共查询到20条相似文献,搜索用时 15 毫秒
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为提升高压旋喷桩施工在滨海滩涂淤泥层的成桩质量,在深圳某陆域形成工程围堰区的插排水板区和非插排水板区进行高压旋喷桩试桩施工。通过对双重管和三重管2种工艺下的水灰比、泥浆泵压力进行调控,分析滨海滩涂淤泥层软基处理中影响高压旋喷桩成桩的主要因素,总结高压旋喷桩在淤泥层成桩过程中存在的主要问题,并给出施工建议。主要结论为:针对滨海滩涂淤泥层的高压旋喷桩软基处理宜采用双重管法施工,施工前应在施工区打设排水板,施工过程中采用较小的水灰比,采用复喷工艺可有效提升成桩质量。 相似文献
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沿海滩涂是江苏重要的后备土地资源,滩涂围垦在为江苏沿海经济发展、缓解人口增长压力、保持耕地总量动态平衡等方面做出重要贡献的同时,对沿海湿地及生态系统也带来了一定的影响。文章主要介绍了江苏沿海滩涂开发利用现状和围垦开发后期所带来的一系列问题,并从土地可持续利用的角度初步探讨了滩涂资源合理开发利用的对策和建议。 相似文献
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Mazen Abualtayef Masamitsu Kuroiwa Kentarou Tanaka Yuhei Matsubara Junichi Nakahira 《Journal of Marine Science and Technology》2008,13(1):40-49
This article describes the development of a three-dimensional (3D) multilayer hydrostatic model of tidal motions in the Ariake
Sea and its application. The governing equations were derived from 3D Navier-Stokes equations and were solved using the fractional
step method, which combines the finite difference method in the horizontal plane and the finite element method in the vertical
plane. This study introduced a 3D, time-dependent, hydrostatic, tidal current model that can compute wetting and drying in
tidal flats due to tidal motion. The 3D model was first tested against analytical solutions for three standard cases in a
rectangular basin in order to investigate the performance of the model. Then, the model was applied to Saigo fishery port
and the Ariake Sea. For standard cases, the numerical solutions were almost identical to the analytical solutions. Finally,
the model results for Saigo port and the Ariake Sea show good agreement with the field observations. 相似文献
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CHRISTOPHER HARTY 《Coastal management》2013,41(4):405-415
Estuarine habitats of southeast Australia have been undergoing changes characterized by a reduction of saltmarsh and an increase of mangroves. Incorporated into these changes have been mangrove migration into saltmarsh areas, thus contributing to the latter's decline. At the same time, rapid and extensive change in the catchments of many estuaries has occurred as a result of urban and rural development. It has been estimated that the changes observed between mangrove and saltmarsh wetland vegetation is caused by a series of processes, including urbanization and increased population pressure, increased rainfall, increased nutrients, mangroves recolonizing previously cleared areas, engineering works and subsequent altered tidal patterns, sea-level rise, and subsidence of intertidal flats. Planning strategies are suggested that can be implemented in an integrated manner to mitigate the threats from these processes and to ensure the sustainable management of mangrove and saltmarsh wetlands. 相似文献
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基于瓯飞浅滩海域多年水文泥沙及地形水深实测资料,分析研究其水动力泥沙特性及地形冲淤演变规律。结果表明:研究海域潮流性质属于非正规半日浅海潮流,各垂线分潮流椭圆率K值在0. 00~0. 20之间,故潮流总体上以往复流为主;含沙量分布呈现外海向口内逐渐增大的趋势,且大潮期含沙量明显大于中潮和小潮期;通过对瓯飞浅滩近几十年的冲淤计算及相关断面分析,认为瓯飞浅滩的潮滩区域总体处于略有淤高基本稳定的状态。不同于潮滩区域,瓯飞浅滩的水下浅滩区域在1987—2010年,年均冲刷幅度为0. 008~0. 02 m,表现为基本稳定略有冲刷的状态。 相似文献
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广州出海航道三期及其配套项目工程是伶仃洋水域内的一项重大工程,工程实施前,必须要研究和论证工程建设对伶仃洋水域内的泥沙输移和滩槽演变的影响.根据二维潮流泥沙数学模型计算分析,工程会对蕉门延伸段下段、伶仃洋西滩、西槽等冲淤变化有一定影响,对蕉门延伸段上段和凫洲水道及龙穴岛以东水域冲淤变化影响不大.从长期滩槽演变趋势来看,工程后近20a内,凫洲水道、蕉门延伸段以及内伶仃洋水域内冲淤演变规律不会发生大的变化,冲淤速率逐渐放缓,伶仃洋三滩两槽的格局将继续维持不变. 相似文献
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针对潮间带地区因大水力梯度交替变化的影响导致地基真空预压施工加固效果较差的问题,对塑料排水板打设、侧向密封系统及抽真空系统施工等方面的技术工艺优化进行研究。采用施工全过程监控方法进行验证,得出大潮差条件下开展真空预压施工的积极结果。结论显示,调整水平排水系统的滤管间距、增设双排淤泥搅拌桩作为侧向密封墙和调整真空泵布设方式等,能有效提升潮间带地区真空预压施工效果。 相似文献
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南汇边滩位于长江口和杭州湾的交汇地带,受长江口和杭州湾北岸两股潮流的控制,近年来由于低潮滩促淤围垦工程导致其水流和泥沙运移、沉积和地貌发生了显著的变化。根据2006—2008年南汇边滩测图及2007年11月—2008年11月每个季度的9个断面测量资料,结合区域内的泥沙沉积特征,探讨南汇边滩对周边涉水围垦工程和流域来水来沙变异做出适应性地貌耦合过程之后的近期冲淤演变规律,着重探讨季节性冲淤特征。结果表明:年度上南汇东滩以淤长为主,南汇南滩以冲刷为主。不同季节南汇边滩冲淤变化过程存在很大差异:平面上,南汇边滩等深线夏、冬季以淤进为主,春、秋季以蚀退为主;垂向上,南汇东滩断面呈春夏秋冲淤交替、冬季淤积的态势,南汇嘴断面呈秋季冲刷、冬夏季淤积的态势,而位于南汇南滩的断面则呈秋冬季冲刷、春夏季淤积态势。南汇东滩沉积物粒径总体上较细,东滩与南滩交汇处的南汇嘴附近中值粒径相对较粗,南汇南滩浅滩沉积物颗粒中值粒径最粗。 相似文献
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David A. Jay Jiayi Pan Philip M. Orton Alexander R. Horner-Devine 《Journal of Marine Systems》2009,78(3):442
Columbia River tidal plume dynamics can be explained in terms of two asymmetries related to plume-front depth and internal wave generation. These asymmetries may be an important factor contributing to the observed greater primary productivity and phytoplankton standing crop on the Washington shelf. The tidal plume (the most recent ebb outflow from the estuary) is initially supercritical with respect to the frontal internal Froude number FR on strong ebbs. It is separated from the rotating plume bulge by a front, whose properties are very different under upwelling vs. downwelling conditions. Under summer upwelling conditions, tidal plume fronts are sharp and narrow (< 20–50 m wide) on their upwind or northern side and mark a transition from supercritical to subcritical flow for up to 12 h after high water. Such sharp fronts are a source of turbulent mixing, despite the strong stratification. Because the tidal plume may overlie newly upwelled waters, these fronts can mix nutrients into the plume. Symmetry would suggest that there should be a sharp front south of the estuary mouth under summer downwelling conditions. Instead, the downwelling tidal plume front is usually diffuse on its upstream side. Mixing is weaker, and the water masses immediately below are low in nutrients. There is also an upwelling–downwelling asymmetry in internal wave generation. During upwelling and weak wind conditions, plume fronts often generate trains of non-linear internal waves as they transition from a supercritical to a subcritical state. Under downwelling conditions, internal wave release is less common and the waves are less energetic. Furthermore, regardless of wind conditions, solition formation almost always begins on the south side of the plume so that the front “unzips” from south to north. This distinction is important, because these internal waves contribute to vertical mixing in the plume bulge and transport low-salinity water across the tidal plume into the plume bulge.FR and plume depth are key parameters in distinguishing the upwelling and downwelling situations, and these two asymmetries can be explained in terms of potential vorticity conservation. The divergence of the tidal outflow after it leaves the estuary embeds relative vorticity in the emerging tidal plume water mass. This vorticity controls the transition of the tidal plume front to a subcritical state and consequently the timing and location of internal wave generation by plume fronts. 相似文献
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It is often advantageous to model a semi-enclosed estuarine or coastal embayment (e.g. fish farms or tidal inlets, or typhoon shelters) as a separate system within a larger water body connected to the outer sea. The water quality of the system depends crucially on its flushing time—the average time of a particle in the system. The flushing time is governed by the barotropic and baroclinic tidal exchanges between the system and the outer sea. We describe herein a general method to determine systematically the flushing time of a stratified water body via a numerical tracer experiment. Numerical solution of the 3D flow and mass transport equations for many practical problems show that the tracer mass removal process depends on the physical topography and bathymetry, tidal range and the degree of stratification in the outer sea. Field application suggests that the tracer mass variation can be well approximated by a double-exponential decay curve that can be described by three flushing coefficients. Using a simple analytical two-segment model, the flushing coefficients can be given a clear physical interpretation, and the flushing time can be easily determined in terms of the coefficients. The method is illustrated by application to a number of tidal inlets in Hong Kong, in both the dry and wet season. The connection between the numerically determined flushing time and the traditional bulk flushing time obtained from salt-balance methods is established. 相似文献
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在分析传统潮位测量方法和潮位模型缺陷的基础上,给出了GPS在航潮位测量方法。基于GPSRTK动态定位技术,系统地研究了GPS RTK在航潮位测量、数据处理的基本理论和流程,并对潮位测量和数据处理中的GPS RTK高程质量控制、姿态改正、动态吃水改正、潮位提取、垂直基准转换5个关键问题进行了深入研究,最终确定了测量船测量期间的在航潮位。将这些研究成果应用到天津新港航道的在航潮位试验中,2 d的试验结果表明,GPS在航潮位测量方法相对传统的潮位测量方法在实施的简便性、精度等方面具有较大的优越性。鉴于该方法的特点以及航道的特点,建议该方法广泛推广应用于航道在航潮位测量中。 相似文献
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田湾核电站海域潮流场数值模拟 总被引:1,自引:0,他引:1
采用MIKE 21水动力模拟软件建立了田湾核电站海域平面二维潮流数学模型,利用该模型对该海域的潮流场进行了数值模拟。根据数值模拟结果,对田湾核电站海域的潮流场特征进行了分析。建立的模型可以用来模拟研究各种工程方案实施前后的潮流场,也可以为局部模型提供边界条件。 相似文献
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