兰新高速铁路高寒地段路基温度场数值模拟分析

兰新高铁浩门至大梁区间所处地区海拔高,气温低,冻结期长,属于深季节性冻土区。为解决该区间路基冻害问题,依据当地气候条件,运用ANSYS有限元分析软件,对低路堤、零断面换填路基及不同深度处铺设保温材料的路基温度场进行数值模拟,分析路基冻结深度的变化规律和最大冻结深度,为高寒区高速铁路路基冻害防治措施设计提供参考。研究表明:(1)由于兰新高铁浩门至大梁区间海拔高、冬季冻结时间长、气温低等原因,导致路基冻结深度大;(2)零断面换填路基实测地温和数值模拟计算结果基本相符,所选计算模型、参数等可以为其他相同条件断面数值模拟分析采用;(3)铺设保温板路基温度场较未铺设保温板的0℃线上移,冻结深度增加速率变小,最大冻结深度明显减小,路基保温效果较好;(4)由于路基边坡、基床以下部位土层性质、厚度、热物理参数等影响,低路堤最大冻结深度比零断面换填路基大。     

洋山深水港区一期工程航行安全模拟试验研究

运用电子操纵模拟器 ,预演了第六代集装箱船在各种不利航行条件下进出洋山深水港区的航行过程 ,分析了风、浪、流等环境因素对船舶操纵的影响 ,确定了船舶安全进出港所需的航道宽度、船舶安全靠泊条件和掉头操纵水域尺度。大量的模拟试验研究结果证实 :洋山深水港区具有良好的船舶航行条件 ,船舶按一期工程小洋山方案 (一 )、小洋山方案 (二 )以及小洋山～镬盖塘方案进行靠离泊和掉头操纵无本质差异 ,主要不同点在于船舶通过窄口后小洋山方案 (一 )和小洋山方案 (二 )比小洋山～镬盖塘方案有较长的制动水域     

南沙龙穴造船基地水下大砂袋封涌施工

介绍南沙龙穴造船基地深水河涌水下大砂袋封截的施工经验。     

盐渍土地基处理的浸水试验研究

盐渍土作为一种不良土体,由于它的盐溶特性严重影响置于其上的建筑物。采用何种有效的处理方法来降低溶陷沉降量将至关重要。文中以西北某盐渍土机场的地基处理为例,采用浸水预溶的处理方法,在现场分别进行了深层浸水试验、直接浸水试验、浸水后晾晒试验,并对施工工艺、浸水控制、渗水速度确定做了研究。通过试验后检测,浸水预溶试验取得了良好的效果,为指导大面积地基处理施工提供了可靠参数。     

帷幕注浆在富水地层桩基施工中的应用

研究目的:帷幕注浆具有施工机具不受空间的限制、无大量返浆和废液需要处理以及对地下水和环境无污染等优点,对不同地层均能取得土体强度增加、渗透系数明显减小的工程效果,并产生良好的护壁作用。采用帷幕注浆可解决在渗透系数大、承压水头高的地层中进行特大桥桩基施工中面临成孔困难的问题,本文进一步探讨了该工艺在西南地区某长江大桥施工中的应用经验。研究方法:结合某长江大桥桩基施工的工程实例,论述了帷幕注浆的设计要点、施工工艺,并且介绍了判定帷幕注浆止水效果的原位测试方法,对测试结果进行了深入的分析。研究结果:在正常的压力状态下,地层的综合渗透系数在10-5cm／s数量级;在水压力大于0．3 Mpa情况下帷幕可能会出现水力劈裂现象,导致渗透系数增大。研究结论:采用帷幕注浆止水效果明显,保证了桩基的顺利施工。     

Coupled transport-reaction pathways and distribution patterns between siliciclastic-carbonate sediments at the Ria de Vigo

This paper examines the linkages between the space-distribution of grain sizes and the relative percentage of the amount of mineral species that result from the mixing process of siliciclastic and carbonate sediments at the Ria de Vigo (NW of Spain).The space-distribution of minerals was initially determined, starting from a detailed mineralogical study based on XRD-Rietveld analysis of the superficial sediments. Correlations between the maps obtained for grain sizes, average fractions of either siliciclastic or carbonates, as well as for individual-minerals, were further stabilised. From this analysis, spatially organized patterns were found between carbonates and several minerals involved in the siliciclastic fraction. In particular, a coupled behaviour is observed between plagioclases and carbonates, in terms of their relative percentage amounts and the grain size distribution.In order to explain these results a conceptual model is proposed, based on the interplay between chemical processes at the seawater–sediment interface and hydrodynamical factors. This model suggests the existence of chemical control mechanisms that, by selective processes of dissolution-crystallization, constrain the mixed environment's long-term evolution, inducing the formation of self-organized sedimentary patterns.     

57 300 t散货船主机轴系负荷测量

文章主要介绍了57 300 t散货船主机轴系各道轴承在静止状态下进行的测量、调整,使各参数调整至工艺要求的范围内,满足使用要求,可供同行参考。     

灌注桩深基坑的有限元计算及影响因素分析

对苏州市轨道交通2号线金民东路站深基坑使用灌注桩作为支挡结构的开挖、支护施工进行了有限元数值模拟,据此分析了灌注桩内力、水平侧移等随施工过程的变化以及主体结构的内力情况,并研究了灌注桩刚度、地基土刚度对支护结构侧移和弯矩的影响,对实际施工起到一定的指导作用。     

提速线路旁深基坑施工的路基防护

在提速线路和高路堤旁开挖深基坑及施工墩台对既有路基稳定性的影响,是工程施工中首要解决的问题.此文结合津浦线澥河大桥护孔工程深基坑钻孔桩支护的成功经验,探讨了路基防护的措施.     

On the fresh balance of the Adriatic Sea

The long-term mean fresh water balance of the Adriatic Sea is studied by ananalysing evaporation, precipitation and river runoff. Evaporation is computed from May latent heat flux and by means of bulk formula. In the latter case two wind speed data sets are used, namely those from the NMC and May. The sea surface temperature is taken from a historical Adriatic data set, and the air temperature and relative humidity come from the NMC data set. Two precipitation data sets are considered, namely the Legates and Willmott climatology and a data set consisting of data measured at 62 rain-gauge stations located on the Adriatic coasts. Runoff contribution to the fresh water balance is estimated from the long-term average flow rates of 39 rivers and the horizontal distribution of salinity in the upper mixed layer.The spatial distribution of the fresh water balance, as well as of its components, is analysed by means of monthly objective maps, from which averages and standard deviations are computed. The results obtained from the different computations are not always univocal, particularly in the evaluation of Summer evaporation, and are affected by relatively large statistical errors. Significant spatial and seasonal variability occurs, with a noticeable fresh water gain along the coastline of the northern and middle basins, while small areas of fresh water loss are found in the middle and southern basins. Nevertheless, on an annual basis, the difference between the fresh water losses by evaporation and the gains by precipitation and runoff is clearly negative, indicating that, unlike the whole Mediterranean, the Adriatic Sea is generally a dilution basin.