψ
ψ′φ′,

1
α

(


1


r^2

+


ψ′

)



1


r^2

=


8 πG
c^2
p+

1


α
φ′′−

1


2 α^2
α′φ′,

1
α

[


ψ′′
ψ


1


2


(


ψ′
ψ

) 2



α′ψ′
2 α ψ

+


1


r

(


ψ′
ψ


α′
α

)]


=


16 πG
c^2

p+

2



φ′,

where the pressurepsatisfies the stationary equations of (7.1.78) withP=0 as follows


(7.1.80)


p′=−

c^2
2
ψ′ρ[ 1 −β(T−T 0 )],
κ
αr^2

d
dr

(


r^2

dT
dr

)


=−Q(r).

The functionsψandαsatisfy the boundary conditions (7.1.33), i.e.


(7.1.81) ψ(r 0 ) = 1 −
2 Gm
c^2 r 0


, α(r 0 ) =

(


1 −


2 Gm
c^2 r 0

)− 1


.


In addition, for the ordinary differential equations (7.1.79)-(7.1.81), we also need the bound-
ary conditions forψ′,φ′andT. Since−^12 c^2 ψ′represents the gravitational force, the condition
ofψ′atr=r 0 is given by


(7.1.82) ψ′(r 0 ) =


2 mG
c^2 r^20

.


Based on the Newton gravitational law,φ′is very small in the external sphere; also see
(Ma and Wang,2014e). Hence we can approximatively take that


(7.1.83) φ′(r 0 ) = 0.


Finally, it is rational to take the temperature gradient in the boundary condition as follows


(7.1.84)


∂T


∂r

(r 0 ) =−A (A> 0 ).

Let the stationary solution of the problem (7.1.79)-(7.1.81) be given by ̃p,T ̃,ψ,α,φ′.
Make the translation transformation


P→P, p→p+ ̃p, T→T+T ̃.

Then equations (7.1.78) are rewritten in the form


(7.1.85)


∂P


∂ τ

+


1


ρ
(P·∇)P=ν∆P−∇p+

c^2 ρ
2 α


dr
β~kT,

∂T
∂ τ

+


1


ρ

(P·∇)T=κ ̃∆T−

1


ρ

dT ̃
dr

Pr,

divP= 0 ,
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