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北仑电厂码头改扩建工程潮流泥沙数值模拟 总被引:2,自引:1,他引:1
运用平面二维水流泥沙数学模型,分别建立了包含金塘水道大范围以及拟建工程区小范围水域的潮流泥沙场,其中大范围模型为小范围模型提供边界条件。计算结果表明:改扩建工程使周边局部海域流场减弱,但影响范围有限,流场变化主要集中于改扩建码头西侧及其后沿驳船码头港池开挖区水域,涨、落急流速变幅在13.3%以内,流向变化值小于8.3°。码头后沿的浅滩区是主要泥沙淤积区,改扩建码头前沿平均淤强约0.76m/a,淤积量2.5万m3/a,驳船泊位区平均淤强1.42m/a,淤积量5.9万m3/a。鉴于岸坡浅滩仍是主要的淤积区,建议保持定期疏浚,以免淤积前伸对驳船港池和码头前沿造成不利影响。 相似文献
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崖门出海航道疏浚工程潮流泥沙变化数值模拟 总被引:1,自引:1,他引:0
崖门出海航道穿越黄茅海,是连接银洲湖和珠海高栏港的重要通道。采用数学模型在对最近的水文数据和地形冲淤资料验证的基础上,对崖门出海航道的进一步浚深方案进行了潮流泥沙运动模拟和航槽回淤计算。计算结果表明:东航道水沙条件相对较优,泥沙回淤主要集中在拦门沙航段,具有进一步提升通航标准的空间,在同等条件下可选择优先开发东航道。 相似文献
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针对三峡水库下游尺八口弯道段在三峡水库蓄水后的新水沙条件下,出现凸冲凹淤(撇弯切滩)的现象,采用原型资料分析、理论分析、数学模型等多种方法,对其演变机理进行研究。结果表明,三峡水库下游尺八口河段发生凸冲凹淤现象的主要影响因素为三峡水库蓄水运用后来水来沙条件的变化,并预测凸冲凹淤的现象持续发展的可能性较大。 相似文献
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粘土含量对粉沙质泥沙沉降速度的影响 总被引:1,自引:0,他引:1
通过对泥沙沉降试验结果进行统计整理和理论分析,研究了粘土含量对粉沙质泥沙沉降速度的影响。结果表明:泥沙沉降速度同时受泥沙中值粒径d50和粘土含量p0.004控制;沉降速度ω随泥沙中值粒径d50增大而增大;粘土含量较小时,沉速随p0.004增大而减小,粘土含量较大时,沉速随粘土含量增大而增大;粘土含量对泥沙沉速影响的分界点为20%~25%。 相似文献
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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
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南黄海辐射沙脊群悬沙特征研究 总被引:2,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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船闸引航道异重流淤积分析计算 总被引:2,自引:2,他引:0
根据异重流运动的特点,从水体重率沿程变化的机理出发,运用能量原理,推导出异重流淤积计算公式,并用于大源渡船闸引航道淤积计算。所得成果与已有3种公式计算结果的平均值相当,通过类比分析,所得淤积量分布与实测资料一致。 相似文献
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