摘要
对于饱和土地震和固结问题 ,用位移 -孔隙水压(u- p)方程来描述。土和孔隙水的相互作用对这样一组耦合方程 ,运用交叉迭代进行解耦。讨论了交叉迭代法的基本思想 ,证明了常规的交叉迭代法是条件稳定的。介绍了Zienkiewicz给出的一种高效的无条件稳定的隐式 /隐式交叉迭代法 ,并依据 Park的思想详细证明其稳定性。
In earthquake and consolidation of saturated soil, the u p formulation can be used to describe the soil pore fluid interaction. An uncoupled staggered procedure was used to efficiently solve these coupled equations. This paper presents the staggered procedure and shows that the conventional implicit staggered procedure is conditionally stable. A computationally robust and unconditionally stable implicit/implicit staggered procedure presented by Zienkiewicz is proved to be stable by Park's method. A numerical example for a soil column subjected to an instantly applied surface load is used to show that this procedure can efficiently reduce the calculating cost.
出处
《清华大学学报(自然科学版)》
EI
CAS
CSCD
北大核心
2001年第6期100-103,共4页
Journal of Tsinghua University(Science and Technology)
基金
国家自然科学基金资助项目 (5 0 0 780 3 0)
关键词
饱和土
土
孔隙水
相互作用
无条件稳定
交叉失代法
saturated soil
soil pore fluid interaction
unconditionally stable
staggered procedure