共查询到19条相似文献,搜索用时 218 毫秒
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金沙江与岷江干支流上水电站调峰发电下泄非恒定流引起下游叙泸段河道水流条件显著变化。结合一维非恒定流数学模型和实测资料分析研究叙泸段河道内代表性非恒定流传播过程及其造成水力参数相对于概化恒定流条件时的变化情况。结果表明:叙泸段河道内典型非恒定流波长为218 km,传播速度3 m/s;随着传播距离增加波衰减幅度减小,波形变得光滑;当宜宾水位处于波峰时,下游沿程流量呈现递减趋势,波谷则正好相反;相对于恒定流条件,其流量变化范围为0~730 m3/s,水位抬升0.5~2 m;断面平均流速变化在-0.5~0.2 m/s,比降变化范围为-0.2‰~0.2‰,比降最大值为1.38‰。 相似文献
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向家坝水电站日调节非恒定流与岷江日调节非恒定流在宜宾合江门汇合形成新的非恒定流过程,波长超过200 km,对宜宾—泸州河段(叙泸段)航道滩险的通航要素产生明显影响。采用平面二维非恒定水流数学模型,计算分析代表工况下日调节非恒定流传播规律及其对叙泸段拴疆碛航道要素的影响。结果表明:1)日调节非恒定流自合江门传递到拴疆碛约1.5 h,拴疆碛水位日变幅最大约1.053 m,相较于合江门衰减约30%,且波峰时期水面比降小于波谷时期,拴疆碛卵石滩采砂对非恒定流运动产生明显影响;2)代表性日调节非恒定流过程中,拴疆碛河段满足航道维护标准2.9 m水深的河宽在204~585 m,现有航标设置存在航道边界不满足最小维护水深情况,须对现有航标设置方案进行优化。 相似文献
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通航河流修建水利枢纽后,调峰发电下泄类似“人造洪峰”的非恒定流和含沙量趋近于零的清水,破坏了河流的平衡,给河床演变、航道整治技术等带来新的课题。通过水槽试验、理论分析等手段,研究枢纽下游非恒定流作用下均匀沙的起动与输移规律。研究认为:非恒定流作用下输沙率变化过程与水流条件具有不同步性,并与水流非恒定强度P有关,当P>032时,水流参数峰值一般先于输沙率峰值;当P<032时,水流参数峰值滞后于输沙率峰值。 相似文献
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对三峡坝区下游的黄陵庙至南津关长约28.5 km的河段进行了一维和二维非恒定流数值模拟。文中采用Presimann四点偏心隐式差分求解一维非恒定流,采用正交曲线坐标系下二维水深平均数学模型进行二维非恒定流计算。根据实测资料,由河段上、下游的黄陵庙、南津关(二)水位站测定的水位过程给定水位边界条件,通过河段中的莲沱、石牌、平善坝水位站的实测水位过程以及黄陵庙(陡)水文站实测的流量过程进行模型验证,结果表明一维和二维数模计算出的水位、流量过程与实测值符合良好。由于二维计算时间远大于一维,因此在拟定和优化三峡—葛洲坝联合调峰运行方案时可主要采用一维非恒定流模型,在某些工况下,因通航限制而需要限定局部河段流速时可采用二维非恒定流模型。 相似文献
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山区河流电站下游河段设计低水位确定方法 总被引:1,自引:0,他引:1
山区河流电站在枯水期通常采用日调节运行方式,电站下泄流量为非恒定流,致使下游河道水位起落不定,航道设计水位的确定难度较大。利用实测资料,对山区河流电站下游河段的设计低水位进行了分析计算。实践表明,对于电站下泄非恒定流,应尽量利用实测波谷时段水位进行下游河道设计低水位推求,能够满足航道整治设计的要求。 相似文献
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船闸引航道内水面波动的二维数学模型研究 总被引:4,自引:5,他引:4
提出船闸引航道内水面波动的二维数学模型,采用二维非恒定流数学模型和船闸灌泄水一维数学模型联解.这一模型考虑了船闸灌泄时水流惯性的影响,较好地模拟了三峡工程上引航道船闸灌水产生的水面波动,同时,给出了水面波动周期和波长的近似计算公式。 相似文献
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为分析乌江渡水电站泄流对下游乌江渡码头通航水流条件的影响,建立了乌江渡码头河段二维非恒定流水流数学模型,并运用实测水位流速资料对模型进行验证。对恒定流通航条件进行模拟分析。针对电站发电泄流代表方式,采用流速和比降历时变化、10 min水位变率,分析电站泄流引起的乌江渡河段通航水动力变化过程。结合船舶上行能力,分析电站泄流对船舶进港靠泊的影响。 相似文献
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Catamaran vessels operating at high-speed can be exposed to deck diving and bow damage and one resolution of this problem is the wave-piercer design of INCAT Tasmania. Owing to the complexity of the unsteady non-linear flow in the bow area during large wave encounter model testing has been undertaken to identify the peak dynamic slam loads on the ship structure. This paper provides experimental benchmark information relating to the wave slam loads on wave-piercing catamaran ferries. Since the time frames of transient slam loadings and whipping vibration of the entire hull in its first bending mode are similar it is important that the test model replicates the whipping response and therefore needs to be a hydro-elastic model. A 2.5 m hydro-elastic segmented catamaran model has been developed based on the 112 m INCAT Tasmania wave-piercer catamaran to establish the peak wave slamming loads acting on the full-scale vessel. Towing tank tests were performed in regular seas at a maximum full-scale operating speed of 38 knots. The model was instrumented to measure the dynamic slam loads acting on the centre bow and vertical bending moments acting in the demihulls of the catamaran model as a function of wave frequency and wave height. Peak slam loads measured on the centre bow were found to approach the total weight of the model, this being a broadly similar result to the peak loads measured at full-scale. It was found that global dimensionless heave and pitch accelerations peaked in the same range of encounter frequency as did the peak slam load. 相似文献
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《船舶与海洋工程学报》2017,(3)
Trapping of oblique surface gravity waves by dual porous barriers near a wall is studied in the presence of step type varying bottom bed that is connected on both sides by water of uniform depths. The porous barriers are assumed to be fixed at a certain distance in front of a vertical rigid wall. Using linear water wave theory and Darcy's law for flow past porous structure, the physical problem is converted into a boundary value problem. Using eigenfunction expansion in the uniform bottom bed region and modified mild-slope equation in the varying bottom bed region, the mathematical problem is handled for solution. Moreover, certain jump conditions are used to account for mass conservation at slope discontinuities in the bottom bed profile. To understand the effect of dual porous barriers in creating tranquility zone and minimum load on the sea wall, reflection coefficient, wave forces acting on the barrier and the wall, and surface wave elevation are computed and analyzed for different values of depth ratio, porous-effect parameter, incident wave angle, gap between the barriers and wall and slope length of undulated bottom. The study reveals that with moderate porosity and suitable gap between barriers and sea wall, using dual barriers an effective wave trapping system can be developed which will exert less wave force on the barriers and the rigid wall. The proposed wave trapping system is likely to be of immense help for protecting various facilities/infrastructures in coastal environment. 相似文献