天然岩石裂隙面粗糙度尺寸效应及方向性研究
梅倩玮,陈刚,罗凤强,马玲,龚红胜,龙妍竹

Research on Size Effect and Directionality of Roughness of Natural Rock Fracture Surface
Qianwei MEI,Gang CHEN,Fengqiang LUO,Ling MA,Hongsheng GONG,Yanzhu LONG
表1 水力隙宽和机械隙宽的代表性经验关系式
Table 1 Representative empirical relationship formulas between hydraulic gap width and mechanical gap width
公式注释文献来源
bh2=bm2CC=1+m?2bm1.5m=17bm为不连续表面粗糙度的量级,m为一个系数刘日成等,2014
bh2=bm2CC=1+m?2bm1.5m=8.8Louis,1969
bh2=bm2CC=1+m?2bm1.5m=20.5刘日成等,2014
bh=bm1-0.9exp-0.56bmσE13σE为机械孔径上不同孔径的标准偏差Patir,1978
bh3=bm31-C1+C在Zimmerman et al.(1996)的研究中C = 0.25 (1992)Walsh,1981
bh=bmJRC2.5bh2=bmC,C=JRC5e2Barton et al.,1978
bh2=bm2CC=1.1~1.7bm = 100~500 μmHakami et al.,1995
bh=bm1+σE2bm2-12Renshaw et al.,1995
bh3bm31-1.5σapert2bm2+...1-2cC为接触比Zimmerman et al.,1996
bh=bmbm/τ1/3<bm>为真实孔隙的调和平均值,τ为曲折度Waite et al.,1999
bh3=bm31-1.131+0.1912bm/σapert1.93σapert为平均机械孔隙的标准偏差Matsuki et al.,1999
bh=bm2JRC2.5us0.75uspJRCmobJRC的变值,us是不超过峰值usp剪切位移的75%Olsson et al.,2001
bh=bm1/2JRCmobususp
bh3=bm31-1.0σapertbm1-σapertbmσslope10Reσslope是断裂面局部斜率的标准偏差Xiong et al.,2011

bh=bm1-0.03dmc-0.565JRCa13

bh=bm1-2.25σEbm13

dmc 是最小闭合距离,而 JRCa 是上、下2个面平均结合粗糙系数Rasouli et al.,2011

bh=bm1+Z22.25Re<1

bh=bm1+Z22.25+(0.00006+0.004)Z22.25(Re-1)Re≥1

Z2是水头的第一偏差的均方根Li et al.,2008
bh3=bm30.94-5.0σs2bm2σs是剪切过程中机械孔隙的标准偏差Xie et al.,2015
bh2=bm2CC=1+m?2bm0.61912m=0.6138张戈等,2019