行星着陆复杂形貌特征匹配与自主导航研究进展

基于行星定点软着陆探测任务的需求,围绕复杂形貌行星着陆过程环境特点,首先分析了行星着陆复杂形貌特征匹配与自主导航所面临的主要技术挑战,随后综述了行星着陆复杂形貌特征匹配与自主导航的研究现状,并概括了行星着陆复杂形貌特征匹配与自主导航所涉及的关键技术。最后对未来行星着陆探测复杂形貌特征匹配与自主导航发展方向进行了展望。     

激光宏观结构化金刚石砂轮磨削氧化铝工艺

为了研究砂轮表面结构化对砂轮磨削性能的影响,利用脉冲激光对树脂结合剂金刚石砂轮进行了表面宏观结构化。采用6种不同类型的金刚石砂轮表面宏观结构进行了氧化铝的磨削实验,建立了激光宏观结构化金刚石砂轮的磨削力模型,比较了6种不同激光宏观结构化金刚石砂轮与非结构化砂轮在不同磨削参数下磨削力的差异,分析了砂轮制造后的表面形貌与结构化砂轮的磨损特性。实验结果表明,砂轮宏观结构化对磨削性能有很大影响,激光宏观结构化砂轮的磨削力可以减小2. 5%~24. 5%,砂轮结构化后的表面形貌出现石墨化现象;宏观结构化砂轮沟槽边缘磨损加剧,但沟槽磨损并没有明显加快宏观结构化砂轮的磨损。     

适用于月面高温环境的嫦娥三号地形地貌相机热设计

“嫦娥三号暠月面探测器上安装的地形地貌相机工作时直接暴露在月面高温环境下,受月表红外辐射影响很大,给热控设计带来很大难题。为解决设备工作时的高温问题,在外热流分析的基础上提出了以“最佳散热位置暠为核心的热控方案,设备处于“最佳散热位置暠时能够获得较好的初始温度和最快的降温速率;另外通过把散热面布置在月表红外辐射热流最小的位置并在除散热面以外的其他表面包覆多层隔热组件这两个措施,可以最大程度减小月表红外辐射的影响。地形地貌相机在轨开机工作前的各飞行阶段遥测数据均满足存储温度指标要求并且有较大余量;开机工作环拍一周的遥测数据满足工作温度指标要求并且与热分析结果符合较好,初始温度与遥测温度数据偏差为-1灡7曟,温升速率和降温速率偏差分别为14灡9%和16灡9%。这表明该热控方案正确可行,可为后续中国深空探测类似热控问题参考。     

地形对低平流层突然增温的可能影响

本文用Nimbus7 SAM卫星观测的温度资料,分析了突然增温事例中地面地形不同的四个子午圈剖面内的温度分布及变化过程。结果表明,高山地区、平原和海面上空的行星波加热和低平流层突然增温有很大的差别。地形的影响是明显的。      

一种新的卫星光学立体测量技术

提出了一种新的立体影像解析方法。在卫星轨道特性和相机交会角已知的条件下,根据对同一地物的摄影时间差提取高度信息,进而确定其三维空间位置。建立了不考虑/考虑地球自转的地物高度测定,以及位置确定模型,给出了地物空间位置计算的流程。讨论了地物高度的测量误差和对卫星平台性能的基本要求。新方法用摄影时间差的测量取代传统方法影像像点坐标的测量,更简捷和准确,更适合数字图像,具有重要应用价值。     

北京地区重力波活动及其波谱的季节分布特性研究

利用激光雷达对北京地区上空Na层进行持续观测,通过连续三年累积的夜间观测数据对北京地区重力波活动及其波谱进行研究.根据重力波的线性理论计算,得到北京地区上空的大气密度扰动规律、空间功率谱和时间频率谱.通过选择重力波波长在1~8 km,具有特定波长以及特定周期为60,45,25 min的重力波活动辅助研究重力波的季节变化规律,结果表明北京地区重力波大气密度扰动具有夏季大、冬季小的活动规律.结合波源与背景风场的季节性变化规律,分析得出北京上空重力波活动季节性变化的主要原因为青藏高原地形和对流因素与我国北方地区季节性背景风场共同作用的结果.     

The Mercury Laser Altimeter Instrument for the MESSENGER Mission

The Mercury Laser Altimeter (MLA) is one of the payload science instruments on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) mission, which launched on August 3, 2004. The altimeter will measure the round-trip time of flight of transmitted laser pulses reflected from the surface of the planet that, in combination with the spacecraft orbit position and pointing data, gives a high-precision measurement of surface topography referenced to Mercury’s center of mass. MLA will sample the planet’s surface to within a 1-m range error when the line-of-sight range to Mercury is less than 1,200 km under spacecraft nadir pointing or the slant range is less than 800 km. The altimeter measurements will be used to determine the planet’s forced physical librations by tracking the motion of large-scale topographic features as a function of time. MLA’s laser pulse energy monitor and the echo pulse energy estimate will provide an active measurement of the surface reflectivity at 1,064 nm. This paper describes the instrument design, prelaunch testing, calibration, and results of postlaunch testing.     

Hybrid method for crater detection based on topography reconstruction from optical images and the new LU78287GT catalogue of Lunar impact craters

Impact craters are ubiquitous and well-studied structures of high geological relevance on the surfaces of the Earth’s Moon, the terrestrial planets, the asteroids and the satellites of the outer planets. Therefore, it is not surprising that crater detection algorithms (CDAs) are one of the most studied subjects of image processing and analysis in lunar and planetary science. In this paper we are proposing a Hybrid CDA: a modified DEM (digital elevation map) reconstruction method used as a step in an existing CDA based on Hough transform. The new Hybrid CDA consists of: (1) reconstruction of topography from optical images using a shape from shading approach; (2) utilization of the DEM-based CDA; (3) correction of brightness and contrast of optical images used in order to be more suitable for evaluation of detections. An additional result of this work is a new method for evaluation of topography reconstruction algorithms, using a DEM-based CDA and an earlier approach for evaluation of CDAs. The new Hybrid CDA was tested using two Chandrayaan-1 Moon Mineralogy Mapper (M³) images and two excerpts of the Lunar Reconnaissance Orbiter (LRO) Wide Angle Camera (WAC) global optical image mosaic. As a result, the number of craters inside these four regions increased considerably from 1754 (as available in the previous LU60645GT catalogue) to 19 396 craters (as available in the resulting new LU78287GT catalogue). This confirmed the practical applicability of the new Hybrid CDA, which can be used in order to considerably extend current crater catalogues.