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Europa 木卫二(英)

Europa 木卫二(英)

Europa is the sixth of Jupiter's known satellites and the fourth largest; it is the second of the Galilean moons. Europa is slightly smaller than the Earth's Moon.
  orbit: 670,900 km from Jupiter
  diameter: 3138 km
  mass: 4.80e22 kg
  Europa was a Phoenician princess abducted to Crete by Zeus, who had assumed the form of a white bull, and by him the mother of Minos.
  Discovered by Galileo and Marius in 1610.
  Europa and Io are somewhat similar in bulk composition to the terrestrial planets: primarily composed of silicate rock. Unlike Io, however, Europa has a thin outer layer of ice. Recent data from Galileo indicate that Europa has a layered internal structure perhaps with a small metallic core.
  But Europa's surface is not at all like anything in the inner solar system. It is exceedingly smooth: few features more than a few hundred meters high have been seen. The prominent markings seem to be only albedo features with very low relief.
  There are very few craters on Europa; only three craters larger than 5 km in diameter have been found. This would seem to indicate a young and active surface. However, the Voyagers mapped only a fraction of the surface at high resolution. The precise age of Europa's surface is an open question.
  The images of Europa's surface strongly resemble images of sea ice on Earth. It is possible that beneath Europa's surface ice there is a layer of liquid water, perhaps as much as 50 km deep, kept liquid by tidally generated heat. If so, it would be the only place in the solar system besides Earth where liquid water exists in significant quantities.
  Europa's most striking aspect is a series of dark streaks crisscrossing the entire globe. The larger ones are roughly 20 km across with diffuse outer edges and a central band of lighter material. The latest theory of their origin is that they are produced by a series of volcanic eruptions or geysers.
  Recent observations with HST reveal that Europa has a very tenuous atmosphere (1e-11 bar) composed of oxygen. Of the many moons in the solar system only five others (Io, Ganymede, Callisto, Titan and Triton) are known to have atmospheres. Unlike the oxygen in Earth's atmosphere, Europa's is almost certainly not of biologic origin. It is most likely generated by sunlight and charged particles hitting Europa's icy surface producing water vapor which is subsequently split into hydrogen and oxygen. The hydrogen escapes leaving the oxygen.
  The Voyagers didn't get a very good look at Europa. But it is a principal focus of the Galileo mission. Images from Galileo's first two close encounters with Europa seem to confirm earlier theories that Europa's surface is very young: very few craters are seen, some sort of activity is obviously occurring. There are regions that look very much like pack-ice on polar seas during spring thaws on Earth. The exact nature of Europa's surface and interior is not yet clear but the evidence is now strong for a subsurface 'ocean'.
  Galileo has found that Europa has a weak magnetic field (perhaps 1/4 of the strength of Ganymede's). And most interestingly, it varies periodically as it passes thru Jupiter's massive magnetic field. This is very strong evidence that there is a conducting material beneath Europa's surface, most likely a salty ocean.
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回复:Europa 木卫二(英)

Europa 是木星的第六颗已知卫星,并是木星的第四大卫星,在伽利略发现的卫星中为离木星第二近。木卫二比地球的卫星月球稍微小一点。

  公转轨道: 距离木星 670,900 千米

  卫星直径: 3138 千米

  质量: 4.80e22 千克

  欧罗巴是腓尼基公主,宙斯化成一头白色的牛,将她诱拐至克里特岛,并生下了米诺斯。

  它由伽利略和Marius于1610年发现。

  木卫二与木卫一的组成与类地行星相似:主要由硅酸盐岩石组成。但是与木卫一不同,木卫二有一个薄薄的冰外壳。最近从伽利略号发回的数据表明木卫二有内部分层结构,并可能有一个小型金属内核。

  但是木卫二的表面不像一个内层太阳系的东西,它极度的光滑:只能看到极少的数百米高的地形。凸出的记号看来只是反照率特性或是一些不大的起伏。

  木卫二上的环形山很少;只发现三个直径大于5千米的环形山。这表面它有一个年轻又活跃的表面。然而,旅行者号做了一小部分的表面高清晰度地图。木卫二的表面精确年龄是一个悬而未决问题。

  木卫二的表面照片与地球海洋上的冰的照片相似。这可能是因为木卫二表面的冰以下有一层液态的水,或许有50千米深,由引潮力带来的热量保持液态。如果是这样的话,这将是除地球之外,太阳系中唯一一个有大量的液态水存在的地方。

  木卫二最醒目的外观是遍布全球的一串串十字条纹。较大的一个向外扩散到淡色物质地带,长近20千米。最近的有关它们的起源理论是:它们由一连串火山喷出物或喷泉产生。

  最近的哈博望远镜观察揭示出木卫二有一个含氧的稀薄大气(1e-11巴)。太阳系中63个卫星里只知道有4颗卫星(木卫一,木卫三,土卫六和海卫一)拥有大气层。不像地球的大气中的氧,木卫二的并不是生物形成的。它最可能是由于太阳光中的电荷粒子撞击木卫二的冰质表面而产生水蒸气,然而分成氢气和氧气。氢气脱离,留下了氧气。

  旅行者号并没有好好观察木卫二,因为它是伽利略号探索的主要任务。来自伽利略号两次接近木卫二发回的图片看来验证了早期的理论:木卫二的表面相当年轻,只看到很少的环形山,一些活动很显然正在发生。有些区域看来很像春天到来时,两极的海洋处冰块融化的情景。木卫二表面和内部的确切性质还不很清楚,但有一个表面“海洋”的确切证据。

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