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推进变频器的冷却系统设计好坏直接关系到船舶电力推进系统运行的稳定性和可靠性。本文设计了一种船用推进变频器冷却方案,并进行了热计算和仿真。计算和仿真结果显示运用此冷却方案变频器各部分温升均不超过使用限制,完全满足变频器船用要求。将此冷却方案应用到了产品上,各项指标正常,此变频器冷却系统工程设计及应用具有理论意义和参考价值。 相似文献
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《舰船科学技术》2021,43(20)
考虑到传统变频器调速控制方法无法满足船舶使用要求,为了确保船用变频器调速控制的稳定性,提出应用改进NLMS算法的船用变频器调速PLC控制方法。利用改进NLMS算法采集了变频器运行过程中的转速调节信号,通过定义控制频率函数,计算出船用变频器调速PLC自动控制的频率,通过对船用变频器进行荷载能力增量处理,完成船用变频器调速PLC控制的优化,应用改进的NLMS算法,并结合触发角组合方式,设计了船用变频器调速PLC控制流程,实现了船用变频器调速PLC控制。实验结果表明,改进NLMS算法的船用变频器调速PLC控制方法不仅可以稳定控制变频器电流,还可以保证转速控制的稳定性。 相似文献
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PLC控制交流变频调速控制系统在船用电梯中的应用 总被引:1,自引:0,他引:1
以OMRON的CQM1 PLC控制安川VS-616G5组成的控制系统为例,介绍了该系统在齿轮齿条驱动的船用电梯中应用的硬件结构、PLC和变频器通讯的相关程序设计及变频器的参数设置,以及基于自定义协议的PLC与环境监测智能仪表之间的通讯.突出了PLC+变频器在船用电梯中的控制特点,为PLC+变频器在船用电梯控制中的应用提供了实际经验. 相似文献
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本文对电力推进系统的变频器输入端谐波进行了理论分析,在建立系统各设备数学模型的基础上构建了针对船用变频器输入端谐波分析的通用用户模型库,对2000方绞吸式挖泥船谐波进行仿真计算,仿真结果符合理论分析且均满足船舶电网谐波要求。 相似文献
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谢纬铠 《交通部上海船舶运输科学研究所学报》1981,(2)
本文就CDJ-4型船用电磁计程仪的现场数据进行了可靠性分析与计算,从而提出了显示器并联冗余及全系统后备冗余方案的论证及数学模式.其结论已用于船用计程仪的设计,并取得较为显著的效果.此文还就有关船用导航仪器的可靠性问题提出了建议和展望. 相似文献
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双PWM变频器在船舶上的应用前景 总被引:1,自引:0,他引:1
因为船舶用电设备的谐波标准日益提高,而现阶段船用变频器会给船用电网注入大量的谐波,为此,PWM整流技术的研究,新型单位功率因数变流器的开发引起广泛的关注,因而双PWM变频器技术在船舶具有良好发展前景 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