环保疏浚土资源化利用途径

针对疏浚污染土的科学处置与资源化利用,指出当前疏浚污染土利用手段的不足之处,介绍疏浚土制备回填土、免烧建材型材、绿化土等资源化利用方式,进而从3个维度即岩性特征、营养盐及重金属等污染情况、有机质及盐分含量定性与定量相结合分析疏浚污染土资源化利用途径选择的依据,并据此对太湖与白洋淀疏浚土分别成功制备免烧砖和绿化土进行实证分析。结果表明,从上述3个维度判别环保疏浚土资源化利用途径是可行有效的。     

青岛前湾港南港区混合土的研究

工程中常见淤泥类土与砂类土相混构成的混合土,其中淤泥类土土质极软但在土工试验中却可得出较大内摩擦角.以青岛港前湾港区南区的混合土为例,阐述混合土的成因和分布特征,分析与评价混合土的物理力学性质和采用混合土工程设计特性指标的原则、方法,并提出该地区混合土工程特性指标.     

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。     

真空预压软基处理工程监测

介绍真空预压软基处理工程中一些常用的监测手段及监测方法.结合工程实例,通过综合运用表层沉降监测、孔隙水压力监测、分层沉降监测、地下水位观测等手段,分析真空预压软土地基处理方法的加固效果,可供软土地基处理设计与施工参考.     

三台阶核心土环形开挖法在广以隧道中的应用

三台阶核心土环形开挖法是在台阶分部法基础上演变而来的,它集中了台阶法、台阶分部法、上下导坑法等优点。广以隧道地层较老,岩石破碎、节理发育、石质较软,围岩以Ⅳ、Ⅴ及Ⅵ级为主,施工难度极大。文中介绍了三台阶核心土环形开挖法,以及与之相匹配的超前支护、初期支护、防排水及二次衬砌施工等工法。     

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.