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Jitse Niesen (talk | contribs) thanks for the correction; I simply edited a bit (for instance, not all implicit methods are unconditionally stable) |
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SIAM J. 3 (1955), 28-41, [http://www.ams.org/mathscinet-getitem?mr=71874 MR71874]</ref>is a [[finite difference]] method for solving parabolic and elliptic partial differential equations. It is most notably used to solve the problem of [[heat conduction]] or solving the [[diffusion equation]] in two or more dimensions.
The traditional method for solving the heat conduction equation is the
== The method ==
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= ( u_{xx} + u_{yy} ) \quad </math>
The implicit
: <math>{u_{ij}^{n+1}-u_{ij}^n\over \Delta t} =
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where <math>\delta_p^2</math> is the central difference operator for the ''p''-coordinate.
After performing a stability analysis, it can be shown that this method will be stable for any ''r''.
The idea behind the ADI method is to split the finite difference equations into two, one with the ''x''-derivative taken implicitly and the next with the ''y''-derivative taken implicitly,
: <math>{u_{ij}^{n+1/2}-u_{ij}^n\over \Delta t/2} =
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: <math>{u_{ij}^{n+1}-u_{ij}^{n+1/2}\over \Delta t/2} =
\left(\delta_x^2 u_{ij}^{n+1/2}+\delta_y^2 u_{ij}^{n+1}\right).</math>
The systems of equations involved are
It can be shown that this method is unconditionally stable. There are more refined ADI methods such as the methods of Douglas<ref>Douglas, J. "Alternating direction methods for three space variables," Numerische Mathematik, Vol 4., pp 41-63 (1962)</ref>, or the f-factor method<ref>Chang, M.J. et al. "Improved alternating-direction implicit method for solving transient three-dimensional heat diffusion problems", Numerical Heat Transfer, Vol 19, pp 69-84, (1991)</ref> which can be used for three or more dimensions.
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