共查询到17条相似文献,搜索用时 93 毫秒
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分析了太阳系探测的发展趋势,认为从月球到火星是未来太阳系探测的主线,太阳系探测将从普查性探测向重点天体探测转变,从技术实现为主向科学牵引转变,国际合作成为太阳系探测的必然趋势。归纳了太阳系探测的关键科学问题,认为太阳系与行星系统的起源和演化是探测的终极科学目标,寻找地外生命和宜居环境是探测的主要驱动力,预防太阳活动和小天体撞击对地球的灾害性影响是探测的现实意义。在探月工程取得进展之后,中国应以月球和火星探测为主线,以火星探测为切入点,有序开展火星、小行星、太阳、金星、木星系统等太阳系探测任务,牵引航天技术进步,推动行星科学发展。 相似文献
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3.2 载人火星探测□□就人类的空间探测而言 ,2 0世纪的壮举是美国的“阿波罗”登月计划 ,2 1世纪则将是载人火星探测。但要实现载人火星探测 ,首先要解决两个问题 :其一是目的和意义 ;其二是技术途径。3.2 .1 载人火星探测的目的和意义载人航天的目的和意义不外乎是对政治、军事、经济和科学技术的影响 ,但载人火星探测的目的和意义主要是其科学价值 ,即探明火星上有没有生命。在太阳系的九大行星中 ,除地球以外火星是最可能存在生命的行星。火星有厚的地壳 ,弱的磁场 ,还有稀薄的大气 ,其大气压相当于地球的 1%。火星表面温度极低 ,平均… 相似文献
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总结了近20年来火星探测的重要发现以及生命、气候和地质3个方面尚未解决的关键科学问题;介绍了美国国家航空航天局(NASA)2020火星探测任务的科学目标、科学载荷和着陆区选择的工程条件限制,并重点分析了经过3次着陆区选择研讨会,上百位行星科学家投票选取的排名前3的预选着陆区的地质情况。在此基础上,提出了对我国2020年火星任务的着陆探测部分的一些思考,并根据不同的任务目标(聚焦生命、气候和地质问题;支持载人火星探测的资源勘察;工程技术验证)提出了3个候选着陆区。 相似文献
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行星保护是每一个开展深空探测的国家都要面对的问题,火星是太阳系里最可能存在地外生命的星球之一,也是行星保护的重点关注对象,在我国火星探测即将正式启动之际,对标国际上行星保护的政策、标准、技术和管理措施,对我国未来在火星探测中满足国际上行星保护的要求至关重要。主要回顾了行星保护的历史,国外在火星探测历史上行星保护正向防护所采取的措施,以及现代科学技术发展对行星保护正向防护相关技术的影响,并对我国未来火星及深空探测活动中应该采取的行星保护正向污染防护技术提出了建议。 相似文献
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Alberto G. Fairén Dirk Schulze-Makuch Lyle Whyte Victor Parro Alexander Pavlov Javier Gómez-Elvira Armando Azua-Bustos Wolfgang Fink Victor Baker 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2019,63(5):1491-1497
Future efforts towards Mars exploration should include a discussion about the effects that the strict application of Planetary Protection policies is having on the astrobiological exploration of Mars, which is resulting in a continued delay in the search for Martian life. As proactive steps in the path forward, here we propose advances in three areas. First, we suggest that a redefinition of Planetary Protection and Special Regions is required for the case of Mars. Particularly, we propose a definition for special places on Mars that we can get to in the next 10–20?years with rovers and landers, where try to address questions regarding whether there is present-day near-surface life on Mars or not, and crucially doing so before the arrival of manned missions. We propose to call those special places “Astrobiology Priority Exploration” regions (APEX regions). Second, we stress the need for the development of robotic tools for the characterization of complex organic compounds as unequivocal signs of life, and particularly new generations of complex organic chemistry and biosignature detection instruments, including advances in DNA sequencing. And third, we advocate for a change from the present generation of SUV-sized landers and rovers to new robotic assets that are much easier to decontaminate such as microlanders: they would be very small with limited sensing capabilities, but there would be many of them available for launch and coordination from an orbiting platform. Implementing these changes will help to move forward with an exploration approach that is much less risky to the potential Mars biosphere, while also being much more scientifically rigorous about the exploration of the “life on Mars” question – a question that needs to be answered both for astrobiological discovery and for learning more definitive lessons on Planetary Protection. 相似文献
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H P Klein D L DeVincenzi 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》1995,15(3):151-156
Of all the other planets in the solar system, Mars remains the most promising for further elucidating concepts about chemical evolution and the origin of life. Strategies were developed to pursue three exobiological objectives for Mars exploration: determining the abundance and distribution of the biogenic elements and organic compounds, detecting evidence of an ancient biota on Mars, and determining whether indigenous organisms exist anywhere on the planet. The three strategies are quite similar and, in fact, share the same sequence of phases. In the first phase, each requires global reconnaissance and remote sensing by orbiters to select sites of interest for detailed in situ analyses. In the second phase, lander missions are conducted to characterize the chemical and physical properties of the selected sites. The third phase involves conducting "critical" experiments at sites whose properties make them particularly attractive for exobiology. These critical experiments would include, for example, identification of organics, detection of fossils, and detection of extant life. The fourth phase is the detailed analysis of samples returned from these sites in Earth-based laboratories to confirm and extend previous discoveries. Finally, in the fifth phase, human exploration is needed to establish the geological settings for the earlier findings or to discover and explore sites that are not accessible to robotic spacecraft. 相似文献
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G Rogovski V Bogomolov M Ivanov J Runavot A Debus A Victorov J C Darbord 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》1996,18(1-2):323-332
Mars surface in-situ exploration started in 1975 with the American VIKING mission. Two probes landed on the northern hemisphere and provided, for the first time, detailed information on the martian terrain, atmosphere and meteorology. The current goal is to undertake larger surface investigations and many projects are being planned by the major Space Agencies with this objective. Among these projects, the Mars 94/96 mission will make a major contributor toward generating significant information about the martian surface on a large scale. Since the beginning of the Solar System exploration, planets where life could exist have been subject to planetary protection requirements. Those requirements accord with the COSPAR Policy and have two main goals: the protection of the planetary environment from influence or contamination by terrestrial microorganisms, the protection of life science, and particularly of life detection experiments searching extra-terrestrial life, and not life carried by probes and spacecrafts. As the conditions for life and survival for terrestrial microorganisms in the Mars environment became known, COSPAR recommendations were updated. This paper will describe the decontamination requirements which will be applied for the MARS 94/96 mission, the techniques and the procedures which are and will be used to realize and control the decontamination of probes and spacecrafts. 相似文献
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R L Mancinelli J R Marshall M R White 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》1992,12(4):111-116
Potential Martian soil components relevant to exobiology include water, organic matter, evaporites, clays, and oxides. These materials are also resources for human expeditions to Mars. When found in particular combinations, some of these materials constitute diagnostic paleobiomarker suites, allowing insight to be gained into the probability of life originating on Mars. Critically important to exobiology is the method of data analysis and data interpretation. To that end we are investigating methods of analysis of potential biomarker and paleobiomarker compounds and resource materials in soils and rocks pertinent to Martian geology. Differential thermal analysis coupled with gas chromatography is shown to be a highly useful analytical technique for detecting this wide and complex variety of materials. 相似文献
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M. Cabane P. Coll C. Szopa G. Israël F. Raulin R. Sternberg P. Mahaffy A. Person C. Rodier R. Navarro-Gonzlez H. Niemann D. Harpold W. Brinckerhoff 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2004,33(12):2240-2245
Observation of Mars shows signs of a past Earth-like climate, and, in that case, there is no objection to the possible development of life, in the underground or at the surface, as in the terrestrial primitive biosphere. Sample analysis at Mars (SAM) is an experiment which may be proposed for atmospheric, ground and underground in situ measurements. One of its goals is to bring direct or indirect information on the possibility for life to have developed on Mars, and to detect traces of past or present biological activity. With this aim, it focuses on the detection of organic molecules: volatile organics are extracted from the sample by simple heating, whereas refractory molecules are made analyzable (i.e. volatile), using derivatization technique or fragmentation by pyrolysis. Gaseous mixtures thus obtained are analyzed by gas chromatography associated to mass spectrometry. Beyond organics, carbonates and other salts are associated to the dense and moist atmosphere necessary to the development of life, and might have formed and accumulated in some places on Mars. They represent another target for SAM. Heating of the samples allows the analysis of structural gases of these minerals (CO2 from carbonates, etc.), enabling to identify them. We also show, in this paper, that it may be possible to discriminate between abiotic minerals, and minerals (shells, etc.) created by living organisms. 相似文献
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