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The modes and its implications of water accumulation near the freezing front during soil freezing with considering ice segregation北大核心CSCD
作者姓名:张莲海  马巍  石亚军  黄永庭  韩大伟  杨成松  尚飞  周成林
作者单位:1.中国科学院西北生态环境资源研究院冻土工程国家重点实验室730000;2.中国科学院大学100049;3.甘肃省科学院地质自然灾害防治研究所730000;4.中国电建集团华东勘测设计研究院有限公司311122;5.磁共振冻融成冰过程动态分析联合实验室730000;
基金项目:国家自然科学基金重点项目(41630636);国家自然科学基金青年项目(41501072);第二次青藏高原综合科学考察研究项目(2019QZKK0902);冻土工程国家重点实验室自主课题(SKLFSE-ZT-202107)资助。
摘    要:Water accumulation associated with water migration is closely related with the ice segregation,but their coupling relationship is still unclear. To decoupling the relationship of water accumulation and ice segrega⁃ tion,herein,the dynamics of water migration and ice segregation during the freezing and thawing of different soil types under different water supplying conditions have been investigated based on pore water pressure mea⁃ surement and layer-scanning technique. Results showed that apparent water accumulation near the freezing front during the freezing of silty clay and loess tested here,but there exist differences in modes. During loess freezing under closed system,no ice segregation was observed,the pore water pressure increased,and there existed ap⁃ parent liquid water accumulation during the early stage of freezing;while during the freezing of silty clay,there existed ice segregation,the pore water pressure decreased,and no apparent liquid water accumulation occurred during the early stage of freezing. The results implied that there exist two modes of water accumulation near the freezing front during soil freezing:one is the water accumulation induced by water pressure gradient induced by pore ice which results in water flowing from the frozen zone and unfrozen zone to the location near the freezing front;the other is the water accumulation induced by cryo-suction of segregation ice which results in the water flowing from the unfrozen zone to the location near the freezing front. Notably,the contribution from each mode associated with water accumulation of soil freezing depends on whether the ice segregation exists. As no ice seg⁃ regation forms,water accumulation induced water pressure gradient predominates during the early stage of freez⁃ ing. As there exists ice segregation during freezing,water accumulation induced cryo-suction predominates dur⁃ ing the later stage of freezing. Investigating on different modes of water accumulations will be helpful for the ex⁃ ploring the mechanisms of freeze-thaw diseases and the ground ice in the cold regions. © 2023 Chinese Journal of General Practitioners. All rights reserved.

关 键 词:冰分凝  水分累积  未冻水  水分迁移  孔隙水压力
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