Banks H T, Birch Malcolm J, Brewin Mark P, Greenwald Stephen E, Hu Shuhua, Kenz Zackary R, Kruse Carola, Maischak Matthias, Shaw Simon, Whiteman John R
Center for Research in Scientific Computation, North Carolina State University Raleigh, NC 27695-8212, USA.
Clinical Physics, Barts Health National Health Service Trust England.
Int J Numer Methods Eng. 2014 Apr 13;98(2):131-156. doi: 10.1002/nme.4631. Epub 2014 Feb 7.
We revisit a method originally introduced by Werder (in Comput. Methods Appl. Mech. Engrg., 190:6685-6708, 2001) for temporally discontinuous Galerkin FEMs applied to a parabolic partial differential equation. In that approach, block systems arise because of the coupling of the spatial systems through inner products of the temporal basis functions. If the spatial finite element space is of dimension and polynomials of degree are used in time, the block system has dimension ( + 1) and is usually regarded as being too large when > 1. Werder found that the space-time coupling matrices are diagonalizable over [Formula: see text] for 100, and this means that the time-coupled computations within a time step can actually be decoupled. By using either continuous Galerkin or spectral element methods in space, we apply this DG-in-time methodology, for the first time, to second-order wave equations including elastodynamics with and without Kelvin-Voigt and Maxwell-Zener viscoelasticity. An example set of numerical results is given to demonstrate the favourable effect on error and computational work of the moderately high-order (up to degree 7) temporal and spatio-temporal approximations, and we also touch on an application of this method to an ambitious problem related to the diagnosis of coronary artery disease. Copyright © 2014 The Authors. published by John Wiley & Sons Ltd.
我们重新审视了一种最初由韦德尔提出的方法(见《计算方法在应用力学与工程中的应用》,第190卷,第6685 - 6708页,2001年),该方法用于将时间间断伽辽金有限元方法应用于抛物型偏微分方程。在那种方法中,由于时间基函数的内积导致空间系统的耦合,从而产生了块系统。如果空间有限元空间的维度为 且在时间上使用 次多项式,那么块系统的维度为( + 1),当 > 1时,通常认为这个维度太大。韦德尔发现,对于 100,时空耦合矩阵在[公式:见原文]上是可对角化的,这意味着在一个时间步内的时间耦合计算实际上可以解耦。通过在空间中使用连续伽辽金方法或谱元方法,我们首次将这种时间间断伽辽金方法应用于二阶波动方程,包括具有和不具有开尔文 - 沃伊特及麦克斯韦 - 齐纳粘弹性的弹性动力学方程。给出了一组数值结果示例,以证明适度高阶(最高到7次)的时间和时空近似对误差和计算量的有利影响,并且我们还涉及了该方法在一个与冠状动脉疾病诊断相关的宏大问题上的应用。版权所有© 2014作者。由约翰·威利父子有限公司出版。