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船舶在实际海洋环境中的性能代表航行性能的优劣,通过结合海洋环境信息数据来探究船舶的耐波性能以达到对船舶辅助航行的目的,首先使用以切片法为理论的seakeeper软件对船舶耐波性进行仿真研究,获得船舶运动的传递函数和船舶纵摇、升沉、横摇有义值曲线,采用莫尔公式对模拟结果进行验证,通过数值模拟找到对耐波性指标较大的因素,根据耐波性指标衡准对船舶耐波性能做出评价,并应用统计学中的正交试验方法对耐波性的影响因素(航速、风速、航向)对耐波性指标的影响程度进行研究,使海洋环境中船舶的耐波性达到最优,从而起到指导船舶航行的目的。 相似文献
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船舶耐波性与船舶航速 总被引:1,自引:0,他引:1
通过对耐波性的分析,总结了船舶在波浪中航行时的耐波性标准,并提出了船舶在考虑了耐波性标准后应采取的经济航速,为船舶在大风浪中的开航安全评估提供了依据。 相似文献
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大风浪中船舶航向优选方法探讨 总被引:2,自引:0,他引:2
依据船舶耐波性理论计算结果,运用灰色关联综合评估理论对大风流中船舶耐波性进行了综合评估,然后根据结果确定船舶在波浪中以某一航速航行时的优选航向,并通过实例应用与分析表明,使用该方法能为船舶安全航行提供科学指导。 相似文献
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依据船舶耐波性理论计算结果,运用灰色关联综合评估理论对大风浪中船舶耐波性进行了综合评估,然后根据评估结果确定船舶在波浪中以某一航速航行时的优选航向,并通过实例应用与分析表明,使用该方法能为船舶安全航行提供科学指导。 相似文献
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船舶在波浪中航行时的纵向运动性能是衡量船舶综合航行性能的重要指标.为了改善船舶在波浪中的纵向运动性能,本文基于首部减摇组合附体技术对某型船首部构型进行改造并通过水池模型试验对其静水阻力和耐波性进行了分析研究.在分析该船作业及航区特点的基础上,通过船首部线型改造及减纵摇组合附体构型优化,给出适用于该船的首部构型方案.应用CFD软件和修正切片法进行水动力性能分析,并对船首构型方案进行优选.将优选出的性能较优复合船型方案和原船型开展水池模型静水阻力与耐波性对比试验分析,验证减摇复合船型的静水阻力性能与耐波性能.试验结果表明,改造后的复合船型减纵摇效果明显,对应实船四级海况18节航速下纵摇与首部加速度有义值较原船型降低15%以上;复合船型静水阻力有所增加,实船18节航速下静水阻力增加13.5%. 相似文献
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采用离差最大化方法对船舶耐波性进行综合评价,引入加权向量和规范化决策矩阵,以及各评价指标的权重和规范化矩阵对耐波性评价的影响,建立了基于横摇、纵摇、垂荡、砰击、甲板上浪、螺旋桨出水和船首垂向加速度的船舶耐波性综合评价体系,并系统阐述了该方法的基本原理和实施步骤.以30组样本数据为输入,对某油船在不同航行状态下的耐波性能开展了评价分析.与耐波性方程评估法相比,该方法理论完备、涵义明确、结果可靠,在船舶耐波性综合评价中具有一定的推广和实用价值. 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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