鄂尔多斯盆地长7段页岩强度与变形尺度效应规律试验研究

Experimental study on the scale effect of strength and deformation of Chang 7 shale in Ordos Basin

  • 摘要: 页岩层理结构发育,非均质性极强,其强度与变形特征存在显著的尺度效应现象,致使室内小尺度岩样测试结果在表征矿场大尺度页岩岩体力学性质时存在局限性。为探究页岩强度与变形的尺度效应规律,以鄂尔多斯盆地延长组长7段陆相页岩露头为研究对象,采用RTR-1000岩石三轴测试系统对11块高径比为2,直径为17,20,25和38 mm等4类岩样尺度进行单轴压缩试验,分析页岩强度与变形的尺度效应规律及其内在机理,在此基础上,提出一种新的适用于页岩的强度尺度效应模型,并初步得到室内岩样在表征页岩矿场岩体时的合理测试尺度。结果表明:绝大多数描述页岩强度与变形的力学参数存在显著的尺度效应现象,其中弹性模量和泊松比随岩样尺度增大而增大,峰值强度、峰值应变、残余应变、残余应力和破裂时间等随岩样尺度增大而减小;不同尺度的页岩在弹性变形向脆性破坏转变时均是瞬态的,不存在明显的塑性屈服段,且破裂前均为线弹性变形,破坏后均为拉伸-剪切破坏,但剪切角较小,均在10°以内;页岩强度与变形参数的尺度效应现象是由岩样的加载方向、层理面方向、层理面力学性质和微观缺陷不均匀分布等共同造成的;基于Griffith微裂纹强度理论模型得到新的适用于页岩的强度尺度效应模型,该模型与试验结果吻合度较好,能准确预测不同尺度的页岩岩样强度;不同矿场页岩岩体力学参数所对应的合理的室内试验岩样尺度不同,当岩样高径比为2,长度超过160 mm时,室内测得的岩样力学参数经现场校正后均可表征矿场岩体力学参数;页岩强度与变形的尺度效应规律可以用于预测储层钻井时的破裂压力,井壁变形特征以及压裂时的起裂和稳定扩展压力,在当前体积压裂施工中,扩大沿层理方向的分支缝压裂规模或对于大而厚、沿层理方向微缺陷极为发育的页岩储层,可以考虑进行直井的分段多簇压裂以充分释放层理面有利于压裂裂缝扩展的力学优势,从而提高页岩气井产量。

     

    Abstract: Shale has an obvious bedding structure and strong heterogeneity,and its strength and deformation characteristics have a significant scale effect,which makes the test results of small-scale rock samples in the laboratory to be limited in characterizing the mechanical properties of large-scale shale rock mass in the mine.In order to explore the scale effect law of shale strength and deformation,taking the continental shale outcrop of Yanchang Formation 7 in Ordos Basin as the research object,the triaxial compression tests of 11 rock samples with height diameter ratio of 2,diameter of 17,20,25 and 38 mm were carried out with RTR-1000 rock triaxial testing system.Based on the analysis of the scale effect law and its internal mechanism of shale strength and deformation,a new scale effect model for shale strength was proposed,and the reasonable test scale of indoor rock sample in characterizing shale field was preliminarily obtained.The results show that most of the mechanical parameters describing the strength and deformation of shale have significant scale effect,and the elastic modulus and Poisson’s ratio increase with the increase of rock sample size,and the peak strength,peak strain,residual strain,residual stress and fracture time decrease with the increase of rock sample size.Shale with different scales changes instantaneously from elastic deformation to brittle failure,and there is no obvious plastic yield section.Before failure,the deformation of shale is linear elastic deformation,and after fracture,it is tensile shear failure,but the shear angle is small,and it is within 10 degrees.The scale effect of shale strength and deformation parameters is caused by loading direction,bedding plane direction,mechanical properties of bedding plane and uneven distribution of micro defects.Based on Griffith micro-crack strength theory model,a new strength scale effect model for shale was obtained.The model is in good agreement with the test results and can accurately predict the strength of shale samples with different scales.Different mechanical parameters of shale rock mass correspond to different sizes of reasonable laboratory test rock samples,and when the height diameter ratio of rock sample is 2 and the length is more than 160 mm,the mechanical parameters of rock sample measured in the laboratory can be used to characterize the mechanical parameters of rock mass in the mine after field correction.The scale effect law of shale strength and deformation can be used to predict the fracture pressure,the deformation characteristics of wellbore during well drilling and the initiation and stable expansion pressure during fracturing.In the current volume fracturing operation,it is very beneficial to expand the fracturing scale of branch fractures along the bedding direction or for the large and thick shale reservoirs with extremely developed micro defects along the bedding direction,it can be considered to conduct the multi-cluster fracturing of vertical wells to fully release the mechanical advantages of the bedding surface conducive to fracture expansion,so as to improve the productivity of shale gas wells.

     

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