1. 中山大学 地球科学系,广州,510275
2. 中山大学 应用力学与工程系,广州,510275
3. 广东省地质过程与矿产资源探查重点实验室,广东,广州,510275
纸质出版日期:2013,
网络出版日期:2013-3-25,
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田管凤, 汤连生. 层状地基分析的超级有限层法[J]. 中山大学学报(自然科学版)(中英文), 2013,52(2):1-7.
TIAN Guanfeng, TANG Liansheng. Super Finite Layer Method for Layered Ground Analysis[J]. Acta Scientiarum Naturalium Universitatis SunYatseni, 2013,52(2):1-7.
基于传统有限层法基本原理提出6参数一般有限层法。层元的位移模式采用5次完全多项式与双重级数相乘的形式;通过应用弹性体静力平衡条件对三维位移函数多项式系数之间的相关性进行分析简化,得到未知的独立位移参数6个,与层元的节面位移数目对应相等,保证了层元位移模式的完备性。通过超级有限层元〖JP2〗与其内部小层元间的运算矩阵转换,进一步推导了6参数超级有限层法,满足了相邻小层元间高阶变形的协调性。通过算例分析表明,6参数一般有限层法仅适用多薄层地基;而超级有限层法可以适用于多种厚度的多层地基。
Firstly
the 6-parameter common finite layer method is proposed based on the basic principle of conventional method. The displacement mode of a layer element is taken in the product form of five complete polynomial and double series. By applying the static equilibrium equations of elastic medium to the layer element
the correlation rules among three-dimensional displacement polynomial coefficients are discovered. Thus six unknown and independent displacement parameters can be obtained
whose number is the same as nodal surface displacement with the result that completeness requirement for the displacement mode can be ensured. Secondly
the 6-paramter super finite layer method has been deduced by transforming operational matrix between the super finite layer element and its interior small elements
in which the coordination of higher order deformations between adjacent small layer elements can be satisfied. At last
it is concluded that the 6parameter common finite layer method is suitable for thin layered ground
while the super finite layer method is for layered ground with various thickness.
超级有限层法6参数一般有限层法位移模式的完备性高阶变形的协调性
super finite layer method6-parameter common finite layer methodcompleteness requirement of displacement modecoordination of higher order deformation
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