钛合金表面镍包石墨喷涂层的耐磨性能

为了提高钛合金的表面耐磨性,利用氧乙炔热喷涂枪,在TC4合金表面上制备出镍包石墨涂层。采用MXP-2000型销盘式摩擦磨损实验机,进行钛合金及其镍包石墨涂层的干摩擦磨损实验,并利用扫描电镜对磨损表面进行观察和分析。实验结果发现,镍包石墨涂层的摩擦系数只有钛合金的一半左右,前者磨损量为后者的1/6,说明镍包石墨涂层可以大大提高钛合金的表面耐磨性能。TC4合金的磨损机制以黏着磨损为主,喷涂层的磨损机制以磨粒磨损为主,喷涂层中的石墨润滑相是其耐磨性高的主要原因。     

光时域反射仪检定装置测量不确定度评定

介绍了光时域反射仪检定装置的测量不确定度评定方法,此方法适用于建立计量标准的测量不确定度评定.     

基于传热与压力损失的气-水换热器耦合设计

针对换热器设计中如何合理兼顾传热效率和压力损失的难题,以矩形流通截面的燃气-水列管式换热器为对象,从理论上分析了设计参数之间的内在联系,揭示了换热面积与燃气流通面积、横向管间距、换热管直径之间的匹配关系,建立了基于压力损失和传热计算的耦合设计方法。这种方法已成功应用于某大型燃气冷却器的设计,也可供其它换热器设计时参考。     

原子氧对Kapton／Al薄膜性能影响研究

模拟空间环境下原子氧辐照条件,通过采用固定的原子氧束流密度进行不同时间辐照试验,研究了温控涂层材料Kapton/Al薄膜的质量损失、光学性能、表面形貌和表面粗糙度的演化规律.试验结果表明,原子氧对材料的剥蚀量与原子氧的作用时间成正比例关系.材料辐照后太阳吸收率发生明显变化,而辐射率几乎不发生变化.辐照后试样表面的粗糙度,是影响太阳吸收率变化主要因素.随着辐照时间的增长,材料表面粗糙度增加,导致太阳吸收率增大.     

高超声速小钝锥尾流化学非平衡辐射研究

本文主要目的是研究化学非平衡对高超声速小钝锥尾流辐射的影响。计算结果表明：激发发射辐射比化学发光辐射重要，红外辐射比可光辐射重要。结果还表明：由化学非平衡瞬时辐射模型计算求得的ＮＯ５．３μ的辐射能比由局部平衡辐射模型求得的辐射能大３０￣７０％。由此可知，小钝锥尾流的化学非平衡辐射模型对辐射的影响是不能忽略的。     

耐高温聚酰亚胺胶黏剂的研究进展

综述了近年来耐高温聚酰亚胺胶黏剂的研究发展状况，对聚酰亚胺胶黏剂尤其是加成型聚酰亚胺胶黏剂的化学合成方法和胶黏剂结构与性能的关系进行了分析与总结，并对耐高温聚酰亚胺胶黏剂的应用和未来发展趋势进行了展望。     

某型发动机新件涡轮叶片叶冠掉块故障分析

为排除某型发动机新件涡轮叶片叶冠掉块故障,对故障件进行尺寸检测、加工制造工艺复查、断口分析、结构和强度分析等,认为:引发故障的主要原因是叶冠转接R不圆滑、存在尖角,造成应力集中;而相邻原机件叶片弦宽尺寸超差,锯齿形工作接触面积小,以及非工作面局部碰磨,是引发故障的次要因素。采取并验证了有针对性的排故措施。     

航空发动机轴承的滑蹭损伤与防止措施

分析了航空燃气涡轮发动机主轴承产生滑蹭损伤的机理与危害。并根据滑蹭损伤的机理，提出了防止轴承出现滑蹭损伤的两项措施：增加驱使滚子一保持架运动的拖动力；减小阻碍滚子一保持架运动的阻力。列举了国外一些发动机中防止滑蹭损伤采用的措施。     

BH新型憎水剂及其憎水膜层“三防腐蚀”性能研究

研究了BH系列(BH 102和BH 103)憎水剂的合成工艺、技术指标、憎水处理成膜工艺以及憎水膜层的憎水效果和耐腐蚀性能。结果表明,BH系列憎水剂的憎水效果良好,在零件表面形成的憎水膜层能达到105°以上的憎水角;同时经BH系列憎水剂处理后的钢铁磷化表面的耐腐蚀性能得到明显改善,具有优良的"三防腐蚀"性能,其中含有复配缓蚀剂的BH 103憎水膜层的耐腐蚀性更优于添加单一缓蚀剂的BH 102憎水膜层。     

A Comparative Study of the Influence of the Active Young Sun on the Early Atmospheres of Earth, Venus, and Mars

Because the solar radiation and particle environment plays a major role in all atmospheric processes such as ionization, dissociation, heating of the upper atmospheres, and thermal and non-thermal atmospheric loss processes, the long-time evolution of planetary atmospheres and their water inventories can only be understood within the context of the evolving Sun. We compare the effect of solar induced X-ray and EUV (XUV) heating on the upper atmospheres of Earth, Venus and Mars since the time when the Sun arrived at the Zero-Age-Main-Sequence (ZAMS) about 4.6 Gyr ago. We apply a diffusive-gravitational equilibrium and thermal balance model for studying heating of the early thermospheres by photodissociation and ionization processes, due to exothermic chemical reactions and cooling by IR-radiating molecules like CO₂, NO, OH, etc. Our model simulations result in extended thermospheres for early Earth, Venus and Mars. The exospheric temperatures obtained for all the three planets during this time period lead to diffusion-limited hydrodynamic escape of atomic hydrogen and high Jeans’ escape rates for heavier species like H₂, He, C, N, O, etc. The duration of this blow-off phase for atomic hydrogen depends essentially on the mixing ratios of CO₂, N₂ and H₂O in the atmospheres and could last from ∼100 to several hundred million years. Furthermore, we study the efficiency of various non-thermal atmospheric loss processes on Venus and Mars and investigate the possible protecting effect of the early martian magnetosphere against solar wind induced ion pick up erosion. We find that the early martian magnetic field could decrease the ion-related non-thermal escape rates by a great amount. It is possible that non-magnetized early Mars could have lost its whole atmosphere due to the combined effect of its extended upper atmosphere and a dense solar wind plasma flow of the young Sun during about 200 Myr after the Sun arrived at the ZAMS. Depending on the solar wind parameters, our model simulations for early Venus show that ion pick up by strong solar wind from a non-magnetized planet could erode up to an equivalent amount of ∼250 bar of O⁺ ions during the first several hundred million years. This accumulated loss corresponds to an equivalent mass of ∼1 terrestrial ocean (TO (1 TO ∼1.39×10²⁴ g or expressed as partial pressure, about 265 bar, which corresponds to ∼2900 m average depth)). Finally, we discuss and compare our findings with the results of preceding studies.