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船舶气囊下水安全性评估方法研究 总被引:4,自引:0,他引:4
气囊下水是船舶下水的一种创新方式,但是气囊下水过程中船体强度和气囊的安全性还没有定量的计算方法.近年采用气囊下水的船舶重量不断增大,下水安全性问题日益突出.本文考虑气囊刚度的非线性、下水过程中船体的力平衡条件等,提出了一种基于全船结构有限元分析的船体结构和气囊安全性评估方法.研究的内容和结果是紧密结合工程实际的.(1)考虑气囊压缩变形的非线性,研究了一种预报气囊刚度的有效方法;(2)基于弹性下水理论,研究了一种考虑弹性基座刚度非线性变化的船体梁运动和受力的计算方法;(3)提出了直接采用全船结构有限元分析计算船体结构应力和气囊受力的方法;(4)对某型实船进行了气囊下水的安全性分析,并与文献的结果进行比较,验证了气囊下水工艺的优越性和本文建议方法的准确性. 相似文献
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船舶纵向气囊下水宽支座弹性计算方法初探 总被引:4,自引:0,他引:4
本文介绍了船舶纵向气囊下水的气囊运动机理,构建了船体与气囊受力模型,并将船体、气囊与船台假定为串联弹簧体系,提出了船舶纵向气囊下水宽支座弹性计算方法。 相似文献
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船舶采用气囊下水工艺的船台压力计算初探 总被引:1,自引:0,他引:1
目前,船舶气囊下水过程中的船舶、船台受力变化计算尚未见较为详细的研究结果,这影响到船舶气囊下水工艺的推广。通过对船舶气囊下水工艺的研究,针对该问题提出宽支座弹性计算模型,并应用该模型进行实例计算分析。结果表明,该模型可用于下水过程中的船台压力分析。 相似文献
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万吨级船舶气囊下水研究 总被引:1,自引:0,他引:1
《中国修船》2015,(2):40-44
气囊下水技术是我国具有自主知识产权的一项高新技术。文章基于气囊下水存在的一系列技术问题,通过气囊压缩试验、实船下水过程测试等方法的不断探索、研究,对大型船舶下水用气囊的结构及性能参数要求、船台坡道参数、牵引力计算以及下水计算等方面进行了深入的研究,总结出了一套完整的计算方法。研究结果已在70 000 DWT和82 000 DWT等船舶下水实践过程中得到了充分的认证,从而为大型船舶的下水提供了一套技术理论支持。 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