特殊条件下的真空预压密封技术

结合广州港南沙港区二期工程软基处理工程实例,针对在局部有抛石地段的软土采取真空预压方法加固时传统的挖密封沟和施打淤泥搅拌墙技术存在相当大困难的情况,提出了在有抛石地段采取高压旋喷桩密封技术。实测结果表明,采取该技术密封效果良好,真空度能达到设计要求。与堆载方案相比,采取本技术经济效益良好,具有较好的推广价值。     

沉箱箱壁计算分析和局部优化

采用结构计算程序AN SY S,对北方某港拟建的15万吨级矿石转水码头大直径圆沉箱箱壁进行了计算。对桥梁计算中通用的影响线加载程序进行修改,编制成适用于卸船机荷载的动态规划程序,并嵌入结构分析程序中,计算出最不利组合工况下的沉箱箱壁受力;同时参考AN SY S拓扑优化结果,对沉箱消浪孔形式和布置位置等进行了调整,计算分析后给出了受力性能更为合理的细部构造布置。     

间歇式沥青搅拌设备称量系统设计

从沥青搅拌设备供料系统到称量系统机构及控制系统设计,全面阐述了影响沥青搅拌设备称量精度的因素及在实际应用中的合理解决办法,并提出沥青搅拌设备称量精度指标要求.     

薄壁杆件六面体网格剖分的组装法

针对箱梁等薄壁杆件的六面体网格自动生成问题,提出以下算法:在内外壳表面上,根据其拓扑关系和几何位置,采用映射和插值的方法布设节点;根据各个壳节点三维位置和拓扑关系对其进行编号;采用动态规划的方法,根据壳之间的拓扑几何关系组装内外壳,统一节点编号,生成单元。应用以该方法编制的相应计算软件对一座三跨连续箱形梁桥进行网格剖分。结果表明:该算法简单,效率高,生成的单元质量好。     

间歇式沥青拌和站冷料供给系统流量的标定方法

以实例介绍间歇式沥青拌和冷料供给系统流量的标定方法和步骤，以确保冷料供给器按目标配合比准确供料，使沥青混合料的生产配比更加接近目标配比，保证拌和成品料的质量。     

双速搅拌工艺

根据传统二次搅拌理论,提出了混凝土双速搅拌工艺,介绍了双速搅拌工艺的原理及优点,并指出了该工艺的实现方案.该工艺的应用可降低生产成本,提高混凝土的强度和生产率.     

深基坑中型钢结合水泥土搅拌桩作为立柱桩的应用

立柱是大面积基坑水平支撑体系的重要组成部分,而在基坑围护设计施工时,采用型钢结合水泥土搅拌桩作为立柱桩的情况较为少见。为此,介绍了某SMW工法桩围护基坑工程中,型钢结合水泥土搅拌桩作为立柱桩的应用情况,以期为类似工程提供一定参考。     

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.     

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.