Issue 44
X.-P. Zhou et alii, Frattura ed Integrità Strutturale, 44 (2018) 64-81; DOI: 10.3221/IGF-ESIS.44.06
/ 3 , q J 2
p I 1
Similarly, Micromechanics-based three-dimensional long-term strength criterion (33) can be rewritten in another form:
(37)
3
2
2
2
F f
q f pq f q
pq f p f q f p
f
0
1
2
3
4
5
6
7
where
f f f f f 1 2 3 4 5 3 4 1 3
4 cos
3 2
2
3 2 cos n
m n
sin
2
m n
cos
f
(0)
n m n
2 3 m m n n m mn n n 3 6 2 2 6 2 2 2
iu
3 2 2
c
s
cos 2
sin 2
iu f t
0 ( )
f
(0
)
2 3
m n s
3 2
.
iu
m n
c
n
3
2
cos
si
n
iu f t
0 ( )
f
(0
)
2
iu
c
m n s
iu f t (
)
0
f
0 ) ( ) (0
1
3 2
2
2
iu
3 4 cos n
m n
c
f
s
si
n
6
iu f t
f 7 3
f
(0)
s m n
2
2
iu
c
iu f t (
)
0
C OMPARISON WITH THE EXPERIMENTAL DATA OF COAL
S
eries of triaxial compressive experimental data were obtained from creep tests on various rocks by Refs [25-27]. The long-term uniaxial compressive strength of rocks and the fitting strength parameters are listed in Tab. 1. Tabs. 2-4 show theoretical strength and the experimental data of Barre granite, Inada granite and Jinping marble. Figs 5-7 show that comparison of predicted strength and the experimental data of Barre granite, Inada granite and Jinping marble. It is found from Tabs 2-4 and Figs 5-7 that the proposed long-term strength criterion agrees well with experimental data of different rocks.
The fitting strength parameter (n)
The fitting strength parameter(m)
Long-term uniaxial compressive strength
The strength parameter(s)
Rocks
Reference
1 1 1
Kranz [25]
Barre granite Inada granite Jinping marble
6.709 1.000
0.737 0.101
158 216
Maranini and Brignoli [26]
Yang et al. [27]
12.184
18.566
80
Table 1 : The fitting strength parameters and uniaxial compressive strength of different rocks.
76
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