Multiscale Modeling of Complex Dynamic Problems: An Overview and Recent Developments

被引:20
|
作者
Jebahi, Mohamed [1 ,2 ]
Dau, Frederic [2 ]
Charles, Jean-Luc [2 ]
Iordanoff, Ivan [2 ]
机构
[1] Univ Laval, Quebec City, PQ G1V 0A6, Canada
[2] Arts & Metiers ParisTech, UMR CNRS 5295, I2M, F-33400 Talence, France
关键词
DISCRETE ELEMENT METHOD; SMOOTHED PARTICLE HYDRODYNAMICS; ESSENTIAL BOUNDARY-CONDITIONS; FINITE POINT METHOD; CONTINUUM MODELS; BRIDGING SCALE; NUMERICAL-INTEGRATION; DOMAIN DECOMPOSITION; MOLECULAR-DYNAMICS; ARLEQUIN METHOD;
D O I
10.1007/s11831-014-9136-6
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
Multiscale modeling aims to solve problems at the engineering (macro) scale while considering the complexity of the microstructure with minimum cost. Generally, two scales are considered in multiscale modeling: small scale, which is designed to capture the mechanical phenomena at the atomistic, molecular or molecular cluster level, and large scale which is connected to continuous description. For each scale, well-established numerical methods have been developed over the years to handle the relevant phenomena. As a first part of this paper, the most popular numerical methods, used at different scales, as well as the coupling approaches between them are classified, according to their features and applications, so that the place of those used in multiscale modeling can be distinguished. Subsequently, the class of concurrent discrete-continuum coupling approaches, which is well adapted for dynamic studies of complex multiscale problems, is reviewed. Several techniques used in this class are also detailed. Among them, the bridging domain (BD) technique is used to develop a discrete-continuum coupling approach, adapted for dynamic simulations, between the Discrete Element Method and the Constrained Natural Element Method (CNEM). This approach is applied to study the BD coupling parameters in dynamics. Several results giving more light on the setting of these parameters in practice are obtained.
引用
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页码:101 / 138
页数:38
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