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寒区冻结层上包气带水分的迁移主要受近地表空气湿度和热力梯度的影响,在计算包气带水分迁移强度时需要考虑这两个因素。通过对寒区冻结层上包气带水分运移分析与计算的研究得出唯象法对复杂自然研究的重要性。不仅因为它对包气带中水分迁移的研究十分重要,还因为它可以更全面地解释完全饱和层和不饱和层中水分运动的联系和统一,揭示冻结层上水水体形成和资源分布特性。
The migration of water vapor in the frost layer of cold region is mainly affected by the near surface air humidity and the thermal gradient. These two factors need to be considered when calculating the moisture migration intensity of the entrained zone. Based on the analysis and calculation of water vapor transport in the zonal zone in the frost layer of cold region, the importance of the phenomenological method to the study of complex nature is obtained. Not only because of its importance to the study of water migration in the aeration zone but also because it can provide a more complete explanation of the connection and unification of the water movement in the fully saturated and unsaturated layers and reveal the water body formation and resource distribution in the frozen layer.