Responses of multi-scale microstructures, physical-mechanical and hydraulic characteristics of roof rocks caused by the supercritical CO2-water-rock reaction

被引:78
作者
Niu, Qinghe [1 ]
Wang, Qizhi [2 ]
Wang, Wei [1 ,3 ,4 ]
Chang, Jiangfang [1 ,4 ]
Chen, Mingyi [3 ,4 ]
Wang, Haichao [5 ]
Cai, Nian [6 ]
Fan, Li [7 ]
机构
[1] Shijiazhuang Tiedao Univ, State Key Lab Mech Behav & Syst Safety Traff Engn, Shijiazhuang 050043, Hebei, Peoples R China
[2] Hebei Univ Sci & Technol, Sch Civil Engn, Shijiazhuang 050018, Hebei, Peoples R China
[3] Shijiazhuang Tiedao Univ, Minist Educ, Key Lab Roads & Railway Engn Safety Control, Shijiazhuang 050043, Hebei, Peoples R China
[4] Hebei Technol & Innovat Ctr Safe & Efficient Mini, Shijiazhuang 050043, Hebei, Peoples R China
[5] Xinjiang Univ, Cent Asian Orogen Belt, Xinjiang Key Lab Geodynam Proc & Metallogen Progn, Urumqi 830047, Xinjiang, Peoples R China
[6] Fujian Coll Water Conservancy & Elect Power, Dept Hydraul Engn, Yongan 366000, Peoples R China
[7] 2 Inst Geol Mineral Resources Survey Henan, Zhengzhou 450000, Peoples R China
关键词
Geochemical reaction; Pore volume; P-wave velocity; Energy transformation; Mechanical property; Permeability; PORE STRUCTURE CHARACTERIZATION; NUCLEAR-MAGNETIC-RESONANCE; COALBED METHANE RECOVERY; CO2; SEQUESTRATION; CLOSED PORES; ADSORPTION; PERMEABILITY; INJECTION; RESERVOIR; BEHAVIOR;
D O I
10.1016/j.energy.2021.121727
中图分类号
O414.1 [热力学];
学科分类号
摘要
The integrality of caprock decides the safety of CO2 enhanced coalbed methane recovery (CO2-ECBM), the inferior caprock may reduce the seal performance and induce gas leakage. However, the attribute of caprock can be modified through the supercritical CO2 (ScCO2)-water-rock reaction. To clarify the responses of multi-scale microstructures, physical-mechanical and hydraulic characteristics of caprock after the geochemical reaction, the rock samples of coal seam roof from Qinshui Basin was first collected to simulate geochemical reactions between ScCO2, water, and caprock, then the scanning electron microscope (SEM), low-temperature liquid nitrogen adsorption (LTLNA), mercury intrusion porosimetry (MIP), P-wave velocity, mechanical and permeability tests were conducted. Results show that the ScCO2-water-rock reaction promotes the formation of dissolution caves, which makes the surface rough and uneven and affects the pore distribution through enlarging the volume of transition pores, mesopores, and macropores and reducing the volume of micropores. The P-wave velocity of the sample is decreased nonlinearly with the increasing ScCO2-water-rock reaction time because of the pore structure damage induced by the chemical dissolution effect. The strain energy evolution is also influenced by the ScCO2-water-rock reaction, the long-time geochemical reaction promotes more elastic energy transform to dissipative energy. The peak strength, elastic modulus and Possion's ratio change regularly with increasing reaction time while the failure pattern is independent of the ScCO2-water-rock reaction. The varieties of mechanical parameters can be ascribed to the considerable increase of macropores and can be predicted by the logistic function. The ScCO2-water-rock reaction has not changed the primary permeability while it largely enhances the permeability peak and elevates the infiltration ability of the loaded rock sample. The main leakage form in the study area is the diffusive loss and the CO2-ECBM recovery is relatively safe, however, the CO2 leakage may be exacerbated if the ScCO2-water-rock geochemical reaction is coupled with the local stress concentration or connected with the pre-existing fractures in the roof rocks. This study deepens the understanding of the consequences of ScCO2-wa-ter-rock reaction on caprock and provides some help for the site selection and the preliminary safety evaluation of CO2-ECBM. (C) 2021 Elsevier Ltd. All rights reserved.
引用
收藏
页数:16
相关论文
共 58 条
[31]   The evolution and formation mechanisms of closed pores in coal [J].
Niu, Qinghe ;
Pan, Jienan ;
Cao, Liwen ;
Ji, Zhongmin ;
Wang, Haichao ;
Wang, Kai ;
Wang, Zhenzhi .
FUEL, 2017, 200 :555-563
[32]   The closed pores of tectonically deformed coal studied by small-angle X-ray scattering and liquid nitrogen adsorption [J].
Pan, Jienan ;
Niu, Qinghe ;
Wang, Kai ;
Shi, Xinghua ;
Li, Meng .
MICROPOROUS AND MESOPOROUS MATERIALS, 2016, 224 :245-252
[33]   CO2 storage in coal to enhance coalbed methane recovery: a review of field experiments in China [J].
Pan, Zhejun ;
Ye, Jianping ;
Zhou, Fubao ;
Tan, Yuling ;
Connell, Luke D. ;
Fan, Jingjing .
INTERNATIONAL GEOLOGY REVIEW, 2018, 60 (5-6) :754-776
[34]   KINETICS OF CALCITE DISSOLUTION IN CO2-WATER SYSTEMS AT 5-DEGREES-C TO 60-DEGREES-C AND 0.0 TO 1.0 ATM CO2 [J].
PLUMMER, LN ;
WIGLEY, TML ;
PARKHURST, DL .
AMERICAN JOURNAL OF SCIENCE, 1978, 278 (02) :179-216
[35]   An experimental investigation of applicability of CO2 enhanced coal bed methane recovery to low rank coal [J].
Ranathunga, A. S. ;
Perera, M. S. A. ;
Ranjith, P. G. ;
Wei, C. H. .
FUEL, 2017, 189 :391-399
[36]   A macro-scale experimental study of sub- and super-critical CO2 flow behaviour in Victorian brown coal [J].
Ranathunga, A. S. ;
Perera, M. S. A. ;
Ranjith, P. G. ;
Ju, Y. ;
Vishal, V. ;
De Silva, N. K. .
FUEL, 2015, 158 :864-873
[37]   CO2-induced mechanical behaviour of Hawkesbury sandstone in the Gosford basin: An experimental study [J].
Rathnaweera, T. D. ;
Ranjith, P. G. ;
Perera, M. S. A. ;
Haque, A. ;
Lashin, A. ;
Al Arifi, N. ;
Chandrasekharam, D. ;
Yang, S. Q. ;
Xu, T. ;
Wanh, S. H. ;
Yasar, E. .
MATERIALS SCIENCE AND ENGINEERING A-STRUCTURAL MATERIALS PROPERTIES MICROSTRUCTURE AND PROCESSING, 2015, 641 :123-137
[38]   A novel experimental system for the exploration of CO2-water-rock interactions under conditions relevant to CO2 geological storage [J].
Rendel, Pedro M. ;
Wolff-Boenisch, Domenik ;
Gavrieli, Ittai ;
Ganor, Jiwchar .
CHEMICAL ENGINEERING JOURNAL, 2018, 334 :1206-1213
[39]  
Shi Yunqing, 2017, Natural Gas Industry, V37, P62, DOI [10.1016/j.ngib.2017.08.013, 10.3787/j.issn.1000-0976.2017.03.008]
[40]   Experimental study on water-rock interactions during CO2 flooding in the Tensleep Formation, Wyoming, USA [J].
Shiraki, R ;
Dunn, TL .
APPLIED GEOCHEMISTRY, 2000, 15 (03) :265-279