论文标题
在地球物理学中产生的无界域中扩散波动方程的分析和HERMITE光谱近似
Analysis and Hermite spectral approximation of diffusive-viscous wave equations in unbounded domains arising in geophysics
论文作者
论文摘要
扩散的粘性波方程(DVWE)广泛用于地震探索中,因为它可以解释带有碳氢化合物的储层中的频率依赖性地震反射。 DVWE的大多数现有数值近似值基于具有临时边界条件的域截断。但是,这将产生人工反射以及截断错误。为此,我们直接考虑了无限域中的DVWE。我们首先显示了DVWE解决方案的存在,独特性和规律性。然后,我们开发了一种HERMITE光谱Galerkin方案,并得出相应的误差估计,表明Hermite光谱Galerkin近似提供了融合光谱速率,提供了足够平滑的溶液。提供了一些具有恒定和不连续系数的数值实验,以验证理论结果并证明该方法的有效性。特别是,我们验证了平滑和非平滑源项和初始条件的误差估计。鉴于误差估计和规律性结果,我们根据源项的规律性显示了收敛率的清晰度。我们还表明,使用本方法不会发生人工反射。
The diffusive-viscous wave equation (DVWE) is widely used in seismic exploration since it can explain frequency-dependent seismic reflections in a reservoir with hydrocarbons. Most of the existing numerical approximations for the DVWE are based on domain truncation with ad hoc boundary conditions. However, this would generate artificial reflections as well as truncation errors. To this end, we directly consider the DVWE in unbounded domains. We first show the existence, uniqueness, and regularity of the solution of the DVWE. We then develop a Hermite spectral Galerkin scheme and derive the corresponding error estimate showing that the Hermite spectral Galerkin approximation delivers a spectral rate of convergence provided sufficiently smooth solutions. Several numerical experiments with constant and discontinuous coefficients are provided to verify the theoretical result and to demonstrate the effectiveness of the proposed method. In particular, We verify the error estimate for both smooth and non-smooth source terms and initial conditions. In view of the error estimate and the regularity result, we show the sharpness of the convergence rate in terms of the regularity of the source term. We also show that the artificial reflection does not occur by using the present method.