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*From*: Bob Sciamanda <trebor@VELOCITY.NET>*Date*: Sun, 11 Feb 2001 12:11:11 -0500

Dave, your method is a version of Smythe's "oblate spheroidal harmonics"

method where he, too, makes a transformation to boundary matching

coordinates (his section 5.271)

His handling of the disc (pg 111-114, section 5.00 & ff) is quite

different and would interest you. Because you'll probably have difficulty

finding Smythe, let me try to outline at least the beginning of his

method:

The equation of a surface is F(x,y,z) = C; for each value of C this will

be used as an equipotential surface: V = f(C).

He then applies Laplace's equation DEL^2 V = 0 and gets

DEL^2 V = f''(C)*{Grad C}^2 + f'(C)*DEL^2 C=0 =>

DEL^2 C/{Grad C}^2 = - f''(C)/f'(C) = G(C) That this is a function only

of C is then the requirement that F(x,y,z)=C can be an equipotential .

He then integrates this to get the potential (much skipped):

V = f(C) = A INT exp{-INT G(C) dC} dC + B. A & B are determined by

specifying the potential on two of the surfaces.

He then applies this to the "nonintersecting confocal conicoids"

x^2/(a^2+C) + y^2/(b^2+C) + z^2/c^2+C) = 1 and explicitly solves the disc

as a special case.

In his section 5.271 he develops the "oblate spheroidal coordinates" by

taking

b=c , y = r*cos(phi) and z = r* sin(phi) . . . .

I hope you can get Smythe, cuz I'm sure the above is over-simplified and

bungled. (I could mail you a photocopy, if needed.)

Bob Sciamanda

Physics, Edinboro Univ of PA (em)

trebor@velocity.net

http://www.velocity.net/~trebor

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