Appendix/Ramblings/ConcentricEllipsoidalCoordinates

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Concentric Ellipsoidal (T6) Coordinates

Background

Building on our general introduction to Direction Cosines in the context of orthogonal curvilinear coordinate systems, and on our previous development of T3 (concentric oblate-spheroidal) and T5 (concentric elliptic) coordinate systems, here we explore the creation of a concentric ellipsoidal (T6) coordinate system. This is motivated by our desire to construct a fully analytically prescribable model of a nonuniform-density ellipsoidal configuration that is an analog to Riemann S-Type ellipsoids.

Orthogonal Coordinates

Primary (radial-like) Coordinate

We start by defining a "radial" coordinate whose values identify various concentric ellipsoidal shells,

λ1

(x2+q2y2+p2z2)1/2.

When λ1=a, we obtain the standard definition of an ellipsoidal surface, it being understood that, q2=a2/b2 and p2=a2/c2. (We will assume that a>b>c, that is, p2>q2>1.)

A vector, n^, that is normal to the λ1 = constant surface is given by the gradient of the function,

F(x,y,z)

(x2+q2y2+p2z2)1/2λ1.

In Cartesian coordinates, this means,

n^(x,y,z)

=

ı^(Fx)+ȷ^(Fy)+k^(Fz)

 

=

ı^[x(x2+q2y2+p2z2)1/2]+ȷ^[q2y(x2+q2y2+p2z2)1/2]+k^[p2z(x2+q2y2+p2z2)1/2]

 

=

ı^(xλ1)+ȷ^(q2yλ1)+k^(p2zλ1),

where it is understood that this expression is only to be evaluated at points, (x,y,z), that lie on the selected λ1 surface — that is, at points for which the function, F(x,y,z)=0. The length of this normal vector is given by the expression,

[n^n^]1/2

=

[(Fx)2+(Fy)2+(Fz)2]1/2

 

=

[(xλ1)2+(q2yλ1)2+(p2zλ1)2]1/2

 

=

1λ13D

where,

3D

[x2+q4y2+p4z2]1/2.

It is therefore clear that the properly normalized normal unit vector that should be associated with any λ1 = constant ellipsoidal surface is,

e^1

n^[n^n^]1/2=ı^(x3D)+ȷ^(q2y3D)+k^(p2z3D).

From our accompanying discussion of direction cosines, it is clear, as well, that the scale factor associated with the λ1 coordinate is,

h12

=

λ123D2.

We can also fill in the top line of our direction-cosines table, namely,

Direction Cosines for T6 Coordinates
γni=hn(λnxi)

n i=x,y,z
1  

x3D
 

q2y3D p2z3D
2

 
---
 

 
---
 

 
---
 

3

 
---
 

 
---
 

 
---
 

Other Coordinate Pair in the Tangent Plane

Let's focus on a particular point on the λ1 = constant surface, (x0,y0,z0), that necessarily satisfies the function, F(x0,y0,z0)=0. We have already derived the expression for the unit vector that is normal to the ellipsoidal surface at this point, namely,

e^1

ı^(x03D)+ȷ^(q2y03D)+ȷ^(p2z03D),

where, for this specific point on the surface,

3D

=

[x02+q4y02+p4z02]1/2.


Tangent Plane
[See, for example, Dan Sloughter's (Furman University) 2001 Calculus III class lecture notes — specifically Lecture 15]


The two-dimensional plane that is tangent to the λ1 = constant surface at this point is given by the expression,

0

=

(xx0)[λ1x]0+(yy0)[λ1y]0+(zz0)[λ1z]0

 

=

(xx0)[Fx]0+(yy0)[Fy]0+(zz0)[Fz]0

 

=

(xx0)(xλ1)0+(yy0)(q2yλ1)0+(zz0)(p2zλ1)0

x(xλ1)0+y(q2yλ1)0+z(p2zλ1)0

=

x0(xλ1)0+y0(q2yλ1)0+z0(p2zλ1)0

xx0+q2yy0+p2zz0

=

x02+q2y02+p2z02

xx0+q2yy0+p2zz0

=

(λ12)0.

Fix the value of λ1. This means that the relevant ellipsoidal surface is defined by the expression,

λ12

=

x2+q2y2+p2z2.

If z=0, the semi-major axis of the relevant x-y ellipse is λ1, and the square of the semi-minor axis is λ12/q2. At any other value, z=z0<c, the square of the semi-major axis of the relevant x-y ellipse is, (λ12p2z02) and the square of the corresponding semi-minor axis is, (λ12p2z02)/q2. Now, for any chosen x02(λ12p2z02), the y-coordinate of the point on the λ1 surface is given by the expression,

y02

=

1q2[λ12p2z0x02].

The slope of the line that lies in the z=z0 plane and that is tangent to the ellipsoidal surface at (x0,y0) is,

mdydx|z0

=

x0q2y0

Speculation1

Building on our experience developing T3 Coordinates and, more recently, T5 Coordinates, let's define the two "angles,"

Z

sinh1(qyx)

      and,      

Υ

sinh1(pzx),

in which case we can write,

λ12

=

x2(cosh2Z+sinh2Υ).

We speculate that the other two orthogonal coordinates may be defined by the expressions,

λ2

x[sinhZ]1/(1q2)=x[qyx]1/(1q2)=x[xqy]1/(q21)=[xq2qy]1/(q21),

λ3

x[sinhΥ]1/(1p2)=x[pzx]1/(1p2)=x[xpz]1/(p21)=[xp2pz]1/(p21).

Some relevant partial derivatives are,

λ2x

=

[1qy]1/(q21)[q2q21]x1/(q21)=[q2q21][xqy]1/(q21)=[q2q21]λ2x;

λ2y

=

[xq2q]1/(q21)[11q2]yq2/(1q2)=[1q21]λ2y;

λ3x

=

[p2p21]λ3x;

λ3z

=

[1p21]λ3z.

And the associated scale factors are,

h22

=

{[(q2q21)λ2x]2+[(1q21)λ2y]2}1

 

=

{(q2q21)2λ22x2+(1q21)2λ22y2}1

 

=

{x2+q4y2}1[(q21)2x2y2λ22];

h32

=

{x2+p4z2}1[(p21)2x2z2λ32].

We can now fill in the rest of our direction-cosines table, namely,

Direction Cosines for T6 Coordinates
γni=hn(λnxi)

n i=x,y,z
1  

x3D
 

q2y3D p2z3D
2

q2yq

xq

0

3

p2zp

0

xp

Hence,

e^2

=

ı^γ21+ȷ^γ22+k^γ23=ı^(q2yq)ȷ^(xq);

e^3

=

ı^γ31+ȷ^γ32+k^γ33=ı^(p2zp)k^(xp).

Check:

e^2e^2

=

(q2yq)2+(xq)2=1;

e^3e^3

=

(p2zp)2+(xp)2=1;

e^2e^3

=

(q2yq)(p2zp)0.

Speculation2

Try,

λ2

=

xy1/q2z1/p2,

in which case,

λ2x

=

λ2x,

λ2y

=

xz1/p2(1q2)y1/q21=λ2q2y,

λ2z

=

λ2p2z.

The associated scale factor is, then,

h22

=

[(λ2x)2+(λ2y)2+(λ2z)2]1

 

=

[(λ2x)2+(λ2q2y)2+(λ2p2z)2]1


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