考虑失效性故障的火星探测器进入段姿态容错控制

火星进入过程中的故障和外部干扰不可避免地降低了火星进入制导和控制算法的性能。利用反步法设计了一种对转动惯量信息变化不敏感的火星进入姿态容错控制算法。首先,将虚拟控制律的微分量视作干扰量,利用自适应技术对其进行补偿,避免了传统反步法微分爆炸的缺陷。同时,控制设计过程中显式地引入了饱和函数,保证了在存在输入饱和的情况下,控制律仍然能使得探测器姿态保持稳定。最后,以“火星科学实验室”探测器为模型进行了数值仿真验证,结果表明该控制律在存在输入饱和约束、转动惯量不确定性、执行机构部分失效甚至完全失效的工况下,仍然能够完成对姿态的精准跟踪。     

Planetary protection issues related to human missions to Mars

In accordance with the United Nations Outer Space Treaties [United Nations, Agreement Governing the Activities of States on the Moon and Other Celestial Bodies, UN doc A/RES/34/68, resolution 38/68 of December 1979], currently maintained and promulgated by the Committee on Space Research [COSPAR Planetary Protection Panel, Planetary Protection Policy accepted by the COSPAR Council and Bureau, 20 October 2002, amended 24 March 2005, http://www.cosparhq.org/scistr/PPPolicy.htm], missions exploring the Solar system must meet planetary protection requirements. Planetary protection aims to protect celestial bodies from terrestrial contamination and to protect the Earth environment from potential biological contamination carried by returned samples or space systems that have been in contact with an extraterrestrial environment. From an exobiology perspective, Mars is one of the major targets, and several missions are currently in operation, in transit, or scheduled for its exploration. Some of them include payloads dedicated to the detection of life or traces of life. The next step, over the coming years, will be to return samples from Mars to Earth, with a view to increasing our knowledge in preparation for the first manned mission that is likely to take place within the next few decades. Robotic missions to Mars shall meet planetary protection specifications, currently well documented, and planetary protection programs are implemented in a very reliable manner given that experience in the field spans some 40 years. With regards to sample return missions, a set of stringent requirements has been approved by COSPAR [COSPAR Planetary Protection Panel, Planetary Protection Policy accepted by the COSPAR Council and Bureau, 20 October 2002, amended 24 March 2005, http://www.cosparhq.org/scistr/PPPolicy.htm], and technical challenges must now be overcome in order to preserve the Earth’s biosphere from any eventual contamination risk. In addition to the human dimension of the mission, sending astronauts to Mars will entail meeting all these constraints. Astronauts present huge sources of contamination for Mars and are also potential carriers of biohazardous material on their return to Earth. If they were to have the misfortune of being contaminated, they themselves would become a biohazard, and, as a consequence, in addition to the technical constraints, human and ethical considerations must also be taken into account.     

Survival and death of the haloarchaeon Natronorubrum strain HG-1 in a simulated martian environment

Halophilic archaea are of interest to astrobiology due to their survival capabilities in desiccated and high salt environments. The detection of remnants of salty pools on Mars stimulated investigations into the response of haloarchaea to martian conditions. Natronorubrum sp. strain HG-1 is an extremely halophilic archaeon with unusual metabolic pathways, growing on acetate and stimulated by tetrathionate. We exposed Natronorubrum strain HG-1 to ultraviolet (UV) radiation, similar to levels currently prevalent on Mars. In addition, the effects of low temperature (4, −20, and −80 °C), desiccation, and exposure to a Mars soil analogue from the Atacama desert on the viability of Natronorubrum strain HG-1 cultures were investigated. The results show that Natronorubrum strain HG-1 cannot survive for more than several hours when exposed to UV radiation equivalent to that at the martian equator. Even when protected from UV radiation, viability is impaired by a combination of desiccation and low temperature. Desiccating Natronorubrum strain HG-1 cells when mixed with a Mars soil analogue impaired growth of the culture to below the detection limit. Overall, we conclude that Natronorubrum strain HG-1 cannot survive the environment currently present on Mars. Since other halophilic microorganisms were reported to survive simulated martian conditions, our results imply that survival capabilities are not necessarily shared between phylogenetically related species.     

火星磁层顶形成和变化的理论研究

考虑太阳风动压与行星电离层中的带电粒子热压及磁压之和平衡,建立了有大气（电离层）的行星磁层顶形成的理论模型,结合卫星对火星的观测数据,对子午面内向日侧火星磁层顶位形进行了数值计算和分析,研究了火星磁层顶位形及其与太阳风动压之间的变化关系．结果认为,火星磁层顶位形与地球磁层顶相似．太阳风动压越大,火星磁层顶越靠近火星;太阳风动压越弱,火星磁层顶越远离火星．根据火星内秉磁矩从古到今逐渐减小的观点,探索了大尺度磁场（内禀磁矩）对火星磁层顶的贡献作用,结果认为大尺度磁场越强,火星磁层顶越远离行星．这对于进一步研究火星磁层的长期演化以及其他行星磁层的位形变化都具有重要的意义．     

火星探测着陆系统开伞控制方法研究

文章通过对火星探测进入轨道的分析，提出了一种以动压为控制目标的开伞控制方法，并借鉴过载-时间控制法的相关思想，结合火星探测进入轨道的特点，研究了该开伞控制法的原理和实现方法。根据火星探路者的实际进入条件，采用该方法的分析结果与实际飞行中的开伞情况基本吻合。     

行星着陆探测中的动力学与控制研究进展

着陆探测是获取行星特性和科学数据最直接、最有效的途径,也是目前技术难度最大、最为复杂的探测方式。在行星着陆探测过程中,动力学与控制是影响任务成败的关键因素之一。文章首先分析了行星着陆探测动力学与控制研究所面临的挑战与难题;然后,针对火星和小行星的着陆探测,重点分析了火星着陆进入段和下降段所涉及的动力学与控制,小行星附着探测动力学建模与制导控制的研究现状与关键问题;最后,提出了我国在行星着陆探测动力学与控制领域的未来重点发展方向。     

论航天火星探测

回顾了 2 0世纪航天火星探测的历史和成就 ,论述了火星探测器飞行轨道的特点 ,展望了 2 1世纪初期航天火星探测的前景     

火星车低气压无风热环境模拟试验技术

为模拟火星车工作时所处大温差、低气压环境,文章以自主研制的调温热沉系统和压力控制系统为依托,实现试验容器热沉系统温度在-135~27℃间任意快速调节,均匀性优于±5℃;试验容器内气体压力控制值与目标压力值之差在±10 Pa之内。在国内首次完成无风环境下的火星车温控模拟舱验证试验,为火星车热分析模型修正以及后续火星车有风热环境试验提供了参考。     

火星轨道交会自主导航与制导方法

对火星采样返回任务中的火星轨道交会自主导航和制导技术进行了研究。采用光学自主导航敏感器测量的火星中心方向和视半径,相对敏感器测量的相对位置等观测量,设计了导航滤波器同时估计轨返组合体和上升器的轨道。在导航滤波器设计中,针对光学自主导航敏感器更新频率远低于滤波解算频率的问题,设计了一种连续观测量构造算法,确保每个滤波周期均可进行测量更新,以提高导航精度。基于导航滤波器估计结果,采用T-H制导设计了4脉冲共椭圆交会策略实施轨道控制,从而构成近程交会自主导航和制导方案用于完成火星轨道交会任务。通过数学仿真校验了所提出方法的有效性。     

磁阻尼对火星探测器降落过程的动力学效应

火星稀薄的大气使得探测器再入火星时难以获得足够的减速阻力,为此,文章提出利用磁阻尼增加阻力的概念。高速再入的探测器与火星大气剧烈摩擦产生等离子体,利用探测器上的磁偶极场将等离子体捕获,同时在火星大气中形成一个“磁泡”区域并跟随探测器。由“磁泡”束缚的等离子体与来流的中性气体发生碰撞获得动量,又通过磁场作用将动量传递给探测器,从而使探测器获得一定的减速阻力。在磁阻尼的作用下,在同样的开伞高度探测器速度可降至更低,而低速开伞又可提高阻力伞打开的可靠性。因此,磁阻尼不仅可加快降低再入速度,而且还有助于提高探测器着陆火星的安全性。