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cylindrical polar coordinates

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21: 36.5 Stokes Sets
For z 0 , the Stokes set is expressed in terms of scaled coordinates
36.5.7 X = 9 20 + 20 u 4 Y 2 20 u 2 + 6 u 2 sign ( z ) ,
36.5.10 160 u 6 + 40 u 4 = Y 2 .
With coordinates
36.5.17 Y S ( X ) = Y ( u , | X | ) ,
22: 31.17 Physical Applications
Introduce elliptic coordinates z 1 and z 2 on S 2 . Then
31.17.2 x s 2 z k + x t 2 z k 1 + x u 2 z k a = 0 , k = 1 , 2 ,
23: 14.19 Toroidal (or Ring) Functions
§14.19(i) Introduction
This form of the differential equation arises when Laplace’s equation is transformed into toroidal coordinates ( η , θ , ϕ ) , which are related to Cartesian coordinates ( x , y , z ) by …
24: Howard S. Cohl
Cohl has published papers in orthogonal polynomials and special functions, and is particularly interested in fundamental solutions of linear partial differential equations on Riemannian manifolds, associated Legendre functions, generalized and basic hypergeometric functions, eigenfunction expansions of fundamental solutions in separable coordinate systems for linear partial differential equations, orthogonal polynomial generating function and generalized expansions, and q -series. …
25: Bibliography T
  • C. A. Tracy and H. Widom (1997) On exact solutions to the cylindrical Poisson-Boltzmann equation with applications to polyelectrolytes. Phys. A 244 (1-4), pp. 402–413.
  • 26: 9.16 Physical Applications
    The use of Airy function and related uniform asymptotic techniques to calculate amplitudes of polarized rainbows can be found in Nussenzveig (1992) and Adam (2002). …
    27: 1.15 Summability Methods
    A ( r , θ ) is a harmonic function in polar coordinates (1.9.27), and …
    28: 19.26 Addition Theorems
    19.26.3 z = ξ ζ + η ζ ξ η ξ η ζ + ξ η ζ ,
    where …
    19.26.14 ( p y ) R C ( x , p ) + ( q y ) R C ( x , q ) = ( η ξ ) R C ( ξ , η ) , x 0 , y 0 ; p , q { 0 } ,
    19.26.24 z = ( ξ ζ + η ζ ξ η ) 2 / ( 4 ξ η ζ ) , ( ξ , η , ζ ) = ( x + λ , y + λ , z + λ ) ,
    29: 30.1 Special Notation
    30: 3.5 Quadrature
    The steepest descent path is given by ( t 2 t ) = 0 , or in polar coordinates t = r e i θ we have r = sec 2 ( 1 2 θ ) . …