Experimental study on liquefaction mechanism by means of micro-mechanical method
微力学方法液化机理实验研究
基本信息
- 批准号:12450187
- 负责人:
- 金额:$ 4.99万
- 依托单位:
- 依托单位国家:日本
- 项目类别:Grant-in-Aid for Scientific Research (B)
- 财政年份:2000
- 资助国家:日本
- 起止时间:2000 至 2002
- 项目状态:已结题
- 来源:
- 关键词:
项目摘要
Our research objectives are first to develop a program based on Distinct Element Method (DEM), which makes it possible to numerically simulate the liquefaction phenomenon ; second to figure out liquefaction mechanism from micro-mechanical point of view ; and finally, to verify experimentally the reality of numerical simulation results. We obtained the following results :1) DEM is programmed such that the interaction between particles and surrounding water can be taken into account. It can successfully be applied to liquefaction associated upward seepage flow.2) Numerical simulation tests were carried out using the distinct element method (DEM) by paying much attention to the micro-deformation mechanism during liquefaction of saturated granular materials. During the cyclic loading, column-like structures are generated in the corresponding direction of major principal stress. The microstructure becomes more anisotropic with cyclic loading. Not only decrease of effective stress but also anisotropy of the microstructure itself accelerate the anisotropy of microstructure. Such anisotropic structure becomes unstable and finally collapses when the major principal stress rotates.3) Undrained cyclic triaxial tests are carried out to clarify the effect of microstructure on liquefaction. Following facts are of particular interest. Voids, randomly distributed at first, are connected in series between the column-like structures. The excess pore water pressure increases markedly under undrained cyclic loading, in particular, when the connected voids are stressed perpendicular to their elongation direction. This is the reason why once liquefied sand loses sharply the liquefaction resistance in a subsequent re-liquefaction test.
我们的研究目标是首先开发一个基于离散单元法(DEM)的程序,使液化现象的数值模拟成为可能;其次从细观力学的角度揭示液化机理;最后从实验上验证数值模拟结果的真实性。1)编制了DEM程序,考虑了颗粒与周围水的相互作用。利用离散单元法(DEM)对饱和散体材料液化过程中的微观变形机理进行了数值模拟试验。在循环荷载作用下,相应的主应力方向上会产生柱状结构。随着循环加载的进行,微观组织变得更加各向异性。不仅有效应力的降低,而且微观组织本身的各向异性也加速了微观组织的各向异性。这种各向异性结构在主应力旋转时变得不稳定并最终坍塌。3)进行了不排水循环三轴试验,以阐明微结构对液化的影响。以下事实特别有意义。最初随机分布的空隙串联连接在柱状结构之间。在不排水循环荷载作用下,超孔压显著增加,特别是当连接的孔洞受到垂直于其伸长方向的应力时。这就是为什么曾经液化过的砂土在随后的再液化试验中急剧丧失抗液化能力的原因。
项目成果
期刊论文数量(56)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
K. Suzuki, M. Oda and K. Kawamoto & H. Fujimori: "Effect of fabric anisotropy on liquefaction of saturated sand using conventional triaxial test apparatus (in Japanese)"46A. 289-298 (2000)
K.铃木、M.小田和K.川本
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M.Oda, K.Iwashita: "Study on couple stress and shear band development in granular media based on numerical simulation analyses"Int. J. Engineering Science. 38. 1713-1740 (2000)
M.Oda,K.Iwashita:“基于数值模拟分析的颗粒介质中的耦合应力和剪切带发展研究”Int。
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鈴木輝一, 小田匡寛, 川本建, 藤森啓之: "三軸試験装置における飽和砂の再液状化抵抗に及ぼす構造異方性の影響"構造工学論文集. 46A. 289-298 (2000)
Teruichi Suzuki、Masahiro Oda、Ken Kawamoto、Hiroyuki Fujimori:“结构各向异性对三轴试验装置中饱和砂的再液化阻力的影响”《结构工程杂志》46A 289-298 (2000)。
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M. Oda, K. Kawamoto, K. Suzuki, H. Fuiimori and M.: "Microstructural Interpretation of reliquefaction of saturated granular soils under cyclic loading"J. Geotechnical and Geoenvironmental Engineering, ASCE. 127(5). 416-423 (2001)
M. Oda、K. Kawamoto、K. Suzuki、H. Fuiimori 和 M.:“循环荷载下饱和颗粒土再液化的微观结构解释”J。
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K. Kawamoto, M. Oda and K. Suzuki: "Hydro-geological study of landslides caused by heavy rainfall on August 1998 in Fukushima. Japan"J. Natural Disaster Science. 22(1). 12-23 (2000)
K. Kawamoto、M. Oda 和 K. Suzuki:“日本福岛 1998 年 8 月强降雨造成滑坡的水文地质研究”J。
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ODA Masanobu其他文献
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{{ truncateString('ODA Masanobu', 18)}}的其他基金
Fundamental study on transition from quasi-static to rapid flow of granular materials
颗粒材料准静态向快速流动转变的基础研究
- 批准号:
16360233 - 财政年份:2004
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Study on time-dependent failure of rock and geological discontinuity under high temperature and pressure.
高温高压下岩石与地质不连续性随时间变化的研究。
- 批准号:
08455217 - 财政年份:1996
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Study on permeability and hydrodynamic dispersion in jointed rock
节理岩石渗透率和水动力弥散研究
- 批准号:
07555443 - 财政年份:1995
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for Scientific Research (B)
Micromechanical model for shear band formation in granular soils and its application to bearing capacity problems
颗粒土中剪切带形成的微力学模型及其在承载力问题中的应用
- 批准号:
03452203 - 财政年份:1991
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$ 4.99万 - 项目类别:
Grant-in-Aid for General Scientific Research (B)
Elasto-Plastic Constitutive Equation for Geological Materials Withffabric
地质材料与织物的弹塑性本构方程
- 批准号:
01550381 - 财政年份:1989
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for General Scientific Research (C)
A SYSTEM OF SURVEY AND ANALYSIS FOR LARGE EXCAVATIONS IN JOINTED ROCK MASSES
节理岩体大型基坑勘察与分析系统
- 批准号:
62850090 - 财政年份:1987
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for Developmental Scientific Research
Coupled Stress and Fluid Flow Analysis for Jointed Rock Masses
节理岩体的应力与流体流动耦合分析
- 批准号:
61550347 - 财政年份:1986
- 资助金额:
$ 4.99万 - 项目类别:
Grant-in-Aid for General Scientific Research (C)
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