The physics and mechanics of snow as a material
The physics and mechanics of snow as a material
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雪作为材料的物理和力学
DOI：
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发表时间：
1962
期刊：
影响因子：
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通讯作者：
黒岩 大助
中科院分区：
文献类型：
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作者：
H. Bader;黒岩 大助
翻译后摘要：雪是多孔的。冰粒的可渗透的集合体。晶粒可以主要是单晶或几种晶体的紧密组合。孔隙中充满了空气和水蒸气。在湿雪中，颗粒被液态水包裹。雪的特性是其固有的热力学不稳定性。因此，大多数有趣的物理参数不可避免地随时间而变化。这种变化过程被称为雪变质作用。
Abstract : Snow is a porous. permeable aggregate of ice grains. The grains can be predominantly single crystals or close groupings of several crystals. The pores are filled with air and water vapor. In wet snow the grains are coated with liquid water. The characteristic property of snow is its inherent thermodynamic instability. Consequently most of the interesting physical parameters inevitably change with time. This process of change is called snow metamorphism.