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Simulating Martian Regolith In The Laboratory

机译:在实验室中模拟火星人雷戈利斯

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Regolith and dust cover the surfaces of the Solar Systems solid bodies, and thus constitute the visible surface of these objects. The topmost layers also interact with space or the atmosphere in the case of Mars, Venus and Titan. Surface probes have been proposed, studied and flown to some of these worlds. Landers and some of the mechanisms they carry, e.g. sampling devices, drills and subsurface probes ("moles") will interact with the porous surface layer. The absence of true extraterrestrial test materials in ample quantities restricts experiments to the use of soil or regolith analogue materials. Several standardized soil simulants have been developed and produced and are commonly used for a variety of laboratory experiments. In this paper we intend to give an overview of some of the most important soil simulants, and describe experiments (penetrometry, thermal conductivity, aeolian transport, goniometry, spectroscopy and exobiology) made in various European laboratory facilities.
机译:go石和灰尘覆盖了太阳系固体的表面,因此构成了这些物体的可见表面。在火星,金星和土卫六的情况下,最顶层也与空间或大气相互作用。表面探针已经被提出,研究并运用于其中的一些领域。着陆器及其携带的一些机制,例如采样设备,钻头和地下探针(“摩尔”)将与多孔表面层相互作用。没有足够数量的真正的地外试验材料,使实验仅限于土壤或硬土类模拟材料的使用。已经开发和生产了几种标准化的土壤模拟物,它们通常用于各种实验室实验。在本文中,我们打算概述一些最重要的土壤模拟物,并描述在欧洲各种实验室设施中进行的实验(渗透率,热导率,风向迁移,测角法,光谱学和外生生物学)。

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