Abstract
We consider the Helmholtz equation: \(\begin{array}{llll}\qquad\qquad-\varDelta u^*\;-k^2u^*\;=\;f\quad \mathrm{in}\quad \varOmega \\ \\ u^*\;=\;g_D\;\mathrm{on}\;\partial{\varOmega_D},\;\frac{\partial u^*}{\partial n}\;=\;g_N\;\mathrm{on}\;\partial {\varOmega_N},\;\frac{\partial u^*}{\partial n}\;+\;iku^*\;=\;g_S\;\mathrm\;\mathrm{on}\;\partial{\varOmega_S}\end{array}\) where \(\varOmega\) is a bounded polygonal region in k2, and the \(\partial{\varOmega_D},\;\partial{\varOmega_N}\;\mathrm{and}\;\partial{\varOmega_S}\) correspond to subsets of \(\varOmega\) where the Dirichlet, Neumann and Sommerfeld boundary conditions are imposed.
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Kimn, JH., Sarkis, M. (2013). Shifted Laplacian RAS Solvers for the Helmholtz Equation. In: Bank, R., Holst, M., Widlund, O., Xu, J. (eds) Domain Decomposition Methods in Science and Engineering XX. Lecture Notes in Computational Science and Engineering, vol 91. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-35275-1_16
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DOI: https://doi.org/10.1007/978-3-642-35275-1_16
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