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Enceladus's measured physical libration requires a global subsurface ocean

机译:土卫二测量的物理解放需要一个全局的地下   海洋

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摘要

Several planetary satellites apparently have subsurface seas that are ofgreat interest for, among other reasons, their possible habitability. Thegeologically diverse Saturnian satellite Enceladus vigorously vents liquidwater and vapor from fractures within a south polar depression and thus musthave a liquid reservoir or active melting. However, the extent and location ofany subsurface liquid region is not directly observable. We use measurements ofcontrol points across the surface of Enceladus accumulated over seven years ofspacecraft observations to determine the satellite's precise rotation state,finding a forced physical libration of 0.120 $\pm$ 0.014{\deg} (2{\sigma}).This value is too large to be consistent with Enceladus's core being rigidlyconnected to its surface, and thus implies the presence of a global oceanrather than a localized polar sea. The maintenance of a global ocean withinEnceladus is problematic according to many thermal models and so may constrainsatellite properties or require a surprisingly dissipative Saturn.
机译:显然,几颗行星状卫星的海面引起人们的极大兴趣,原因之一除其他原因是其可能的可居住性。土星卫星的地质学上各不相同,它们从南极凹陷内的裂缝中大力排出了液态水和蒸气,因此必须具有液态储层或活跃的熔融作用。但是,任何地下液体区域的范围和位置都无法直接观察到。我们使用在七年的航天器观测中积累的整个土卫二表面控制点的测量结果,来确定卫星的精确旋转状态,确定了0.120 $ \ pm $ 0.014 {\ deg}(2 {\ sigma})的强迫物理释放。它太大而无法与土卫二的核心刚性连接到其表面相一致,因此暗示存在着全球性的海洋而不是局部的极地海。根据许多热模型,在土卫二中维持全球海洋存在问题,因此可能会限制卫星特性或需要令人惊讶地耗散性的土星。

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