SSC/Stability/NeutralMode: Difference between revisions

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<math>
<math>
-\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2}
-\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2}
-\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 - \biggl(\frac{g_0 \rho_0 r_0}{P_0}\biggr)\biggr]\frac{dx_t}{dr_0}
-\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 + \frac{d\ln P_0}{d\ln r_0}\biggr]\frac{dx_t}{dr_0}
- \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr)
- \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr)
\biggl[ (4-3\gamma_g)\frac{g_0}{r_0} + \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t
\biggl[ (4-3\gamma_g)\frac{g_0}{r_0} + \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t
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<math>=</math>
  </td>
  <td align="left">
<math>
-\biggl(\frac{r_0^2}{b}\biggr)\frac{d^2 x_t}{dr_0^2}
-\biggl(\frac{r_0}{b}\biggr)\biggl[ 4 + \frac{d\ln P_0}{d\ln r_0}\biggr]\frac{dx_t}{dr_0}
+ \biggl(\frac{1}{b}\biggr) \frac{1}{\gamma_g} \biggl( \frac{d\ln P_0}{d \ln r_0}\biggr)
(4-3\gamma_g)x_t
- \biggl(\frac{r_0^2}{b}\biggr) \biggl( \frac{\rho_0}{\gamma_g P_0}\biggr)
\biggl[ \sigma_c^2\biggl(\frac{2\pi G\rho_c}{3}\biggr)\biggr]x_t
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Revision as of 17:45, 3 September 2021

LAWE

Most General Form

In an accompanying discussion, we derived the so-called,

Adiabatic Wave (or Radial Pulsation) Equation

d2xdr02+[4r0(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(43γg)g0r0]x=0

where the gravitational acceleration,

g0

GMrr02=1ρ0dP0dr0g0ρ0r0P0=dlnP0dlnr0.

The solution to this equation gives eigenfunctions that describe various radial modes of oscillation in spherically symmetric, self-gravitating fluid configurations. The boundary condition conventionally used in connection with the adiabatic wave equation is,

r0dlnxdr0

=

1γg(43γg+ω2R3GMtot)        at         r0=R.

Polytropic Configurations

Part 1

If the initial, unperturbed equilibrium configuration is a polytropic sphere whose internal structure is defined by the function, θ(ξ), that provides a solution to the,

Lane-Emden Equation

1ξ2ddξ(ξ2dΘHdξ)=ΘHn

then,

r0

=

anξ,

ρ0

=

ρcθn,

P0

=

Kρ0(n+1)/n=Kρc(n+1)/nθn+1,

g0

=

GM(r0)r02=Gr02[4πan3ρc(ξ2dθdξ)],

where,

an

=

[(n+1)K4πGρc(1n)/n]1/2.

Hence, after multiplying through by an2, the above adiabatic wave equation can be rewritten in the form,

d2xdξ2+[4ξg0an(an2ρ0P0)]dxdξ+(an2ρ0γgP0)[ω2+(43γg)g0anξ]x

=

0.

In addition, given that,

g0an

=

4πGρc(dθdξ),

and,

an2ρ0P0

=

(n+1)(4πGρc)θ=an2ρcPcθcθ,

we can write,

0

=

d2xdξ2+[4(n+1)V(ξ)ξ]dxdξ+[ω2(an2ρcγgPc)θcθ(34γg)(n+1)V(x)ξ2]x

 

=

d2xdξ2+[4(n+1)V(ξ)ξ]dxdξ+(n+1)[ω2(an2ρcγgPc)ξ2θc(n+1)θ(34γg)V(x)]xξ2

where we have adopted the function notation,

V(ξ)

ξθdθdξ.

Part 2

Drawing from an accompanying discussion, we have the following:

Polytropic LAWE (linear adiabatic wave equation)

0=d2xdξ2+[4(n+1)Q]1ξdxdξ+(n+1)[(σc26γg)ξ2θαQ]xξ2

where:    Q(ξ)dlnθdlnξ,    σc23ω22πGρc,     and,     α(34γg)

In order to reconcile with the "Part 1" expression, we note first that V(ξ)Q(ξ). We note as well that since,

(an2ρcPc)θc

=

(n+1)4πGρc,

we have,

ω2(an2ρcγgPc)ξ2θc(n+1)θ

ω2γg[(n+1)4πGρc]ξ2(n+1)θ=16γg[3ω22πGρc]ξ2θ=(σc26γg)ξ2θ.

All physically reasonable solutions are subject to the inner boundary condition,

dxdξ=0         at         ξ=0,

but the relevant outer boundary condition depends on whether the underlying equilibrium configuration is isolated (surface pressure is zero), or whether it is a "pressure-truncated" configuration. As is the case with the pressure-truncated isothermal spheres, discussed above, if the polytropic configuration is truncated by the pressure, Pe, of a hot, tenuous external medium, then the solution to the LAWE is subject to the outer boundary condition,

dlnxdlnξ=3         at         ξ=ξ~.

But, for isolated polytropes, the sought-after solution is subject to the more conventional boundary condition,

dlnxdlnξ=(3nn+1)+nσc26(n+1)[ξθ']         at         ξ=ξsurf.

Radial Pulsation Neutral Mode

The integro-differential version of the statement of hydrostatic balance is

dPdr=GMrρr2

From our separate discussion, we have found that,

Exact Solution to the (3n<) Polytropic LAWE

σc2=0

      and      

xP3(n1)2n[1+(n3n1)(1ξθn)dθdξ].

Let's rewrite the significant functional term in this expressions in terms of basic variables. That is,

(1ξθn)dθdξ

=

(anρcr0ρ0)g04πGρcan

 

=

M(r0)4πr03ρ0.

Let's adopt the following trial solution:

xt

=

abMr4πr03ρ0=abg04πGr0ρ0.

Then we have,

(1b)dxtdr0

=

ddr0[Mr4πr03ρ0]

 

=

[14πr03ρ0]dMrdr0[Mr4πr03ρ02]dρ0dr0[3Mr4πr04ρ0]

 

=

1r0[3Mr4πr04ρ0][Mr4πr03ρ02]dρ0dr0

(1b)d2xtdr02

=

ddr0{1r0[3Mr4πr04ρ0][Mr4πr03ρ02]dρ0dr0}

 

=

1r02[34πr04ρ0]dMrdr0+[3Mr4πr04ρ02]dρ0dr0+4[3Mr4πr05ρ0]

 

 

[Mr4πr03ρ02]d2ρ0dr02[14πr03ρ02]dρ0dr0dMrdr0+[3Mr4πr04ρ02]dρ0dr0+[2Mr4πr03ρ03](dρ0dr0)2

 

=

4r02+3Mr4πr05ρ0[4+dlnρ0dlnr0]+1r02[3Mr4πr03ρ01]dlnρ0dlnr0[Mr4πr03ρ02]d2ρ0dr02+[2Mr4πr05ρ0](dlnρ0dlnr0)2.

Given that,

ΔMr4πr03ρ0

=

14πG(g0r0ρ0),

these expression can be rewritten as,

(r02b)dxtdr0

=

r0{13ΔΔdlnρ0dlnr0},

and,

(r02b)d2xtdr02

=

4+3Δ[4+dlnρ0dlnr0]+[3Δ1]dlnρ0dlnr0Δ(r02ρ0)d2ρ0dr02+2Δ(dlnρ0dlnr0)2.

Finally, plugging our trial radial displacement function, xt, into the LAWE gives,

d2xdr02+[4r0(g0ρ0P0)]dxdr0+(ρ0γgP0)[ω2+(43γg)g0r0]x=0

LAWE

=

(r02b)d2xtdr02(r0b)[4+dlnP0dlnr0]dxtdr0(r02b)(ρ0γgP0)[(43γg)g0r0+σc2(2πGρc3)]xt

 

=

(r02b)d2xtdr02(r0b)[4+dlnP0dlnr0]dxtdr0+(1b)1γg(dlnP0dlnr0)(43γg)xt(r02b)(ρ0γgP0)[σc2(2πGρc3)]xt

See Also

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