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洋山港及邻近海域悬沙输运特征研究* 总被引:1,自引:0,他引:1
基于SWEM2D数值模型,建立了一个范围包括洋山港、长江口及杭州湾的二维水流泥沙数学模型。根据2004年5月洋山港实测水文泥沙资料,认为洋山港区域悬沙垂向切变输运较小,可忽略该项对悬沙输运的影响,采用二维泥沙数学模型能基本反映出该区域悬沙输运特点。利用2004年5月洋山港及邻近海域实测水文泥沙资料对模型计算结果进行验证,验证结果表明模型计算结果与实际情况吻合良好。在此基础上,根据模型计算结果计算了洋山港及邻近海域大、中、小潮期间悬沙输运速度。结果表明,洋山港区域悬沙主要以欧拉输运为主,斯托克斯漂移、潮泵输运为辅。该区域西口门高含沙量主要是受到长江口及杭州湾悬沙输运富集的影响。其邻近海域主要的悬沙输运在近南汇边滩以东区域分成两股,一股向北,一股沿着南汇南岸的水下泥沙通道,径直流向杭州湾,并在杭州湾的悬沙输运的带动下,向洋山港流去。 相似文献
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南黄海辐射沙脊群悬沙特征研究 总被引:1,自引:1,他引:1
为了探明南黄海海域悬沙场的特征,以指导港口建设,通过人工神经网络,将平面二维潮流数值模型、天气图和水文测验数据联系起来,构建了平面二维悬浮泥沙模型。首先运用人工神经网络求出实测含沙量与水动力之间的函数关系,再把潮流模型和风场计算值代入此关系式,最后求出该海域含沙量平面分布。模型的计算结果表明:波浪掀沙和水流输沙是整个海域宏观水动力特征;西洋潮流水道处于冲刷状态,有利于深槽的维持;含沙量等值线与等水深线形状大体一致。 相似文献
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浅水方程无结构网格有限体积法研究进展 总被引:1,自引:0,他引:1
回顾了近些年国内外基于无结构网格的有限体积法模拟浅水流动的发展,着重论述了无结构网格的有限体积法的应用、高性能的法向数值通量的计算格式、物理量的重构和浅水流动静水压力项与底坡项的平衡问题.讨论了无结构网格有限体积法隐式求解、减小局部一维化误差和构造具有明确物理意义的消除虚假流动的计算方法等有待于进一步研究的方向. 相似文献
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基于2013年洪枯季三门湾海域12个测站潮流和含沙量同步观测资料,运用机制分解法研究三门湾枯季和洪季悬沙输移变化特征,探讨不同水动力因子的贡献率。结果表明:1)无论是洪季还是枯季,三门湾的欧拉余流和斯托克斯余流从小潮至大潮逐渐增大。欧拉余流方向基本向海,斯托克斯余流绝大部分向陆。单宽输水量的大小和方向主要由欧拉余流决定。2)枯季时三门湾海域“平流输沙(T1+T2)”对单宽输沙量绝对值的贡献率最大,其中T1项最大贡献率可达83%;“潮泵输沙项(T3+T4+T5)”的贡献率在湾中区域最大。洪季时,三门湾的平流输沙项的贡献率降低,而潮泵输沙项贡献率增大。3)无论是洪季和枯季时,三门湾泥沙净输运个别站位(SM08和SM11)输沙方向相反,其他站位的规律基本一致。 相似文献
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本文采用网格节点型有限体积法求解二维瞬态雷诺方程,采用矢量化方法离散雷诺方程,从而构建并得到新的数值模型,该模型既有有限体积法守恒性的特点,又能适用于结构复杂的求解域.通过与相关算例的对比验证,证明了该模型可适用于滑动轴承润滑特性的研究,同时精度也可以得到保证;根据计算得到的压力分布特点,采用不同的网格类型和网格数量重新划分求解域,并对计算结果和时间进行了对比,结果表明可以采用不同的稀疏网格来提高计算效率;通过计算圆锥形织构轴承的压力分布,证实了该模型对复杂求解域的良好适用性. 相似文献
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有限体积法在求解传热学中温度场的应用初探 总被引:2,自引:0,他引:2
通过把有限体积法应用到传热学中求解温度场,初步探讨了有限体积法的原理和方法以及用此方法在求解温度场中的特点和作用,并计算了简单的实例;为今后更进一步深入地研究和探讨打下了良好的基础。 相似文献
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以一维平底溃坝问题为例,讨论了有限体积法的应用。从溃坝基本方程入手,采用Roe方法计算界面数值通量,采用空间一阶、时间二阶格式(预测校正二步格式)计算溃坝问题,得到了满意的结果。 相似文献
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基于无规则网格的有限体积海岸海洋模型(FVCOM),建立适用于辐射沙脊群海域的三维潮流数学模型。为了更好地贴合不规则海岸边界,平面采用三角形网格剖分,垂向采用σ坐标进行模拟。结果表明,模型的计算值与观测值吻合良好,较好地反映了研究海域流场的时空分布特征。整个海域流场由南、北两股潮流向弶港辐聚辐散,各深槽流速较大而集中,流向与深槽走向十分一致;弶港以北,表、底层余流方向都是从南到北的沿岸流,南部海域的近岸余流有逆时针的旋转流,近深槽余流大都指向深槽。 相似文献
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In this paper, we present a Finite pointset method (FPM) for the numerical simulation of free surface flow around a ship in calm water. It is a Lagrangian and meshless particle scheme which is applied to the projection method for the incompressible governing equations. This requires the solution of Poisson problems in each time step, so a moving least squares (MLS) interpolants is used for the spatial derivatives in order to discretize the Poisson equation with pressure-Dirichlet condition of free surface flow in meshless structure. Meanwhile, an additional problem of the periodic particle locations redistribution in the present approach is still handled by MLS interpolants. With the proposed FPM technique, problems associated with the free surface flow around a ship are circumvented. A verification of numerical modeling is made using the Wigley hull and the validity of the proposed methodology is examined by comparing the detail of wave profile and wave-making resistance with Series 60 model. The results demonstrate that FPM is able to perform efficient and stable simulations of free surface flow around a ship. 相似文献
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Peter Frenzel Corinna Borrmann Beate Lauenburg Bjrn Bohling Jan Bartholdy 《Journal of Marine Systems》2009,75(3-4):430-440
An experimental sediment dumping was carried out in the southern part of the Mecklenburg Bight in June 2001. Foraminiferans and ostracods from superficial sandy sediment were studied in a time series from before dumping until March 2004 in order to assess changes in associations and recolonization patterns of both groups. Additionally, an area sampling covering the dumping site and its surroundings from 15.5 to 20.7 m water depth made it possible to compare associations inside and outside the dumping area as well as the water depth dependent distribution of foraminiferans and ostracods. Salinity values vary within the high alpha-mesohaline and low polyhaline range. The dominating species are Ammotium cassis (Foraminifera) and Sarsicytheridea bradii (Ostracoda). The diversity is low (Fisher alpha index from 0.4 to 3.2 for foraminiferans and 1.0 to 2.5 for ostracods), but higher within the dumping site samples. These higher values are explainable by input of allochthonous tests and valves representing additional species. After the sediment dumping it took two and a half years to re-establish the total foraminiferan association and the total foraminifer/ostracod ratio within the dumping site. Total foraminiferan abundance increases remarkably with water depth (mean 83 tests in 100 ml) driven by higher nutrient availability and more suitable salinity and temperature values within the zone of the oscillating halocline. The distribution of shallow water species such as Cribroelphidium excavatum, Eucythere argus and Hirschmannia viridis, within the transient water layer A. cassis, Nodulina dentaliniformis, S. bradii and Palmoconcha laevata and below Eggerella scabra indicate the depth position of the halocline. Water depth and sediment dumping influence are the main driving factors for the distribution of foraminifer and ostracod associations within the study area. However, a significant sedimentological difference between samples inside and outside the dumping area is not recognizable. 相似文献
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文中介绍了海上砂石无序开采给社会带来的负面影响,分析了砂石运输船治理存在的问题,提出了砂石船运输治理的相应对策。 相似文献