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船冰碰撞载荷下船舶结构加强方案研究 总被引:3,自引:0,他引:3
为了探究水介质对船—冰碰撞结构响应的影响,文章首次对考虑水介质中的船—冰碰撞问题进行了研究。模拟了船舶与冰体在水介质中的碰撞场景,研究船—水—冰三者共同耦合作用对船—冰碰撞的影响。将该计算方法应用于船—冰碰撞的多种工况计算,对比分析了增加外板厚度、横隔板厚度以及肋骨间距等多种加强方案对船体结构响应的差异。揭示了碰撞区域的损伤变形、碰撞力、结构吸能随外板厚度、横隔板厚度和肋骨间距的变化而变化的规律,分析了船舶肩部各主要构件对于抵抗冰载荷作用的能力及贡献。所得结论对于进行冰区船舶结构设计具有参考作用。 相似文献
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针对破冰船冰致疲劳强度的问题,提出一种基于长时历计算的船冰碰撞模拟方法,通过船冰碰撞有限元模拟筛选出疲劳热点,运用雨流计数法对各个疲劳热点的应力时历曲线进行统计,得出应力循环下的均值和范围,进行平均应力修正,结合Miner线性累积损伤理论给出在设计寿命周期内的总损伤.结果表明:采用周期性介质分析方法计算到600s时破冰船应力时历统计特性已经稳定,且满足Weibull分布;船冰碰撞所造成的高应力结构多发生在船体外板区域,进行破冰船疲劳强度校核时应该多着重考虑船体结构与海冰发生碰撞的外板区域. 相似文献
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《中国航海》2017,(1)
为探究船-冰碰撞载荷下横骨架式和纵骨架式2种船体结构的耐撞性能,利用MSC/PATRAN软件建立油船及冰体有限元模型,运用非线性有限元软件Dytran对船中舷侧结构与冰体棱角发生碰撞进行仿真。通过2种舷侧结构的船体与冰体碰撞,对比不同船体结构的损伤变形、碰撞力和能量吸收的差异,探究各种船体结构的优劣性。利用不同船体结构的优劣性能对现有的2种船体舷侧结构进行改进,合理布置横骨材、纵骨材的数量及尺度,在船舶总质量改变不大的前提下,采用优化混合骨架设计结构方法提高舷侧结构的耐撞性能。计算结果表明,该方案对冰区船舶结构加强具有重要的参考意义,可为提高冰区船舶耐撞性设计提供建议。 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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