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Water and Salt Migration with Phase Change in Saline Soil during Freezing and Thawing Processes

机译:冻融过程中盐渍土中水和盐的迁移及其相变

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摘要

Water and salt transfer coupled with phase change may cause serious damage to engineering structures in saline soil regions. In this study, the migration of water and salt in silty clay collected from the Qinghai-Tibet Plateau is explored experimentally and numerically during freezing and thawing processes. The results revealed that there are significant differences in the variations of liquid water content and solution concentration for different initial salt contents, due to salt crystallization and dissolution. The temperature-induced water migration is determined by the soil properties, which can be well explained by the thermodynamics of mass transfer. The amount of salt migrated upward during cooling is slightly larger than that transported downward in the warming period, implying that salt may be accumulated in the surface soil after a large number of circulations and finally result in soil salinization.
机译:水分和盐分的转移以及相变可能会严重破坏盐碱土地区的工程结构。在这项研究中,水和盐在青藏高原粉质黏土中的迁移在冻融过程中进行了实验和数值研究。结果表明,由于盐的结晶和溶解,对于不同的初始盐含量,液体水含量和溶液浓度的变化存在显着差异。温度引起的水迁移取决于土壤的性质,这可以通过传质的热力学很好地解释。在冷却过程中向上迁移的盐量略大于在暖化时期向下迁移的盐量,这意味着盐可能会在大量循环之后积聚在表层土壤中,并最终导致土壤盐碱化。

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  • 来源
    《Ground water》 |2018年第5期|742-752|共11页
  • 作者单位

    Guizhou Univ, Key Lab Karst Environm & Geohazard, Minist Land & Resources, Huaxi New Campus, Guiyang 550025, Guizhou, Peoples R China;

    Guizhou Univ, Coll Resource & Environm Engn, Guiyang 550025, Guizhou, Peoples R China;

    Guizhou Univ, Coll Resource & Environm Engn, Guiyang 550025, Guizhou, Peoples R China;

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