Experimental and numerical investigation into rapid cooling of rock salt related to high frequency cycling of storage caverns

被引:31
作者
Blanco-Martin, Laura [1 ]
Rouabhi, Ahmed [1 ]
Billiotte, Joel [1 ]
Hadj-Hassen, Faouzi [1 ]
Tessier, Bruno [1 ]
Hevin, Gregoire [2 ]
Balland, Cyrille [3 ]
Hertz, Emmanuel [4 ]
机构
[1] PSL Res Univ, Dept Geosci, MINES ParisTech, 35 Rue St Honore, F-77300 Fontainebleau, France
[2] Storengy, 12 Rue Raoul Nordling, F-92270 Bois Colombes, France
[3] Ecole Mines Nancy, Ineris, 92 Rue Sergent Blandan, F-54042 Nancy, France
[4] Compagnie Salins Midi & Salins Est, 17 Rue Gabriel Peri, F-54110 Varangeville, France
关键词
Field test; Temperature drop; Tensile stresses; Salt caverns; High frequency cycling; Thermo-mechanical modeling; PERMEABILITY;
D O I
10.1016/j.ijrmms.2018.01.008
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
High frequency cycling of salt caverns is becoming common practice to meet the needs of energy markets and to foster underground energy storage. In the case of rapid cooling, tensile stresses and thermally-induced fractures can appear in the surrounding rock, with potential detrimental consequences to the integrity of the storage project. To further investigate the effects of rapid cycles on the integrity of rock salt, a thermo-mechanical test was performed in a salt mine. It consisted in cooling rapidly several times a salt surface of 10 m(2) (Delta T = -20 degrees C in about 8 h). Extensive monitoring allowed tracking the thermo-mechanical response of the rock, including possible fracture creation and propagation. Although more research is needed, the test demonstrated that tensile fracturing due to rapid cooling is possible. Thermo-mechanical modeling allowed reproducing fairly well the location, orientation and timing of the first fracture; indeed, fractures should be avoided to ensure cavern integrity, and therefore knowledge about the critical zones where fractures could appear is sufficient at the design stage.
引用
收藏
页码:120 / 130
页数:11
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