地震地质
地震地質
지진지질
SEISMOLOGY AND GEOLOGY
2010年
1期
162-173
,共12页
有限元%数值模拟%华北地区
有限元%數值模擬%華北地區
유한원%수치모의%화북지구
finite element method%numerical simulation%North China
文中综述了近30年来有限元数值模拟方法在华北地区地震地质研究中的应用和发展情况,从华北地区地震地质数值模拟的有限元模型、有限元数值模拟所采用的实测资料以及模拟结果3方面进行了讨论,综合分析了华北地区有限元数值模拟从弹性到弹塑性、黏弹性和蠕变性,从二维线性到三维非线性,从连续变形到非连续变形,从个别资料的应用到GPS网络观测资料拟合的发展过程.简单阐述了华北地区有限元数值模拟工作的意义、存在问题和发展趋势.
文中綜述瞭近30年來有限元數值模擬方法在華北地區地震地質研究中的應用和髮展情況,從華北地區地震地質數值模擬的有限元模型、有限元數值模擬所採用的實測資料以及模擬結果3方麵進行瞭討論,綜閤分析瞭華北地區有限元數值模擬從彈性到彈塑性、黏彈性和蠕變性,從二維線性到三維非線性,從連續變形到非連續變形,從箇彆資料的應用到GPS網絡觀測資料擬閤的髮展過程.簡單闡述瞭華北地區有限元數值模擬工作的意義、存在問題和髮展趨勢.
문중종술료근30년래유한원수치모의방법재화북지구지진지질연구중적응용화발전정황,종화북지구지진지질수치모의적유한원모형、유한원수치모의소채용적실측자료이급모의결과3방면진행료토론,종합분석료화북지구유한원수치모의종탄성도탄소성、점탄성화연변성,종이유선성도삼유비선성,종련속변형도비련속변형,종개별자료적응용도GPS망락관측자료의합적발전과정.간단천술료화북지구유한원수치모의공작적의의、존재문제화발전추세.
The paper summarizes the application and development of finite element numerical simulation methods in the seismo-geological study in North China in the last 30 years, and the discussion is focused on the following three aspects: the finite element model for North China, actual data used in the simulation and numerical simulation results. The study of finite element numerical simulation in North China began in 1980,since then,it has experienced the phases of development from elastic to elasto-plastic,viscoelastic and creep simulations,from 2D to 3D,from linear to nonlinear,from continuous deformation to discontinuous deformation, and from the use of individual data to the use of multiple synthetic data. It shows that finite element numerical simulation is an effective means for studying seismology and geology in North China,and distinguished results have been achieved by using simulation methods. The achievement will be the foundation for the future simulation study in North China. The paper also discusses the significance, existing problems and development tendency of finite element numerical simulation in seismo-geology in North China.