增强有限元法及其在岩土工程非连续变形分析中的应用
[Abstract]:The shear zone is a common form of rock - soil engineering disaster . It is of great significance to reveal the mechanism of shear band generation and expansion to reveal the catastrophe mechanism of geotechnical engineering and to establish disaster prevention and control measures . The simulation involves discontinuous deformation analysis , it is one of the hot research topics .
( 1 ) The traditional finite element mesh is separated into a physical grid which is geometrically independent and used to construct displacement interpolation , and a finite element displacement interpolation technique based on the conventional finite element method is proposed . The geometric separation and displacement mapping rules of the mathematical grid and the physical grid are introduced so that the structure of the displacement interpolation function is easier to realize , and the flexibility and applicability of the finite element method are greatly enhanced . The conventional finite element method is a special form of the reinforcement finite element method , and the reinforcement finite element method is the reinforcement form of the conventional finite element method .
( 2 ) Introducing the transition unit , this paper proposes a unified mapping rule consisting of the reconstruction rule Rr of the displacement of the associated mathematical unit and the transition unit and the covering rule Rc of the displacement of the associated transition unit and the physical unit . The basic determinant , the smooth stress calculation method and the integral technique of the element matrix are derived . A method for enhancing the finite element method based on the conventional finite element software is presented .
( 3 ) Based on the unified mapping rule , this paper presents the corresponding reconstruction rules by using the approximate displacement field structure idea of non - grid method , semi - analytic finite element method and so on , so that the enhanced finite element method has the advantages of no grid method , semi - analytic finite element method and smooth finite element method .
( 4 ) Maintaining the rule of displacement mapping is not the same . Through enriching the mathematical node and the transition node , the corresponding transition unit and the mathematical unit are constructed for the two physical units formed after the crack crossing , and the method suitable for describing the non - continuous deformation and the simulation of any multi - crack propagation inside the crossing unit is proposed . The limitation of the conventional finite element method that the crack is set to the boundary of the unit is broken , and the difficulty of the extended finite element method and the Hansbo & Hansbo method in dealing with the complicated multi - crack propagation problem is overcome .
( 5 ) The unified method of dealing with arbitrary order non - rule nodes at the unit level is put forward , and the simulation grid adaptation strategy based on the crack tip cell scale and the crack tip influence range is established . The results show that the grid adaptive technique improves the calculation precision of the stress field near the tip of the crack tip and the analysis accuracy of the crack propagation process .
The grid density near the crack tip has great influence on the load - displacement curve , but the influence on the crack propagation path is not large .
( 6 ) The softening characteristic and the shear band energy dissipation mechanism of shear band cohesion - shear displacement are characterized by using friction - type cohesive zone model , and the simulation method of shear zone expansion process is described by means of the enhanced finite element method . The influence of the flow law and the softening characteristics of shear zone on the rupture of overlying soil layer is studied . The results show that the shear band inclination determined based on the correlation flow rule is closer to the experimental results .
【学位授予单位】:浙江大学
【学位级别】:博士
【学位授予年份】:2014
【分类号】:TU433
【参考文献】
相关期刊论文 前10条
1 赵雷;李小军;霍达;;数值模拟软夹层对基岩上覆土层破裂的影响[J];北京工业大学学报;2007年03期
2 郭恩栋,冯启民,薄景山,洪峰;覆盖土层场地地震断裂实验[J];地震工程与工程振动;2001年03期
3 郭恩栋,邵广彪,薄景山,石兆吉;覆盖土层场地地震断裂反应分析方法[J];地震工程与工程振动;2002年05期
4 徐锡伟;闻学泽;叶建青;马保起;陈杰;周荣军;何宏林;田勤俭;何玉林;王志才;孙昭民;冯希杰;于贵华;陈立春;陈桂华;于慎鄂;冉勇康;李细光;李陈侠;安艳芬;;汶川M_S8.0地震地表破裂带及其发震构造[J];地震地质;2008年03期
5 赵纪生;陶夏新;师黎静;王海云;;An approach to evaluate ground surface rupture caused by reverse fault movement[J];Earthquake Engineering and Engineering Vibration;2006年01期
6 杨杰;陈新民;沈建;;断层错动在砂土中传播规律的模型试验研究[J];防灾科技学院学报;2011年02期
7 张国新,金峰,王光纶;用基于流形元的子域奇异边界元法模拟重力坝的地震破坏[J];工程力学;2001年04期
8 方修君;金峰;;基于ABAQUS平台的扩展有限元法[J];工程力学;2007年07期
9 方修君;金峰;王进廷;;用扩展有限元方法模拟混凝土的复合型开裂过程[J];工程力学;2007年S1期
10 金峰;方修君;;扩展有限元法及与其它数值方法的联系[J];工程力学;2008年S1期
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