Mechanism of Freeze-thaw Action in Land Salinization Process
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Mechanism of Freeze-thaw Action in Land Salinization Process
Bulletin of Soiland Water ConservationVol. 19, Issue 6, Pages: 14-17(2000)
作者机构:
中国科学院地球化学研究所环境地球化学国家重点实验室,贵州,贵阳,550002
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Published:2000
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Zhang Dianfa, Wang Shijie. Mechanism of Freeze-thaw Action in Land Salinization Process[J]. Bulletin of Soiland Water Conservation, 2000, 19(6): 14-17.
DOI:
Zhang Dianfa, Wang Shijie. Mechanism of Freeze-thaw Action in Land Salinization Process[J]. Bulletin of Soiland Water Conservation, 2000, 19(6): 14-17.DOI:
Mechanism of Freeze-thaw Action in Land Salinization Process
freeze-thaw action is differing from salification process by violent evaporation
it has distinct control action on springtime salification
but it has not been much accounted adequately. In the process of feezing and thawing
soil profile constitution is divided into three layers frozen layer
semi-frozen layer and unfrozen layer
special travel of water and salt was made.In the process of soil freezing
soil water and salt move towards fozen layer from the underlayers
salinity in the frozen layer increased evidently. In the process of soil thawing
the salinity of frozen ayer assembles in the upper soil layer along with violent vaporizing in springtime. Its intensity level of salification like“eruption”this time
the land salinization has no relation with ground water table
because frozen layer by way of waterproof layer insulate unconfined water. So it is unauthentic that the critical depth of unconfined water controlled that“eruption”salification in springtime.
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