PSI - Issue 37
Fekete, Tamás et al. / Procedia Structural Integrity 37 (2022) 779–787 Fekete, T.: The Fundaments of Structural Integrity … / Structural Integrity Procedia 00 (2021) 000 – 000
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7
a framework theory addressing methodological issues of SI problems to LSPSs that will provide a coherent and comprehensive description of ageing and fracture phenomena. In the next, the fundamental relationships of such a thermodynamics-based model will be outlined in a nutshell. 3.3. Sketch of a thermodynamics-based model for Structural Integrity Calculations of Large-Scale Pressure Systems As shown above, modern thermodynamics is a sound scientific umbrella theory for the methodology of SICs for LSPSs . To construct methodology from the general theory for specific engineering problems, the key engineering problems must be identified, and then a problem-specific, yet general, theoretical model tailored to the problem area must be constructed. A cornerstone in SI of LSPSs is the identification of a basic model able to describe ageing and fracture mechanics simultaneously. In 1921, Griffith published the foundations of linear elastic fracture mechanics – Griffith (1921) – , using a global energy balance approach. About 90 years later, Chen developed a thermodynamics based version of Griffith's method, which: (1) considers processes in energy picture, (2) starts from global energy balance and the global form of the 2 nd law of thermodynamics, resulting in a nonlinear field theory of fracture mechanics allowing to address strongly coupled multi-field problems, including bulk dissipation – see Chen and Mai (2013) – . Below, along the lines of the general theory, an outline of a theoretical model is illustrated that seems promising for solving coupled thermo-visco-elastoplastic problems. The underlying theoretical framework used in development of the model is a form of the Thermomechanics with Internal Variables ( TIV ). Given a solid body, its deformation in the ambient space is described by the mapping ( ) ( ) , t t = x χ X , x denoting the positions in Euler and X in Lagrange coordinates, denotes the gradient in Euler, X in Lagrange picture. 1 2 = − E C I is the Green-Lagrangian strain tensor. t d = A A is Lagrange time derivative of a field, t d = v u means velocity. 1 t t T j − − = Σ F σ F is the second Piola-Kirchhoff stress tensor. Following the line of thought of Chen and Mai (2013), the governing equations – i.e., the balances and the constitutive laws – of the model are as follows: = − u x X is the displacement vector, = X F χ is deformation gradient, j =det( F ), T = C F F is right Cauchy-Green tensor, ( )
t t
0
balanceof mass
d dV
=
t
V
V
balanceof linear momentum
d dV v
σ n
f
dA
dV
=
+
t
ext
V
V
t
t
(
)
(
)
(
)
V
balanceof angular momentum
dV = r v r σ n
r f
d
dA
dV
+
t
ext
V
V
t
t
t
st energy balance equation (1 law of thermodynamics)
(
)
(
)
(
)
(
)
: σ v
dV = − + + j σ f
v
d E E +
E dV
dV
dV
+
+
t
kin
H th
X q
X
ext
X
V
V
V
V
t
t
t
t
nd dissipation requirement (2 law of thermodynamics)
(
)
(
)
(
)
(
)
V
(4)
j
T dA j n
j
T d s dV
T dV sd T dV
= − −
− −
+
t i
q
s
s
X
t
V
V
V
t
t
t
t
(
)
1
0
: Σ C t
v v
−
dV j +
d dV d E E d − + V
+
1 2
t
t
kin
H
V
V
V
t
t
t
with:
(
)
; , , E K A E = = kin j
the kinetic energy density
i v α X C
(
)
, , T T A X i
, , ,
the Helmholtz free energydensity the thermal energy density
α X
H
j
E T s =
th
and the constitutive relations: 2 , , t s = = Σ
(
)
,
g
G
K dV +
0 = −
= −
0
C
α
T
i
j
A
i
j
V
t
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