汉江雅口航运枢纽泄水闸工程地基处理

汉江雅口航运枢纽工程泄水闸地基为不均匀的砂砾石土层,建基面局部为粉细砂薄层,砂砾石土层局部含有粉细砂透镜体或大块卵石。针对地基沉降量大和砂砾石土层分布不均匀的问题,提出了长螺旋钻孔压灌桩复合地基处理方案,并在现场代表性区域进行了成桩试验检测。结果表明:该地基处理方案技术可行、质量稳定、生态环保,适宜于本工程的应用,具有推广价值。     

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。     

浅析港口工程地质勘察项目管理

为了适应当前的发展形势,又好又快地完成各项岩土工程勘察任务,需要考虑如何在保证质量的同时满足工期与经济效益的要求。着重阐述在港口工程地质勘察中,引进项目管理的方法,从地质钻探、士工试验和室内报告编写等方面提出流程化管理的思路,为实践中遇到的一些问题提供建议及参考。     

西沙群岛珊瑚砂运动特性试验研究

珊瑚砂具有颗粒密度较大、孔隙率较高、干密度较小、压缩性较高等物理特性。其形成过程相对短暂,搬运距离有限,珊瑚砂磨圆度较低,颗粒形态差异明显,颗粒之间有效接触面积较小,粘着力较低。这些特性决定了珊瑚砂在动力作用下易于起动搬运的运动特征。文章对西沙群岛珊瑚砂的比重、孔隙率、休止角和渗透性等物理性质以及水流、波浪作用下的起动特性进行了试验测定,试验结果也表明了珊瑚砂起动特性符合目前经验公式计算值。     

铁矿尾矿砂在公路基层中的应用研究

对铁尾矿砂及尾矿砂加入石灰水泥后的物理力学性能进行了试验研究,并与石灰土进行对比。结果表明：铁尾矿砂掺加石灰、水泥后,其强度随着龄期而增长,具有半刚性材料的特性,用石灰、水泥稳定尾矿砂作为路面基层材料具有很好的路用性能,同时用石灰和水泥稳定的效果更佳。     

连云港庙岭三期突堤砂被堤工程施工工艺

根据连云港庙岭三期的特殊情况,采用了砂被筑堤法。介绍了连云港庙岭三期突堤砂被堤工程的概况,从砂桩打设、吹填砂被模袋混凝土护坡等几个方面介绍了砂被堤施工的工艺流程。陈述了施工中出现的技术问题和解决方法以及对原施工工艺的改进。这一工艺取得了良好的施工效果。     

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.     

Characteristic flow patterns generated by macrozoobenthic structures

A laboratory flume channel, equipped with an acoustic Doppler flow sensor and a bottom scanning laser, was used for detailed, non-intrusive flow measurements (at 2 cm s^− 1 and 10 cm s^− 1) around solitary biogenic structures, combined with high-resolution mapping of the structure shape and position. The structures were replicates of typical macrozoobenthic species commonly found in the Mecklenburg Bight and with a presumed influence on both, the near-bed current regime and sediment transport dynamics: a worm tube, a snail shell, a mussel, a sand mound, a pit, and a cross-stream track furrow. The flow was considerably altered locally by the different protruding structures (worm tube, snail, mussel and mound). They reduced the horizontal approach velocity by 72% to 79% in the wake zone at about 1–2 cm height, and the flow was deflected around the structures with vertical and lateral velocities of up to 10% and 20% of the free-stream velocity respectively in a region adjacent to the structures. The resulting flow separation (at flow Reynolds number of about 4000 and 20,000 respectively) divided an outer deflection region from an inner region with characteristic vortices and the wake region. All protruding structures showed this general pattern, but also produced individual characteristics. Conversely, the depressions (track and pit) only had a weak influence on the local boundary layer flow, combined with a considerable flow reduction within their cavities (between 29% and 53% of the free-stream velocity). A longitudinal vortex formed, below which a stagnant space was found. The average height affected by the structure-related mass flow rate deficit for the two velocities was 1.6 cm and 1.3 cm respectively (80% of height and 64%) for the protruding structures and 0.6 cm and 0.9 cm (90% and 127% of depth) for the depressions. Marine benthic soft-bottom macrozoobenthos species are expected to benefit from the flow modifications they induce, particularly in terms of food particle capture due to altered particle pathways and residence times, but also for the exchange of gases, solutes and spawn. The present results confirm previous studies on flow interaction effects of various biogenic structures, and they add a deeper level of detail for a better understanding of the fine-scale effects.