大型上单翼飞机机翼三维全场变形测量方案

针对大型上单翼飞机在飞行过程中机翼大挠度变形检测难题,提出了大倾角相机视场下机翼的非接触三维全场变形测量方案。根据上单翼飞机结构特点,将预先标定内参数和相机外参数的共轭相机组安装于飞机垂直尾翼上,采集飞行中的机翼变形图像。首先,提出了大倾角弱相关散斑匹配方法,解决了相机在大倾斜角度状态下采集到的机翼变形弱相关图像相关性差,难以相关匹配的问题。其次,由于测量相机安装于垂直尾翼,飞行测量过程中相机会受到气流扰动产生振动,本文提出了一种相机动态校正方法,通过在机背布置预拉伸刚性不动编码标志点,实时解算基准相机的绝对外参数,进而确定共轭相机的绝对外参数,实现所有测量相机外参数的动态校正。最后,开发了机翼变形全场测量软硬件系统,搭建了缩小比例机翼模型试验台并进行了仿真测量,对系统测量精度进行了比对分析。测量结果验证了本方案的有效性、可行性,对实机测量有一定的指导意义。     

基于L_1自适应的超低空空投抗侧风控制律设计

针对超低空空投过程中侧风干扰与装备投放过程相耦合,影响载机飞行安全和空投任务的完成等问题,提出了基于L_1自适应的控制律设计方法。利用最优控制对系统线性部分做状态反馈并确定匹配参考模型,在此基础上,考虑系统的匹配和非匹配不确定性,设计L_1自适应控制器实现姿态保持,结合外环PID侧向轨迹控制器实现对航迹的稳定和保持。仿真结果表明,控制器具有优良的控制性能,对复杂侧风干扰和系统非线性不确定性具有很强的鲁棒性,且在高自适应增益下能有效抑制输入信号高频抖振。     

浅析大飞机数字化设计与制造技术

大飞机工程是一个国家具有战略性的高技术产业链,而数字化技术在大飞机设计制造过程中的应用有效推进了大飞机的设计制造进程.论述了大飞机数字化技术的几个典型特征,并从设计制造的9个方面浅析了数字化技术在大飞机设计制造中的应用,涵盖了大飞机设计制造的大多数领域.展望未来数字化技术将会越来越深入地融入到大飞机设计与制造的每个角落.     

缺口件疲劳寿命预测新方法

采用有限元方法针对缺口件多轴疲劳实验结果进行模拟。结果表明,相同路径条件下,随着缺口半径减小缺口根部附近的应力梯度显著增加。基于缺口根部应变值,采用等效应变法进行疲劳寿命预测,预测结果随缺口半径的减小而偏于保守。采用应力梯度法确定有效距离,相同路径下,随着缺口半径的减小有效距离减小;依据该有效距离处的等效应变进行疲劳寿命预测,总体预测结果较为分散且偏于不安全。基于实验及有限元模拟结果,提出了基于应变梯度的有效距离确定的新方法,大部分疲劳寿命预测结果位于2倍分散带内。     

基于可变滑动窗口与3σ准则的脉冲星信号去噪算法

针对地面接收射电观测脉冲星信号较弱、信噪比较低的问题,提出了基于可变滑动窗口与两层3σ准则的信号去噪算法。该算法引入可变滑动窗口,对信号进行分步连续处理,同时在筛选噪声时使用两层3σ准则算法,解决了噪声遗漏及过度去噪问题。为证明算法可靠性与实用性,利用佳木斯66 m观测站实测数据进行算法验证,针对J1939+2134与J1744—1134脉冲星的实测数据进行分析处理。结果表明,该算法能够对脉冲星数据进行有效去噪,普遍提高信噪比约10dB。     

FCD1软脆光学镜片的高效研磨加工

针对FCD1软脆光学镜片高效高成品率的精密加工问题,本研究提出了一种使用复合结合剂金刚石丸片的精研加工技术,其金刚石丸片研具采用了金属、树脂和添加剂等复合结合剂。在精研过程中,丸片表层金刚石磨粒对工件的切深一致性避免了工件表面易出现的深划痕,可有效减少后道抛光工序加工时间,从而提高FCD1软脆光学镜片的生产效率和成品率。     

硅氮烷环体的催化聚合及热解制备Si3 N4 材料

采用甲基氢二氯硅烷的氨解产物硅氮烷环体(MHSZ)为原料,以四丁基氟化铵为催化剂,制备了高分子量的硅氮烷聚合物(PHSZ),结合红外、核磁、凝胶色谱仪和热重分析了反应时间对合成的PHSZ结构、组成、分子量和陶瓷产率的影响。考察了低温氨气,高温N2气氛处理工艺对热解产物结构和组成的影响。结果表明,随着反应时间的延长,PHSZ高聚物的分子量提高,热失重降低;采用该热解方式PHSZ可转化为含碳量仅为0.5wt%的Si3N4材料,热解样品在1 600℃时完全结晶,晶相主要是α-Si3N4。     

双脉冲发动机点火过程三维数值模拟

以喷射棒式双脉冲发动机燃烧室、级间隔离装置和喷管一体化为研究对象,采用数值仿真技术对Ⅱ脉冲点火过程三维流场特性进行分析研究。计算结果表明,点火初期燃气压力波峰超前于火焰峰到达级间隔离装置,并以压强冲击波形式传播,Ⅱ脉冲燃烧室相对高压区位置不断发生改变;级间孔打开过程对药柱末端压强影响较大,但对Ⅱ脉冲燃烧室压强整体上升过程影响较小;级间孔打开后,燃气经级间孔加速后形成高度欠膨胀射流,并在Ⅰ脉冲燃烧室内形成非对称带状低压区;级间孔分布的非对称性,导致压强及温度在发动机燃烧室中呈现显著的三维分布特性;高温区出现在隔板附近,而在装药前端、装药末端及外围级间孔轴线附近出现低温区。     

Initial nighttime ionospheric observations with advanced ionospheric probe onboard FORMOSAT-5

FORMOSAT-5 satellite was launched into a sun-synchronous orbit at 720 km altitude with 98.28° inclination on 25 August 2017. The onboard scientific payload, Advanced Ionospheric Probe (AIP) is capable of measuring topside ionospheric ion density, cross-track flow velocities, ion composition and temperature, and electron temperature. Initial observations of nighttime midlatitude ionospheric density and vertical flow velocity variations at 2230 LT sector during a few quiet magnetic days in December 2017 are studied here. Longitudinal density variations in the equatorward edge of midlatitude ionospheric trough (MIT) region are noticed. Accompanied with this density variation, the vertical flow velocities also behave differently. Although the density difference has been stated due to zonal wind effect related to the declination of the geomagnetic field lines, the vertical flow velocity variation seems to play the opposite role. All these density and vertical flow observations in the northern winter hemisphere can only be explained by the longitudinal differences in the diffusion velocity coming down from the protonsphere (plasmasphere). In addition, the hemispheric asymmetry in the vertical flow velocity can also be explained by the interaction between the topside ionosphere and the protonsphere. The observed vertical flow variations near MIT at different longitudes should present a new potential tool for the study of MIT formation.     

Global ionospheric scintillations revealed by GPS radio occultation data with FY3C satellite before midnight during the March 2015 storm

Global observations of S4 amplitude scintillation index by the GPS Occultation Sounder (GNOS) on FengYun-3 C (FY3C) satellite reveal global dynamic patterns of a strong pre-midnight scintillations in F-region of the ionosphere during the St. Patrick’s Day geomagnetic super storm of 17–19 March 2015. The observed strong scintillations mainly occurred in the low latitudes, caused by equatorial plasma bubbles. During the main storm phase (March 17), the scintillations were first triggered in the New Zealand sector near 160°E longitudes, extending beyond 40°S dip latitude. They were also enhanced in the Indian sector, but significantly suppressed in East Asia near 120°E longitude and in Africa around 30°E longitude. During the initial recovery phase (March 18–19), the global scintillations were seldom observed in GNOS data. During the later recovery phase (after March 19), the scintillations recovered to the pre-storm level in Indian, African, and American sectors, but not in East Asian and any of Pacific sectors. These results closely correlate with observations of the density depletion structures by the Communication/Navigation Outage Forecasting System (C/NOFS) satellite, and ground-based instruments. Such consistency indicates reliability of our scintillation sensing approach even in a case-by-case comparison study. The prompt penetration electric field and disturbance dynamo electric field are suggested as the main factors that control the enhancement and inhibition of the scintillations during the storm, respectively.