Issue 53
Y.D. Shou et alii, Frattura ed Integrità Strutturale, 53 (2020) 434-445; DOI: 10.3221/IGF-ESIS.53.34
damage variable d and the cumulative inverse strain
p . The total strain are divided into two parts, namely the elastic
strain
e and the plastic strain p .
and
(1)
e
p
e p d d d = +
= +
where d is the incremental total strain, e d is the incremental plastic strain. As stated by Shao et al. [9], the damage process is coupled with plastic deformation and plastic hardening. Therefore, the thermodynamic potential can be expressed as e d is the incremental elastic strain
1
(
)
(
)
p
p
(2)
= −
− +
( , ) d
: ( ) : C d
p p
2
where ( ) C d is the fourth-order elastic stiffness tensor of the damaged coal-rock and
( , ) p p d is the closed plastic
potential of the damaged coal-rock related to plastic hardening. Then, the equation of state can be obtained by deriving the elastic strain
e from the thermodynamic potential as [9]
e = =
(
)
p
(3)
−
C d
( ) :
According to works by Nemat-Nasser and Hori [26], the fourth-order elastic stiffness tensor can be expressed as
(4)
( ) 3 ( ) 2 ( ) C d k d J d K = +
where ( ) k d is the bulk modulus of damaged materials and
( ) d is shear modulus of damaged materials. The other two
symmetric four-order tensors J and K are
1 3
= and K I J = −
(5)
J
where is the two-order unit tensor, I is the symmetric four-order unit tensors. The thermal forces related to the damage variable is expressed as [9]
( , ) d
1 = − = − −
C d
( )
(
)
(
)
p p
(6)
p
p
− −
Y
:
:
d
d
2
d
d
According to the non-negativity of the internal energy dissipation, the following expression can be obtained [9]
(7)
p
: d Y d +
0
where is the stress tensor of coal-rock,
p is the derivation of
p to time t and d is the derivation of d to time t .
Then, the derivative form of the constitutive equation of coal-rock can be obtained as [9]
C d
( )
e
e
=
+
C d
( ) :
:
d
d
(8)
C d
( )
p
p
=
) − +
−
C d
( ) : (
: (
)
d
d
where is the derivation of to time t .
439
Made with FlippingBook Publishing Software