碎石桩软土复合地基整体抗剪强度研究

振冲碎石桩作为散体材料桩与周围的软土形成的复合地基,同钢筋混凝土桩、钢管桩等刚性桩形成的复合地基在工作原理、承载力分析等方面存在着本质的不同。与刚性桩相比,碎石桩作为垂直排水通道,能够加快周围软土的排水固结,提高桩间土的整体强度。同时碎石桩自身的承载力发挥又取决于周围土体的侧向支撑作用。如何确定碎石桩复合地基的整体抗剪强度对于发挥碎石桩的作用至关重要。以港珠澳大桥香港口岸人工岛项目碎石桩的工程应用为例,对比碎石桩软土复合地基整体抗剪强度计算的异同,通过数值模拟和现场监测等手段对参数取值进行分析,对今后类似工况条件下碎石桩复合地基的抗剪强度计算具有指导意义。     

桥梁深水钻孔灌注桩施工技术

随着大型跨海、跨江桥梁的相继建设,桥梁跨度越来越大,对基础的要求也越来越高,超长、大直径的钻孔灌注桩已被广泛应用于大型深水桥梁建设中。结合工程实例,介绍大型桥梁深水钻孔灌注桩施工技术及其施工过程中的关键控制要点。     

基于Kubernetes的铁路客运营销深度学习平台的设计与实现

为解决铁路客运营销深度学习平台Tensorflow框架存在的环境配置复杂,资源利用率低、模型设计周期长等问题,提出了基于Kubernetes容器的PaaS平台构建TensorFlow容器的统一资源调度管理及API访问控制服务架构.经平台实践证明,该架构为客运营销提供了可靠、稳定的分析环境,降低了模型的训练难度,提高了模...     

北京地铁深基坑支护结构设计优化与施工

北京地铁9号线军事博物馆站北换乘厅南侧紧邻复兴路和既有1号线,附近管线众多,周边环境复杂,对地层扰动影响较高,地层中下部以黏土岩、砾岩为主,整体稳定性较好,原设计方案采取咬合桩止水及基坑底部换撑等加强措施。在保证施工安全的前提下,为了合理缩短工期、减少造价,结合实际工程经验对原设计方案进行了优化。和原设计方案相比,优化设计方案取消了咬合桩及换撑,对第4道支撑位置进行了调整,并更换了防水材料。同时,采用北京理正深基坑分析软件对优化设计前后的基坑开挖情况进行了对比分析。最后,在按优化设计方案施工的过程中进行严密的监控量测,并对监测数据进行了分析。最终给出以下建议:1)深基坑支护尽量不采取换撑的方式;2)设计方案要结合实际情况进行动态设计,要以软件计算作为参考依据;3)在基坑开挖过程中要进行严密的监控量测,并重视数据反馈。     

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.     

深海极限波浪运动特性的简便算法(英文)

本文基于五阶Stokes规则波理论,提出了一种快速求解深海极限波浪运动特性的数学模型.研究中,按照上跨零点和下跨零点的方法由计算或实测的极限波浪波面时间历程确定包含极限波峰或波谷的相邻两个周期的平均值为五阶Stokes规则波的波浪周期,然后根据极限波峰或波谷值反推确定波浪入射波幅.通过与已有的数值结果和实验数据对比,验证了本文所建立的数值模型可以快速准确的计算出极限波浪下的速度场,相比其他模型,更适合于工程应用.     

援潜救生系统装备概况

援潜救生是复杂的系统工程,在提倡立体救援的新形势下,各种援潜救生装备的配套使用,扬长避短,协同作战,才能真正满足援潜救生的要求,文章主要论述援潜救生装备的分类及深潜救生艇的技术性能分析类比.     

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.     

船舶机械零件的深孔工艺及其改进方法

很多机械零件具有深孔,如车床主轴、液压传动轴的油缸等。加工深孔时,刀具细长,钻头容易将孔钻偏,使孔中心歪斜;切屑不易排出,散热能力较差,刀具易磨损;当工件精度和光洁度要求较高时,受刀具刚度的限制,需要采取适当措施,以保证工件质量和生产效率。