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分散式布置的通航水利枢纽引航道口门区水流流态主要受到与其相衔接的河道形态影响。以广西邕宁水利枢纽工程可行性研究阶段布置方案为例,对分散式布置枢纽上下游引航道口门区流态与主流的衔接关系和通航水流条件优化措施进行研究。通过在船闸口门区增设导流堤和合理开挖右岸滩地的方式解决邕宁枢纽上游引航道口门区回流较大的问题;通过合理调整下游左岸岸边开挖线,压缩下游回流区,解决因下游引航道口门区主流流向与船闸中心线夹角较大而造成的回流严重问题。使得上下游引航道口门区均具有良好的通航条件。 相似文献
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建立大藤峡水利枢纽水工整体物理模型,对大藤峡水利枢纽船闸上游口门区布置方案进行试验验证,结合上游引航道口门区布置及附近地形分析,对工程方案进行优化,通过调整引航道中心线制动段弯道弧度和半径、调整口门区与上游主航道连接形式、增设导航墩和优化口门区附近区域地面高程等工程措施,使口门区的水流条件满足通航要求,并节省工程量。 相似文献
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渠江风洞子枢纽是以航运为主、结合发电的枢纽工程。本文结合模型试验成果,论述了船闸上、下引航道口门区的通航水流条件、船闸引航道平面布置及泥沙淤积对引航道及口门区通航条件的影响,提出了改善引航道口门区通航水流条件的工程措施。该研究成果已被设计采用。 相似文献
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针对渠江四九滩枢纽上、下游引航道口门区通航水流条件,结合国内外研究情况,简要介绍了枢纽布置、枢纽整体水工模型试验和自航船模试验的部分成果,并提出改善口门区通航水流条件的工程措施。 相似文献
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结合凤仪场电航枢纽船闸引航道口门区通航水流条件试验成果,分析了低闸坝枢纽船闸引航道导墙的结构、布置对口门区水流条件的影响,提出了改善引航道口门区水流条件的措施。 相似文献
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西津水利枢纽二线船闸工程对发展西江航运和流域经济具有重要作用。为研究二线船闸布置方案与原一线船闸布置的相互影响,采用水工模型试验研究二线船闸下引航道两类不同布置方案下的水流条件,通过分别测定一、二线船闸下引航道口门区纵、横向及回流流速三项指标,并进行对比分析得知:一、二线船闸下引航道口门区采用共用布置方案时,在中洪水流量情况下,口门区内横向及回流流速难以满足规范要求;当采用下引航道口门区分开布置形式时,二线船闸下引航道口门区多项流速在各级通航流量下基本满足规范要求。 相似文献
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介绍了我国港口资源的整合现状,指出港口整合可以提升港口的形象和地位,也为区域经济和城市的发展注入强大的动力。最后指出在港口资源整合中要避免的几个问题。 相似文献
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广州集装箱码头的轮胎式场桥小车制动器使用10多年后,出现了许多问题,故进行了改造.分析了轮胎式集装箱龙门起重机小车制动器的主要故障现象,提出了改造方案,并加以实施. 相似文献
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本文对现有的选定球面轴承的三种工程方法进行了分析比较.引入了“合力系数”,并给出了合力方向上投影面积的精确解. 相似文献
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分析柴油机故障中常见的机体裂纹故障原因,认为由于设计缺陷和管理及操作不当,易造成船舶柴油机缸体上的裂纹多发生在气缸套凸肩处。如不及时处理这些裂纹和故障,就会造成缸套的裂纹直至出现缸套漏水等严重后果,针对NANTAIQUEEN轮柴油机对该类型故障的检修提出具体措施。 相似文献
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The hydrophysical and hydrochemical structure of the Sea of Azov, with developed bottom anoxia, was studied during the RV “Akvanavt” cruise from July 31 to August 03, 2001. The anoxic zone with a thickness from 0.5 to 4 m above the bottom was found in all deep regions of the Sea. Concentrations of hydrochemical parameters were similar to the pronounced anoxic conditions (about 90 mmol m− 3 of hydrogen sulfide, 17 mmol m− 3 of ammonia, 6 mmol m− 3 of phosphate, 7 mmol m− 3 of total manganese). The hydrophysical structure was characterized by the uniform distribution of temperature in the upper 6–7 m mixed layer (UML). Below this a thin (0.4–0.8 m) thermocline layer was observed, just above the anoxic waters. Formation of this phenomenon was connected with that summer weather conditions. Intensive rains led to increased influx of river waters in June. That resulted in large input of allochtonous organic matter (OM) and inorganic nutrients; the latter were consumed on the additional autochthonous organic matter production. In July the weather was characterized by a significant rise in the daily averaged air temperature and large oscillations of temperature during the day. In this period a wind of constant direction was absent, but wind bursts were observed. The completed analyses showed that the formation of such a structure could be connected with the following factors: (i) positive growth trends of the daily averaged temperature and the daily oscillations of temperature, (ii) presence of wind bursts. The joint action of these factors resulted in the formation of the UML. The amplitude of wind bursts determined the depth of UML, and the value of trend determined the value of the temperature change in the thermocline. An initial presence of bottom halocline (caused by the Black Sea water influx to the bottom of the Sea of Azov) prevented the heating of the bottom layer and therefore led to an increase of vertical gradient of temperature in the thermocline. The spatial distribution of the turbulent exchange coefficient confirmed the existence of a “stagnation” area located above the anoxia zone, which is also, apparently, the reason for its occurrence. 相似文献