研究结果表明：时间和温度决定了水分迁移的充分性，温度的变化随深度的增加而具有衰减性，并且在冻结峰面附近形成一个冻结含水量峰值；
The results indicate that a peak of frozen moisture content is formed in frozen peak surface, which is developed for depth change with time increased.
研究结果表明：时间和温度决定了水分迁移的充分性，温度的变化随深度的增加而具有衰减性，并且在冻结峰面附近形成一个冻结含水量峰值；
The results indicate that a peak of frozen moisture content is formed in frozen peak surface, which is developed for depth change with time increased.
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