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Modeling and Simulation of Random Processes and Fields in Civil Engineering and Engineering Mechanics

机译:土木工程与工程力学中随机过程和场的建模与仿真

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摘要

This thesis covers several topics within computational modeling and simulation of problems arising in Civil Engineering and Applied Mechanics. There are two distinct parts. Part 1 covers work in modeling and analyzing heterogeneous materials using the eXtended Finite Element Method (XFEM) with arbitrarily shaped inclusions. A novel enrichment function, which can model arbitrarily shaped inclusions within the framework of XFEM, is proposed. The internal boundary of an arbitrarily shaped inclusion is first discretized, and a numerical enrichment function is constructed "on the fly" using spline interpolation. This thesis considers a piecewise cubic spline which is constructed from seven localized discrete boundary points. The enrichment function is then determined by solving numerically a nonlinear equation which determines the distance from any point to the spline curve. Parametric convergence studies are carried out to show the accuracy of this approach, compared to pointwise and linear segmentation of points, for the construction of the enrichment function in the case of simple inclusions and arbitrarily shaped inclusions in linear elasticity. Moreover, the viability of this approach is illustrated on a Neo-Hookean hyperelastic material with a hole undergoing large deformation. In this case, the enrichment is able to adapt to the deformation and effectively capture the correct response without remeshing. Part 2 then moves on to research work in simulation of random processes and fields. Novel algorithms for simulating random processes and fields such as earthquakes, wind fields, and properties of functionally graded materials are discussed. Specifically, a methodology is presented to determine the Evolutionary Spectrum (ES) for non-stationary processes from a prescribed or measured non-stationary Auto-Correlation Function (ACF). Previously, the existence of such an inversion was unknown, let alone possible to compute or estimate. The classic integral expression suggested by Priestley, providing the ACF from the ES, is not invertible in a unique way so that the ES could be determined from a given ACF. However, the benefits of an efficient inversion from ACF to ES are vast. Consider for example various problems involving simulation of non-stationary processes or non-homogeneous fields, including non-stationary seismic ground motions as well as non-homogeneous material properties such as those of functionally graded materials. In such cases, it is sometimes more convenient to estimate the ACF from measured data, rather than the ES. However, efficient simulation depends on knowing the ES. Even more important, simulation of non-Gaussian and non-stationary processes depends on this inversion, when following a spectral representation based approach. This work first examines the existence and uniqueness of such an inversion from the ACF to the ES under a set of special conditions and assumptions (since such an inversion is clearly not unique in the most general form). It then moves on to efficient methodologies of computing the inverse, including some established optimization techniques, as well as proposing a novel methodology. Its application within the framework of translation models for simulation of non-Gaussian, non-stationary processes is developed and discussed. Numerical examples are provided demonstrating the capabilities of the methodology. Additionally in Part 2, a methodology is presented for efficient and accurate simulation of wind velocities along long span structures at a virtually infinite number of points. Currently, the standard approach is to model wind velocities as a multivariate stochastic process, characterized by a Cross-Spectral Density Matrix (CSDM). In other words, the wind velocities are modeled as discrete components of a vector process. To simulate sample functions of the vector process, the Spectral Representation Method (SRM) is used. The SRM involves a Cholesky decomposition of the CSDM. However, it is a well known issue that as the length of the structure, and consequently the size of the vector process, increases, this Cholesky decomposition breaks down (from the numerical point of view). To avoid this issue, current research efforts in the literature center around approximate techniques to simplify the decomposition. Alternatively, this thesis proposes the use of the frequency-wavenumber (F-K) spectrum to model the wind velocities as a stochastic "wave," continuous in both space and time. This allows the wind velocities to be modeled at a virtually infinite number of points along the length of the structure. In this work, the relationship between the CSDM and the F-K spectrum is first examined, as well as simulation techniques for both. The F-K spectrum for wind velocities is then derived. Numerical examples are then carried out demonstrating that the simulated wave samples exhibit the desired spectral and coherence characteristics. The efficiency of this method, specifically through the use of the Fast Fourier Transform, is demonstrated.
机译:本文涵盖了土木工程和应用力学领域的计算建模和问题模拟中的多个主题。有两个不同的部分。第1部分介绍了使用具有任意形状的夹杂物的扩展有限元方法(XFEM)对非均质材料进行建模和分析的工作。提出了一种新颖的富集函数,可以在XFEM框架内对任意形状的夹杂物进行建模。首先将任意形状的夹杂物的内部边界离散化,并使用样条插值“即时”构造数值富集函数。本文考虑了由七个局部离散边界点构成的分段三次样条。然后,通过数值求解非线性方程来确定富集函数,该方程确定了从任何点到样条曲线的距离。进行了参数收敛研究,以证明与点的点向和线性分割相比,这种方法的准确性,在线性弹性的简单夹杂物和任意形状的夹杂物的情况下,可以构建富集函数。此外,这种方法的可行性在具有较大变形的孔的新霍克超弹性材料上得到了说明。在这种情况下,富集能够适应变形并有效捕获正确的响应而无需重新网格化。然后,第2部分继续研究随机过程和领域的仿真工作。讨论了模拟随机过程和场(例如地震,风场和功能梯度材料的特性)的新颖算法。具体而言,提出了一种方法,该方法可根据规定的或测量的非平稳自相关函数(ACF)确定非平稳过程的演化谱(ES)。以前,这种反转的存在是未知的,更不用说计算或估计了。 Priestley建议的经典积分表达式(从ES提供ACF)不是以唯一的方式可逆的,因此可以从给定的ACF确定ES。但是,从ACF高效转换为ES的好处是巨大的。例如,考虑涉及模拟非平稳过程或非均匀场的各种问题,包括非平稳地震地震动以及非均匀材料特性(例如功能梯度材料的特性)。在这种情况下,有时从测量数据而不是ES估计ACF更为方便。但是,有效的仿真取决于对ES的了解。更重要的是,在遵循基于频谱表示的方法时,非高斯和非平稳过程的仿真取决于此反演。这项工作首先研究了在一系列特殊条件和假设下从ACF到ES的这种反转的存在和唯一性(因为这种反转在最一般的形式中显然不是唯一的)。然后,它转向计算逆的有效方法,包括一些已建立的优化技术以及提出一种新颖的方法。在模拟非高斯,非平稳过程的翻译模型框架内的应用得到了开发和讨论。提供了数值示例,说明了该方法的功能。另外,在第2部分中,提出了一种方法,可以在几乎无限个点上高效,准确地模拟沿大跨度结构的风速。当前,标准方法是将风速建模为一个多变量随机过程,其特征在于互谱密度矩阵(CSDM)。换句话说,将风速建模为矢量过程的离散成分。为了模拟矢量过程的样本函数,使用了频谱表示方法(SRM)。 SRM涉及CSDM的Cholesky分解。但是,众所周知的问题是,随着结构长度的增加以及矢量过程的大小增加,这种Cholesky分解会崩溃(从数值的角度来看)。为了避免这个问题,文献中的当前研究工作围绕着简化分解的近似技术。另外,本论文提出使用频率-波数(F-K)谱将风速建模为随机的“波”,在空间和时间上都是连续的。这允许沿着结构的长度在几乎无限个点上模拟风速。在这项工作中,首先检查了CSDM和F-K频谱之间的关系,以及两者的仿真技术。然后得出风速的F-K谱。然后进行数值示例,证明模拟波样本表现出所需的光谱和相干特性。这种方法的效率特别是通过使用快速傅立叶变换进行了演示。

著录项

  • 作者

    Benowitz Brett Alexander;

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  • 年度 2013
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  • 原文格式 PDF
  • 正文语种 English
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