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DOI10.1016/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; Yun, Hanbo
发表日期2021
ISSN0001-8686
EISSN1873-3727
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
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
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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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