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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

邮发代号 80-963

2019 Impact Factor: 1.62

Frontiers of Earth Science  2023, Vol. 17 Issue (3): 691-700   https://doi.org/10.1007/s11707-022-1019-9
  本期目录
Pore structure evolution of mudstone caprock under cyclic load-unload and its influence on breakthrough pressure
Junchang SUN1, Zhiqiang DONG2, Sinan ZHU3, Shifeng TIAN2, Junping ZHOU2()
1. Bohai Rim Energy Research Institute, Northeast Petroleum University, Qinghuangdao 066004, China
2. State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400044, China
3. Sinopec Petroleum Exploration and Production Research Institute, Beijing 100083, China
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Abstract

The pore structure of caprock plays an important role in underground gas storage security, as it significantly influences the sealing capacity of caprock. However, the pore structure evolution of caprock with the cyclic stress perturbations triggered by the cyclic gas injection or extraction remains unclear. In this study, the pore structure changes of mudstone caprock under cyclic loading and unloading were obtained by the nuclear magnetic resonance (NMR) tests system, then the influence of the changes on the breakthrough pressure of caprock was discussed. The results indicated that the pore structure changes are depending on the stress loading-unloading path and stress level. In the first cyclic, at the loading stage, with the increase of confining stress, the NMR T2 spectra curve moved to the left, the NMR signal amplitude of the first peak increased, while the amplitude of the second peak decreased gradually. This indicated that the larger pores of mudstone are compressed and transformed into smaller pores, then the number of macropores decreased and the number of micro- and meso-pores increased. For a certain loading-unloading cycle, the porosity curve of mudstone in the loading process is not coincide with that in the unloading process, the porosity curve in the loading process was located below that in the unloading process, which indicated that the pore structure change is stress path dependent. With the increase of cycle numbers, the total porosity shown an increasing trend, indicating that the damage of mudstone occurred under the cyclic stress load-unload effects. With the increase of porosity, the breakthrough pressure of mudstone decreased with the increase of the cyclic numbers, which may increase the gas leakage risk. The results can provide significant implication for the underground gas storage security evaluation.

Key wordsunderground gas storage    pore structure    nuclear magnetic resonance    cyclic loading-unloading    breakthrough pressure
收稿日期: 2022-01-18      出版日期: 2023-12-12
Corresponding Author(s): Junping ZHOU   
 引用本文:   
. [J]. Frontiers of Earth Science, 2023, 17(3): 691-700.
Junchang SUN, Zhiqiang DONG, Sinan ZHU, Shifeng TIAN, Junping ZHOU. Pore structure evolution of mudstone caprock under cyclic load-unload and its influence on breakthrough pressure. Front. Earth Sci., 2023, 17(3): 691-700.
 链接本文:  
https://academic.hep.com.cn/fesci/CN/10.1007/s11707-022-1019-9
https://academic.hep.com.cn/fesci/CN/Y2023/V17/I3/691
Core sampleThe X-ray diffraction analysisInitial porosity and permeability
Quartz/%Plagioclase/%Calcite/%Clay minerals/%Others/%Porosity/%Permeability/10?3 μm2
Mudstone33.216.20.937.212.50.780.00240
Tab.1  
Fig.1  
Fig.2  
Fig.3  
Fig.4  
Fig.5  
Confining stress1st10th20th30th40th50th
loadunloadloadunloadloadunloadloadunloadloadunloadloadunload
2 MPaMicropore/%4.644.384.294.304.564.604.404.374.384.344.314.20
Mesopore/%94.0393.2793.9294.4094.0093.6593.8793.9994.3594.3094.4794.43
Macropore/%1.332.351.791.301.441.741.731.641.271.361.221.36
Porosity/%0.450.440.550.480.550.590.590.690.60.640.680.71
10 MPaMicropore/%4.474.584.394.364.374.364.304.376.464.284.424.23
Mesopore/%93.6693.9894.0594.2794.0394.3894.2394.2394.0392.2093.8694.33
Macropore/%1.861.441.561.371.601.261.471.601.351.871.251.30
Porosity/%0.430.450.510.590.540.610.580.620.620.740.650.79
18 MPaMicropore/%4.454.274.224.304.234.384.454.274.224.304.234.38
Mesopore/%94.6294.7794.9294.8594.2493.6094.6294.7794.9294.8594.2493.60
Macropore/%0.930.960.870.851.532.020.930.960.870.851.532.02
Porosity/%0.470.470.540.540.550.550.560.560.630.630.660.66
Tab.2  
Fig.6  
Fig.7  
Fig.8  
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