公路隧道洞口斜交、偏压段施工技术

以云山隧道右线进口不良地质段为实例,详细介绍了洞身与山体斜交、偏压时,采用双层超前小导管注浆加固隧道围岩进洞时小导管的设计参数、施工工艺、施工要点等,对同类工程施工有一定借鉴作用。     

桥面防水粘结层性能试验分析

采用室内剪切试验和拉拔试验,分析桥面防水粘结层材料性能,认为层间抗剪强度及粘结强度受温度影响大,并且随着试验环境温度的升高而减小.现场拉拔试验研究了不同温度下4种粘结层材料与桥面板的粘结强度变化规律,其粘结强度同样随着试验环境温度的升高而减小.研究表明,剪切试验与拉拔试验结果能够综合评价高、低温情况下沥青混合料与粘结层的整体性能,还可以作为桥面粘结层是否满足抗剪要求的验证指标.     

船舶烧伤病房气流组织分析与优化

针对舰船舱室气流组织的形式特点,以烧伤病房作为研究对象建立数学模型,通过使用Airpak软件对烧伤病房不同设计方案下的气流组织进行了计算仿真,通过舱室温湿度,空气流速,热舒适指标等参数的对比,获得舱室的压力、温度、速度、热舒适性指标等的分布特性,对烧伤病房气流组织进行了分析并提出了优化方法,可以有效提高人员的舒适性和气流组织效果。     

淤泥质海岸波致液化及航道骤淤问题初步研究

研究波浪与淤泥海床相互作用导致的海床液化、体积冲刷和高浓度近底悬沙的层移输运问题。采用de Wit提出的液化判别条件及计算方法,结合连云港近岸波浪和淤泥力学特征,计算不同来波条件下淤泥质海床的液化深度;进一步考虑浑水中含沙量对流速的折减影响,计算液化层运移速度分布。计算结果表明,大浪条件下,淤泥质海床可能有较大的液化深度,但层移厚度不大。由于层移含沙量较高,在近底水流驱动下仍能形成较大的输沙率和一定规模的大风天航道骤淤。有关研究成果为海床稳定性分析和输沙计算提供了新的思路和方法。     

阿赛线改造工程管道防腐保温补口方法

文中介绍了"防腐层+保温层+防护层+封口"复合防腐保温补口结构在阿赛线安全扩能改造工程中的应用,介绍了复合防腐保温补口结构的施工方法和检验方法,总结了现场施工中出现的问题和解决方法,对这种复合补口结构的优点和缺点进行了分析,最后提出了改进建议。     

海上救生保温用具的设计与试验要求

主要介绍了PH2702型（PH2707型）海上救生保温用具的设计依据、材料和结构型式的选择,以及试验方法和结果。     

基于ATP协议的恒温液态食品罐车热工性能测试研究

针对冷链物流系统中恒温液态食品罐车的热工性能测试实验的现状进行研究分析,指出了其中存在的问题。着重研究了液态食品罐车的热工性能测试内容,包括综合测控系统和外围硬件设备的设计。实际应用效果显示,构建的系统能够满足ATP标准的要求。     

客运专线路基褥垫层施工技术

本文主要介绍哈尔滨至大连铁路客运专线褥垫层施工工艺。     

Non-local simulation of the stable boundary layer with a third order moments closure model

A new higher order closure model for the stable boundary layer is presented and compared with Large Eddy Simulation data. The model includes numerical solutions for the mean values, second and third order moments equations. A satisfactory agreement is found between the calculated vertical profiles of the turbulent quantities with those provided by the LES. Furthermore the new model results are compared with profiles obtained with a lower order closure model in order to verify the effective importance of including third order dynamical equations in the model.     

Impact of macrozoobenthic structures on near-bed sediment fluxes

Sandy sediments in shallow coastal waters of the Baltic Sea are often characterised by large numbers of biogenic structures which are produced by macrozoobenthos species. A series of experiments was devised to quantify how the interaction of such structures with the near-bed flow regime affects the sediment flux. Most experiments were done with simplified replicates of structures generated by typical species commonly found in the Mecklenburg Bight, starting with solitary structures and regularly-spaced arrays in a range of characteristic population densities, followed by a complex benthic macrofauna community, both artificial and alive. A laboratory flume channel, equipped with an acoustic Doppler flow sensor and a topography scanning laser, was used for high-resolution measurements (2 mm horizontal step size and 0.3 mm vertical resolution) of sand erosion (220 µm median grain size, at 20 cm s^− 1) and fine particle deposition (8 µm grain size, at 5 cm s^− 1). Sediment transport threshold values were measured for each layout. As a rule-of-thumb, both the erosion fluxes and the deposition of suspended matter increased considerably at low population densities (below 2%, expressed as percent of the sediment surface covered, i.e. roughness density RD). Above densities of 4%, erosion almost stopped inside the test arrays, and deposition remained well below the level of unpopulated areas. An attempt to extrapolate these findings to field conditions (using field current velocity data from 2001) showed that the net flux switched from erosion to deposition for densities above 5%. These parameters can now be integrated into a numerical sediment transport model coupling waves, currents, sediment dynamics and biological processes, which is currently under construction at the Baltic Sea Research Institute (IOW), Rostock, Germany.