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港珠澳大桥所跨越的珠江口水域是我国水上运输最繁忙、船舶密度最大的水域之一,桥建设水域海面宽阔,大型船舶以及高速客船航行频繁,桥区水域船舶通航密度大通航环境极为复杂,大桥施工期间,更加重了桥区及人工岛附近水域的水上交通安全问题。为了保证大桥水域通航有序和施工顺利进行.就大桥水域的水上交通安全进行简要分析,并对大桥建设期间水上交通安全提出信息化监管方案。 相似文献
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随着社会经济的发展需求越来越高,消防水域救援形势日益严峻,消防水域救援能力考验越来越高。水域救援是消防队伍新的职能使命,近年来,多地区发生大型洪涝灾害,消防水域救援专业队伍发挥作用日益凸显。消防应急救援的任务量不断攀升,部分城市已经占到了总任务量的50%至70%,水域救援的任务需求也逐渐日益凸显。但面对“全灾种、大应急”的总要求,水域救援专业队在体系建设、能力建设和职能划分等方面还存在不足。本文从当前消防救援队伍水域救援现状入手,提出了当前影响水域救援能力的因素,最后提出了水域救援队伍建设一些思考,以期更好地发挥水域救援专业队作用。 相似文献
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桥梁布设在通航水域的桥墩以及通航孔在一定程度上限制了船舶的航行,划定桥区水域对指导船舶安全航行具有重要意义。通过梳理当前桥区水域法规中船舶航行限制,分析划定桥区水域的影响因素;以桥梁涉水桥墩对航道内在航船舶的影响为依据,基于船舶领域理论设计了桥区水域宽度和纵向长度计算方法,可依据桥梁特点及航道水域特征对桥区水域进行划定,实现桥区水域划定的一桥一策;利用该方法对长江某大桥的桥区水域进行划定。结果表明,与传统桥区水域划定方法相比,该划定方法能够在保障船舶桥区航行安全的基础上,减少对航道内正常航行船舶的约束,同时可避免岸线资源的浪费。 相似文献
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我国内河水域新建桥梁在对主墩进行施工过程中,为了确保船舶正常通航,海事部门要求实行单向通航。因此,主墩施工期间桥区水域可能出现船舶排队等候过桥的现象,船舶等候过桥势必增加桥区水域复杂的通航环境,目前海事部门规定桥区水域(单向通航)航行的船舶之间应保持足够的安全距离。通过建立数学计算模型对桥区水域(单向通航)通航船舶之间安全距离进行量化研究,探讨出桥区水域船舶之间安全距离计算方法。为海事部门制定桥区水域通航安全管理规定、维护桥区水域良好的通航秩序和船舶过桥安全提供科学的理论依据。 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
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