1) continuous deformation
连续变形
1.
, the continuous and the discontinuous deformation analysis methods.
常用的数值分析方法分为连续变形分析方法与非连续变形分析方法两大类,归纳和总结了前人关于数值分析方法的研究成果,对各种方法的研究现状和最新进展进行评述,并作了岩体工程问题的现代数值分析方法总的概论,最后提出了解决问题的思路、方法和建议。
2.
The research status in quo and the last evolution of all these numerical methods are summarized through dividing them into two classes,that is,the continuous and the discontinuous deformation analysis methods.
将岩土力学常用的数值分析方法分为连续变形分析方法与非连续变形分析方法两大类,对各种方法的研究现状和最新进展进行了评述,着重介绍了各种方法的优缺点,并提出了解决问题的思路、方法和建议。
2) continuous deformation
连续形变
1.
Recognition of 2-dimensional continuous deformation image;
二维连续形变图像的识别
2.
In this paper, we adopt a skill of remeshing procedure and an idea in classification of continuous deformation into those with and without preserving topological structures, and introduction of a new method for identifying continuous deformation.
采用网格分层细化技术并且用对网格的处理代替已有的逐点处理,把连续形变过程分为拓扑保持性连续形变和拓扑非保持性连续形变。
3) discontinuous deformation
非连续变形
1.
Viscoelastic analysis method of discontinuous deformation computational mechanics model Ⅱ: numerical analyses;
非连续变形计算力学模型的粘弹性分析方法Ⅱ:算例分析
2.
Viscoelastic analysis method of discontinuous deformation computational mechanics model Ⅰ: Fundamental theory;
非连续变形计算力学模型的粘弹性分析方法Ⅰ:基本理论
3.
Application Study of Numerical Manifold Method in Discontinuous Deformation for Rockmass;
数值流形方法在岩体非连续变形中的应用研究
4) discontinuous deformation
不连续变形
1.
Simulation and analysis for the effects of discontinuous deformation on the metal forming;
不连续变形对金属塑性影响的模拟与分析
2.
Based on the numerical simulation with complicated geologic characteristics, discontinuous deformation character of surroundings with complicated structure plane is presented to research its spatial and mechanical character of structural plane, and the influence law of the different mining process to deformation rules of surroundings is achieved.
在复杂构造矿区 ,通过数值模拟手段 ,分析了富有复杂结构面的上覆围岩不连续变形特性 ,研究了结构面的空间特征和力学特征 ,及不同的开挖过程对围岩变形特性的影响规律 ,对于非线性力学对策设计具有重要意义。
3.
The advantages and disadvantages of these methods for analyzing discontinuous deformation of jointed rocks are discussed.
讨论了这些方法用于节理岩体不连续变形分析时的各自优势和不足。
5) Continuous deformation tape
连续变形带
6) variable dimension fraction
连续变维分形
补充资料：大坝内部变形观测(见水工建筑物变形观测)
大坝内部变形观测(见水工建筑物变形观测)
daba neibubianxing guanCe大坝内部变形观测见水工建筑物变形观测。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条