月尘环境效应及地面模拟技术

介绍了月球尘的特点及其对探月活动的影响。在分析月球尘环境及其对月面探测器污染、磨损、阻塞、静电效应的基础上,对月球尘环境模拟技术、月球尘扬尘及其运动学和动力学规律、月球尘效应防护及试验评价方法等研究方向和重点提出了一些初步看法。针对研究内容的需求,梳理出一台完整的月球尘地面模拟试验设备应具备真空、温度、太阳风、太阳紫外、月球尘、月面电场、月面磁场等环境因素。在此基础上,设计了一种月球尘地面模拟试验装置方案,并对月球尘环境效应试验方法进行了初步讨论。为月球探测后期任务条件保障建设及相关研究工作提供参考。     

发动机羽流作用下的实时月尘运动仿真

月尘运动是月球探测器软着陆过程中不可或缺的重要环节,针对发动机羽流作用下月尘运动真实感不强和月尘颗粒运动模型过于简单的问题,提出了一种逼真的实时月尘运动仿真方法.通过计算流体动力学(CFD, Computational Fluid Dynamics)和二次谢别德插值(Quadratic Shepard)方法,分析和计算单个月尘颗粒的运动学模型,得到一定初始条件下粒子运动的二维轨迹曲线;通过分析粒子的数量、初始位置、初始速度、生命周期等参数对粒子运动学的影响和变化规律,抽象出月尘系统的粒子集;建立基于月尘粒子集的月尘运动模型.实验结果显示:该运动模型逼真的模拟了发动机羽流作用下月尘腾起、飞溅、弥漫、消散等运动过程,视觉真实感和实时性能良好,对研究真空环境中的月尘运动及月球软着陆等相关领域具有一定的参考意义.目前该方法已应用于北航虚拟现实国家重点实验室月球软着陆仿真系统.     

Mars Phobos and Deimos Survey (M-PADS) – A martian Moons orbiter and Phobos lander

We describe a Mars ‘Micro Mission’ for detailed study of the martian satellites Phobos and Deimos. The mission involves two ∼330 kg spacecraft equipped with solar electric propulsion to reach Mars orbit. The two spacecraft are stacked for launch: an orbiter for remote investigation of the moons and in situ studies of their environment in Mars orbit, and another carrying a lander for in situ measurements on the surface of Phobos (or alternatively Deimos). Phobos and Deimos remain only partially studied, and Deimos less well than Phobos. Mars has almost always been the primary mission objective, while the more dedicated Phobos project (1988–89) failed to realise its full potential. Many questions remain concerning the moons’ origins, evolution, physical nature and composition. Current missions, such as Mars Express, are extending our knowledge of Phobos in some areas but largely neglect Deimos. The objectives of M-PADS focus on: origins and evolution, interactions with Mars, volatiles and interiors, surface features, and differences. The consequent measurement requirements imply both landed and remote sensing payloads. M-PADS is expected to accommodate a 60 kg orbital payload and a 16 kg lander payload. M-PADS resulted from a BNSC-funded study carried out in 2003 to define candidate Mars Micro Mission concepts for ESA’s Aurora programme.     

Report on the Kiso cometary dust trail survey

Cometary dust trails were first observed by IRAS; they are widely known to be the origins of meteoric showers. A new window has been opened for the study of dust trails, using ground-based observations. We succeeded in obtaining direct images of the 22P/Kopff dust trail with the Kiso 1.05-m Schmidt telescope. Following this initial success, we have continued to perform a dust trail survey at Kiso. As a result of this survey, we have detected dust trails along the orbit of six periodic comets, between February 2002 and March 2004. The optical depth of these dust trails are 10⁻⁹ to 10⁻⁸, which is consistent with IRAS measurements. In this paper, we describe the observations and data reduction procedures, and report the brief result obtained between February 2002 and March 2004.     

防风网对煤堆遮风效果的风洞实验研究

为了考察防风网对堆场煤堆的遮风效果,进行了防风网与煤堆之间区域的流场可视化实验。使用风洞模拟大气边界层条件,并将开孔率为38.5%的防风网模型布置在煤堆模型前方。实验中采用粒子成像测速(PIV)系统测量了防风网和堆场区域的平均风速分布,并且获得了煤堆表面的摩擦风速分布,进一步估算煤堆起尘量的变化情况。实验发现,防风网可有效降低煤堆表面迎风区域的摩擦风速,而对背风面的流场分布影响较小。研究结果可为防风网的遮护作用提供一定的实验支持。     

Multimodal characteristics of a piezoelectric lead zirconate titanate element impacted with iron particles having velocities above 20 km/s

The responses of a piezoelectric lead zirconate titanate (PZT) element to hypervelocity collisions were experimentally studied. In this study, the particles of masses ranging from 0.3 to 10 fg were made to collide with PZT at velocities between 20 and 96 km/s. The amplitude and the corresponding rise time of the single-pulse output signals that were produced in the piezoelectric PZT element were measured to determine the possible collision states. The results revealed an apparently multimodal output; three classes were assumed to be involved in the pulse formation mechanism. The amplitude and rise time were sensitive to the collision velocity. The multimodal behavior implied that the PZT-based cosmic dust detectors should be calibrated according to the class they belong to.     

计算模拟月壤颗粒吸收及散射特性的一种球叠加模型

针对模拟月壤复杂的外形特征以及多相非均质的微观结构,提出了一种计算模拟月壤颗粒吸收及散射特性的球叠加模型。根据模拟月壤颗粒的形状指数和分形特征识别结果,归纳了4种主要的模拟月壤颗粒类型,并采用蒙特卡罗光线跟踪法研究了这4种颗粒在单色平行光照射下的吸收及散射特性。与已有的非球形颗粒辐射特性的算法比较显示,该模型具有良好的计算准确性。在数值计算的基础上,分析了颗粒尺度参数及光学常数对其自身辐射特性的影响,并通过改变平行光照下的光线入射角度,分析了非球形颗粒的朝向对其自身辐射特性的影响。由计算结果推断,该模型不仅可以应用于计算模拟月壤颗粒的辐射特性,还可以满足其他适用于几何光学近似的非球形粒子。     

“嫦娥三号”探测器月尘环境分析及试验要求

"嫦娥三号"是我国首个成功实施地外天体表面就位探测的航天器,在其研制过程中充分考虑了月面环境对探测器的影响,开展了针对性设计及地面验证工作。文章综述了探测器针对月尘环境方面的设计因素,总结了月面月尘激扬的因素及其相关数值分析工作,对月尘验证试验的设计及条件制定进行了说明。相关结果或工作思路可为后续月面探测器及火星表面探测器的研制提供参考。     

太阳矢量在行星际探测器姿态估计中的应用研究

在基于矢量观测的行星际探测器姿态确定中,参考矢量的几何关系是影响姿态估计精度的一个重要因素。针对这一问题,本文提出了一种利用太阳矢量来提高探测器姿态估计精度的最优算法。该方法在引入太阳矢量的基础上,将星敏感器测得的姿态四元数转化为两个互相垂直的参考矢量,并根据敏感器的测量精度计算相应的规范化权值系数;结合姿态四元数估计算法,给出最小二乘意义下的探测器最优姿态估计。最后,以深度撞击任务的实际飞行数据对本文所提算法进行验证。仿真结果表明,引入太阳矢量后的三轴姿态角估计误差小于150μrad,完全满足深度撞击任务的要求。     

月尘对热控系统的退化影响

月尘对热控系统的退化影响直接威胁到探测器在月面的生存,是探测器热控系统设计时所必须考虑的技术重点和难点之一。随着我国探月工程的深入,急需开展月尘对热控系统影响程度的研究,文章在调研的基础上,阐述了目前国内外在月尘的特性、危害性和防护方面的研究现状,并探讨了针对月面探测器设计上的一些可行的防尘措施。