Issue 44
X.-P. Zhou et alii, Frattura ed Integrità Strutturale, 44 (2018) 64-81; DOI: 10.3221/IGF-ESIS.44.06
C C 22 2
1
3
C
3
2
C
2
22
C C
C C
2
11
11 21
3
(30)
2
cl
c
c
csc
t
t
2
0
0
csc
2 2
2 2 2 2
+1
2
cl
sin cos
c
sin
cl
t
cl
0
From Eq. (30), micromechanics-based three-dimensional long-term strength criterion of rocks expressed by long-term uniaxial compressive strength of rocks can written as A A A A A 4 3 2 1 1 3 2 1 3 3 1 3 4 1 3 5 0 (31)
where
2
C C C 11 21 22
A C C C C A C C C A C C C C C C C C A C C C C A C C C C C C C C 1 11 4 11 21 2 2 11 22 4 2 3 11 3 4 11 21 4 11 3 4 22 4 11 3 3 11 21 3 4 11 3 4 4 4 2 2 4 2 5
2
22
2
4
2 ( sin
1)si
n
2
2
2
2
2
2
2 +2 c
+1 +2
sin cos
sin
cos
2
3
2
2
2
2
2
2
sin cos
C c
cos
sin
3
2
3
2 3
2
cl
c
c
csc
t
t
2
0
0
C
csc
4
2 2
2 2 2 2
+1
2
cl
sin cos
c
sin
cl
t
cl
0
It is observed from Eq. (31) that
is related to the friction coefficient , the coefficient of mixed-mode
1 3
fracture criterion, the long-term uniaxial compressive strength cl
, the short-term uniaxial tensile strength t
, the time
iu f t 0 ( ) , the dip angle of penny-shaped microcracks θ and Poisson’s ratio .
factor
Assumed that
C C 11 21
2
0 ,
,
cl 2
m n
C s 22
cl m n 2
C s
3
3
3
Eq.(31) can be simplified to:
s m n 3 1 3 2 cl
2
2
(32)
s
s
s
m n
0
cl
cl
cl
3 1 3
2
3
where s n , and m are the strength parameters which are determined by experiments.
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