Appendix/Ramblings/T4Integrals

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Integrals of Motion in T4 Coordinates

In an accompanying Wiki document, we have derived the properties of an orthogonal, axisymmetric, T3 coordinate system in which the first coordinate, λ1, defines a family of concentric oblate-spheroidal surfaces whose (uniform) flattening is defined by a parameter qReq/Zpole. In a separate, but related, Wiki document, we attempt to derive the 3rd isolating integral of motion for massless particles that move inside a flattened, axisymmetric potential whose equipotential surfaces align with λ1=constant surfaces in the special (quadratic) case when q2=2. While examining this special case, we noticed that, in T3 Coordinates, the h1 and h2 scale factors are only a function of the coordinate ratio λ1/λ2. This has led us to wonder whether it might be more fruitful to search for the 3rd isolating integral using a coordinate system in which one of the coordinates is defined by this T3-coordinate ratio.

It is with this in mind that we explore the development of a new T4 coordinate system. From the very beginning we will restrict the T4-coordinate definition to the special case of q2=2 because, at present, we think that the coordinate T3-coordinate ratio λ1/λ2 is only interesting in the quadratic case. (See, for example, the polynomial root derived to complete the T1-coordinate inversion for the cubic case q2=3; it is another combination of the T3 coordinates that appears to be relevant in the cubic case.)

STOP!

(7/06/2010)

As defined, below, this is not an orthogonal coordinate system.

Definition

In what follows, the coordinates (λ1,λ2,λ3) refer to T3 Coordinates. Let's define a set of orthogonal T4 Coordinates for the special (quadratic) case q2=2 such that,

ξ1

(λ12+λ22)1/2

=

ϖ[1+sinh2Z+(sinhZ)2/(1q2)]1/2

(q2=2)

ϖ[1+sinh2Z+1sinh2Z]1/2;

ξ2

λ2λ1

=

[(sinhZ)2/(1q2)1+sinh2Z]1/2

(q2=2)

[1sinh2Z(1+sinh2Z)]1/2;

tanξ3

yx,

 

 

 

 

where,

sinh2Z(qzϖ)2(q2=2)2z2ϖ2.

The coordinate inversion — from (ξ1,ξ2,ξ3) back to (λ1,λ2,λ3) — is straightforward. Specifically,

λ1

=

ξ1cos[tan1ξ2];

λ2

=

ξ1sin[tan1ξ2];

λ3

=

ξ3.

Here are some relevant partial derivatives:

sinh2Zϖ=4z2ϖ3;

sinh2Zz=+4zϖ2.

Partial derivatives with respect to cylindrical coordinates are,

 

ϖ

z

ϕ

ξ1

ϖξ1z2(ϖ2+z2)

12ξ1z3(4z4ϖ4)

0

ξ2

2ξ23z2ϖ5(ϖ2+4z2)

2ξ23zϖ4(ϖ2+4z2)

0

ξ3

0

0

1

Hence, the partials with respect to Cartesian coordinates are,

 

x

y

z

ξ1

x(1q2)ξ1[1+q4z2ϖ2q2ξ12ϖ2]

(q2=2)xξ1z2(ϖ2+z2)

y(1q2)ξ1[1+q4z2ϖ2q2ξ12ϖ2]

(q2=2)yξ1z2(ϖ2+z2)

ϖ2(1q2)ξ1z[1+q4z2ϖ2ξ12ϖ2]

(q2=2)+12ξ1z3(4z4ϖ4)

ξ2

ξ3

yϖ2

+xϖ2

0


The scale factors are,

h12

=

[(ξ1x)2+(ξ1y)2+(ξ1z)2]1

=

[(ξ1ϖ)2+(ξ1z)2]1

=

[4ξ12z6(ϖ2+4z2)(ϖ6+4z6)]

h22

=

[(ξ2x)2+(ξ2y)2+(ξ2z)2]1

=

[(ξ2ϖ)2+(ξ2z)2]1

=

ϖ104ξ26z2[1(ϖ2+4z2)2(ϖ2+z2)]

h32

=

[(ξ3x)2+(ξ3y)2+(ξ3z)2]1

=

ϖ2

 

 

where,        .

The position vector is,

x

=

ı^x+ȷ^y+k^z

=

See Also

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