射阳港拦门沙航道整治工程建设前后水沙特征分析     

陈可锋  王乃瑞  徐俊辉  陆培东 《海洋工程》2018,36(4):129-137

为研究工程区海域水沙特征的时空分布、运动规律,采用不同时期的现场水文泥沙资料,对射阳港拦门沙航道工程建设前后的水流、含沙量、悬沙粒径和底质特征进行了对比分析。研究表明:射阳港一期航道工程建设后航道内潮波发生变形,涨潮流速大、历时短;落潮流速小、历时长,进入到航道内泥沙很难被带出航道,容易导致航道淤积。工程区海域整体含沙量较大,一期工程建设后导堤内涨潮含沙量明显增大,口门净输沙向口内,通过口门进入到航道的高含沙水体是航道淤积的重要沙源之一。导堤间边滩表层存在部分淤泥,且具有一定流动性,在水流及自身重力作用下,边滩淤泥可归入航道内。  相似文献   

Video DCIV measurements of mass and momentum fluxes and kinetic energies in laboratory waves breaking over a bar     

K. Govender  H. Michallet  M.J. Alport  U. Pillay  G.P. Mocke  M. Mory 《Coastal Engineering》2009

The experimental investigation of water waves breaking over a barred beach in a glass walled flume is presented. The time series of the water levels along the flume were measured using wave gauges and video imaging of the water surface, providing estimates of the mean wave-heights and water levels at various positions along the flume. The instantaneous velocity fields were measured using digital correlation image velocimetry for positions beyond the initial breaking point. The mass (/velocity) and momentum fluxes, and kinetic energies were computed from the velocity flow fields by means of phase ensemble averaging and then time averaging of relevant quantities derived from the instantaneous velocity fields. These parameters reached a maximum value some distance shorewards of the break point on the bar. The relative density of the fluid in the crest of the wave, estimated using the forward and reverse velocity fluxes, was found to be in the range from 0.4 to 0.8. Preliminary analysis of the momentum fluxes and mean water levels indicates a decreasing dynamic pressure shorewards of a peak that occurs shortly after wave breaking.  相似文献   

青岛汇泉湾海滩剖面变化特征   总被引：1，自引：0，他引：1  

庄丽华  阎军  范奉鑫  陈长安 《海洋科学》2008,32(9):46-51

在海滩地形测量的基础上,分析了汇泉湾前滨海滩剖面沙坝、沟槽的短时间尺度变化特征。研究结果表明,2005年3～11月．海滩剖面沙坝顶沟槽底相对高度均变小,沙坝顶部宽度出现不同程度的变宽或变窄现象;在西北侧前滨海滩上,沟槽最底部淤高0．1-0．35m,沟槽轴线向陆移动距离较大,为17．5-3．5m,沙坝顶部淤高0～0．2m,沙坝顶部轴线向陆移动0～42．25m。而东南部前滨海滩上,大部分剖面沙坝顶被削平蚀低0．1-0．2m,沙坝项部轴线向海移动7～23．75m。在海滩西北部和中部的前滨海滩上,2005年11月沟槽最底部轴线到高潮线的距离为44～58m,沙坝顶轴线到高潮线的距离为63．75-98．5m。  相似文献   

桅杆结构竖向杆件损伤位置识别的时域方法   总被引：1，自引：0，他引：1  

瞿伟廉  彭琦 《地震工程与工程振动》2007,27(5):110-116

桅杆结构在工程上应用广泛,但破坏事故时有发生,竖向杆件是其损伤发生的主要部位之一。由于桅杆结构具有强非线性,已经发展得比较完善的基于频域的损伤识别方法不适用于桅杆结构,对其进行损伤诊断成为一大难题。本文利用桅杆结构长细比大、柔性强的特点,探讨了竖向杆件刚度变化与节点水平位移响应的关系,并提出了基于水平位移时程响应的竖向杆件损伤位置识别的指标,说明了竖向杆件损伤的时域识别步骤,通过几个数值算例证明该指标能对损伤的竖向杆件位置准确地进行识别,最后,分析了信号测量噪声对识别指标的影响。  相似文献   

MapInfo在黄河口拦门沙研究中的应用     

张彩云  杨作升  张勇  黄海挺 《海岸工程》2002,21(1):1-5

根据MapInfo所具有的功能特点,讨论了MapInfo在黄河口拦门沙中的应用.在黄河口拦门沙的研究中,通过使用MapInfo软件,使我们对拦门沙的研究从定性走向定量,从简单的文字描述达到直观的地图展示,为拦门沙的研究提供了一种新的手段.  相似文献   

Sedimentation in a meandering gravel-bed river: The River Tywi,South Wales     

Simon A. Smith 《Geological Journal》1989,24(3):193-204

Previous studies of meandering gravel-bed rivers have illustrated a wide range of bar types. The River Tywi of South Wales shows that significant variations of accretionary style can also occur within a single river. There is a downstream decrease in the proportion of lateral bars to point bars and changes in the morphological characteristics of these point bars. Three types are recognized: simple, linguoid and multi-unit point bars. Sedimentation on the concave sides of meander bends is locally important. The changes of bar type are accompanied by different styles of channel behaviour. The River Tywi is interpreted to have deposited multilateral gravel sheets, composed of partially reworked and abandoned bars and dissected by palaeochannels and sloughs. Bar deposits consist of parallel-bedded gravel, inclined laterally-accreted gravel, local angle-of-repose foresets and inclined lenses of heterolithic beds. The proportion of the various sedimentary structures and the geometry of the abandoned bars varies along the Tywi valley because of the patterns of bar distribution and channel behaviour. The deposits of this river have strong affinities with Tertiary sequences in the Italian Apennines, previously interpreted as the deposits of meandering gravel-bed rivers. This type of river is not readily distinguished from ‘Scott type’ braided streams in the geological record, unless exposures are particularly good. In this respect, the presence of abundant, inclined heterolithic wedges and lenses may be a useful diagnostic criterion.  相似文献