超临界CO_2/清水压裂煤体起裂和裂缝扩展试验研究
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  • 英文篇名:Experimental study on fracture initiation and growth in coal using hydraulic fracturing with supercritical CO_2 and normal water
  • 作者:王磊 ; 梁卫国
  • 英文作者:WANG Lei;LIANG Weiguo;Institute of Mining Technology,Taiyuan University of Technology;Key Laboratory of In-situ Property-improving Mining of Ministry of Education,Taiyuan University of Technology;
  • 关键词:岩石力学 ; 超临界CO2压裂 ; 清水压裂 ; 起裂 ; 裂缝扩展 ; 裂缝宽度
  • 英文关键词:rock mechanics;;supercritical CO2 fracturing;;water fracturing;;initiation;;fracture growth;;fracture width
  • 中文刊名:YSLX
  • 英文刊名:Chinese Journal of Rock Mechanics and Engineering
  • 机构:太原理工大学矿业工程学院;太原理工大学原位改性采矿教育部重点实验室;
  • 出版日期:2019-04-15
  • 出版单位:岩石力学与工程学报
  • 年:2019
  • 期:v.38;No.360
  • 语种:中文;
  • 页:YSLX2019S1009
  • 页数:10
  • CN:S1
  • ISSN:42-1397/O3
  • 分类号:95-104
摘要
为了探究超临界CO_2与清水压裂煤体的压裂效果,运用TCHFSM–I型大尺寸真三轴压裂渗流装置,对尺寸为100 mm×100 mm×100 mm煤试样施加三轴压力来模拟煤系地层压裂过程,结合压裂理论基础和试验数据,对比分析了压力–时间曲线、表面裂缝形态及裂缝宽度,结果表明:相比于清水压裂,相同的3种三轴压力条件下,超临界CO_2压裂更容易起裂,起裂压力分别减小了28.3%,28.0%,27.4%,且随着约束压力的增大,减少比例逐渐减小;超临界CO_2压裂能够生成明显的层理裂缝及分叉裂缝,其数量越多主裂缝扩展范围越小;压裂过程中超临界CO_2易渗透到煤样内部的层理裂隙及微孔裂隙内导致压力变化迟缓,而且试样破裂后压力不易保持,裂缝宽度较狭窄;清水压裂的裂缝宽度集中分布于0.450~0.650 mm和>1.250 mm区间,而超临界CO_2的裂缝宽度集中分布于0.050~0.250 mm区间,两者相差3~6倍,对于局部分叉裂缝及层理裂缝,甚至相差2个数量级左右。
        In order to investigate the fracturing characteristics of coal in hydraulic fracturing with supercritical CO_2and water,the TCHFSM–I large-size true triaxial fracturing seepage device was used to simulate the process of fracturing coal seam by applying triaxial stress to 100 mm×100 mm×100 mm coal samples.Based on the theoretical basis of fracturing and experimental data,the pressure-time curves,surface fractures morphology and fractures width were compared and analyzed.The results showed that,compared to water fracturing,under the same three kinds of triaxial stress conditions,supercritical CO_2 initiated the fractures more easily.The initiation pressure decreased by 28.3%,28.0%and 27.4%,respectively,and the reduction gradually decreased with confining pressure increasing.Supercritical CO_2 fracturing could generate obvious bedding plane fractures and bifurcation fractures,and the more those fractures were generated,the smaller the growth range of main fractures was.The supercritical CO_2 penetrated easily into the original bedding plane fissures and micro-fissures or pores in coal during the fracturing process,which caused the pressure to change gradually.Moreover,the fractured coal with supercritical CO_2 could not easily maintain the pressure,so that the fractures width was narrow.The fractures width of water fracturing was mainly distributed in the interval of 0.450–0.650 mm and>1.250 mm,while the fractures width of supercritical CO_2 was concentrated in the interval of 0.050–0.250 mm.The gap between the two kinds of fractures width was approximately 3–6 times,and for some local bifurcation and bedding plane fractures,even reaching about 2 orders of magnitude.
引文
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