Synthetic salt rock prepared by molten salt crystallization and its physical and mechanical properties

被引:4
|
作者
Liu, Xin [1 ,2 ,3 ]
Shi, Xilin [1 ,2 ,6 ]
Li, Yinping [1 ,2 ,4 ]
Ye, Liangliang [1 ,2 ]
Wei, Xinxing [1 ,2 ]
Zhu, Shijie [1 ,5 ]
Bai, Weizheng [1 ,2 ]
Ma, Hongling [1 ,2 ]
Yang, Chunhe [1 ,2 ,6 ]
机构
[1] Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn, Wuhan 430071, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Univ Bodenkultur, Inst Geotech, Feistmantelstr 4, A-1180 Vienna, Austria
[4] Chinese Acad Sci, Inst Rock & Soil Mech, Hubei Key Lab Geoenvironm Engn, Wuhan 430071, Peoples R China
[5] Chongqing Univ, State Key Lab Coal Mine Disaster Dynam & Control, Chongqing 400044, Peoples R China
[6] Jiangsu Suyan Jingshen Co Ltd, Huaian 223200, Jiangsu, Peoples R China
基金
中国国家自然科学基金;
关键词
Energy storage; Salt rock; Properties test; Molten salt; Crystallization mechanism; THERMAL-ENERGY STORAGE; SOLAR POWER-PLANTS; PERMEABILITY; CAVERNS; DISSOLUTION; ANHYDRITE; STABILITY; BEHAVIOR; REPAIR; JINTAN;
D O I
10.1016/j.energy.2023.126711
中图分类号
O414.1 [热力学];
学科分类号
摘要
Physical simulation is an important research method for salt cavern energy storage construction technology. However, its progress is constrained by lack of effective model salt. Exploratory experiments were conducted to prepare salt rock by molten salt crystallization. A well-made synthetic salt rock was obtained from repeated adjustment of staged cooling conditions and controlled crystal growth procedures. Samples were taken for microscopic, physical, and mechanical tests, and compared with natural salt rock. SEM, CT and p-wave velocity results show that synthetic salt rock achieved crystallization. Its crystal structure, grain size and intercrystalline relationship are consistent with those of natural salt rock. Its density distribution is uniform and compaction is good. X-ray results prove a high crystallinity and stable mineral composition. Porosity of synthetic specimens ranges from 2.3% to 5.9%, permeability is in the range of E-13 to E-16 m2. Uniaxial compression stress-strain curves, strengths, deformation modulus and poisson's ratios are close to those of natural salt rock. It has obvious ductility and damage occurs after dilation deformation. We initially illustrate energy storage and heat storage-transfer principles of molten salt. The mechanism of layered growth in molten salt crystallization is revealed. The findings provide new insight on salt rock preparation, crystallography, molten salt and salt cavern study.
引用
收藏
页数:18
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