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MELTING PROBES AT LAKE VOSTOK AND EUROPA

机译:沃斯托克湖和欧罗巴地区的融化问题

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摘要

Signatures indicative of a subglacial ocean on the Jovian satellite Europa have been discovered by the Galileo spaceprobe. The structure and chemistry of this postulated ocean, have received considerable attention, and its exploration is seen as an important goal for the fields of comparative planetology and astrobiology. Terrestrial subglacial lakes (e.g., Lake Vostok) have been considered as analogues for several aspects of a Europan ocean and the means of exploring such an environment will be discussed. We review the concept of melting probes, i.e. small probes with a heated tip ("hot point"), that melt through the ice. Such devices can carry instruments for in-situ measurements, or act as sample-return probes by the new concept of melting "upwards" once the sampling in the liquid ocean has been performed. Experience with melting probes in Antarctica exists; a demonstration mission to, e.g., Lake Vostok is proposed, and a possible design for a mission to Europa is outlined. Although, for a Europan mission, a probe capable of in-situ analysis might differ substantially from the terrestrial 'sample-return' version.
机译:伽利略太空探测器已经发现了在木星欧罗巴卫星上的冰下海洋的标志。该假定海洋的结构和化学性质已引起广泛关注,其探索被视为比较行星学和天体生物学领域的重要目标。陆地冰湖以下的湖泊(例如沃斯托克湖)被认为是欧洲泛欧海洋多个方面的类似物,并将讨论探索这种环境的方法。我们回顾了融化探针的概念,即具有在冰中融化的带有加热尖端(“热点”)的小型探针。一旦在液态海洋中进行了采样,这种设备就可以携带用于原位测量的仪器,或者通过融化“向上”的新概念充当采样返回探针。在南极洲有熔化探针的经验;提出了对例如沃斯托克湖的示范任务,并概述了前往欧罗巴的任务的可能设计。尽管对于Europan任务而言,能够进行原位分析的探头可能与地面“样品返回”版本大不相同。

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