扰动半空间中带有狄里赫特边界条件的亥姆霍兹方程的坐标复合化

Charles L. Epstein, Leslie Greengard, Jeremy Hoskins, Shidong Jiang, Manas Rachh
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引用次数: 0

摘要

我们提出了一种基于经典双层势的新复数化方案,用于求解二维和三维紧凑扰动半空间中具有迪里希特边界条件的亥姆霍兹方程。双层势的核是自由空间格林函数的法向导数,作为目标和源位置的函数,它在复平面内有众所周知的解析延续。在这里,我们证明了--当入射数据是解析的并满足精确的渐近估计时--边界积分方程的解本身在复平面的特定区域内具有解析延续,并满足相关的渐近估计(这类数据包括平面波和点源引起的场)。然后我们证明,通过精心选择的轮廓变形,振荡积分可以转换为指数衰减积分,从而有效地将无限域缩小为有限域。我们的方案不同于现有的使用复杂坐标变换(如完全匹配层)或吸收区域(如治理文数的逐步复杂化)的方法。更确切地说,在我们的方法中,我们仍然在求解边界积分方程,尽管是在原始边界的截断、复合版本上。换句话说,没有引入任何体积/域修改。该方案可以扩展到其他边界条件、开放波导和层状介质。我们用二维和三维的例子来说明该方案的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Coordinate complexification for the Helmholtz equation with Dirichlet boundary conditions in a perturbed half-space
We present a new complexification scheme based on the classical double layer potential for the solution of the Helmholtz equation with Dirichlet boundary conditions in compactly perturbed half-spaces in two and three dimensions. The kernel for the double layer potential is the normal derivative of the free-space Green's function, which has a well-known analytic continuation into the complex plane as a function of both target and source locations. Here, we prove that - when the incident data are analytic and satisfy a precise asymptotic estimate - the solution to the boundary integral equation itself admits an analytic continuation into specific regions of the complex plane, and satisfies a related asymptotic estimate (this class of data includes both plane waves and the field induced by point sources). We then show that, with a carefully chosen contour deformation, the oscillatory integrals are converted to exponentially decaying integrals, effectively reducing the infinite domain to a domain of finite size. Our scheme is different from existing methods that use complex coordinate transformations, such as perfectly matched layers, or absorbing regions, such as the gradual complexification of the governing wavenumber. More precisely, in our method, we are still solving a boundary integral equation, albeit on a truncated, complexified version of the original boundary. In other words, no volumetric/domain modifications are introduced. The scheme can be extended to other boundary conditions, to open wave guides and to layered media. We illustrate the performance of the scheme with two and three dimensional examples.
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