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===Primary (''radial-like'') Coordinate=== We start by defining a "radial" coordinate whose values identify various concentric ellipsoidal shells, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\lambda_1</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~(x^2 + q^2 y^2 + p^2 z^2)^{1 / 2} \, .</math> </td> </tr> </table> When <math>~\lambda_1 = a</math>, we obtain the standard definition of an ellipsoidal surface, it being understood that, <math>~q^2 = a^2/b^2</math> and <math>~p^2 = a^2/c^2</math>. (We will assume that <math>~a > b > c</math>, that is, <math>~p^2 > q^2 > 1</math>.) A vector, <math>~\bold{\hat{n}}</math>, that is normal to the <math>~\lambda_1</math> = constant surface is given by the gradient of the function, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~F(x, y, z)</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~(x^2 + q^2 y^2 + p^2 z^2)^{1 / 2} - \lambda_1 \, .</math> </td> </tr> </table> In Cartesian coordinates, this means, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\bold{\hat{n}}(x, y, z)</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \hat\imath \biggl( \frac{\partial F}{\partial x} \biggr) + \hat\jmath \biggl( \frac{\partial F}{\partial y} \biggr) + \hat{k} \biggl( \frac{\partial F}{\partial z} \biggr) </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \hat\imath \biggl[ x(x^2 + q^2 y^2 + p^2 z^2)^{- 1 / 2} \biggr] + \hat\jmath \biggl[ q^2y(x^2 + q^2 y^2 + p^2 z^2)^{- 1 / 2} \biggr] + \hat{k}\biggl[ p^2 z(x^2 + q^2 y^2 + p^2 z^2)^{- 1 / 2} \biggr] </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \hat\imath \biggl( \frac{x}{\lambda_1} \biggr) + \hat\jmath \biggl( \frac{q^2y}{\lambda_1} \biggr) + \hat{k}\biggl(\frac{p^2 z}{\lambda_1} \biggr) \, , </math> </td> </tr> </table> where it is understood that this expression is only to be evaluated at points, <math>~(x, y, z)</math>, that lie on the selected <math>~\lambda_1</math> surface — that is, at points for which the function, <math>~F(x,y,z) = 0</math>. The length of this normal vector is given by the expression, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~[ \bold{\hat{n}} \cdot \bold{\hat{n}} ]^{1 / 2}</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \biggl[ \biggl( \frac{\partial F}{\partial x} \biggr)^2 + \biggl( \frac{\partial F}{\partial y} \biggr)^2 + \biggl( \frac{\partial F}{\partial z} \biggr)^2 \biggr]^{1 / 2} </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \biggl[ \biggl( \frac{x}{\lambda_1} \biggr)^2 + \biggl( \frac{q^2y}{\lambda_1} \biggr)^2 + \biggl(\frac{p^2 z}{\lambda_1} \biggr)^2 \biggr]^{1 / 2} </math> </td> </tr> <tr> <td align="right"> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~ \frac{1}{\lambda_1 \ell_{3D}} </math> </td> </tr> </table> where, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\ell_{3D}</math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~\biggl[ x^2 + q^4y^2 + p^4 z^2 \biggr]^{- 1 / 2} \, .</math> </td> </tr> </table> It is therefore clear that the ''properly normalized'' normal unit vector that should be associated with any <math>~\lambda_1</math> = constant ellipsoidal surface is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~\hat{e}_1 </math> </td> <td align="center"> <math>~\equiv</math> </td> <td align="left"> <math>~ \frac{ \bold\hat{n} }{ [ \bold{\hat{n}} \cdot \bold{\hat{n}} ]^{1 / 2} } = \hat\imath (x \ell_{3D}) + \hat\jmath (q^2y \ell_{3D}) + \hat{k} (p^2 z \ell_{3D}) \, . </math> </td> </tr> </table> From our [[Appendix/Ramblings/DirectionCosines#Scale_Factors|accompanying discussion of direction cosines]], it is clear, as well, that the scale factor associated with the <math>~\lambda_1</math> coordinate is, <table border="0" cellpadding="5" align="center"> <tr> <td align="right"> <math>~h_1^2</math> </td> <td align="center"> <math>~=</math> </td> <td align="left"> <math>~\lambda_1^2 \ell_{3D}^2 \, .</math> </td> </tr> </table> We can also fill in the top line of our direction-cosines table, namely, <table border="1" cellpadding="8" align="center" width="60%"> <tr> <td align="center" colspan="4"> '''Direction Cosines for T6 Coordinates''' <br /> <math>~\gamma_{ni} = h_n \biggl( \frac{\partial \lambda_n}{\partial x_i}\biggr)</math> </td> </tr> <tr> <td align="center" width="10%"><math>~n</math></td> <td align="center" colspan="3"><math>~i = x, y, z</math> </tr> <tr> <td align="center"><math>~1</math></td> <td align="center"> <br /> <math>~x\ell_{3D}</math><br /> <td align="center"><math>~q^2 y \ell_{3D}</math> <td align="center"><math>~p^2 z \ell_{3D}</math> </tr> <tr> <td align="center"><math>~2</math></td> <td align="center"> <br /> --- <br /> <td align="center"> <br /> --- <br /> <td align="center"> <br /> --- <br /> </td> </tr> <tr> <td align="center"><math>~3</math></td> <td align="center"> <br /> --- <br /> </td> <td align="center"> <br /> --- <br /> </td> <td align="center"> <br /> --- <br /> </td> </tr> </table>
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