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船舶在航行过程中,螺旋桨在不均匀的伴流场中工作产生周期性的弯曲力矩作用在螺旋桨轴上,使推进轴系在螺旋桨或转轴上旋转的横向力矩作用下,旋转轴绕其静平衡曲线产生振动,从而出现回旋振动现象,而严重的轴系回旋振动引起轴承反力的动力放大而引起船体尾部结构的振动.本文对一艘尾部结构振动严重的船舶进行了推进轴系回旋振动计算分析及实船振动测量验证,分析了推进轴系回旋振动对船体尾部结构振动影响,通过更换尾管前轴承、调整中间轴承的位置,解决了轴系回旋振动引起的船体尾部结构严重振动问题,为解决类似船体尾部振动问题分析提供参考. 相似文献
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在船舶推进轴系运行过程中,油膜力发生变化会对轴承的刚度产生重要影响.为准确描述船舶推进轴系的运行状态,分析其变化规律,以油膜动力学为基础,结合油膜刚度系数计算方法,推导出四参数可变油膜刚度系数计算方程.以某64 000载重吨散货船为研究对象,建立船舶推进轴系有限元模型,并对其进行模态仿真计算,比较分析船舶推进轴系主要阶... 相似文献
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由于轴承油膜非线性特性的影响,轴承支承位置及其支承点数目对轴系回旋振动影响较大,运用滑动轴承的流体动力润滑原理计算分析轴承油膜刚度和阻尼动态特性分析,结果表明轴承内油膜刚度和阻尼呈非线性分布,各系数在方向上大小也不同。在此基础上,对某试验平台轴系上各轴承离散成等间距分布的多支撑点,分别计算每个支承点上的油膜动态性能系数,分析比较油膜动态性能系数各向同性和异性时对轴承回旋振动特性的影响,结果表明油膜动态性能耦合系数对轴承回旋振动在低频和共振频率阶段有较大影响。这一结论对轴系回旋振动低频噪声分析提供了一定理论依据,为更进一步研究其噪声辐射提供更为准确的分析方法。 相似文献
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轴系的回旋振动是影响船舶安全、稳定和持续运行的重要因素之一。本文以某轴系试验平台为对象,研究不同校中状态对其回旋振动的影响。根据该轴系试验平台的实际尺寸建立其有限元模型,以此为基础进行直线校中计算。以艉轴承上负荷最小为目标函数,采用IWO算法进行轴系双向优化校中,使得轴承位置优化后艉轴承上负荷明显减小。基于轴承支撑结构,运用雷诺方程计算轴承支撑油膜压力分布及其刚度特性,依此建立ANSYS计算的轴承支撑模型,计算和对比该轴系试验平台的不同校中状态对其回旋振动的影响,为在优化轴系校中过程中减小轴系回旋振动提供了一定的理论支撑。 相似文献
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分析国外在船舶推进轴系轴承油膜刚度计算方面的缺陷,根据船舶推进轴系的工作特点,提出了一种较为切合实际的航船推进系轴承油膜刚度的计算方法,并进行了实船计算。 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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