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为了提高船舶龙骨结构在受力过程中应力分布的均匀性和提高材料的利用率,本文采用Hypermesh软件建立了龙骨结构有限元模型,并结合其MORPH功能定义筋板形状变量,建立形状优化模型。随后,将全局优化算法与形状优化模型相结合,对船舶龙骨结构进行优化设计。结果表明,在筋板交错位置增加筋板高度能够有效提升龙骨结构整体刚度,其余位置可以采用较小的筋板高度。本文研究可为船舶龙骨结构改进设计提供参考。 相似文献
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DOE技术在起重臂优化设计中的应用 总被引:1,自引:1,他引:0
为提高某船用起重机起重臂结构刚度,减小其最大应力以及结构质量,首先对各变量进行灵敏度计算,去除对目标函数不灵敏的设计变量,以提高后续计算效率。基于DOE试验设计理论及有限元法构建优化问题的近似模型,借助拉丁采样对该近似模型拟合精度进行检验。基于遗传优化算法(GA)对该近似模型进行优化。优化结果表明:刚度提高9.4%,最大应力值减小21.4%,结构质量减轻9.3%。 相似文献
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基于CFD的船舶船体总阻力预报方法 总被引:1,自引:1,他引:0
为了对船体航行阻力大小进行预测,使得设计人员在设计阶段便能够对船身结构进行优化改进,以获得性能优良的船身结构。基于UG建立船身与水流相互作用的几何模型,并借助hypermesh环境对几何模型进行离散化,得到高质量的流体动力学计算网格。将船头前部网格作为入口边界条件,后部以及侧面网格作为出口边界条件,船身对称面网格作为对称边界条件,建立有效的有限元计算模型。采用Fluent求解器对有限元模型进行求解,设定最大迭代步数为100步。通过对求解过程中动力粘度、速度、压力等重要的动力学参数残差收敛情况进行监控,表明整个计算过程收敛,得到的计算结果与实际情况相符合。通过CFD计算,得到了船身周围水压分布情况,根据船身前后方向水压差以及船身截面积,计算得到了船舶航行阻力。 相似文献
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环境干扰力作用下船舶操纵运动仿真数学模型研究 总被引:1,自引:2,他引:1
《舰船科学技术》2015,(7):153-156
为研究外界干扰因素对船身运动的影响,本文假设船舶航行环境中是小幅度波浪,船身摆动不是剧烈晃动。水流载荷采用切片理论进行计算,船身为一细长结构。以此为基础,建立基于船身局部坐标系的船体运动微分方程,并将其投射至全局坐标系。基于Matlab的Simulink工具对船舶运动微分方程进行计算,结果与现有文献结果较为一致,本文建立模型能够较好地反映外界干扰对船体运动的影响规律。 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