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Freezing mechanism of NaCl solution ultra-confined on surface of calcium-silicate-hydrate: A molecular dynamics study
被引:14
|作者:
Liang, Te
[1
,2
]
Lai, Yuanming
[1
,2
]
Hou, Dongshuai
[3
]
Yang, Qingrui
[3
]
Yang, Yi
[4
]
Bai, Ruiqiang
[1
]
Zhang, Jing
[1
]
Jiang, Jing
[1
]
机构:
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Gansu, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Qingdao Univ Technol, Dept Civil Engn, Qingdao 266033, Peoples R China
[4] Jiangnan Univ, Jiangsu Key Lab Adv Food Mfg Equipment & Technol, Wuxi 214122, Peoples R China
基金:
中国国家自然科学基金;
关键词:
Calcium silicate hydrate;
Ultra-confined water;
Molecular dynamics;
Hexagonal ice;
Freezing mechanism;
C-S-H;
PHASE-TRANSITIONS;
CHLORIDE PENETRATION;
CRYSTAL-STRUCTURE;
NANO-PORE;
FLY-ASH;
WATER;
CEMENT;
CONCRETE;
ICE;
D O I:
10.1016/j.cemconres.2022.106722
中图分类号:
TU [建筑科学];
学科分类号:
0813 ;
摘要:
Cement-based materials in cold regions usually suffer deicer-frost deterioration. To better understand the frozen behavior of the calcium silicate hydrate (C-S-H), molecular dynamics is utilized to investigate the freezing processes of gel surface NaCl solution. The presence of C-S-H substrate significantly reduces the freezing temperature of water molecules ultra-confined on the C-S-H surface, which is 17 K lower than that of bulk water. While majority of random distributed water molecules crystalize to hexagonal ice (Ih) structure, molecules within 0.6 nm of C-S-H substrate cannot form ordered ice crystal at 225 K. The non-icing water layer and lower freezing point are mainly due to oxygen atoms on the silicate chains that provide strong hydrogen bonds with neighboring water and restrict the water orientation. Ionic clusters formed in unfrozen solution are important influence factor for water freezing. Hopefully, this work can provide molecular insights of cement-based materials design in cold regions.
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页数:16
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