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DOI | 10.1016/j.cis.2021.102465 |
Spatial state distribution and phase transition of non-uniform water in soils: Implications for engineering and environmental sciences | |
Zhang, Lianhai; Zhuang, Qianlai; Wen, Zhi; Zhang, Peng; Ma, Wei; Wu, Qingbai![]() | |
发表日期 | 2021 |
ISSN | 0001-8686 |
EISSN | 1873-3727 |
卷号 | 294 |
英文摘要 | The physical behaviors of water in the interface are the fundamental to discovering the engineering properties and environmental effects of aqueous porous media (e.g., soils). The pore water pressure (PWP) is a key parameter to characterize the pore water state (PWS) and its phase transition in the micro interface. Traditionally, the water in the interface is frequently believed to be uniform, negative in pressure and tensile based on macroscopic tests and Gibbs interface model. However, the water in the interface is a non-uniform and compressible fluid (part of tensile and part of compressed), forming a spatial profile of density and PWP depending on its distance from the substrate interface. Herein, we introduced the static and dynamic theory methods of non-uniform water based on diffuse interface model to analyze non-uniform water state dynamics and water density and PWP. Based on the theory of non-uniform water, we gave a clear stress analysis on soil water and developed the concepts of PWS, PWP and matric potential in classical soil mechanics. In addition, the phase transition theory of non-uniform water is also examined. In nature, the generalized Clausius-Clapeyron equation (GCCE) is consistent with Clapeyron equation. Therefore, a unified interpretation is proposed to justify the use of GCCE to represent frozen soil water dynamics. Furthermore, the PWP description of non-uniform water can be well verified by some experiments focusing on property variations in the interface area, including the spatial water density profile and unfrozen water content variations with decreasing temperature and other factors. In turn, PWP spatial distribution of non-uniform water and its states can well explain some key phenomena on phase transition during ice or hydrate formation, including the discrepancies of phase transition under a wide range of conditions |
英文关键词 | Non-uniform water; GCCE; Matric potential; Hydrate formation; Phase transition; Diffuse interface model |
语种 | 英语 |
WOS研究方向 | Chemistry |
WOS类目 | Chemistry, Physical |
WOS关键词 | GAS-HYDRATE PHASE ; DENSITY ; ICE ; PRESSURES ; INTERFACE ; SYSTEM ; MODEL ; CLAY |
WOS记录号 | WOS:000685473700015 |
来源期刊 | ADVANCES IN COLLOID AND INTERFACE SCIENCE
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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/240309 |
作者单位 | [Zhang, Lianhai; Wen, Zhi; Zhang, Peng; Ma, Wei; Wu, Qingbai; Yun, Hanbo] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Beilu He Observat & Res Stn Tibetan Plateau, Lanzhou 730000, Peoples R China; [Zhang, Lianhai; Zhuang, Qianlai; Yun, Hanbo] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA; [Zhang, Lianhai; Wen, Zhi] State Key Lab Frozen Soil Engn & Suzhou Niumag An, Dept Joint NMR Lab Freeze Thaw Proc, Lanzhou 730000, Peoples R China; [Yun, Hanbo] Univ Copenhagen, Ctr Permafrost CENPERM, DK-1350 Copenhagen, Denmark |
推荐引用方式 GB/T 7714 | Zhang, Lianhai,Zhuang, Qianlai,Wen, Zhi,et al. Spatial state distribution and phase transition of non-uniform water in soils: Implications for engineering and environmental sciences[J]. 中国科学院西北生态环境资源研究院,2021,294. |
APA | Zhang, Lianhai.,Zhuang, Qianlai.,Wen, Zhi.,Zhang, Peng.,Ma, Wei.,...&Yun, Hanbo.(2021).Spatial state distribution and phase transition of non-uniform water in soils: Implications for engineering and environmental sciences.ADVANCES IN COLLOID AND INTERFACE SCIENCE,294. |
MLA | Zhang, Lianhai,et al."Spatial state distribution and phase transition of non-uniform water in soils: Implications for engineering and environmental sciences".ADVANCES IN COLLOID AND INTERFACE SCIENCE 294(2021). |
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