User:Tohline/Appendix/Ramblings/ConcentricEllipsodalCoordinates
From VisTrailsWiki
Contents |
Concentric Ellipsoidal (T6) Coordinates
![]() |
---|
| Tiled Menu | Tables of Content | Banner Video | Tohline Home Page | |
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,
|
|
|
When , we obtain the standard definition of an ellipsoidal surface, it being understood that,
and
. (We will assume that
, that is,
.)
A vector, , that is normal to the
= constant surface is given by the gradient of the function,
|
|
|
In Cartesian coordinates, this means,
|
|
|
|
|
|
|
|
|
where it is understood that this expression is only to be evaluated at points, , that lie on the selected
surface — that is, at points for which the function,
. The length of this normal vector is given by the expression,
|
|
|
|
|
|
|
|
|
where,
|
|
|
It is therefore clear that the properly normalized normal unit vector that should be associated with any = constant ellipsoidal surface is,
|
|
|
From our accompanying discussion of direction cosines, it is clear, as well, that the scale factor associated with the coordinate is,
|
|
|
We can also fill in the top line of our direction-cosines table, namely,
Direction Cosines for T6 Coordinates
|
|||
![]() |
![]() | ||
![]() |
| ![]() | ![]() |
![]() |
|
|
|
![]() |
|
|
|
Other Coordinate Pair in the Tangent Plane
Let's focus on a particular point on the = constant surface,
, that necessarily satisfies the function,
. We have already derived the expression for the unit vector that is normal to the ellipsoidal surface at this point, namely,
|
|
|
where, for this specific point on the surface,
|
|
|
Tangent Plane The two-dimensional plane that is tangent to the
|
Fix the value of . This means that the relevant ellipsoidal surface is defined by the expression,
|
|
|
If , the semi-major axis of the relevant x-y ellipse is
, and the square of the semi-minor axis is
. At any other value,
, the square of the semi-major axis of the relevant x-y ellipse is,
and the square of the corresponding semi-minor axis is,
. Now, for any chosen
, the y-coordinate of the point on the
surface is given by the expression,
|
|
|
The slope of the line that lies in the z = z0 plane and that is tangent to the ellipsoidal surface at is,
|
|
|
Speculation1
Building on our experience developing T3 Coordinates and, more recently, T5 Coordinates, let's define the two "angles,"
|
|
|
and, |
|
|
|
in which case we can write,
|
|
|
We speculate that the other two orthogonal coordinates may be defined by the expressions,
|
|
|
|
|
|
Some relevant partial derivatives are,
|
|
|
|
|
|
|
|
|
|
|
|
And the associated scale factors are,
|
|
|
|
|
|
|
|
|
|
|
|
We can now fill in the rest of our direction-cosines table, namely,
Direction Cosines for T6 Coordinates
|
|||
![]() |
![]() | ||
![]() |
| ![]() | ![]() |
![]() |
|
|
|
![]() |
|
|
|
Hence,
|
|
|
|
|
|
Check:
|
|
|
|
|
|
|
|
|
Speculation2
Try,
|
|
|
in which case,
|
|
|
|
|
|
|
|
|
The associated scale factor is, then,
|
|
|
|
|
|
See Also
![]() |
---|
© 2014 - 2020 by Joel E. Tohline |