共查询到18条相似文献,搜索用时 156 毫秒
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《固体火箭技术》2021,44(2)
对目前在研究的Al/AP、金属粉末/空气、金属粉末/CO_2、金属粉末/H_2O等推进剂体系的多种粉末发动机发展现状进行了综述,表明粉末发动机可分为粉末火箭发动机、粉末冲压发动机、粉末爆震发动机三大类,不同推进剂体系的粉末发动机应用方向差异较大:Al/AP推进剂火箭发动机是最典型的粉末发动机,应用领域和常规火箭发动机的相同,其技术成熟度相对较高;金属粉末/空气冲压发动机主要用于超音速导弹或高超音速导弹推进领域;金属粉末/CO_2推进剂体系主要应用于火星开发;金属粉末/H_2O推进剂体系可用于水下推进、空间推进、金属制氢等领域,应用前景广阔,是目前的研究热点。各种粉末发动机都涉及三项关键技术,即粉末推进剂配方技术、粉末推进剂输送及流量调节技术、粉末燃料燃烧组织技术,文中提出了这些技术的基本要求,同时认为粉末推进剂输送及流量调节技术是粉末发动机的技术瓶颈。 相似文献
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美国“火星大气与挥发演化”(MAVEN)探测器于2014年9月22日进入火星轨道,开始了其为期1年的科学探测任务。MAVEN的主要使命是调查火星大气失踪之谜,并寻找火星上早期拥有的水源及二氧化碳消失的原因。为完成使命,MAVEN的研制者在充分继承之前火星探测器的研制经验基础上,为其精心打造了各项独具功能的探测设备。 相似文献
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针对火星飞行器探测需求,提出了一种共轴双旋翼式火星飞行器,基于计算流体力学方法优选了桨叶翼型、平面形状和扭转角等结构参数,基于叶素动量理论建立了旋翼气动力学模型,利用数值模拟方法选择了旋翼转速、旋翼间距和桨叶安装角等飞行参数,设计了原理样机"火星飞鸟-I"的结构与控制系统。构建了火星大气环境模拟器和重力补偿与运动约束装置,开展了模拟火星环境下旋翼式飞行器地面飞行试验,验证了共轴双旋翼式火星飞行器的推进性能,展望了旋翼式火星飞行器技术的发展方向。研究成果对我国开展的火星探测工程具有重要借鉴价值。 相似文献
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核反应堆空间应用研究 总被引:3,自引:0,他引:3
对美国、俄罗斯等国家的核反应堆空间应用进行了研究。其中包括:美国最早研究的SNAP-8系列,可提供多种组合输出的SP-100布雷顿能量系统,应用于火星表面的核反应堆MSR系统等;俄罗斯和日本在月球表面或火星表面应用的核反应堆。重点对空间核反应堆的堆型、堆芯冷却方式、热电转换方式、废热排放方式、辐射屏蔽模式等进行比对分析。结合月球基地能源系统的应用背景,对实现核反应堆空间应用需要解决的关键技术进行了分析,如发射安全技术、无人自主管理技术、空间低重力环境适应性及辐射防护技术等,可为我国未来空间探测任务的能源系统研究提供借鉴和参考。 相似文献
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We compare a variety of mission scenarios to assess the strengths and weaknesses of options for Mars exploration. The mission design space is modeled along two dimensions: trajectory architectures and propulsion system technologies. We examine direct, semi-direct, stop-over, semi-cycler, and cycler architectures, and we include electric propulsion, nuclear thermal rockets, methane and oxygen production on Mars, Mars water excavation, aerocapture, and reusable propulsion systems in our technology assessment. The mission sensitivity to crew size, vehicle masses, and crew travel time is also examined. Many different combinations of technologies and architectures are applied to the same Mars mission to determine which combinations provide the greatest potential reduction in the injected mass to LEO. We approximate the technology readiness level of a mission to rank development risk, but omit development cost and time calculations in our assessment. It is found that Earth–Mars semi-cyclers and cyclers require the least injected mass to LEO of any architecture and that the discovery of accessible water on Mars has the most dramatic effect on the evolution of Mars exploration. 相似文献
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A revolutionary new concept for the early establishment of robust, self-sustaining Martian colonies is described. The colonies would be located on the North Polar Cap of Mars and utilize readily available water ice and the CO2 Martian atmosphere as raw materials to produce all of the propellants, fuel, air, water, plastics, food, and other supplies needed by the colony. The colonists would live in thermally insulated large, comfortable habitats under the ice surface, fully shielded from cosmic rays. The habitats and supplies would be produced by a compact, lightweight (~4 metric tons) nuclear powered robotic unit termed ALPH (Atomic Liberation of Propellant and Habitat), which would land 2 years before the colonists arrived. Using a compact, lightweight 5 MW (th) nuclear reactor/steam turbine (1 MW(e)) power source and small process units (e.g., H2O electrolyzer, H2 and O2 liquefiers, methanator, plastic polymerizer, food producer, etc.) ALPH would stockpile many hundreds of tons of supplies in melt cavities under the ice, plus insulated habitats, to be in place and ready for use when the colonists landed. With the stockpiled supplies, the colonists would construct and operate rovers and flyers to explore the surface of Mars. ALPH greatly reduces the amount of Earth supplied material needed and enables large permanent colonies on Mars. It also greatly reduces human and mission risks and vastly increases the capability not only for exploration of the surrounding Martian surface, but also the ice cap itself. The North Polar Cap is at the center of the vast ancient ocean that covered much of the Martian Northern Hemisphere. Small, nuclear heated robotic probes would travel deep (1 km or more) inside the ice cap, collecting data on its internal structure, the composition and properties of the ancient Martian atmosphere, and possible evidence of ancient life forms (microfossils, traces of DNA, etc.) that were deposited either by wind or as remnants of the ancient ocean. Details of the ALPH system, which is based on existing technology, are presented. ALPH units could be developed and demonstrated on Earth ice sheets within a few years. An Earth-Mars space transport architecture is described, in which Mars produced propellant and supplies for return journeys to Earth would be lifted with relatively low DeltaV to Mars orbit, and from there transported back to Earth orbit, enabling faster and lower cost trips from Earth to Mars. The exploration capability and quality of life in a mature Martian colony of 500 persons located on the North Polar Cap is outlined. 相似文献
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The considerable evidence that Mars once had a wetter, more clement, environment motivates the search for past or present life on that planet. This evidence also suggests the possibility of restoring habitable conditions on Mars. While the total amounts of the key molecules--carbon dioxide, water, and nitrogen--needed for creating a biosphere on Mars are unknown, estimates suggest that there may be enough in the subsurface. Super greenhouse gases, in particular, perfluorocarbons, are currently the most effective and practical way to warm Mars and thicken its atmosphere so that liquid water is stable on the surface. This process could take approximately 100 years. If enough carbon dioxide is frozen in the South Polar Cap and absorbed in the regolith, the resulting thick and warm carbon dioxide atmosphere could support many types of microorganisms, plants, and invertebrates. If a planet-wide martian biosphere converted carbon dioxide into oxygen with an average efficiency equal to that for Earth's biosphere, it would take > 100,000 years to create Earth-like oxygen levels. Ethical issues associated with bringing life to Mars center on the possibility of indigenous martian life and the relative value of a planet with or without a global biosphere. 相似文献