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。     

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.     

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.     

就地热再生沥青混合料均匀性的细观评价指标

就地热再生能直接在现场一次性完成路面修复,但因其材料组成和施工工艺复杂等极易出现混合料不均匀问题,为解决此问题,尝试从集料入手,对就地热再生沥青混合料均匀性的评价指标进行研究。首先,采用数码相机获取就地热再生沥青混合料试件截面的数字图像,基于数字图像处理技术识别截面中所有新旧集料的细观结构;然后,采用环扇分割法将截面分成36个等面积区域,基于区域集料颗粒面积比和新集料颗粒偏离度分别提出集料均匀性评价指标D和新集料均匀性评价指标H;最后,通过改变RAP加热温度、RAP拌和时间、新沥青混合料拌和温度与新旧料混合时间4个因素,进行正交试验,进一步分析均匀性指标的变化规律和可靠性。结果表明：环形分区结合OTSU阈值分割方法可准确识别沥青混合料截面图像中的集料信息,保留绿色通道的方法可有效识别不同灰度值的新旧集料;对试件截面均匀性的定性分析初步验证了这2个均匀性指标的有效性;RAP加热温度与新沥青混合料拌和温度对D影响显著,RAP加热温度和新旧料混合时间对H影响显著;而且,随着RAP加热温度、新沥青混合料温度和新旧料混合时间的增加,就地热再生混合料的均匀性变好,这与以往的研究结论相一致,进一步验证了这2个均匀性评价指标的可靠性。     

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。     

就地冷再生技术在市政道路改造中的应用

以山西省太原市市政道路改造工程为依托,维特根泡沫沥青就地冷再生施工技术为基础,结合太原市学府街沥青旧路面的实际路况,设计了旧路面大修方案,进行了泡沫沥青混合料的配合比设计,介绍了泡沫沥青就地冷再生基层的施工工艺、施工组织。     

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.