组合型水泥粉煤灰碎石桩(CFG桩)复合地基在深厚软基处理中的应用

在深厚软土地基(fak≤100 kPa)上建造储罐等建筑物,承载力要求高、不均匀沉降变形要求严,若采用单一CFG桩复合地基加固,可能导致桩距过小或桩长太长,需要采用组合型复合地基,CFG桩+振冲碎石桩复合地基是组合型复合地基的一种。根据CFG桩+碎石桩组合型复合地基的加固机理,分析了其受力特性以及CFG桩和碎石桩的作用,研究表明CFG桩对提高地基承载力和减小沉降起控制作用。基于优化理论,建立了组合复合地基的优化设计方法。通过工程实例讨论了组合复合地基的优化设计方法,结果表明:复合地基的承载力、沉降量和经济效益均满足工程要求。     

平面二维k-ε紊流模型不同壁函数的对比及研究

在平面二维紊流模型中壁函数起到连接流固的桥梁作用,克服了边界附近网格过密的困难,也是紊流模型应用中的一个重要环节,因此壁函数的选择对模型的模拟结果起着至关重要的作用。将3种不同形式的壁函数引入平面二维k-ε模型中,对丁坝绕流进行了数值计算,并将计算结果与实测数据进行了对比,从流场、流速、紊动动能分布及紊动耗散率等方面对3种壁函数进行优选验证,结果表明对数率壁函数优于其他两种形式的壁函数,其数值计算结果更接近实测数据。     

混流泵内流场的数值模拟

利用FLUENT软件,采用标准k-ε双方程紊流模型和SIMPLE算法对混流泵内部的三维紊流流动进行数值模拟.通过对其内部流动速度、压力分布的分析,揭示了其内部流动的主要特征,对其性能及改进提供相关信息.     

桩群绕流阻力物理模型试验测量技术研究

由于压强差的存在和桩群表面的摩擦力,水流流过桩群时将产生绕流阻力。对于单根桩的复杂水流条件下绕流阻力的理论分析尚待进一步研究,桩群的阻力计算更显复杂,限于理论计算桩群绕流阻力的复杂程度,桩群水流阻力数值模拟和物理模拟技术仍处在概化模拟阶段。为了通过实测数据辅助研究桩群阻力概化方法,依托物理模型技术、传感器发展水平、软硬件系统集成技术而提出一整套对桩群阻力测量技术的解决方案,并分析了测量结果的合理性。     

高级PHP泥浆在深水大直径钻孔桩施工中的应用

结合国道主干线广州绕城公路西环南段北江特大桥主墩直径250cm桩基施工实践．介绍了高级PHP泥浆原材料组成、调制方法、泥浆性能,重点阐述了高级PHP泥浆在深水大直径钻孔桩施工应用中的控制要点及重要作用。     

人工挖孔桩施工与质量控制

在地质奈件允许的情况下,可采用人工挖孔方法对桥梁进行桩基础的施工。人工挖孔受地形限制小,可以多孔同时作业,能加快工程进度并降低工程造价,是比较成熟的成孔方法。     

The structure of dissipation in the western Irish Sea front

We report on an intensive campaign in the summer of 2006 to observe turbulent energy dissipation in the vicinity of a tidal mixing front which separates well mixed and seasonally stratified regimes in the western Irish Sea. The rate of turbulent dissipation ε was observed on a section across the front by a combination of vertical profiles with the FLY dissipation profiler and horizontal profiles by shear sensors mounted on an AUV (Autosub). Mean flow conditions and stratification were obtained from a bed mounted ADCP and a vertical chain of thermistors on a mooring. During an Autosub mission of 60 h, the vehicle, moving at a speed of ~ 1.2 m s^− 1, completed 10 useable frontal crossings between end points which were allowed to move with the mean flow. The results were combined with parallel measurements of the vertical profile of ε which were made using FLY for periods of up to 13 h at positions along the Autosub track. The two data sets, which show a satisfactory degree of consistency, were combined to elucidate the space–time variation of dissipation in the frontal zone. Using harmonic analysis, the spatial structure of dissipation was separated from the strong time dependent signal at the M₄ tidal frequency to yield a picture of the cross-frontal distribution of energy dissipation. A complementary picture of the frontal velocity field was obtained from a moored ADCP and estimates of the mean velocity derived from the thermal wind using the observed density distribution. which indicated the presence of a strong (0.2 m s^− 1) jet-like flow in the high gradient region of the front. Under neap tidal conditions, mean dissipation varied across the section by 3 orders of magnitude exceeding 10^− 2 W m^− 3 near the seabed in the mixed regime and decreasing to 10^− 5 W m^− 3. in the strongly stratified interior regime. The spatial pattern of dissipation is consistent in general form with the predictions of models of tidal mixing and does not reflect any strong influence by the frontal jet.     

A dense water outflow from the Ross Sea, Antarctica: Mixing and the contribution of tides

We use hydrographic, current, and microstructure measurements, and tide-forced ocean models, to estimate benthic and interfacial mixing impacting the evolution of a bottom-trapped outflow of dense shelf water from the Drygalski Trough in the northwestern Ross Sea. During summer 2003 an energetic outflow was observed from the outer shelf ( 500 m isobath) to the  1600 m isobath on the continental slope. Outflow thickness was as great as  200 m, and mean speeds were  0.6 m s^− 1 relative to background currents exceeding  1 m s^− 1 that were primarily tidal in origin. No outflow was detected on the slope in winter 2004, although a thin layer of dense shelf water was present on the outer shelf. When the outflow was well-developed, the estimated benthic stress was of order one Pascal and the bulk Froude number over the upper slope exceeded one. Diapycnal scalar diffusivity (K_z) values in the transition region at the top of the outflow, estimated from Thorpe-scale analysis of potential density and measurements of microscale temperature gradient from sensors attached to the CTD rosette, were of order 10^− 3−10^− 2 m² s^− 1. For two cases where the upper outflow boundary was particularly sharply defined, entrainment rate w_e was estimated from K_z and bulk outflow parameters to be  10^− 3 m s^− 1 ( 100 m day^− 1). A tide-forced, three-dimensional primitive equation ocean model with Mellor-Yamada level 2.5 turbulence closure scheme for diapycnal mixing yields results consistent with a significant tidal role in mixing associated with benthic stress and shear within the stratified ocean interior.     

苏通大桥大型桩承台桥墩基础的局部冲刷防护试验研究

为探讨特大型桩套箱桥墩基础的护底防冲工程问题,通过实验室试验,分别对墩基防冲护底的方案选择、防护工程结构分层和范围确定、防护材料的稳定及成型情况以及护底工程的防冲效果进行了试验研究。并将试验成果应用在苏通长江大桥护底防冲工程的设计、施工中。施工期为期4年的监测结果证明,实施的防护工程及时、有效,确保了桥墩基础的安全。可为相关大桥采取防护措施提供借鉴。     

地铁牵引供电框架保护及功能性改造

针对广州地铁1号线不能远程区分框架保护类型和不能远程复归的状况,结合西门子S5系列PLC技术、SINAUT技术、牵引供电技术,对框架保护进行功能性改造,大大减少了框架保护故障的处理时间.改造技术方案主要通过研究数据的传递方式、协议转换、控制逻辑关系,修改组态软件、监控程序、接口程序、PLC程序的方式来实现.