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介绍深圳港引航站对引航员登离船安全风险的识别与控制措施,包括引航员登离船装置存在的风险识别与控制、港区交通的风险识别与控制、从码头上下引航艇/拖船的风险识别与控制、在引航艇/拖船上的风险识别与控制、来自被引船舶的风险与控制以及应急措施。阐释安全措施的落实与保障机制的运行。指出安全措施的持续改进与完善需要将好的做法、好的措施引入,提升引航员登离船安全水平,以及发现问题、分析原因、制定整改措施,并将措施制度化。 相似文献
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针对海上风电机组运维需求,设计海上风电运维船的小型化波浪补偿登乘栈桥。进行登乘栈桥的总体设计、力学分析和软件设计,并对登乘栈桥的三维模型进行有限元仿真。仿真结果表明,所进行的设计可满足海上风电运维船的小型化和轻量化要求,保证人员与物料的安全和作业环境的稳定。 相似文献
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根据国际标准规定的登离船装置登乘梯和引航员梯的可靠性验证要求,通过一种尼龙改性材料及其制成的塑料踏板进行长达一年多的试验,研究材料老化、材料吸水性和不同的结构设计对塑料踏板本身强度的影响规律.结果表明:即使是塑料材料本身满足一年老化强度试验,且采用其做成的塑料踏板初期也满足整梯标准要求,但如果不增加塑料踏板本身的耐老化... 相似文献
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引航员安全登离船的过程主要涉及两个方面,一方面是符合公约要求的引航员登离船装置,另一个方面是合适的、用于接送的引航船艇。国际海上人命安全公约(Internationa Convention for the Safety of Life at Sea.SOLAS)对引航员登离船装置有强制要求。尽管国际海事组织(IMO)、国际引航协会(IMPA)、世界各国船级社、航海界和各国的引航机构一直非常重视引航员的登离船安全,但是引航员登离船过程中的伤残事故还是一次又一次地发生,从而促使IMO、IMPA等不断修改、完善引航员登离船装置。2012年7月1日生效的SOLAS第V章全面修改了第23条,对引航员登离船装置又提出了新要求, 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
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