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Water retention of selected microorganisms and Martian soil simulants under close to Martian environmental conditions

机译:在接近火星环境的条件下,某些微生物和火星土壤模拟物的保水率

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摘要

Based on the latest knowledge about microorganisms resistant towards extreme conditions on Earth and results of new complex models on the development of the Martian atmosphere we quantitatively examined the water-bearing properties of selected extremophiles and simulated Martian regolith components and their interaction with water vapor under close to Martian environmental conditions. Three different species of microorganisms have been chosen and prepared for our study: Deinococcus geothermalis, Leptothrix sp. OT_B_406, and Xanthoria elegans. Further, two mineral mixtures representing the early and the late Martian surface as well as montmorillonite as a single component of phyllosilicatic minerals, typical for the Noachian period on Mars, were selected. The thermal mass loss of the minerals and bacteria-samples was measured by thermoanalysis. The hydration and dehydration properties were determined under close to Martian environmental conditions by sorption isotherm measurements using a McBain-Bakr quartz spring balance. It was possible to determine the total water content of the materials as well as the reversibly bound water fraction as function of the atmospheres humidity by means of these methods. Our results are important for the evaluation of future space mission outcomes including astrobiological aspects and can support the modeling of the atmosphere/surface interaction by showing the influence on the water inventory of the upper most layer of the Martian surface.
机译:基于有关地球上对极端条件具有抗性的微生物的最新知识以及有关火星大气发展的新复杂模型的结果,我们定量研究了所选极端微生物和模拟火星重生石成分的含水特性及其在近距离下与水蒸气的相互作用受火星环境影响。为我们的研究选择并准备了三种不同的微生物:地热球菌,Leptothrix sp。 OT_B_406和Xanthoria elegans。此外,还选择了两种矿物混合物,它们代表火星的早期和晚期表面,以及蒙脱石(一种单一的叶硅质矿物成分),是火星上Noachian时期的典型成分。矿物和细菌样品的热质量损失通过热分析测量。通过使用McBain-Bakr石英弹簧秤进行的吸附等温线测量,在接近火星环境的条件下确定了水合和脱水性能。通过这些方法可以确定材料的总水含量以及可逆结合的水含量随大气湿度的变化。我们的结果对于评估未来的太空任务结果(包括天文生物学方面)非常重要,并且可以通过显示对火星表面最上层水库的影响来支持大气/表面相互作用的建模。

著录项

  • 来源
    《Planetary and space science》 |2014年第8期|163-168|共6页
  • 作者单位

    Technical University of Applied Sciences Wildau, c/o Zeosolar e.v., volmeretr. 13, 12489 Berlin, Germany;

    DLR Institute of Aerospace Medicine, Linder Hoehe, 51147 Koeln, Germany;

    TU Berlin, Institute of Environmental Microbiology, Ernst-Reuter-Platz 1, 10587 Berlin, Germany;

    DLR Institute of Planetary Research, Rutherfordstrasse 2, D-12489 Berlin, Germany;

    DLR Institute of Aerospace Medicine, Linder Hoehe, 51147 Koeln, Germany;

    University of Duisburg/Essen, Biofilm Center, Universitaetsstrasse 5, 45141 Essen, Germany;

    TU Berlin, Institute of Environmental Microbiology, Ernst-Reuter-Platz 1, 10587 Berlin, Germany;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Mars; Micoorganism; Mineral; Water sorption isotherms; Thermogravimetry;

    机译:火星;微生物矿物;吸水等温线;热重法;

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