{"title":"Implicit and Semi‐Implicit SPH Schemes for Large Deformation Problems in Geomechanics","authors":"Jun Geng, Ronaldo I. Borja","doi":"10.1002/nag.70445","DOIUrl":null,"url":null,"abstract":"We present an implicit time integration scheme for smoothed particle hydrodynamics (SPH) employing multiplicative elastoplasticity in the finite deformation range. Time integration is based on the one‐step, unconditionally stable Newmark method formulated using an updated Lagrangian description. A novelty of the paper is an implicit evaluation of all variables including the neighbor lists of the SPH particles. The implicit scheme simplifies to a predictor–corrector (semi‐implicit) scheme when the zeroth iteration is taken as the predictor phase and the first iteration is taken as the corrector phase. We show that both schemes provide significant numerical stabilization of the SPH solution even with larger time steps and without the use of an artificial viscosity—a marked improvement over existing explicit SPH algorithms that rely on the satisfaction of the Courant–Friedrichs–Lewy condition and on artificial viscosity for stabilization. We demonstrate the robustness of the implicit and predictor–corrector schemes using benchmark examples that include sand column collapse and granular flow on an inclined flume.","PeriodicalId":13786,"journal":{"name":"International Journal for Numerical and Analytical Methods in Geomechanics","volume":"475 1","pages":""},"PeriodicalIF":3.6000,"publicationDate":"2026-09-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal for Numerical and Analytical Methods in Geomechanics","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1002/nag.70445","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENGINEERING, GEOLOGICAL","Score":null,"Total":0}
引用次数: 0
Abstract
We present an implicit time integration scheme for smoothed particle hydrodynamics (SPH) employing multiplicative elastoplasticity in the finite deformation range. Time integration is based on the one‐step, unconditionally stable Newmark method formulated using an updated Lagrangian description. A novelty of the paper is an implicit evaluation of all variables including the neighbor lists of the SPH particles. The implicit scheme simplifies to a predictor–corrector (semi‐implicit) scheme when the zeroth iteration is taken as the predictor phase and the first iteration is taken as the corrector phase. We show that both schemes provide significant numerical stabilization of the SPH solution even with larger time steps and without the use of an artificial viscosity—a marked improvement over existing explicit SPH algorithms that rely on the satisfaction of the Courant–Friedrichs–Lewy condition and on artificial viscosity for stabilization. We demonstrate the robustness of the implicit and predictor–corrector schemes using benchmark examples that include sand column collapse and granular flow on an inclined flume.
期刊介绍:
The journal welcomes manuscripts that substantially contribute to the understanding of the complex mechanical behaviour of geomaterials (soils, rocks, concrete, ice, snow, and powders), through innovative experimental techniques, and/or through the development of novel numerical or hybrid experimental/numerical modelling concepts in geomechanics. Topics of interest include instabilities and localization, interface and surface phenomena, fracture and failure, multi-physics and other time-dependent phenomena, micromechanics and multi-scale methods, and inverse analysis and stochastic methods. Papers related to energy and environmental issues are particularly welcome. The illustration of the proposed methods and techniques to engineering problems is encouraged. However, manuscripts dealing with applications of existing methods, or proposing incremental improvements to existing methods – in particular marginal extensions of existing analytical solutions or numerical methods – will not be considered for review.