ParabolicDensity/Axisymmetric/Structure

From JETohlineWiki
Revision as of 20:59, 7 November 2024 by Joel2 (talk | contribs) (8th Try)
Jump to navigation Jump to search

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

=

[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]

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

IBT =

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

A

=

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

As =

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

a2A

=

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

32a2Ass

=

(4e23)e4(1e2)+3(1e2)1/2e4[sin1ee];

a2As

=

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

where the eccentricity,

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

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 through by length (a) and dividing through by the square of the velocity (πGρca2), we have,

e^z:    

0

=

[1ρPz+Φz]a(πGρca2)

 

 

=

ρcρζ[P(πGρc2a2)]ζ[Φ(πGρca2)]

e^ϖ:    

j2ϖ3a(πGρca2)

=

[1ρPϖ+Φϖ]a(πGρca2)

 

1χ3j2(πGρca4)

=

ρcρχ[P(πGρc2a2)]χ[Φ(πGρca2)]

9th Try

Starting Key Relations

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]

Play With Vertical Pressure Gradient

[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 …

[1(πGρc2a2)][Pζ]dζ =

[(Asa2χ2As)(Asa2χ4Asχ2)]ζ2+12[Assa2Assa2χ2(1e2)1(Asa2χ2As)]ζ4+13[(1e2)1Assa2]ζ6+const

  =

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

Now Play With Radial Pressure Gradient

[1(πGρca2)]Φχ =

ρρc{2Aχ+12[4(Asa2)ζ2χ+4(Aa2)χ3]}

  =

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

Add a term j2(j42χ4+j62χ6) to account for centrifugal acceleration …

[1(πGρc2a2)]Pχ=[1(πGρca2)]Φχ+j2χ3[ρρc] =

2[(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)]χ+2[Aa2+(AAsa2ζ2)(1e2)1Aa2ζ2]χ32Aa2χ5+j2χ3[1χ2ζ2(1e2)1]

  =

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

   

+(j42χ4+j62χ6)χ3(j42χ4+j62χ6)χ3[χ2](j42χ4+j62χ6)χ3[ζ2(1e2)1]

  =

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

   

+(j42χ+j62χ3)(j42χ+j62χ3)[ζ2(1e2)1](j42χ3+j62χ5)

  =

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

   

[j42ζ2(1e2)1j42]χ[j42+j62ζ2(1e2)1j62]χ3[j62]χ5

  =

[2(Asa2ζ2A)+2(1e2)1(Aζ2Asa2ζ4)j42ζ2(1e2)1+j42]χ

   

+[2Aa2+2(AAsa2ζ2)2(1e2)1Aa2ζ2j42j62ζ2(1e2)1+j62]χ3+[j622Aa2]χ5

Integrate over χ gives …

[1(πGρc2a2)][Pχ]dχ =

[(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)12j42ζ2(1e2)1+12j42]χ2

   

+[12Aa2+12(AAsa2ζ2)12(1e2)1Aa2ζ214j4214j62ζ2(1e2)1+14j62]χ4[16j62+13Aa2]χ6

Compare Pair of Integrations

  Integration over ζ Integration over χ
χ0 Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6 none
χ2

Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)

(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)12j42ζ2(1e2)1+12j42

χ4

Asa2ζ2

12Aa2+12(AAsa2ζ2)12(1e2)1Aa2ζ214j4214j62ζ2(1e2)1+14j62

χ6

none

16j6213Aa2

Try, j62=[2Aa2] and 12j42=[A+(Asa2)ζ2].

  Integration over ζ Integration over χ
χ0 Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6 none
χ2 Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)

(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)12j42ζ2(1e2)1+12j42
=
(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)[A+(Asa2)ζ2]ζ2(1e2)1+[A+(Asa2)ζ2]
=
2(Asa2)ζ2[1ζ2(1e2)1]

χ4

Asa2ζ2

12Aa2+12(AAsa2ζ2)12(1e2)1Aa2ζ214j4214[2Aa2]ζ2(1e2)1+14[2Aa2]
=
14[2(AAsa2ζ2)2[A+(Asa2)ζ2]]=Asa2ζ2

χ6

none

0

What expression for j42 is required in order to ensure that the χ2 term is the same in both columns?

12j42[1ζ2(1e2)1] =

[Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)][(Asa2ζ2A)+(1e2)1(Aζ2Asa2ζ4)]

  =

[Asζ212Assa2ζ412(1e2)1(Asa2ζ4)]+[(A)(1e2)1(Aζ2)+(1e2)1(Asa2ζ4)]

  =

[Asζ212Assa2ζ4+12(1e2)1(Asa2)ζ4]+A[1(1e2)1ζ2]

12j42[1ζ2(1e2)1]A[1ζ2(1e2)1] =

12(1e2)1(Asa2)ζ4+[As]ζ212[Assa2]ζ4

Now, considering the following three relations …

32(Assa2)

=

(1e2)1(Asa2);

As

=

A+e2(Asa2);

e2(Asa2)

=

23A;

we can write,

12j42[1ζ2(1e2)1]A[1ζ2(1e2)1] =

12(1e2)1(Asa2)ζ4+[A+e2(Asa2)]ζ213[(1e2)1(Asa2)]ζ4

3j42[1ζ2(1e2)1]3A[22ζ2(1e2)1] =

3(1e2)1(Asa2)ζ4+6[A+e2(Asa2)]ζ22[(1e2)1(Asa2)]ζ4

 

=

(Asa2){2ζ4+3ζ4(1e2)1+6e2ζ2}2ζ4(1e2)1+6Aζ2

 

=

2ζ4(1e2)1+6Aζ2+[23A]{2ζ4+3ζ4(1e2)1+6e2ζ2}1e2

 

=

2ζ4(1e2)13A{2ζ4+3ζ4(1e2)1+4e2ζ2}1e2+{4ζ4+6ζ4(1e2)1+12e2ζ2}1e2


3j42[1ζ2(1e2)1] =

2ζ4(1e2)1+3A(1e2)1e2{[2e2(1e2)2e2ζ2][2ζ4(1e2)+3ζ4+4e2(1e2)ζ2]}+{4ζ4+6ζ4(1e2)1+12e2ζ2}1e2

10th Try

Repeating Key Relations

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!

Shift to ξ1 Coordinate

In an accompanying chapter, we defined the coordinate,

(ξ1as)2

(ϖa)2+(zas)2=χ2+ζ2(1e2)1.

Given that we want the pressure to be constant on ξ1 surfaces, it seems plausible that ζ2 should be replaced by (1e2)(ξ1/as)2=[(1e2)χ2+ζ2] in the expression for Pz. That is, we might expect the expression for the pressure at any point in the meridional plane to be,

Ptest01 =

Pc*As[(1e2)χ2+ζ2]1+12[Assa2+(1e2)1As][(1e2)χ2+ζ2]213(1e2)1Assa2[(1e2)χ2+ζ2]3

  =

Pc*As[(1e2)χ2+ζ2]1+12[Assa2+(1e2)1As][(1e2)2χ4+2(1e2)χ2ζ2+ζ4]13(1e2)1Assa2[(1e2)χ2+ζ2][(1e2)2χ4+2(1e2)χ2ζ2+ζ4]

  =

Pc*As[(1e2)χ2+ζ2]+12[Assa2+(1e2)1As][(1e2)2χ4+2(1e2)χ2ζ2+ζ4]

   

13Assa2[(1e2)2χ6+2(1e2)χ4ζ2+χ2ζ4]13Assa2[(1e2)χ4ζ2+2χ2ζ4+(1e2)1ζ6]

  =

χ0{Pc*Asζ2+12[Assa2+(1e2)1As]ζ413Assa2(1e2)1ζ6}+χ2{As(1e2)+12[Assa2+(1e2)1As]2(1e2)ζ213Assa2ζ423Assa2ζ4}

   

+χ4{12[Assa2+(1e2)1As](1e2)223Assa2(1e2)ζ213Assa2(1e2)ζ2}+χ6{13Assa2(1e2)2}

  =

χ0{Pc*Asζ2+12[Assa2+(1e2)1As]ζ413Assa2(1e2)1ζ6}+χ2{As(1e2)+12[Assa2+(1e2)1As]2(1e2)ζ2Assa2ζ4}

   

+χ4{12[Assa2+(1e2)1As](1e2)2Assa2(1e2)ζ2}+χ6{13Assa2(1e2)2}

  Integration over ζ Pressure Guess
χ0 Asζ2+12Assa2ζ4+12(1e2)1Asζ413(1e2)1Assa2ζ6

Pc*Asζ2+12[Assa2+(1e2)1As]ζ413Assa2(1e2)1ζ6

χ2

Asa2ζ2+Asζ212Assa2ζ412(1e2)1(Asa2ζ4)

As(1e2)+12[Assa2+(1e2)1As]2(1e2)ζ2Assa2ζ4

χ4

Asa2ζ2

12[Assa2+(1e2)1As](1e2)2Assa2(1e2)ζ2

χ6

none

13Assa2(1e2)2

Compare Vertical Pressure Gradient Expressions

From our above (9th try) derivation we know that the vertical pressure gradient is given by the expression,

[1(πGρc2a2)]Pζ =

[1χ2ζ2(1e2)1][2Asa2χ2ζ2Asζ+2Assa2ζ3]

  =

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

  =

[2As(χ21)+2Asa2(1χ2)χ2]ζ+[2Assa2(1χ2)2Asa2(1e2)1χ2+2(1e2)1As]ζ3+[2Assa2(1e2)1]ζ5.

By comparison, the vertical derivative of our "test01" pressure expression gives,

Ptest01 =

χ0{Pc*Asζ2+12[Assa2+(1e2)1As]ζ413Assa2(1e2)1ζ6}+χ2{As(1e2)+12[Assa2+(1e2)1As]2(1e2)ζ2Assa2ζ4}

   

+χ4{12[Assa2+(1e2)1As](1e2)2Assa2(1e2)ζ2}+χ6{13Assa2(1e2)2}

Ptest01ζ =

χ0{2Asζ+2[Assa2+(1e2)1As]ζ32Assa2(1e2)1ζ5}+χ2{2[Assa2+(1e2)1As](1e2)ζ4Assa2ζ3}+χ4{2Assa2(1e2)ζ}

  =

ζ1{2As+2[Assa2+(1e2)1As](1e2)χ22Assa2(1e2)χ4}+ζ3{2[Assa2+(1e2)1As]4Assa2χ2}+ζ5{2Assa2(1e2)1}

  =

ζ1{2As(χ21)+2Assa2(1e2)χ2(1χ2)}+ζ3{2Assa2(12χ2)+2(1e2)1As}+ζ5{2Assa2(1e2)1}

Instead, try …

Ptest02Pc =

p2(ρρc)2+p3(ρρc)3

ζ[Ptest02Pc] =

2p2(ρρc)ζ[ρρc]+3p3(ρρc)2ζ[ρρc]

  =

(ρρc){2p2+3p3(ρρc)}ζ[ρρc]

  =

(ρρc){2p2+3p3[1χ2ζ2(1e2)1]}ζ[1χ2ζ2(1e2)1]

  =

(ρρc){(2p2+3p3)3p3χ23p3ζ2(1e2)1}[2ζ(1e2)1]

  =

(ρρc)(1e2)2{6p3χ2ζ(1e2)2(2p2+3p3)(1e2)ζ+6p3ζ3}

Compare the term inside the curly braces with the term, from the beginning of this subsection, inside the square brackets, namely,

2Asa2χ2ζ2Asζ+2Assa2ζ3 =

2e4[(3e2)Υ]χ2ζ[4e2(113Υ)]ζ+43e4[4e23(1e2)+Υ]ζ3

  =

13e4(1e2){6[(3e2)Υ](1e2)χ2ζ[12e2(113Υ)](1e2)ζ+4[(4e23)+Υ]ζ3}.

Pretty Close!!

Alternatively:   according to the third term, we need to set,

6p3 =

4[(4e23)+Υ]

Υ =

32p3+(34e2)

in which case, the first coefficient must be given by the expression,

[(3e2)Υ] =

(3e2)32p3+(4e23)]=[3e232p3].

And, from the second coefficient, we find,

2(2p2+3p3) =

[12e2(113Υ)]

2p2 =

2e2(3Υ)3p3

 

=

3p3+6e22e2[32p3+(34e2)]

 

=

3p3+6e2[3e2p3+6e28e4]

 

=

8e43p3(1+e2);

or,

p2

=

4e4(1+e2)[(4e23)+Υ]

 

=

4e4(1+e2)(4e23)(1+e2)Υ

 

=

4e4[4e23+4e43e2](1+e2)Υ

 

=

3e2(1+e2)Υ


SUMMARY:

Ptest02Pc =

p2(ρρc)2+p3(ρρc)3,

p2

=

3e2(1+e2)Υ=e4(Asa2)e2Υ,

p3 =

23[(4e23)+Υ]=e4(Assa2)+23e2Υ.


Note:   according to the first term, we need to set,

p3 =

[(3e2)Υ]

Υ =

[(3e2)p3],

in which case, the third coefficient must be given by the expression,

4[(4e23)+Υ] =

4[(4e23)+(3e2)p3]=4[3e2p3].

And, from the second coefficient, we find,

2(2p2+3p3) =

[12e2(113Υ)]

2p2 =

2e2(3Υ)3p3

 

=

2e2[3[(3e2)p3]]3p3

 

=

2e2[e2+p3]3p3

 

=

2e4+(2e23)p3;

or,

2p2

=

2e4+(2e23)[(3e2)Υ]

 

=

2e4+(2e23)(3e2)(2e23)Υ

 

=

2e4+(6e22e49+3e2)(2e23)Υ

 

=

9(e21)(2e23)Υ

Better yet, try …

Ptest03Pc =

p2(ρρc)2[1β(1ρρc)]=p2(ρρc)2[(1β)+β(ρρc)]

ζ[Ptest03Pc] =

where, in the case of a spherically symmetric parabolic-density configuration, β=1/2. Well … this wasn't a bad idea, but as it turns out, this "test03" expression is no different from the "test02" guess. Specifically, the "test03" expression can be rewritten as,

Ptest03Pc =

p2(1β)(ρρc)2+p2β(ρρc)3,

which has the same form as the "test02" expression.

Test04

From above, we understand that, analytically,

[1(πGρc2a2)]Pζ =

[1χ2ζ2(1e2)1][2Asa2χ2ζ2Asζ+2Assa2ζ3]

  =

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

  =

[2As(χ21)+2Asa2(1χ2)χ2]ζ+[2Assa2(1χ2)2Asa2(1e2)1χ2+2(1e2)1As]ζ3+[2Assa2(1e2)1]ζ5.

Also from above, we have shown that if,

Ptest02Pc =

p2(ρρc)2+p3(ρρc)3

SUMMARY from test02:

p2

=

3e2(1+e2)Υ=e4(Asa2)e2Υ,

p3 =

23[(4e23)+Υ]=e4(Assa2)+23e2Υ.

ζ[Ptest02Pc] =

(ρρc)(1e2)2{6p3χ2ζ(1e2)2(2p2+3p3)(1e2)ζ+6p3ζ3}

  =

(ρρc)(1e2)2{6[e4(Assa2)+23e2Υ]χ2ζ(1e2)2[2e4(Asa2)+3e4(Assa2)](1e2)ζ+6[e4(Assa2)+23e2Υ]ζ3}




Here (test04), we add a term that is linear in the normalized density, which means,

Ptest04Pc =

Ptest02Pc+p1(ρρc)

ζ[Ptest04Pc] =

ζ[Ptest02Pc]+ζ[p1(ρρc)]=ζ[Ptest02Pc]+p1ζ[1χ2ζ2(1e2)1]

See Also

Tiled Menu

Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS |