ParabolicDensity/Axisymmetric/Structure: Difference between revisions

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(\mathrm{coef1}) \cdot \biggl[ \zeta^2 - (1-e^2)( 1 - \chi^2 \biggr]  
(\mathrm{coef1}) \cdot \biggl[ \zeta^2 - (1-e^2)( 1 - \chi^2) \biggr]  
+  (\mathrm{coef2} )\cdot \biggl[ \zeta^4 - (1-e^2)^2( 1 - \chi^2)^2 \biggr]
+  (\mathrm{coef2} )\cdot \biggl[ \zeta^4 - (1-e^2)^2( 1 - \chi^2)^2 \biggr]
+  ( \mathrm{coef3}) \cdot \biggl[ \zeta^6 - (1-e^2)^3( 1 - \chi^2)^3\biggr]
+  ( \mathrm{coef3}) \cdot \biggl[ \zeta^6 - (1-e^2)^3( 1 - \chi^2)^3\biggr]

Latest revision as of 15:36, 16 November 2024

Parabolic Density Distribution[edit]


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[edit]

Tentative Summary[edit]

Known Relations[edit]

Density:

ρ(ϖ,z)ρc

=

[1χ2ζ2(1e2)1],

Gravitational Potential:

Φgrav(ϖ,z)(πGρca2)

=

12IBTAχ2Asζ2+12[(Assa2)ζ4+2(Asa2)χ2ζ2+(Aa2)χ4].

 

ζ[Φgrav(πGρca2)]

=

2(Asa2)χ2ζ2Asζ+2(Assa2)ζ3.

 

and,     χ[Φgrav(πGρca2)]

=

2(Asa2)χζ22Aχ+2(Aa2)χ3.

where, χϖ/a and ζz/a, and the relevant index symbol expressions are:

IBT =

2A+As(1e2)=2(1e2)1/2[sin1ee];

[1.7160030]

A

=

1e2[sin1ee(1e2)1/2](1e2)1/2;

[0.6055597]
As =

2e2[(1e2)1/2sin1ee](1e2)1/2;

[0.7888807]

a2A

=

14e4{(3+2e2)(1e2)+3(1e2)1/2[sin1ee]}=[12(AsA)4e2];       

[0.3726937]

a2Ass

=

23{(4e23)e4(1e2)+3(1e2)1/2e4[sin1ee]}=23[(1e2)1(AsA)e2];       

[0.7021833]

a2As

=

1e4{(3e2)3(1e2)1/2[sin1ee]}=(AsA)e2,

[0.5092250]

where the eccentricity,

e[1(asa)2]1/2.

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

=

[1ρPz+Φz]

e^ϖ:    

j2ϖ3

=

[1ρPϖ+Φϖ]

Multiplying the e^z component through by length (a) and dividing through by the square of the velocity (πGρca2), we have,

0

=

[1ρPz+Φz]a(πGρca2)

 

=

ρcρζ[P(πGρc2a2)]ζ[Φ(πGρca2)]

ζ[P(πGρc2a2)]

=

ρρcζ[Φ(πGρca2)]

 

=

ρρc[2(Asa2)χ2ζ2Asζ+2(Assa2)ζ3]

Multiplying the e^ϖ component through by length (a) and dividing through by the square of the velocity (πGρca2), we have,

e^ϖ:    

j2ϖ3a(πGρca2)

=

[1ρPϖ+Φgravϖ]a(πGρca2)

 

1χ3j2(πGρca4)

=

ρcρχ[P(πGρc2a2)]χ[Φgrav(πGρca2)]

Play With Vertical Pressure Gradient[edit]

[1(πGρc2a2)]Pζ =

[1χ2ζ2(1e2)1][2Asa2χ2ζ2Asζ+2Assa2ζ3]

  =

[(2Asa2χ22As)ζ+2Assa2ζ3]χ2[(2Asa2χ22As)ζ+2Assa2ζ3]ζ2(1e2)1[(2Asa2χ22As)ζ+2Assa2ζ3]

  =

(2Asa2χ22As)ζ+2Assa2ζ3(2Asa2χ42Asχ2)ζ2Assa2χ2ζ3(1e2)1[(2Asa2χ22As)ζ3+2Assa2ζ5]

  =

[(2Asa2χ22As)(2Asa2χ42Asχ2)]ζ+[2Assa22Assa2χ2(1e2)1(2Asa2χ22As)]ζ3+[(1e2)12Assa2]ζ5.

Integrate over ζ gives …

Pdeduced*[1(πGρc2a2)][Pζ]dζ =

[(Asa2χ2As)(Asa2χ4Asχ2)]coef1ζ2+12[Assa2Assa2χ2(1e2)1(Asa2χ2As)]coef2ζ4+13[(1e2)1Assa2]coef3ζ6+const

  =

[Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6]χ0+[Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)]χ2+[Asa2ζ2]χ4+const.

If I am interpreting this correctly, Pdeduced* should tell how the normalized pressure varies with ζ, for a fixed choice of 0χ1. 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 =

(1e2)[1χ2ρρc0]=(1e2)(1χ2).

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

Cχ =

[(Asa2χ2As)(Asa2χ4Asχ2)]coef1=0.38756[(1e2)(1χ2)]+12[Assa2Assa2χ2(1e2)1(Asa2χ2As)]coef2=0.69779[(1e2)(1χ2)]2+13[(1e2)1Assa2]coef3=0.36572[(1e2)(1χ2)]3=0.66807.

Central Pressure

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

Cχ|χ=0 =

[(As)](1e2)+12[Assa2+(1e2)1As](1e2)2+13[(1e2)1Assa2](1e2)3

  =

As(1e2)+12[Assa2(1e2)2+(1e2)As]13[(1e2)2Assa2]

  =

12[As(1e2)]+16[Assa2(1e2)2]

Hence, the central pressure is,

Pc*[Pdeduced*]central=Cχ|χ=0 =

12[As(1e2)]16[Assa2(1e2)2].      [0.2045061]


For an oblate-spheroidal configuration having eccentricity, e=0.6as/a=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

Inserting the expression for Cλ into our derived expression for Pdeduced* gives,


Pdeduced* =

(coef1)[ζ2(1e2)(1χ2)]+(coef2)[ζ4(1e2)2(1χ2)2]+(coef3)[ζ6(1e2)3(1χ2)3].




Note for later use that,

Cχχ =

Isobaric Surfaces[edit]

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, the relevant mathematically prescribed density distribution is,

ρ(χ,ζ)ρc

=

[1χ2ζ2(1e2)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; see, for example, the accompanying relevant excerpt drawn from p. 466 of 📚 Lebovitz (1967).) In an effort to make this determination for our e=0.6 spheroid, we first examine the iso-density surface for which ρ/ρc=0.3. Via the expression,

ζ2

=

(1e2)[1χ2ρρc]=0.64[1χ20.3],

we can immediately determine that our three chosen radial cuts (χ=0.0,0.6,0.75) intersect this iso-density surface at the vertical locations, respectively, ζ=0.66933,0.46648,0.29665; these numerical values have been recorded in the following table. The table also contains coordinates for the points where our three cuts intersect the (e=0.6) iso-density surface for which ρ/ρc=0.6.

diamond
marker
color
chosen
ρ/ρc
chosen
χ
resulting …
    ζ     normalized
pressure
green 0.3 0.00 0.66933 0.060466
0.60 0.46648 0.057433
0.75 0.29665 0.055727
purple 0.6 0.00 0.50596 0.292493
0.60 0.16000 0.280361
0.75 n/a n/a

For each of these five (χ,ζ) coordinate pairs, we have used our above derived expression for Pdeduced*/Pc* to calculate the "normalized pressure" at the relevant point inside the configuration. These results appear in the last column of the table; they also have been marked in the accompanying figure: dark green diamonds mark the points relevant to our choice of ρ/ρc=0.3 and purple diamonds mark the points relevant to our choice of ρ/ρc=0.6. Notice that the normalized density is everywhere lower than 0.6 along the χ=0.75 cut, so the final row in the table has been marked "n/a" (not applicable).

The dark green diamond-shaped markers in the figure — along with the associated tabular data — show that at three separate points along the ρ/ρc=0.3 iso-density surface, the normalized pressure is nearly — but not exactly — the same; its value is approximately 0.057. Similarly, the purple diamond-shaped markers show that at two separate points along the ρ/ρc=0.6 iso-density surface, the normalized pressure is nearly the same; in this case its value is approximately 0.28. This seems to indicate that, throughout our configuration, the isobaric surfaces are almost — but not exactly — aligned with iso-density surfaces.

Now Play With Radial Pressure Gradient[edit]

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

ρρc[1(πGρca2)]Φgravχ =

2[1χ2ζ2(1e2)1][(Asa2ζ2A)χ+Aa2χ3]

  =

2[(Asa2ζ2A)χ+Aa2χ3]2χ2[(Asa2ζ2A)χ+Aa2χ3]2ζ2(1e2)1[(Asa2ζ2A)χ+Aa2χ3]

  =

2(Asa2ζ2A)χ+2[Aa2+(AAsa2ζ2)]χ32Aa2χ5+2(1e2)1[(Aζ2Asa2ζ4)χAa2ζ2χ3]

  =

2[(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)]χ+2[Aa2+(AAsa2ζ2)(1e2)1Aa2ζ2]χ32Aa2χ5.

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

Pdeduced*χ =

χ{[Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6]χ0+[Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)]χ2+[Asa2ζ2]χ4+Pc*}

  =

2[Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)]χ+4[Asa2ζ2]χ3

Hence,

1χ3j2(πGρca4)ρρc

=

[Pdeduced*χ]ρρcχ[Φgrav(πGρca2)]

10th Try[edit]

Repeating Key Relations[edit]

Density:

ρ(ϖ,z)ρc

=

[1χ2ζ2(1e2)1],

Gravitational Potential:

Φgrav(ϖ,z)(πGρca2)

=

12IBTAχ2Asζ2+12[(Assa2)ζ4+2(Asa2)χ2ζ2+(Aa2)χ4].

Vertical Pressure Gradient: [1(πGρc2a2)]Pζ =

ρρc[2Asa2χ2ζ2Asζ+2Assa2ζ3]

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(πGρc2a2)][Pζ]dζ =

[Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6]χ0+[Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)]χ2+[Asa2ζ2]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(πGρc2a2)][Pζ]dζ}χ=0 =

Pc*Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6.

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

Pc* =

As(1e2)12Assa2(1e2)212(1e2)1As(1e2)2+13(1e2)1Assa2(1e2)3

  =

As(1e2)12As(1e2)+13Assa2(1e2)212Assa2(1e2)2

  =

12As(1e2)16Assa2(1e2)2.

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

Pz{[1(πGρc2a2)][Pζ]dζ}χ=0 =

Pc*Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6.

Pzζ =

2Asζ+2Assa2ζ3+2(1e2)1Asζ32(1e2)1Assa2ζ5.

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

{[1(πGρc2a2)]Pζ}χ=0 =

[1χ20ζ2(1e2)1][2Asa2ζχ202Asζ+2Assa2ζ3]

  =

[2Asζ+2Assa2ζ3]+ζ2(1e2)1[2Asζ2Assa2ζ3]

Yes! The expressions match!

See Also[edit]

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