首页 | 本学科首页   官方微博 | 高级检索  
     

主应力轴旋转下小偏压固结密实粉土崩塌特性及孔压模型研究
引用本文:沈扬,张朋举,闫俊,刘汉龙,张弛. 主应力轴旋转下小偏压固结密实粉土崩塌特性及孔压模型研究[J]. 岩土力学, 2012, 33(9): 2561-2568
作者姓名:沈扬  张朋举  闫俊  刘汉龙  张弛
作者单位:1.河海大学 岩土力学与堤坝工程教育部重点实验室,南京 210098;2.河海大学 岩土工程研究所,南京 210098
基金项目:国家自然科学基金资助项目(No.50909039);教育部博士点基金新教师基金项目(No.200802941019);中央高校基本科研业务费专项资金(No.2010B04514)
摘    要:为研究主应力轴旋转复杂动应力对偏压固结粉土的性状演变影响,以空心圆柱试样为对象,开展具有不同初始固结比的密实粉土(Dr=70%)在不排水主应力轴循环旋转下的系列试验。结果表明:①初始固结比不大于1.5时,主应力轴旋转导致试样发生中低应变崩塌,进而液化的脆性破坏模式;而固结比大于1.5时,试样变为应变持续稳定开展至高应变,孔压最终进入动态平衡的延性破坏模式,且不同固结比下试样发生崩塌液化和稳态延性破坏的孔压峰值间不存在交叉。②小偏压固结试样的液化峰值孔压和崩塌孔压均随固结比增加而有规律地下降,但受动剪应力水平影响很小,这与等压固结试样的崩塌孔压值受控于剪应力水平有很大差异。③相同初始球应力水平下,崩塌振次反映的小偏压固结试样强度高于等压固结试样,但在偏压条件下强度与固结比不存在单调变化关系,表明小偏压固结试样崩塌除受制初始围压水平外,很大程度上还取决于偏压程度。④基于上述试验结果,提出了主应力轴循环旋转下小偏压固结粉土的孔压预测模型,该模型不仅突显了崩塌状态对相变及液化破坏的重要预测作用,还反映了固结比和动剪应力对孔压开展的综合影响。

关 键 词:主应力轴旋转  固结比  粉土  崩塌  孔隙水压力  
收稿时间:2011-04-25

Collapse characteristics and unified pore water pressure model of slightly-anisotropically consolidated dense silt under principal stress axis rotation
SHEN Yang , ZHANG Peng-ju , YAN Jun , LIU Han-long , ZHANG Chi. Collapse characteristics and unified pore water pressure model of slightly-anisotropically consolidated dense silt under principal stress axis rotation[J]. Rock and Soil Mechanics, 2012, 33(9): 2561-2568
Authors:SHEN Yang    ZHANG Peng-ju    YAN Jun    LIU Han-long    ZHANG Chi
Affiliation:1. Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing 210098, China; 2. Geotechnical Research Institute, Hohai University, Nanjing 210098, China
Abstract:In order to study the properties of anisotropically consolidated silt subjected undrained cyclic principal stress rotation,series of tests are performed.The tested hollow cylinder silt samples have the initial relative density of 70%,and are consolidated with different consolidation ratio(Kc) before cyclic principal stress rotation.The results show that for the samples with Kc≤1.5,they collapsed at low or medium strain and liquefied,but when Kc > 1.5,the samples’ strain increases stably and the pore water pressure developed into dynamic equilibrium states;and the peak values of pore pressure in dynamic equilibrium states are lower than those in the liquefaction failure states.On the other hand,differing from the isotropically consolidated samples,the samples with Kc between 1.1 and 1.5 have the maximum pore water pressure at liquefaction lower than the initial effective spherical stress.Furthermore they decrease with the increase of Kc,but barely dependent of dynamic shear stress.So do the pore water pressure at collapse states.The collapse cycles of anisotropically consolidated samples are larger than that of the isotropically consolidated ones with the same shear stress level.But there are no monotonic relationship between collapse cycles and Kc.Finally,a model of pore water pressure development for the anisotropically consolidated silt under cyclic principal stress rotation is put forward,which could reflect the collapse characteristics as well as the effects of consolidation ratio and dynamic shear stress level.
Keywords:principal stress axis rotation  consolidation ratio  silt  collapse  pore water pressure
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《岩土力学》浏览原始摘要信息
点击此处可从《岩土力学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号