Bearing capacity of a cohesive-frictional soil under non-eccentric inclined loading
Cohesive fracture growth in a thermoelastic bimaterial medium
Transcript of Cohesive fracture growth in a thermoelastic bimaterial medium
Computers and Structures 82 (2004) 1875–1887
www.elsevier.com/locate/compstruc
Cohesive fracture growth in a thermoelastic bimaterial medium
S. Secchi a, L. Simoni b,*, B.A. Schrefler b
a CNR, Ladseb, Padova, Italyb Department of Structural and Transportation Engineering, University of Padova, Via F. Marzolo, 9, Padova 35131, Italy
Received 12 December 2002; accepted 24 March 2004
Available online 28 July 2004
Abstract
The paper presents a fully-coupled numerical model for the analysis of fracture initiation and propagation in a two
dimensional non-homogeneous elastic medium driven by mechanical loads and transient thermal fields. Cohesive crack
behaviour is assumed for the solid. The solution of the coupled problem is obtained by using the finite element method
without using special approximation techniques nor interface elements. Evolution of the process zone results in contin-
uous changes of the domain topology. This is accounted for by updating the boundary geometry and successive remesh-
ing of the domain. Optimality of the shape of the finite elements generated is controlled and the mesh density is adjusted
adaptively on the basis of an error estimator. Two numerical applications are presented, which demonstrate the effec-
tiveness of the proposed procedure. In the first, comparison is made with a laboratory experiment, whereas the second
handles a problem with crack path completely unknown.
� 2004 Civil-Comp Ltd. and Elsevier Ltd. All rights reserved.
Keywords: Discrete crack models; Cohesive fracture; Thermal loads; Adaptive remeshing; Bimaterial sample; PMMA
1. Introduction
Many engineering structures experience thermal
loads during their life, i.e., imposed temperature along
the boundaries and/or heat production within their inte-
rior. Whereas the former situation is the consequence of
changes in the environment, the latter can be attributed
to different causes for instance to chemical reactions, as
in the hydration of cement for concrete structures, or to
internal transformation of mechanical work. For the lat-
ter case, we refer for instance to the significant tempera-
ture increase which has been observed at the tip of a
stationary crack subjected to dynamic loading [1].
0045-7949/$ - see front matter � 2004 Civil-Comp Ltd. and Elsevier
doi:10.1016/j.compstruc.2004.03.059
* Corresponding author.
E-mail address: [email protected] (L. Simoni).
The applied thermal loads may result in fracture enu-
cleation and growth, for instance due to the presence of
flaws along the boundary and/or within the domain and/
or simply due to the attainment of the tensile strength
for brittle materials. While on one hand, temperature
rise near a crack tip significantly affects the micromech-
anisms of fracture [2], on the other, the formation and
propagation of fractures involve changes in the bound-
ary and related conditions. For example, the spalling
of concrete during a tunnel fire suddenly exposes parts,
previously insulated by the broken off chips of concrete,
to very high temperatures. Similar problems arise in de-
lamination of composites and with expanding insulation
varnishes. All these problems exhibit a strong coupling
between mechanical and thermal effects. The thermal
field is further characterized by its variation in space
and time, hence numerical models assuming steady state
Ltd. All rights reserved.
1876 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
conditions for temperature distribution suffer of strong
limitations in simulating the real physical phenomena.
Models of this type have been presented recently, e.g.,
[3–5] using boundary element method in a two and three
dimensional context, both for elastic and elastoplastic
materials. These models are further characterized by
fixed fracture configuration and are usually intended
for the calculation of the stress field and stress intensity
factors.
In the present approach the problem of fracture for-
mation and propagation is formulated within the frame
of cohesive fracture, which is very realistic for geoma-
terials, but is also widely applied to metallic materials
[6]. The medium is assumed as non-homogeneous and
the fracture(s) can enucleate and propagate according
to the maximum tensile stress criterion. At the same
time, the temperature field can evolve in space and time
according to energy balance equation, where heat
source terms and the effect of mechanical coupling
are accounted for. Internal heat production can depend
on thermoelastic effects, plastic work and friction be-
tween the fracture lips. The governing equations are
stated by using the phenomenological approach [7]
and the numerical solution for the mechanical problem
is limited to a 2-D context. Governing equations are
discretized in space by the finite element method and
in time by finite differences and monolithic solution
procedures are used. No special approximations are
used, for instance as in [3], to represent the field singu-
larities: bilinear interpolations are assumed for both
field variables and the solution is controlled and im-
proved by using an efficient error measure [8] with an
a posteriori refinement technique. Spatial discretization
is continuously updated as the phenomenon evolves
and the domain of definition changes. An efficient mesh
generator [9] is used to this scope. This technique, to-
gether with the assumption of non-homogeneous mate-
rial, differentiates the present approach from the one
used in [10]. As a result, the proposed model does
not suffer from the limits of those previously referred
to and the initial mesh can also be defined without spe-
cial care. In particular, cracks may enucleate every-
where depending only on the stress field and
propagate along paths and with a velocity of the tip
that is unknown a priori. The determination of the
crack path and the velocity of the tip propagation rep-
resent an important part of the solution, as the temper-
ature and stress fields and allows for correct updating
of the domain, boundaries and related conditions.
2. Field equations
Governing equations are obtained within the frame-
work of the phenomenological theory [7]. Small dis-
placements and displacement gradients are assumed.
2.1. Local balance equations
The local linear momentum balance at the generic
point of the domain X reads as
rji;j þ qgi ¼ q€ui in X; ð1Þ
where rij is the stress tensor, q the density of the mate-
rial, gi the gravity acceleration vector and ui the displace-
ment vector. Dots represent time derivatives. The
natural boundary conditions are
rjinj ¼ pi on C and rjinj ¼ ci on C0: ð2Þ
C is the external boundary and pi the forced traction, C0
the boundary of the process zone and ci the cohesive
force. Forced conditions represent fixed displacement
along the constrained boundary and completely define
the problem.
The local form of energy balance equation (first law
of thermodynamics), under the assumption of small
strains requires that
q _e ¼ rij _eij þ qr � qj;j in X; ð3Þ
where e is the specific internal energy, eij is the infinites-
imal strain tensor, r is the strength per unit mass of a
distributed internal heat source and qj the heat flux vec-
tor. Forced conditions fix the temperature along the
boundary, whereas natural conditions represent the im-
posed heat flux. The latter include also the convective
heat transfer towards the surrounding. Both the fluxes
will be defined by means of suitable constitutive mod-
els.
The topology of the domain X and boundary
change with the evolution of the fracture phenomenon.
In particular, the fracture path, the position of the
process zone and the cohesive forces are unknown
and must be determined during the analysis. After def-
inition of the constitutive models, the governing Eqs.
(1) and (3) are solved simultaneously to obtain the dis-
placement and temperature fields together with the
fracture path.
2.2. Constitutive models
The model must be completed by the constitutive
relations for solid mechanical behaviour, cohesive forces
as function of the crack opening, specific internal energy
and heat flux vectors.
2.2.1. Continuous medium: mechanical behaviour and heat
transfer
In the framework of discrete crack models, a hyper-
elastic material is assumed for the solid away from the
process zone. The stress tensor rij depends on effective
strain according to the relationship
S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887 1877
rij ¼ cijrsðers � drseT Þ; eT ¼ a3T ; ð4Þ
where eij is the total strain, eT the strain associated to
temperature T changes, according to cubic expansion
coefficient a, drs the Kronecker symbol. The elastic coef-
ficients cijrs depend on the strain energy function W and
can be expressed in terms of the Lame constants k and las
cijrs ¼o2Woeijoers
¼ lðdisdjr þ dirdjsÞ þ kdijdrsdij ði; j; r; s ¼ 1; 2; 3Þð5Þ
and depend on strain level and temperature [2,7].
In the case of plane problems , as in the applications
presented, Eq. (5) is condensed in the standard way,
assuming the pertinent conditions for plane stress or
plane strain states.
As a constitutive assumption for heat flux, Fourier�slaw is assumed
qi ¼ �kijT j; ð6Þ
kij being the effective thermal conductivity tensor, which
can be dependent on temperature.
As far as convective flux is concerned, Newton�s lawis used
qconvi ¼ hðT � T1Þ; ð7Þ
being h the convective heat transfer coefficient and T1the temperature in the far field of the undisturbed sur-
roundings.
2.2.2. Cohesive fracture model: mode I crack opening
Let the complete domain be composed of a set of dif-
ferent homogeneous subdomains. Within a generic one
of these, a fracture can initiate or propagate under the
assumption of mode I crack opening, provided that
the tangential relative displacements of the fracture lips
are negligible. In the process zone cohesive forces are
transmitted, which are orthogonal to the fissure sides.
Following the Barenblatt–Dugdale model [11,12] and
cr
σ0
G
0δσ
δσ
σ
(a) (b
Fig. 1. Fracture energy (a) and loading/unloading
Hilleborg et al. proposals [13], the cohesive law is
(Fig. 1)
r ¼ r0 1� drdrcr
� �; ð8Þ
r0 being the maximum cohesive traction (closed crack),
dr the relative displacement normal to the crack, drcr themaximum opening with exchange of cohesive tractions
and G=r0·drcr/2 the fracture energy. Fig. 1 also pre-
sents the unloading/reloading paths represented by
r ¼ r0 1� dr1drcr
� �drdr1
; ð9Þ
where dr1 is the maximum attained opening in the previ-
ous loading process.
The individual homogeneous components differ only
due to different values attributed to the fundamental
parameters defining the mechanical behaviour (Eqs. (8)
and (9)). The aspect of the constitutive relationship re-
mains the same.
2.2.3. Cohesive fracture model: mixed mode crack opening
When tangential relative displacements of the sides of
a fracture in the process zone cannot be disregarded,
mixed mode crack opening takes place. This is usually
the case with a crack moving along an interface separat-
ing two solid components. Whereas the crack path in a
homogeneous medium is governed by the principal
stress direction, the interface has an orientation that is
generally different from the principal stress direction.
The mixed cohesive mechanical model involves the
simultaneous activation of normal and tangential dis-
placement discontinuity with respect to the crack and
corresponding tractions. The interaction between the
two cohesive mechanisms is treated as in Margolin [14]
and Dienes [15], by defining an equivalent or effective
opening displacement d and the scalar effective traction
t as
d ¼ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffib�2d2s þ d2r
q; t ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffib2t2s þ t2r
q: ð10Þ
σ
σ
σ
0
1
2
δσ1 δσ2 δσcr
A
B
0δσ
σ
)
law (b) for each homogeneous component.
1878 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
The resulting cohesive law is
t ¼ td
b2ds þ dr� �
: ð11Þ
b is a suitable material parameter and the cohesive law
takes the same aspect as in Fig. 1, by replacing displace-
ment and traction parameters with the corresponding
effective ones. For the choice of the value of parameter
b the original proposals of [14,15] are referred to, to-
gether with Ref. [10].
2.2.4. Internal energy and sources
In a generic thermodynamic phenomenon, for an
infinitesimal increment of deformation, the specific
internal energy can be assumed as a function of absolute
temperature, a set of observable variables (the displace-
ment field) and internal variables vi [7]. It is assumed for
the following applications that mechanical terms in en-
ergy balance equation are negligible compared with ther-
mal effects. This is not always the case. Sometimes, in
experimental investigations a significant temperature in-
crease has been observed in the zone of crack initiation
and propagation [1]. To account for these situations, dis-
sipation terms related to mechanical effects have to be
introduced in the energy balance equation, following
[16] for instance.
When mechanical terms are neglected, internal en-
ergy depends on temperature only and is related to heat
capacity at constant volume Cv. As a consequence, and
taking into account Eq. (6) for the flux term, the energy
balance equation takes the form
qðCv_T Þ ¼ qr � qj;j: ð12Þ
Volume heat sources of Eq. (12) can represent very dif-
ferent phenomena, e.g., heat production due to hydra-
tion of concrete, heat production due to plastic work
[16], hence sometimes are linked to coupling effects be-
tween stress and thermal fields. Source terms may also
arise along the boundary and represent frictional effects.
The rate at which heat is generated at the contact sur-
faces is
r0 ¼ t � kvk; ð13Þwhere t is the contact traction and ivi is the jump in
velocity across the contact. This effect can be incorpo-
rated in the weak form of the energy balance, which, fol-
lowing the usual approach takes the formZXqðCv
_T ÞhdXþZC0r0hdC0 þ
ZC0qconvhdCþ
ZC0qhdC
¼ZXqdivhdXþ
ZXshdX; ð14Þ
being h an admissible virtual temperature qconv and q the
convective and imposed heat flux normal to the bound-
ary. Except for the convective and boundary fluxes, this
equation is similar to the one used by Camacho and
Ortiz [10].
3. Discretized governing equations
Eqs. (1) and (3) (or (14)) are discretized in space by
the usual Galerkin residual method, incorporating the
constitutive equations at the same time. The values of
nodal displacements d and temperature T are the un-
knowns. This results in the following system (dot repre-
sents time derivative) at element level
KE �TUE
0 TSE
� � _dE_TE
" #þ
0 0
0 TRE
� �dE
TE
� �
¼_FE
0
" #þ
0
TGE
� �; ð15Þ
where adopting the usual symbols [17], the submatrices
of Eq. (15) are
KE ¼ZV E
BTDBdV ; ð15aÞ
TUE ¼ZV E
BTDma3NdV ; ð15bÞ
TSE ¼ZV E
NTqNdV ; ð15cÞ
TRE ¼ZV E
ðrNÞTkrNdV ; ð15dÞ
TGE ¼ZV E
NT sdV �ZCcrack
NT r0 dC�ZCNT qE dC
�ZCNT qconvE dC; ð15eÞ
_FE ¼ZV E
NT _fE dV þZCE
NT _tE dCþZCEcrack
NT _cE dC:
ð15fÞ
In Eq. (15f) �E represents the cohesive traction rate and is
applied along Ccrack of the generic element. In the
present formulation, non-linear terms arise through
cohesive forces in the process zone only. Under the
hypothesis of dropping the effects of stresses in the
energy equation, coupling comes from the boundary
terms defined along Ccrack.
Global equations are assembled and integrated in
time by means of the generalized trapezoidal rule
[17] and Newton–Raphson method is used for the
solution of the non-linear algebraic system of
equations. In a generic step, once the displacement
field is obtained, crack opening is calculated and, by
using Eqs. (10) and (11), cohesive tractions and
length process zone are determined. This is the part
of the crack where cohesive tractions are different
from zero.
S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887 1879
4. Mesh generation and remeshing operations
Initial discretization and successive remeshing are car-
ried out using the procedure for unstructured Delaunay
mesh generation presented in detail in [9]. This algorithm
produces the initial mesh with element dimensions con-
trolled by a spacing function initially defined by the user
and then automatically updated to account for geometri-
cal domain singularities, improves mesh quality and
curved boundary representation. At each successive step
of the solution the domain is first updated, accounting
for fracture movements, then is triangulated by control-
ling the dimension of the elements using the a posteriori
error measure proposed by Zhu and Zienkiewicz [8]. The
refinement strategy suggested in [8] is followed and the
required element size is obtained by updating the current
spacing function values. The value of the spacing func-
tion represents the required dimension of each triangular
element. As far as the area surrounding the process zone
is concerned, this strategy is no more applicable. Near
the fracture tip, the element spacing is simply controlled
by locating a point source of elements [9], the weight of
which is determined in order to properly model the proc-
ess zone and the cohesive forces and to yield mesh inde-
pendent results. In the applications presented, this last
requirement always resulted the most strict one. The
meshing procedure proceeds then to regularize the mesh
size distribution. The discretization of the process zone
will be further discussed in Section 6.
A quadrilateral mesh, sometimes preferred in frac-
ture mechanics, can also be obtained, preserving mesh
quality control. In both cases, bilinear approximation
of the field variables is used.
To reduce computation time, the successive refine-
ment and/or derefinement operations can be limited to
suitable subdomains containing the singularities zones.
The dimensions of these areas and local density of dis-
cretization can be decided on the basis of the solution
at the actual and previous steps. This possibility is
strictly dependent on the used data structure [9], how-
ever, at present, the remeshing operations are made for
each crack increment in the whole domain.
Some changes to the procedure shown in [9] are re-
quired by the presence of non-homogeneity of the med-
ium [18]. Each homogeneous region is meshed
independently of the others, using different spacing func-
tion values within each one, with the only requirement
of assuming the same nodes along the interfaces. Fur-
ther, it is necessary to check that the triangulation com-
pletely represents the boundary of each region and the
complete domain. It should be remembered that Delau-
nay triangulation is a unique geometric construction for
an assigned set of points, hence it does not guarantee the
consistency of a generic contour defined through a sub-
set of points of the initial set. To this end, the discretiza-
tion procedure has been updated in this way:
� the nodes are inserted, beginning with those at the
boundary. The topological entities defining the
boundary handle the node distribution by accounting
for the spacing function at the end points. The
boundary entities recognize the regions connected
to them by means of non-zero pointers in the data
structure, not through searches in special lists and
without any orientation rules, and require the re-
gion/s topological entities to locate the new common
node. Each region then handles the generation of tri-
angles and contours separately, and checks conform-
ity, following the usual procedure (Bowyer–Watson
algorithm) [9];
� consistency check along each interface. Once the
node location phase has been accomplished, there is
no guarantee that the interface boundary is repre-
sented by the triangulation edges. The geometric con-
sistency is controlled and, if necessary, can be
reached by inserting new nodes as in [9]. In the pres-
ence of non-homogeneities, the region entities indi-
cate the existence of the anomaly and require the
boundary to locate a new node in a fixed position.
The boundary entity continues with the insertion of
the node, but informs all other regions linked to it
of this operation. This procedure is repeated until
the consistency of all boundaries is reached.
From the computational point of view and to im-
prove the efficiency of the generator, all above men-
tioned operations are performed by special Euler
operators which exploit the information contained in
the data structure representing the fundamental
entities, Vertices, Edges and Faces. Owing to the
data structure used, conditional loops are almost en-
tirely avoided, resulting in a highly efficient computer
code.
5. Nucleation and propagation of fractures
Let us consider a non-homogeneous two dimensional
domain under plane strain or stress assumptions. In a
generic solution step, once the displacement field has
been obtained, strain and stress fields are calculated.
The latter are constant within each triangular element,
given that a bilinear approximation of field variables is
used. Nodal values of stresses are calculated by applying
a smoothing procedure to elements of the same material
only. Stress discontinuities can, therefore, be present
only at nodes of an interface, whereas the smoothed
stress field is continuous within each homogeneous re-
gion. Assuming that unstructured meshes are used, each
node can be shared in general by n elements with nm dif-
ferent material properties. The topological entity node is
required to handle nm stress and strain tensors together
with fracture enucleation/propagation. This implies that,
1880 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
at the same node, all cracks required by the stress field
can nucleate/propagate.
Even in the presence of non-homogeneous materials,
when the crack moves within a homogeneous subregion
it is assumed that nucleation and propagation take place
according to Barenblatt and Dugdale�s [11,12] cohesive
model for homogeneous and isotropic bodies under
mode I assumptions. Crack nucleation takes place when
the traction principal stress reaches the ultimate value rtof the material, the propagation direction being orthog-
onal to the same principal stress. The opened lips are as-
sumed as interacting and transmitting tractions as
dependent on crack opening, and vanishing when this
reaches the critical value drcr (Fig. 1). Once this value
is exceeded, the only possible tractions for the opposite
lips are in compression when the fracture reaches a con-
tact position when closing. When the fracture path ap-
proaches an interface between two different materials
the direction of propagation is different from the previ-
ous case. It is chosen to maximize the energy fracture re-
lease.
The computational procedure to find the point of
crack formation consists in finding the node Ni with the
highest principal positive stress. When this exceeds the
limiting value of the material, a new crack is created or
an existing one moves its tip. A detailed analysis of the
possible situations and related procedure can be found
in [18].
6. Applications
It is quite difficult to find a benchmark test for the
model presented. As previously pointed out, current
Fig. 2. Geometry of the three-point bend
Table 1
Mechanical and thermal properties of the materials at 25 �C
Young�s modulus
(GPa)
Poisson coefficient Thermal expan
coefficient (�C�
Al6061 69 0.33 2.36·10�5
PMMA 3.338 0.35 7.45·10�5
numerical models evaluate the stress intensity factors
for thermal loads in a stationary situation, both for
the crack geometry and thermal field, hence they
do not match the complexity of the present formula-
tion.
For comparison purposes, reference is made to the
laboratory experiment presented in [2]. A three-point
bending test is performed on a bimaterial specimen sub-
jected to a thermo-mechanical loading. One part of the
sample is made of aluminium 6061 and the other in poly-
methylmethacrylate (PMMA), bonded with methacry-
late adhesive. The geometry is presented in Fig. 2: the
sample has a notch with a sharp tip of 1 mm width
and 30 mm height shifted 3 mm from the interface in
the PMMA zone. The two materials present very differ-
ent Young�s moduli and thermal expansion coefficients,
so that, when the system is subjected to heat, stresses
arise near the interface as a result of the mismatch in
thermal expansion. Mechanical and thermal properties
of the two materials are presented in Table 1. Further,
a variation of PMMA Young�s modulus with tempera-
ture has been experimentally observed and values shown
in Table 2 were measured. Fracture energy was not de-
fined in [2], owing to the different approach to fracture
mechanics, hence it has been calculated in the present
application. Fracture energy has been obtained on the
basis of the stress intensity factors declared in [2] for
the two limiting cases (T=25 and 60 �C), whereas the
ultimate stress r0 is assumed of 25 MPa at the tempera-
ture of 60 �C. Linear variation with temperature of both
these parameters has been adopted. A second assump-
tion of the numerical simulation is the linear elasticity
of the PMMA. Following [19], a more suitable mechan-
ical model requires non-linear elasticity for this material.
ing test for a bimaterial specimen.
sion1)
Thermal
conductivity (W/mK)
Fracture energy
(MPam�1)
r0 (MPa)
167
0.2 320.0 50.0
Table 2
Dependence of PMMA Young�s modulus on temperature
25 �C 35 �C 45 �C 60 �C
Young�s modulus (GPa) 3.4 3.4 2.6 2.05
S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887 1881
For the moment, however, the application is intended to
demonstrate the capability of the model presented, not
to closely match the laboratory results. For the same
reason no particular care is used in the determination
of parameter b (Eq. (10)), which value is assumed equal
to 0.866 according to [10]. Nevertheless, as it will be
shown in the following, the obtained results compare
quite well with the experimental ones also under the
assumption of linear elastic materials.
Two different experiments were performed in [2]. In
the first, at a room temperature of 25 �C, a load was ap-
plied 3 mm from the interface in the PMMA zone (Fig.
2) in order to trigger the fracture process. The loading
rate was very low and the resulting speed of crack prop-
agation at the initial stages was also quite slow, so that
quasi-static conditions can be assumed. The crack path
was individuated and stresses near the crack tip in the
PMMA were measured using a shearing interferometer.
In the second experiment the same operations were
performed when the temperature of the aluminium was
60 �C in steady state conditions. To reach these condi-
tions, a cartridge heater (Q in Fig. 2) was inserted into
the aluminium part near the external vertical side. The
Fig. 3. Zoom of the notch of the specimen with crack paths trajecto
numerical. Case A: uniform temperature (25 �C); case B: thermal load
with E=E(25 �C), r0=r0 (25 �C), drcr=drcr (25 �C).
variation in time of the PMMA temperature was
checked before the fracture test, which was performed
when steady state conditions were reached. The temper-
ature of PMMA was recorded at the crack tip location,
at 5 and 7 mm from the interface. Also in this case, the
crack path was spotted. From the differences between
the two situations, the authors gathered the thermal ef-
fects, which were independent of the magnitude of the
applied mechanical load.
In the two experiments the crack propagation trajec-
tories are remarkably different as shown in Fig. 3a and b
where a zoom of the fractured specimens in correspond-
ence of the notch is presented. In particular the crack
path is closer to the interface when the temperature is
higher. A strongly representative parameter is the crack
initiation angle, which experimental values are listed in
Table 3 for the two temperature levels.
Due to the fact that the numerical model used is 2-D,
whereas the real heat transfer problem is 3-D, the con-
vection effect on the lateral surfaces of the specimen is
accounted for through the pertinent terms in the heat
transfer equation. According to [20], convection matrix
Kc of a generic finite element is
ries: (a) and (b) experimental results (reproduced from [2]), (c)
with E, r0,drcr varying with temperature; case C: thermal load
Table 3
Comparison for crack initiation angle: Case A: uniform
temperature (25 �C); Case B: thermal load with E, r0, drcrvarying with temperature; Case C: thermal load with E=E (25
�C), r0=r0 (25 �C), drcr=drcr (25 �C)
Crack initiation angle (deg)
Case Experimental Numerical
A 24 25
B 13 12
C – 25
0.0
10.0
20.0
30.0
40.0
50.0
60.0
0 200 400 600 800 1000 1200time [s]
Tem
pera
ture
[°C
]
2.5 3.5 5.010.017.0
Fig. 5. Time histories of temperature calculated at 2.5, 3.5, 5.0,
10.0, 17.0 mm distance from the interface, at 30 mm height
from the bottom level.
1882 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
Kc ¼ZCkNTNdC; ð16Þ
being C the part of the boundary where convection takes
place, k the convection coefficient of air (25 W/m2K)
and N the shape functions of the boundary edge of the
element. In addition to this term, a second contribution
is introduced which accounts for the convection across
the element surface, hence is of the form
Kc ¼ 2
ZXkNTNdX: ð17Þ
In Eq. (17), X represents the element domain and N the
element shape functions. It is further assumed that heat
can propagate inside the notch. To this end, a material is
assumed to fill this zone which presents no mechanical
resistance with a fictious thermal conductivity of 0.1
W/m2K.
The calculated temperatures in PMMA near the
interface are shown in Fig. 4, together with the values
obtained in [2], both by an uncoupled finite element
analysis and by experiment. The results of the present
model compare very well with the experimental one.
Fig. 5 shows both for the steep gradient near the inter-
face and the numerically calculated time histories at
points located at different distance from the interface.
0.0
10.0
20.0
30.0
40.0
50.0
60.0
70.0
0 5 10 15 20 25 30Distance from the interface [mm]
Tem
pera
ture
[°C
]
Present solutionExperimental results
Fig. 4. Temperature distribution of PMMA versus distance
from the interface.
Due to the different approach to the fracture prob-
lem, comparison of the present solution with the exper-
imental results is performed on the basis of crack path.
Fig. 3c presents calculated crack paths in three cases.
Case A considers uniform temperature (25 �C) in con-
junction with a mechanical load of 835 N. In case B
the effects of the thermal load due to heating and vertical
load of 650 N are analysed, assuming the PMMA
Young�s modulus, limiting stress r0 and critical opening
drcr varying with temperature. Case C is equal to the
previous one, except for parameters E, r0 and drc whichare assumed constant and corresponding to the ones atroom temperature. The obtained crack path configura-
tions are of the same nature of the experimental onesand compare quite well with them (Fig. 3a,b), in partic-ular showing that the path is closer to the interface whenthe temperature is higher. The agreement is corrobo-
rated by the crack initiation angle values listed in Table3: numerical and experimental results are in goodaccordance.
Limited to Case B, Fig. 6 shows the ultimate stress
and temperature at crack tip as it moves during the evo-
lution of the fracture phenomenon. The decrease of the
ultimate stress depends on the increase of the tempera-
ture while the fracture propagates. This is a physical jus-
tification for the moving of the crack path closer to the
interface, where temperature is higher and limit stress is
lower.
Fig. 7 shows the temperature map contours in the
whole sample at different times before the crack enucle-
ation. It is remarkable that these distributions soon be-
come nearly constant over the height of the specimen
and always exhibit a steep temperature gradient near
the interface. Further, the effect of the elements located
30.0
35.0
40.0
45.0
50.0
0 20 40 60 80s [mm]
σo [MPa]
T [°C]
Fig. 6. Case B Limit stress r0 and temperature T at crack tip
during fracture evolution (s representing the distance of the tip
from the notch).
S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887 1883
in the notch is evident, which results in a continuous
temperature distribution.
Fig. 7. Temperature map contour at time t=60, 300 and 1200
Displacement and stress fields are on the contrary
discontinuous across the notch and the fracture path.
The map contour of vertical displacements is shown in
Fig. 8 together with the amplified deformed configura-
tion.
Fig. 9 presents the contour map of the maximum
principal stress and cohesive force distribution in the
process zone in an initial stage of fracture propagation.
The calculated length of the process zone is very limited.
The maximum length is nearly 0.8 mm at the beginning
and decreases during the evolution of the phenomenon.
Application of Barenblatt [11] theory for calculation
of characteristic cohesive zone size yields for PMMA
‘ ¼ pEGc
8ð1� m2Þr20
ffi 0:75 mm ð18Þ
and numerical results are in good accordance with this
value.
The knowledge of the length of the process zone al-
lows for important remarks on mesh discretization. To
s. Point heat source of 3.0804·105 J/s/m3 located in Q.
Fig. 8. Amplified deformed configuration with vertical displacement contour map for Case B.
Fig. 9. Contour map of maximum principal stress and cohesive forces at fracture tip (Case B).
1884 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
obtain a mesh independent solution it is necessary to
properly discretize the process zone, hence severe limits
are introduced depending on the approximation of the
used elements. An heuristic assessment has been made
on the influence of the mesh size in the process zone:
using linear elements of decreasing size, the value of
the force P (Fig. 2), corresponding to an applied verti-
cal displacement on the same point, is calculated. Re-
sults are summarized in Fig. 10. As can be seen the
peak of the external load and the softening branch re-
sult independent of discretization when the process
zone is subdivided into at least five elements with edges
of 0.15 mm or smaller. This situation is handled by the
mesh generator simply by locating an element source
600
800
1000
1200
1400
0 0.2 0.4 0.6Mesh size [mm]
Max
F [N
]
0
200
400
600
800
1000
1200
1400
-1.40-1.20-1.00-0.80-0.60-0.40-0.200.00Vertical disp. [mm]
F [N
] < 0.15 mm
0.50 mm
1.00 mm
Fig. 10. External force versus vertical displacement and mesh
size.
S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887 1885
[9] in correspondence of the crack tip. Its weight may
be a priori stated (using Eq. (18)) and/or can be a
Fig. 11. Geometry of the three-point bending test for a bimaterial
aluminium; Case 2: the upper part is PMMA with Young�s modulus
posteriori updated during the adaptive remeshing pro-
cedure once the length of the process zone has been
determined.
The second application is intended to demonstrate
the capabilities of the proposed method, in particular
as far as the study of crack path evolution is concerned.
To this end the bimaterial specimen is assumed as in
Fig. 11. The lower part of the sample is made of PMMA
having the mechanical characteristics shown in Tables 2
and 3. Three different cases are obtained by changing
the material in the upper part of the sample. In Case
1 the upper part is aluminium with mechanical proper-
ties as in Table 2; Case 2 presents in the upper part
PMMA with Young�s modulus three times larger than
in Table 2; in Case 3 an homogeneous sample of
PMMA with characteristics as in Tables 2 and 3 is as-
sumed.
The analysed sample is loaded by a concentrated
force acting along the axis of symmetry and a distributed
heat source is present in the upper region.
Fig. 11 presents the different crack paths obtained by
the application of the proposed procedure. Depending
on the mechanical characteristics the paths are differ-
ently influenced by the interface. Fig. 12 shows the max-
imum principal stress contour for Case 2 and in Fig. 13 a
zoom is presented containing the process zone where the
cohesive forces are different from zero.
It is interesting to remark that only the use of the
mesh generator proposed in [9] can handle such type
of problems. The unique alternative is a very fine
mesh in large areas, resulting in a huge numerical
model. On the contrary the use of interface elements
is prevented by the fact that crack path is a priori un-
known.
specimen and resulting crack paths. Case 1: the upper part is
three times larger; Case 3: homogeneous sample.
Fig. 13. Zoom of the maximum principal stress contour.
Fig. 12. Maximum principal stress contour.
1886 S. Secchi et al. / Computers and Structures 82 (2004) 1875–1887
7. Conclusions
The paper presents a fully-coupled numerical model
for the analysis of fracture initiation and propagation
in a two dimensional non-homogeneous elastic medium
driven by transient thermal and mechanical fields.
Cohesive crack behaviour is assumed for the solid.
The comparison with a laboratory experiment and
the solution of a purely numerical test validate the
model and demonstrate the capabilities of the proposed
procedure.
One of the key points to obtain meaningful numer-
ical simulation is the correct discretization of the
process zone, as demonstrated by the presented
mesh-independency test. In order to follow the evolu-
tion of the crack, the process zone and the continuous
changes of the domain topology a successive remesh-
ing of the domain is advisable on the basis of fracture
evolution and using an a posteriori refinement tech-
nique.
Acknowledgments
This research was partially supported by the Italian
Ministry of University and Scientific and Technological
Research (Grant MURST ex 60%) and (Cofinanzia-
mento MURST MM08161945_003).
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