If a rocky planet is big enough - say, 10 times the mass of Earth - it can vacuum up so much hydrogen that its atmosphere ends up constituting most of the planet.
如果一个由岩石组成的行星足够的大——比方说,质量是地球的10倍——它可以吸收如此多的氢,以至于他的大气层最终会形成大部分的行星。
But with a fifth planet, the simulations produced familiar solar systems 10 times more often.
但是加入第五个行星后,模拟10多次都重新了我们所熟知的太阳系。
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