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Enabling Martian habitability with silica aerogel via the solid-state greenhouse effect

机译:通过固态温室效应使二氧化硅气凝胶具有火星人的可居住性

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摘要

The low temperatures and high ultraviolet radiation levels at the surface of Mars today currently preclude the survival of life anywhere except perhaps in limited subsurface niches. Several ideas for making the Martian surface more habitable have been put forward, but they all involve massive environmental modification that will be well beyond human capability for the foreseeable future. Here, we present a new approach to this problem. We show that widespread regions of the surface of Mars could be made habitable to photosynthetic life in the future via a solid-state analogue to Earth’s atmospheric greenhouse effect. Specifically, we demonstrate via experiments and modelling that under Martian environmental conditions, a 2–3 cm-thick layer of silica aerogel will simultaneously transmit sufficient visible light for photosynthesis, block hazardous ultraviolet radiation and raise temperatures underneath it permanently to above the melting point of water, without the need for any internal heat source. Placing silica aerogel shields over sufficiently ice-rich regions of the Martian surface could therefore allow photosynthetic life to survive there with minimal subsequent intervention. This regional approach to making Mars habitable is much more achievable than global atmospheric modification. In addition, it can be developed systematically, starting from minimal resources, and can be further tested in extreme environments on Earth today.
机译:目前,火星表面的低温和高紫外线辐射水平阻碍了任何地方生命的生存,除了可能在有限的地下壁ni中。提出了一些使火星表面更宜居的想法,但它们都涉及大规模的环境改造,在可预见的将来这将远远超出人类的能力。在这里,我们提出了解决此问题的新方法。我们的研究表明,未来通过与地球大气温室效应的固态类似物,可以使火星表面的广阔区域变得适于光合作用。具体而言,我们通过实验和建模证明,在火星环境条件下,厚度为2–3厘米的二氧化硅气凝胶层将同时透射足够的可见光以进行光合作用,阻挡有害的紫外线辐射并将其下方的温度永久升高至熔点以上。无需任何内部热源。因此,将二氧化硅气凝胶防护罩放置在火星表面上足够冰层丰富的区域上,可以使光合作用的生命在那里存活下来,而只需很少的后续干预。这种使火星适合居住的区域性方法比全球大气改造要容易得多。此外,它可以从最少的资源开始系统地开发,并且可以在当今地球上的极端环境中进行进一步测试。

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  • 来源
    《Nature Astronomy》 |2019年第10期|898-903|共6页
  • 作者单位

    Harvard Paulson School of Engineering and Applied Sciences Department of Earth and Planetary Sciences Harvard University Cambridge MA USA Department of Earth and Planetary Sciences Harvard University Cambridge MA USA;

    Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA;

    UK Centre for Astrobiology School of Physics and Astronomy University of Edinburgh Edinburgh UK;

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