ParabolicDensity/Axisymmetric/Structure

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Parabolic Density Distribution


Part I:   Gravitational Potential

 


Part II:   Spherical Structures

 


Part III:   Axisymmetric Equilibrium Structures

 Old: 1st thru 7th tries
 Old: 8th thru 10th tries


Part IV:   Triaxial Equilibrium Structures (Exploration)

 

Axisymmetric (Oblate) Equilibrium Structures

Tentative Summary

Known Relations

Density:

ρ(ϖ,z)ρc

=

[1−χ2−ζ2(1−e2)−1],

Gravitational Potential:

Φgrav(ϖ,z)(−πGρcaℓ2)

=

12IBT−Aℓχ2−Asζ2+12[(Assaℓ2)ζ4+2(Aℓsaℓ2)χ2ζ2+(Aℓℓaℓ2)χ4].

 

⇒∂∂ζ[Φgrav(−πGρcaℓ2)]

=

2(Aℓsaℓ2)χ2ζ−2Asζ+2(Assaℓ2)ζ3.

 

and,     ∂∂χ[Φgrav(−πGρcaℓ2)]

=

2(Aℓsaℓ2)χζ2−2Aℓχ+2(Aℓℓaℓ2)χ3.

where, χ≡ϖ/aℓ and ζ≡z/aℓ, and the relevant index symbol expressions are:

IBT =

2Aℓ+As(1−e2)=2(1−e2)1/2[sin−1ee];

[1.7160030]

Aℓ

=

1e2[sin−1ee−(1−e2)1/2](1−e2)1/2;

[0.6055597]
As =

2e2[(1−e2)−1/2−sin−1ee](1−e2)1/2;

[0.7888807]

aℓ2Aℓℓ

=

14e4{−(3+2e2)(1−e2)+3(1−e2)1/2[sin−1ee]}=[12−(As−Aℓ)4e2];       

[0.3726937]

aℓ2Ass

=

23{(4e2−3)e4(1−e2)+3(1−e2)1/2e4[sin−1ee]}=23[(1−e2)−1−(As−Aℓ)e2];       

[0.7021833]

aℓ2Aℓs

=

1e4{(3−e2)−3(1−e2)1/2[sin−1ee]}=(As−Aℓ)e2,

[0.5092250]

where the eccentricity,

e≡[1−(asaℓ)2]1/2.

NOTE:   The posted numerical evaluations (inside square brackets) assume that the configuration's eccentricity is e=0.6⇒as/aℓ=0.8.

Drawing from our separate "6th Try" discussion — and as has been highlighted here for example — for the axisymmetric configurations under consideration, the e^z and e^ϖ components of the Euler equation become, respectively,

e^z:    

0

=

[1ρ∂P∂z+∂Φ∂z]

e^ϖ:    

j2ϖ3

=

[1ρ∂P∂ϖ+∂Φ∂ϖ]

Multiplying the e^z component through by length (aℓ) and dividing through by the square of the velocity (πGρcaℓ2), we have,

0

=

[1ρ∂P∂z+∂Φ∂z]aℓ(πGρcaℓ2)

 

=

ρcρ⋅∂∂ζ[P(πGρc2aℓ2)]−∂∂ζ[Φ(−πGρcaℓ2)]

⇒∂∂ζ[P(πGρc2aℓ2)]

=

ρρc⋅∂∂ζ[Φ(−πGρcaℓ2)]

 

=

ρρc⋅[2(Aℓsaℓ2)χ2ζ−2Asζ+2(Assaℓ2)ζ3]

Multiplying the e^ϖ component through by length (aℓ) and dividing through by the square of the velocity (πGρcaℓ2), we have,

e^ϖ:    

j2ϖ3⋅aℓ(πGρcaℓ2)

=

[1ρ∂P∂ϖ+∂Φgrav∂ϖ]aℓ(πGρcaℓ2)

 

⇒1χ3⋅j2(πGρcaℓ4)

=

ρcρ⋅∂∂χ[P(πGρc2aℓ2)]−∂∂χ[Φgrav(−πGρcaℓ2)]

Play With Vertical Pressure Gradient

[1(πGρc2aℓ2)]∂P∂ζ =

[1−χ2−ζ2(1−e2)−1][2Aℓsaℓ2χ2ζ−2Asζ+2Assaℓ2ζ3]

  =

[(2Aℓsaℓ2χ2−2As)ζ+2Assaℓ2ζ3]−χ2[(2Aℓsaℓ2χ2−2As)ζ+2Assaℓ2ζ3]−ζ2(1−e2)−1[(2Aℓsaℓ2χ2−2As)ζ+2Assaℓ2ζ3]

  =

(2Aℓsaℓ2χ2−2As)ζ+2Assaℓ2ζ3−(2Aℓsaℓ2χ4−2Asχ2)ζ−2Assaℓ2χ2ζ3−(1−e2)−1[(2Aℓsaℓ2χ2−2As)ζ3+2Assaℓ2ζ5]

  =

[(2Aℓsaℓ2χ2−2As)−(2Aℓsaℓ2χ4−2Asχ2)]ζ+[2Assaℓ2−2Assaℓ2χ2−(1−e2)−1(2Aℓsaℓ2χ2−2As)]ζ3+[−(1−e2)−12Assaℓ2]ζ5.

Integrate over ζ gives …

Pdeduced*≡[1(πGρc2aℓ2)]∫[∂P∂ζ]dζ =

[(Aℓsaℓ2χ2−As)−(Aℓsaℓ2χ4−Asχ2)]⏞coef1ζ2+12[Assaℓ2−Assaℓ2χ2−(1−e2)−1(Aℓsaℓ2χ2−As)]⏟coef2ζ4+13[−(1−e2)−1Assaℓ2]⏞coef3ζ6+const

  =

[−Asζ2+12Assaℓ2ζ4+12(1−e2)−1Asζ4−13(1−e2)−1Assaℓ2ζ6]χ0+[Aℓsaℓ2ζ2+Asζ2−12Assaℓ2ζ4−12(1−e2)−1(Aℓsaℓ2ζ4)]χ2+[−Aℓsaℓ2ζ2]χ4+const.

If I am interpreting this correctly, Pdeduced* should tell how the normalized pressure varies with ζ, for a fixed choice of 0≤χ≤1. Again, for a fixed choice of χ, we want to specify the value of the "const." — hereafter, Cχ — such that Pdeduced*=0 at the surface of the configuration; but at the surface where ρ/ρc=0, it must also be true that,

at the surface   …   ζ2 =

(1−e2)[1−χ2−ρρc0]=(1−e2)(1−χ2).

Hence (numerical evaluations assume χ = 0.6 as well as e = 0.6),

−Cχ =

[(Aℓsaℓ2χ2−As)−(Aℓsaℓ2χ4−Asχ2)]⏞coef1=−0.38756[(1−e2)(1−χ2)]+12[Assaℓ2−Assaℓ2χ2−(1−e2)−1(Aℓsaℓ2χ2−As)]⏟coef2=0.69779[(1−e2)(1−χ2)]2+13[−(1−e2)−1Assaℓ2]⏞coef3=−0.36572[(1−e2)(1−χ2)]3=−0.66807.

Central Pressure

At the center of the configuration — where ζ=χ=0 — we see that,

−Cχ|χ=0 =

[(−As)](1−e2)+12[Assaℓ2+(1−e2)−1As](1−e2)2+13[−(1−e2)−1Assaℓ2](1−e2)3

  =

−As(1−e2)+12[Assaℓ2(1−e2)2+(1−e2)As]−13[(1−e2)2Assaℓ2]

  =

−12[As(1−e2)]+16[Assaℓ2(1−e2)2]

Hence, the central pressure is,

Pc*≡[Pdeduced*]central=Cχ|χ=0 =

12[As(1−e2)]−16[Assaℓ2(1−e2)2].      [0.2045061]


For an oblate-spheroidal configuration having eccentricity, e=0.6⇒as/aℓ=0.8, the figure displayed here, on the right, shows how the normalized gas pressure (Pdeduced*/Pc*) varies with height above the mid-plane (ζ) at three different distances from the symmetry axis: (blue) χ=0.0, (orange) χ=0.6, and (gray) χ=0.75.

circular
marker
color
chosen
χ
resulting …
surface ζ mid-plane
pressure
blue 0.00 0.8000 1.00000
orange 0.60 0.6400 0.32667
gray 0.75 0.52915 0.13085
Ferrers Vertical Pressure
Ferrers Vertical Pressure

Isobaric Surfaces

By design, the mass within our oblate-spheroidal configuration is distributed in such a way that iso-density surfaces are concentric spheroids. As stated earlier, mathematically the relevant density distribution is,

ρ(χ,ζ)ρc

=

[1−χ2−ζ2(1−e2)−1].

In order to determine the relative stability of each configuration, it will be important to ascertain whether or not isobaric surfaces are also concentric spheroids. If they are, then we can say that each configuration obeys a barotropic — but not necessarily a polytropic — equation of state.

Note for later use that,

∂Cχ∂χ =

…

Now Play With Radial Pressure Gradient

After multiplying through by ρ/ρc, the last term on the RHS of the e^ϖ component is given by the expression,

ρρc⋅[1(−πGρcaℓ2)]∂Φgrav∂χ =

2[1−χ2−ζ2(1−e2)−1][(Aℓsaℓ2ζ2−Aℓ)χ+Aℓℓaℓ2χ3]

  =

2[(Aℓsaℓ2ζ2−Aℓ)χ+Aℓℓaℓ2χ3]−2χ2[(Aℓsaℓ2ζ2−Aℓ)χ+Aℓℓaℓ2χ3]−2ζ2(1−e2)−1[(Aℓsaℓ2ζ2−Aℓ)χ+Aℓℓaℓ2χ3]

  =

2(Aℓsaℓ2ζ2−Aℓ)χ+2[Aℓℓaℓ2+(Aℓ−Aℓsaℓ2ζ2)]χ3−2Aℓℓaℓ2χ5+2(1−e2)−1[(Aℓζ2−Aℓsaℓ2ζ4)χ−Aℓℓaℓ2ζ2χ3]

  =

2[(Aℓsaℓ2ζ2−Aℓ)+(1−e2)−1(Aℓζ2−Aℓsaℓ2ζ4)]χ+2[Aℓℓaℓ2+(Aℓ−Aℓsaℓ2ζ2)−(1−e2)−1Aℓℓaℓ2ζ2]χ3−2Aℓℓaℓ2χ5.

If we replace the normalized pressure by Pdeduced*, the first term on the RHS of the e^ϖ component becomes,

∂Pdeduced*∂χ =

∂∂χ{[−Asζ2+12Assaℓ2ζ4+12(1−e2)−1Asζ4−13(1−e2)−1Assaℓ2ζ6]χ0+[Aℓsaℓ2ζ2+Asζ2−12Assaℓ2ζ4−12(1−e2)−1(Aℓsaℓ2ζ4)]χ2+[−Aℓsaℓ2ζ2]χ4+Pc*}

  =

2[Aℓsaℓ2ζ2+Asζ2−12Assaℓ2ζ4−12(1−e2)−1(Aℓsaℓ2ζ4)]χ+4[−Aℓsaℓ2ζ2]χ3

Hence,

1χ3⋅j2(πGρcaℓ4)⋅ρρc

=

[∂Pdeduced*∂χ]−ρρc⋅∂∂χ[Φgrav(−πGρcaℓ2)]

10th Try

Repeating Key Relations

Density:

ρ(ϖ,z)ρc

=

[1−χ2−ζ2(1−e2)−1],

Gravitational Potential:

Φgrav(ϖ,z)(−πGρcaℓ2)

=

12IBT−Aℓχ2−Asζ2+12[(Assaℓ2)ζ4+2(Aℓsaℓ2)χ2ζ2+(Aℓℓaℓ2)χ4].

Vertical Pressure Gradient: [1(πGρc2aℓ2)]∂P∂ζ =

ρρc⋅[2Aℓsaℓ2χ2ζ−2Asζ+2Assaℓ2ζ3]

From the above (9th Try) examination of the vertical pressure gradient, we determined that a reasonably good approximation for the normalized pressure throughout the configuration is given by the expression,

[1(πGρc2aℓ2)]∫[∂P∂ζ]dζ =

[−Asζ2+12Assaℓ2ζ4+12(1−e2)−1Asζ4−13(1−e2)−1Assaℓ2ζ6]χ0+[Aℓsaℓ2ζ2+Asζ2−12Assaℓ2ζ4−12(1−e2)−1(Aℓsaℓ2ζ4)]χ2+[−Aℓsaℓ2ζ2]χ4+const.

If we set χ=0 — that is, if we look along the vertical axis — this approximation should be particularly good, resulting in the expression,

Pz≡{[1(πGρc2aℓ2)]∫[∂P∂ζ]dζ}χ=0 =

Pc*−Asζ2+12Assaℓ2ζ4+12(1−e2)−1Asζ4−13(1−e2)−1Assaℓ2ζ6.

Note that in the limit that z→as — that is, at the pole along the vertical (symmetry) axis where the Pz should drop to zero — we should set ζ→(1−e2)1/2. This allows us to determine the central pressure.

Pc* =

As(1−e2)−12Assaℓ2(1−e2)2−12(1−e2)−1As(1−e2)2+13(1−e2)−1Assaℓ2(1−e2)3

  =

As(1−e2)−12As(1−e2)+13Assaℓ2(1−e2)2−12Assaℓ2(1−e2)2

  =

12As(1−e2)−16Assaℓ2(1−e2)2.

This means that, along the vertical axis, the pressure gradient is,

Pz≡{[1(πGρc2aℓ2)]∫[∂P∂ζ]dζ}χ=0 =

Pc*−Asζ2+12Assaℓ2ζ4+12(1−e2)−1Asζ4−13(1−e2)−1Assaℓ2ζ6.

∂Pz∂ζ =

−2Asζ+2Assaℓ2ζ3+2(1−e2)−1Asζ3−2(1−e2)−1Assaℓ2ζ5.

This should match the more general "vertical pressure gradient" expression when we set, χ=0, that is,

{[1(πGρc2aℓ2)]∂P∂ζ}χ=0 =

[1−χ20−ζ2(1−e2)−1]⋅[2Aℓsaℓ2ζχ20−2Asζ+2Assaℓ2ζ3]

  =

[−2Asζ+2Assaℓ2ζ3]+ζ2(1−e2)−1[2Asζ−2Assaℓ2ζ3]

Yes! The expressions match!

See Also

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