Layered interiors of Uranus and Neptune (IMAGE)
Caption
Models for the interior structures of the ice-giant planets Uranus and Neptune have two distinct, intermediate layers: an upper, water-rich convecting layer where disorganized magnetic fields are generated, and a lower, non-convecting hydrocarbon-rich layer. New computer simulations show that icy materials naturally separate at high pressure and temperature into these two layers.
Credit
Burkhard Militzer, UC Berkeley
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