A study of the geological environmental of suprapermafrost water in the headwater area of the yellow river 黄河源区冻结层上水地质环境影响研究
3.
The results shows that temperature in the porous dried layer varies - as a exponential discipline whose changing scope is determined by the mass flux and a linear distribution in temperature exists across the frozen layer 结果表明，多孔干燥层温度按指数规律变化，变化幅度取决于水汽流率，冻结层温度按线性分布，预测冻干时间与实际结果相符。
