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DOI | 10.1007/s10064-020-02052-x |
An experimental study of the relationship between the matric potential, unfrozen water, and segregated ice of saturated freezing soil | |
Xue, Ke; Wen, Zhi; Zhu, Zhanyuan; Wang, Dayan; Luo, Fei; Zhang, Mingli | |
通讯作者 | Xue, K (通讯作者),Sichuan Agr Univ, Coll Water Conservancy & Hydropower Engn, Yaan 635000, Peoples R China. ; Xue, K (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China. |
发表日期 | 2021 |
ISSN | 1435-9529 |
EISSN | 1435-9537 |
起始页码 | 2535 |
结束页码 | 2544 |
卷号 | 80期号:3 |
英文摘要 | Frost heave damage is caused by the in situ freezing of pore water and segregated ice due to moisture migration. Previous studies have shown that in freezing soil, moisture migration is related to the pore water pressure gradient, and moisture migration is the dominant reason for the formation of an ice lens. However, the essential relationship between ice segregation and the matric potential is still controversial. Using a pF meter sensor, a 5TM volume water content sensor, and a digital image capture system, the relationship between the matric potential and the unfrozen water in saturated freezing soil was monitored in real time, and digital images of the formation of segregated ice were collected. Furthermore, the time space coupling relationships between the unfrozen water, the matric potential, the frost-heaving amount, the moisture migration, and the formation of an ice lens were systematically analyzed during soil freezing. The results demonstrate that there is an internal relationship between the moisture migration driven by the matric potential (from the micro-perspective) and the segregated ice layer effect (from the macroscopic perspective). In addition, the unfrozen water and the matric potential in the frozen area have a significant impact on the distribution of the segregated ice lenses. |
关键词 | FROST HEAVEFROZENTRANSPORTLENSES |
英文关键词 | Freezing soil; Matric potential; Segregated ice; Unfrozen water; pF meter |
语种 | 英语 |
WOS研究方向 | Engineering ; Geology |
WOS类目 | Engineering, Environmental ; Engineering, Geological ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000605098500003 |
来源期刊 | BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT |
来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/254245 |
作者单位 | [Xue, Ke; Zhu, Zhanyuan; Luo, Fei] Sichuan Agr Univ, Coll Water Conservancy & Hydropower Engn, Yaan 635000, Peoples R China; [Xue, Ke; Wen, Zhi; Wang, Dayan] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China; [Wen, Zhi] Lanzhou Jiao Tong Univ, Sch Civil Engn, Lanzhou 730100, Peoples R China; [Zhang, Mingli] Lanzhou Univ Technol, Sch Civil Engn, Lanzhou 730050, Peoples R China |
推荐引用方式 GB/T 7714 | Xue, Ke,Wen, Zhi,Zhu, Zhanyuan,et al. An experimental study of the relationship between the matric potential, unfrozen water, and segregated ice of saturated freezing soil[J]. 中国科学院西北生态环境资源研究院,2021,80(3). |
APA | Xue, Ke,Wen, Zhi,Zhu, Zhanyuan,Wang, Dayan,Luo, Fei,&Zhang, Mingli.(2021).An experimental study of the relationship between the matric potential, unfrozen water, and segregated ice of saturated freezing soil.BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT,80(3). |
MLA | Xue, Ke,et al."An experimental study of the relationship between the matric potential, unfrozen water, and segregated ice of saturated freezing soil".BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT 80.3(2021). |
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