共查询到20条相似文献,搜索用时 47 毫秒
1.
2.
基于长江上游东溪口卵石滩段的物理模型,开展了典型系列年卵石输移特征的试验。根据不同水动力条件下卵石输移的实测数据,从动力机理出发确定砾石输移速度。以此为基础,改进了二维数值模型,并将其应用于东溪口河段卵石输移过程模拟。将计算的卵石输沙分布及泥沙冲淤过程与实测值进行对比,卵石走沙轨迹与河道内走沙基本吻合,模拟泥沙冲淤变化与该河段实测分布一致。说明改进后的平面二维卵石推移质运动模型能较为真实地反映河道内卵石输移特性,可为解决长江上游卵石河段泥沙问题与航道整治工程提供理论与数据支撑。 相似文献
3.
二维泥沙数学模型的改进——模型的建立 总被引:1,自引:2,他引:1
本文针对河道弯曲、狭长的特点,引进贴体坐标.将复杂的河道计算域转换成规则矩形域,使问题在规则域上求解.拟合坐标系下模型改进表现在以下两方面,一是引进紊动动能和紊动耗散率闭合雷诺方程,使模型能够回答整治工程局部水流结构,如回流现象,二是建立了一种新的悬沙输移模式,该泥沙模型能体现悬沙与床沙交换机理,既适用于水库上游淤积计算,也适用于水库下游冲刷计算. 相似文献
4.
5.
6.
7.
8.
床面形态与河床阻力关系 总被引:1,自引:0,他引:1
从波运动尺度出发,建立了床面形态与河床阻力的关系式。该式可用于均匀沙与非均匀沙的动床阻力计算,并经室内外轻质沙及天然沙的507组实测资料验证,吻合程度较好,表明该式可用于沙质、卵石河床等各种床面形态的阻力计算。 相似文献
9.
论述了沙卵石滩的成因是河流历史演变的结果,近期年内"冲淤平衡",它不是落水冲刷不力所造成,这是枯水整治的根据;提出以整治为主或以疏浚为主的确定条件,并对几种建筑物治滩的条件、坝位选择和布置要求作了研究,并对坝头局部冲刷坑最大深度,汊流滩开辟副槽所需的流量和锁坝调节流量分配比坝高的确定等,得出了可行的计算方法. 相似文献
10.
11.
关于推移质不平衡输沙问题 总被引:2,自引:1,他引:1
本文考虑到悬移质、推移质和床沙的相互交换,从沙量守恒原理出发,获得出了推移质泥沙连续方程及河床变形方程.该方程表明,推移质河床变形不仅与推移质本身不平衡输沙有关,而且还与悬移质非饱和输沙有关,推移质河床变形实质就是全沙河床变形. 相似文献
12.
悬移质不平衡输沙水流挟沙能力 总被引:1,自引:0,他引:1
本文从悬移质挟沙能力的基本概念出发,推导出悬移质非均匀沙平衡输沙的挟沙能力及不平衡输沙的挟沙能力公式,这些公式进一步揭示了非均匀沙的输沙机理,全面地描述了各种河床组成在不同的来水来沙条件下的输沙规律,适用性广,计算简便。 相似文献
13.
粉沙质海岸泥沙运动推悬比的确定 总被引:8,自引:2,他引:6
提出了海岸泥沙运动中均匀沙和非均匀沙输沙率推悬比和航道淤积推悬比的计算方法。计算数值显示 ,粉沙质海岸上必须同时考虑推移质和悬移质。计算结果与水槽试验结果很接近 相似文献
14.
M. Perez-Arlucea G. Mendez F. Clemente M. Nombela B. Rubio M. Filgueira 《Journal of Marine Systems》2005,54(1-4):209
The aim of this study is to provide a budget study with calculated erosion rates. Three methods have been used to calculate sediment yield and denudation rates in the Ria de Vigo: (1) measurements of sediment loads, (2) measurements of sediment accumulation rates at the coast, (3) theoretical calculations of potential denudation. Sediment loads and water discharge were measured over a period of 14 months from May 1997 to July 1998. Two of the tributaries entering the Ria de Vigo were monitored for 12 more months, from May 2000 to May 2001, to observe changes in discharge and sediment loads. This period corresponded with atypical precipitation, with peak monthly values (600 mm) three times higher than those on record.Water rating curves are typically exponential. Suspended and dissolved loads vary for different rivers, showing values of 1.5 to 130 mg/l during 1997/1998. For 2000/2001, these values are twice as high. Suspended load versus discharge relationships for 1997/1998 were logarithmic, but data from 2000/2001 does not fit the same equation. Dissolved loads are several times higher than suspended loads in almost all cases. Dissolved load concentrations vary more widely with discharge than suspended loads. This is probably due to local pollution and contamination from marine spray in areas closer to the sea.Second, erosion rates and bed load sediment yields were calculated from accumulation rates at the Ramallosa Complex. Well-preserved estuarine and tidal sediments, associated with the Minor River, have accumulated in this area during the Holocene. 14C ages allow calculation of sedimentation rates (SR) for two intervals. The lower interval extends from 2001 to 484 years BP and yields an SR of 1.12 mm/a. The upper interval extends from 484 years BP to the present and has an SR of 3.3–4.4 mm/a. These differences may be explained by basin dynamics as the beach progressively encloses the area and also by human interference. From sedimentary facies analysis it is concluded that 90% to 95% of the accumulated deposits were transferred to the basin as bed load. Muddy deposits (mostly marshes) are better developed at the upper part of the sediment pile, and inner areas, indicating a progressive shallowing and filling up of the basin. Most of suspended load is exported to the ria, whereas the Ramallosa Complex acts as a sediment sink for bed load derived material.Calculated potential erosion rates using Ahnert's [Am. J. Sci. 268 (1970) 243] equation show lower values than those estimated from river load concentrations. Potential erosion rates for the Minor River are higher than for the Lagares River which contrast with mechanical denudation rate values from river loads during 1997/1998 which are higher for the Lagares River. During 2000/2001 MDR values were higher than those of the potential erosion rates for both rivers, in line with the extremely high precipitation. Higher values in the Lagares could be in part due to human interference. 相似文献
15.
16.
弹性设计准则下,极区船舶通常需要过度的结构加强以确保航行安全。若采用极限载荷设计准则,考虑结构的塑性承载能力,利用一部分屈服点之后的强度储备,则能大大减轻结构重量。本文以中国船舶及海洋工程设计研究院(MARIC)研发的某20000吨级PC5级极地多用途运输船为目标船型,基于IACS URI规范关于冰载荷及相应计算工况的要求,进行了非线性有限元分析。基于计算结果,工程计算推荐100mm×100mm的网格尺寸,材料定义推荐使用理想弹塑性材料。通过对比不同极限载荷准则,认为两倍弹性斜率准则相对更适用于船舶构件。研究成果可为极区船舶结构的设计与强度验证提供参考。 相似文献
17.
利用潮流和泥沙淤积数学模型计算了天津港的流场分布、含沙量分布以及悬沙落淤强度分布 ,其结果与实测资料基本一致 . 相似文献
18.
19.
20.
悬移质运动扩散方程的应用 总被引:1,自引:1,他引:0
从悬移质运动剖面二维扩散方程出发 ,通过适当假定 ,获得了饱和含沙量垂线分布公式、悬移质运动一维质量守恒方程和剖面二维实用型方程 ;重新定义了“α系数” ,给出了理论计算公式 ,使数值模拟的理论基础和可操作性得到了强化 相似文献