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建立在“无齿间滑动摩擦”理论基础上的渐开线齿轮传统理论认为,只要主动轮的输入扭矩保持恒定,从动轮的输出扭矩必维持不变。然而,该文研究表明,由于齿间滑动摩擦的存在,即使输入扭矩保持恒定不变,输出扭矩仍会发生波动,且波动率随齿间滑动摩擦系数增加而增大。减小齿间滑动摩擦系数是使输出扭矩保持平稳的一个有效措施。 相似文献
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不计齿间及轴颈与轴承间摩擦的经典渐开线齿轮理论认为,若输入扭矩保持恒定,则齿轮机构运行平稳,不会振动。本文的研究充分表明:尽管齿轮机构的输入扭矩保持不变,然而,由于滑动摩擦及轴承间隙的存在,齿轮必产生振动。本文指出,对于具备足够刚性的齿轮机构而言,降低齿间及轴颈与轴承间滑动摩擦系数并减小轴承间隙是抑制齿轮振动的有效措施。 相似文献
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船舶航行时船体中拱及中垂弯曲变形使沿船体纵向布置的齿轮机构的轴承支座中心距产生缩减.这种中心距缩减会导致互相啮合的两齿轮间产生附加的径向压力,从而使齿轮机构处于双面啮合工作状态.本文分析及计算了齿轮机构在该双面啮合工作状态时齿间摩擦及轴承摩擦所消耗的功率,并提出能满足船用齿轮机构正常运行要求的输入功率补偿公式. 相似文献
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该文就非正确安装条件下渐开线直齿圆柱齿轮机构稳定运行时齿轮副机械效率与齿间滑动摩擦系数等有关参数间的关系展开了分析及研究,并推导出一组可直接确定齿轮副效率数值的计算方程组。由该方程组所显示的数学关系式可知,齿轮副效率不仅与齿间滑动摩擦系数有关,而且还受齿数及中心距增量系数等参数变化的影响。 相似文献
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齿间摩擦对增速齿轮机构主动轮齿根弯曲疲劳强度之影响 总被引:1,自引:0,他引:1
该文分析了渐开线增速齿轮机构主动轮轮齿处于齿顶啮合位时的实际受载状况,并就主动轮轮齿齿根危险剖面上的弯曲应力作了深入的研究,进而推导出一组计及齿间滑动摩擦力影响的主动轮齿根弯曲疲劳强度计算公式。 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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