深基坑工程安全评价的尖点突变模型

为评价深基坑工程失稳的突变特征,采用突变理论建立了深基坑工程尖点突变安全评价模型.根据工程安全监控理论,引入突变理论,以基坑水平变形为例,考虑深基坑土体的流变特性,建立了基于时效影响因子的深基坑工程尖点突变安全评价模型.实例分析表明,尖点突变安全评价模型克服了采用常规设置监控值评价时参数选择困难,并能反映基坑失稳突变性的特点,可以量化评价基坑安全程度,正确评价安全状态,具有适应性强、精度高的优点.     

考虑中主应力效应Gudehus-Bauer亚塑性模型的改进

针对Gudehus-Bauer亚塑性模型不能考虑中主应力影响,在Gudehus提出的响应包络线理论基础上,提出了在模型的非线性项乘以一个考虑中主应力的因子进行改进.这种改进增加了土体剪切时的强度,改变了土体受压时的变形.新模型对中主应力的变化在中主应力参数影响程度能够有一定反映.同时将改进后的模型与中主应力参数为常量的真三轴实验进行了比较.结果表明改进后的模型可以模拟中主应力对砂土强度和变形特性的影响,能够定量预测由于中主应力影响产生的体积应变.     

两郧断裂带十漫高速公路隧道围岩稳定性研究

应用非线性有限元法和施工过程力学的基本原理,研究十漫公路隧道的开挖、支护的原理,根据两陨断裂带的岩体特征,采用分步加载和荷载释放的原理,对隧道的整体稳定性以及围岩和支护结构的受力特征进行了详细分析.由数值模拟结果可知:隧道环向处产生应力集中,且初次衬砌和二次支护结构应力较大;局部断裂破碎带对二道垭隧道的影响较大.因此需要在施工中采用合理的开挖支护方法,确保隧道的施工期及正常运营期的稳定性.     

长北气田山2段小层砂体三维建模

鄂尔多斯盆地长北气田山西组2段为一套海相辫状河三角洲沉积体系,为揭示不同时期小层砂体发育规模及空间分布,以高分辨率层序地层分析为基础,相控建模为指导思想,短期基准面旋回为地层单元,等时地层格架为约束条件,采用序贯指示数学方法对长北气田山2段4个短期层序的水上分流河道、水下分流河道及河口坝微相小层砂体的发育规模及空间分布进行了随机模拟.砂体展布的三维模拟结果表明,河道自北向南沿物源方向延展,其中SSC1～SSC4短期基准面上升时期,河道加宽,小层砂体沉积厚度加大,物性较好,有利储层发育;下降时期河道变窄,小层砂体沉积厚度减小,物性变差.小层砂体的三维模拟结果在该区勘探实践中得到了很好的验证.     

Constitutive equations and finite element implementation of strain localization in sand deformation

A recently proposed model coupling with the solid-fluid of the saturated sand was utilized to study the deformation band. Based on the critical state plasticity model by Borja and Andrade, the hydraulic conductivity tensor was naturally treated as a function of the spatial discretization matrix about the displacement and the stress field, allowing a more realistic representation of the physical phenomenon. The fully Lagrangian form of the Darcy law was resolved by Piola algorithm, and then the flow law was gained, leading to the implementation of a modified model of the saturated sand. Then the criterion for the onset of localization was derived and utilized to detect instability. The constitutive model was implemented in a finite element program coded by FORTRAN, which was used to predict the formation and development of shear bands in plane strain compression of saturated sand. At last, the formation mechanism of the shear band was discussed. It is shown that the model works well, and the simulation sample bifurcates at 1.18% axial strain, which is in a good qualitative agreement with the experiment. The pore pressure greatly affects the onset and development of the deformation band, and it obviously increases around the localization-prone regions with the direction toward the outer side of the normal of the shear band, while the pore stress flows nearly horizontally and is distributed equally far away the shear band region. Foundation item: Project(2006G007-C) supported by the Foundation of the Science and Technology Section of Ministry of Railway of China; Project(77206) supported by the Excellent PhD Thesis Innovation Foundation of Central South University, China     

Comprehensive assessment on dynamic roof instability under fractured rock mass conditions in the excavation disturbed zone

The damage process of fractured rock mass showed that the fracture in rocks induced roof collapse in Yangchangwan Coal Mine,China.The rock mass was particularly weak and fractured.There occurred 6 large-scale dynamical roof falls in the excavation disturbed zone (EDZ) with the collapsing volume of 216 m3.First,the field detailed geological environment,regional seismic dy-namics,and dynamic instability of roadways were generally investigated.Second,the field multiple-index monitoring measurements for detecting the deep delamination of the roof,convergence deformation,bolt-cable load,acoustic emission (AE) characteristic pa-rameters,total AE events,AE energy-releasing rate,rock mass fracture,and damage were arranged.Finally,according to the time-space-strength relations,a quantitative assessment of the influence of rock-mass damage on the dynamic roof instability was accomplished.     

埕岛油田馆上段沉积砂体及其夹层分布特征

通过岩矿特征、剖面结构、砂岩粒度和砂体形态分析,认为埕岛油田馆陶组上段为曲流河沉积。按砂体发育特点和成因类型划分出主河道连片砂体、河道边缘连续窄带状砂体、天然堤断续带状砂体、决口水道扇形席状砂体及废弃河道成因的透镜状砂体等5种类型。在研究区383口井精细地质研究的基础上,从不同成因储油砂体角度总结出夹层分布特征。建立了储油砂体内夹层的空间分布模式：主河道砂体内夹层分布复杂,一般底部发育钙质夹层,中部多发育物性夹层,上部为泥质夹层;河道边缘砂体主要发育泥质夹层;决口扇砂体内泥质夹层分布稳定;天然堤和废弃河道仅发育极少的钙质夹层。     

夯扩挤密碎石桩处理液化砂土

目的 消除砂土液化,保证处理深度范围内地基土上下均匀,为液化砂土桩处理探索新的途径.方法 夯扩挤密碎石桩采用相同的夯击能量和贯入度控制桩体质量,以高能量施工设备进行孔内夯击填料,振动和挤密桩底和桩间土,使松散砂土颗粒重排,提高砂土的承载力和压缩模量.笔者对比分析夯扩挤密碎石桩在沿海高速路基工程上的应用实例.结果 采用夯扩挤密碎石桩复合加固地基,可提高砂层标贯锤击数30%,消除砂土液化现象,提高地基承载力,与振冲桩相比节省造价约20%.结论 夯扩挤密碎石桩方法工艺简单,施工质量易保证,节约水资源;夯扩挤密碎石桩对于公路路基工程,具有广阔的应用前景,开辟了处理砂土液化的新途径.     

人工砂高性能混凝土的配合比设计

以京沪高速铁路为工程背景,结合混凝土施工中河砂资源紧张的实际情况,进行了人工砂制备高性能混凝土的研究,研究了泥粉含量、用水量、砂率对混凝土性能的影响,采用矿物掺合料技术等高性能混凝土配合比技术,采用人工砂设计制备出了C30、C35高速铁路桩体、承台、墩身用高性能混凝土。对于人工砂在高速铁路工程混凝土中的应用具有指导意义。     

拉森钢板桩基坑支护施工工艺

文章介绍了拉森钢板桩基坑支护施工工艺、沉桩措施;指出了拉森钢板桩支护是切实可行的.