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Seasonal and diurnal variations in Martian surface ultraviolet irradiation: biological and chemical implications for the Martian regolith

机译:火星表面紫外线照射的季节和日变化:对火星风化层的生物和化学影响

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摘要

The issue of the variation of the surface ultraviolet (UV) environment on Mars was investigated with particular emphasis being placed on the interpretation of data in a biological context. A UV model has been developed to yield the surface UV irradiance at any time and place over the Martian year. Seasonal and diurnal variations were calculated and dose rates evaluated. Biological interpretation of UV doses is performed through the calculation of DNA damage effects upon phage T7 and Uracil, used as examples for biological dosimeters. A solar UV 'hotspot' was revealed towards perihelion in the southern hemisphere, with a significant damaging effect upon these species. Diurnal profiles of UV irradiance are also seen to vary markedly between aphelion and perihelion. The effect of UV dose is also discussed in terms of the chemical environment of the Martian regolith, since UV irradiance can reach high enough levels so as to have a significant effect upon the soil chemistry. We show, by assuming that H2O is the main source of hydrogen in the Martian atmosphere, that the stoichiometrically desirable ratio of 2:1 for atmospheric H and O loss rates to space are not maintained and at present the ratio is about 20:1. A large planetary oxygen surface sink is therefore necessary, in contrast with escape to space. This surface oxygen sink has important implications for the oxidation potential and the toxicology of the Martian soil. UV-induced adsorption of {m O}_{2}^{-} super-radicals plays an important role in the oxidative environment of the Martian surface, and the biologically damaging areas found in this study are also shown to be regions of high subsurface oxidation. Furthermore, we briefly cover the astrobiological implications for landing sites that are planned for future Mars missions.
机译:研究了火星表面紫外线(UV)环境变化的问题,尤其着重于生物学背景下的数据解释。已经开发了一个紫外线模型,以在火星年中的任何时间和地点产生表面紫外线辐照度。计算季节性和昼夜变化并评估剂量率。 UV剂量的生物学解释是通过计算DNA对噬菌体T7和Uracil的损伤作用来进行的,这些噬菌体被用作生物剂量计的实例。太阳紫外线的“热点”向南半球的近日点曝光,对这些物种具有重大破坏作用。紫外线辐照度的昼夜曲线在角膜和近日点之间也有明显变化。紫外线剂量的影响也根据火星长石的化学环境进行了讨论,因为紫外线辐照度可以达到足够高的水平,从而对土壤化学产生重大影响。通过假设H2O是火星大气中氢的主要来源,我们证明了大气H和O对空间的损失率的化学计量比为2:1并没有得到维持,目前该比率约为20:1。因此,与逃逸到太空相反,需要一个较大的行星式氧表面沉。该表面氧汇对火星土壤的氧化潜力和毒理学具有重要意义。紫外线诱导的{ rm O} _ {2} ^ {-}超自由基的吸附在火星表面的氧化环境中起着重要作用,并且该研究中发现的对生物有害的区域也显示为地下氧化程度高。此外,我们简要介绍了计划用于未来火星任务的着陆点的天文生物学意义。

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