Firstly, the ice slush characteristics of Yellow River Inner Mongolia reach are analyzed from history datum.
首先,基于历史冰情资料,分析了黄河内蒙古段的凌情特征。
The slush is compacted by an unknown mechanism, and solid, bubble-free ice is formed from water high in soluble organic substances.
半融雪通过一种未知的物理过程被压实,而固态、无气泡的冰是由富含可溶性有机物的水形成的。
But a new look at Titan's insides reveals even more oddities: Beneath the brittle crust of ice lies a layer of slush. Deeper still is an underground ocean over a solid core of rock and ice.
但最近对泰坦内部的一项新研究却揭开了这颗奇异星球更为怪诞的一面:脆弱的甲烷冰地表之下,覆盖着一层冰泥,更深处依然是一个地下海洋,最中间是冰和岩石并存的固态核心。
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