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随着船舶向高速化方向发展,首部砰击问题变得异常突出。本文通过楔形体入水砰击试验模拟船舶首部入水砰击现象并通过有限元仿真软件Ansys/Ls-dyna对楔形体入水砰击过程进行仿真分析,通过改变斜升角角度和楔形体下落高度研究砰击载荷的变化规律,并对楔形体入水时的压力变化及入水时液面抬升现象展开分析。研究结果表明,当楔形体表面与水面接触时,砰压立即增加,随后砰压会慢慢减小,最终趋于稳定。当楔形体的斜升角在变化时,楔形体的砰击压力也会随之变化,即当斜升角的角度越大,楔形体的砰击压力值就越小;当入水速度越快时,即入水高度越高时,砰击载荷的峰值也会越来越大,但处于同一速度(即同一高度),在楔形体以不同角度入水时,当它们的角度越来越大,最后的砰击载荷峰值就会越来越小。研究成果可为船体首部砰击作用下砰击载荷的变化规律提供参考。 相似文献
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当船舶航行于恶劣海况时,船舶会发生砰击现象。砰击现象是指船体发生剧烈的摇荡运动导致出水并再次入水,由于船舶入水砰击是瞬态过程,所以会在短时间内产生巨大的砰击压力,造成船体的变形甚至失效,因此准确预报入水砰击压力对保证船舶安全航行和作业具有重要意义。本文建立三维楔形体模型来模拟船首部位,结合有限体积法与动网格技术,引入VOF模型,数值模拟了波浪作用下不同刚度三维楔形体垂直入水的过程。研究发现不同刚度的三维楔形体分别入水的过程中,弹性结构入水砰击压力的峰值要小于刚性结构,弹性效应会一定程度减缓砰击的发生,为今后工程实践提供有价值的参考。 相似文献
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合理预报船首局部结构砰击载荷是船舶设计和研究者重点关心的问题。文章针对无转角和有转角楔形体舱段入水砰击问题,采用OpenFOAM开源软件,开发了基于两相流求解器InterDyMFOAM数值模拟结构入水砰击的程序包,开展了预报研究工作。数值模拟了入水过程的压力和加速度时域响应历程,与入水砰击模型实验进行了对比分析,吻合很好。同时讨论了网格划分等对结果的影响和砰击的三维效应。结果表明,本文提出的入水砰击载荷预报方法计算效率高,具有推广应用到预报复杂三维船首结构砰击问题的潜力。 相似文献
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航天器水上回收、两栖飞机水上降落、高海况下船舶航行等过程中均涉及结构的入水过程,入水过程的砰击现象一直是上述工程项目研制过程中的重点和热点基础研究之一。对求解结构入水砰击的3种技术途径(数值、仿真、试验)进行综合研究,介绍了3种方法的基本原理及工程实现方法并证明了其适用性,分别对楔形体结构自由入水砰击问题进行求解并进行对比分析,给出了楔形体上物面压力分布特点、典型测点处的砰击压力时历特征、入水过程中结构加速度特性及液面变化,可为入水结构设计、载荷条件制定、入水参数选取提供参考。 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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