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Trang 1DOI 10.1007/s10704-004-7138-3 © Springer 2005
Interaction between a cracked hole and a line crack under uniform heat flux
PHAM CHI VINH1, NORIO HASEBE2,∗, XIAN-FENG WANG2 and
TAKAHIRO SAITO2
1Faculty of Mathematics, Mechanics and Informatics, Hanoi National University, 334 Nguyen Trai Str., Thanh Xuan, Hanoi, Vietnam
2Department of Civil Engineering, Nagoya Institute of Technology, Gokiso-cho, Showa-ku, Nagoya 466-8555 Japan
∗Author for correspondence (E-mail: hasebe@kozo4.ace.nitech.ac.jp; Fax: +81-52-735-5482)
Received 21 July 2004; accepted in revised form 2 December 2004
Abstract This article deals with the interaction between a cracked hole and a line crack under
uniform heat flux Using the principle of superposition, the original problem is converted into three particular cracked hole problems: the first one is the problem of the hole with an edge crack under uniform heat flux, the second and third ones are the problems of the hole under distributed tem-perature and edge dislocations, respectively, along the line crack surface Singular integral equations satisfying adiabatic and traction free conditions on the crack surface are obtained for the solution of the second and third problems The solution of the first problem, as well as the fundamental solutions
of the second and third, is obtained by the complex variable method along with the rational mapping function approach Stress intensity factors (SIFs) at all three crack tips are calculated Interestingly, the results show that the interaction between the cracked hole and the line crack under uniform heat flux can lead to the vanishing of the SIFs at the hole edge crack tip The fact has never been seen for the case of a cracked hole and a line crack under remote uniform tension.
Key words: Cracked hole, dislocation, heat flux, interaction, integral equation, mapping function, stress
intensity factor, thermal stress.
1 Introduction
Due to the stress concentration effect, cracks are likely to initiate at a hole bound-ary under the action of monotonous or fatigue loading A number of papers deal-ing with the hole edge crack problem are available (Bowie, 1956; Tweed and Rooke, 1973; Hasebe and Ueda, 1980; Schijve, 1983; Hasebe et al., 1988, 1994a, b; Zhang and Hasebe, 1993; Chao and Lee, 1996; Hasebe and Chen, 1996) Among them, the rational mapping function approach is significant to solve the hole edge crack prob-lem (Hasebe and Ueda, 1980; Hasebe et al., 1988, 1994a, b; Hasebe and Chen, 1996)
Up to now, there seem to be only a few papers concerning the interaction between the crack emanating from a hole and another independent crack Hasebe et al (1994a) solved a second mixed boundary value problem analytically and as an exam-ple of the solution, the interaction of a square hole with an edge crack and a line crack was investigated for a geometrically symmetric case Hasebe and Chen (1996) treated a cracked circular hole and a crack when the remote stresses were applied at
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d
f -a
e
2b
y
temperature dislocation
edge dislocation
A
B
C
y
x
y
x 0
y
x 0
C
A
B
0
I
γπ(1−γ)π
I
B
A I
A
B
no crack
C
y
x
A temperature dislocation
y
x 0
C
zo
zo edge dislocation
Problem A
Problem B
Problem C
Problem E (a)
(b)
Figure 1 Superposition of problems.
infinity The interactions of a hole and a rigid inclusion, respectively, with a crack were considered by Hasebe et al., (2003a) The problem of a crack initiating from a rigid inclusion interacting with a line crack was also solved by Hasebe et al (2003b)
It is known that when steady heat flow is disturbed by the presence of crack, there is a high local intensification of temperature gradient at the crack tips and large thermal stresses arise around them Thermal disturbances of this kind may, in some cases, cause crack propagation resulting in serious damage to structural components Consequently, the study of the behavior of thermal stresses near the crack tips is of importance in fracture mechanics
The aim of this paper is to investigate the interaction between a cracked hole and
a line crack under uniform heat flux The hole edge and the faces of the cracks are assumed to be adiabatic and traction free The problem to be considered is shown in Figure 1a It is clear that the original problem A can be reduced to three following problems by the principle of superposition:
Problem B: Problem of the hole with an edge crack under uniform heat flux
(Fig-ure 1b)
Problem C: Problem of the hole with an edge crack under distributed temperature
dislocation along the line crack surface (Figure 1c)
Problem D: Problem of the cracked hole under distributed edge dislocation along
the line crack surface (Figure 1d)
In order to solve these problems we apply the complex function method along with the rational mapping function approach By means of the principle of superposition,
Trang 3problem C (D) can be reduced to a problem named problem E (F), in which the cracked hole subjected to a temperature point dislocation (an edge point dislocation) placed at some point on the crack line AB After problem E (F) is solved, the solu-tion of problem C (D) can be obtained by integrating the Green’s funcsolu-tions of prob-lem E (F) along the line AB By summation of the solutions of probprob-lems B, C and
D, we can ascertain problem A’s solution, in which there are two unknown functions: the distribution density of temperature dislocation along AB (coming from prob-lem C’s solution) and the distribution density of edge dislocation along AB (com-ing from problem D’s solution) These functions are determined from the s(com-ingular integral equations which are derived from the adiabatic and traction-free conditions along the faces of the line crack AB Finally, by numerical integration of the singular integral equation, stress intensity factors (SIFs) at crack tips are obtained It is inter-esting to find that the interaction between the cracked hole and the line crack under uniform heat flux can lead to the vanishing of the SIFs at the hole edge crack tip The fact has never been seen for the case of a cracked hole and a line crack under remote uniform tension
2 Rational mapping function
As mentioned above, the rational mapping function technique is used to deal with the cracked hole with arbitrary shapes in an infinite plane In the computation, we will consider a cracked elliptical hole and a cracked square hole as examples Here, with-out loss of generality, the general form of rational mapping function is given (Hasebe and Ueda, 1980; Hasebe et al., 2003b):
z = ω(ς) = E0ς +
N
k=1
Ek
which maps the exterior of the cracked hole in the z-plane onto the exterior of the unit circle in the ς-plane as shown in Figure 2 Here E−1, E0, Ek, ςk(k = 1, 2, 3, , N) are
complex constants and |ς k | < 1 for all k = 1, 2, 3, , N It should be noted that other configurations can be readily tackled using this general formulation Taking E0= 0 and
Ek = 0 (k = 1, 2, 3, , N) in (1), the mapping function is reduced to the one for a circle Likewise, when E0= (a + b)/2 and E1= (b − a)/2, ς1= 0 and E k = 0 (k = 2, 3, , N) are taken, the mapping function is for ellipse with semi-axes on the x and y-axes being a and
b, respectively.
3 Basic formulae
3.1 Temperature field
In the ς-plane, the temperature function θ(ς, ς) for the two-dimensional steady-state
thermoelasticity satisfies the Laplace equation Thus, the temperature function can be
expressed as the real part of an analytic function Y (ς), which gives temperature and
heat flux (Hasebe et al., 1988; Han and Hasebe, 2001) as:
Trang 4370 P.C Vinh et al.
Figure 2 Rational mapping functions for a cracked square hole and a cracked elliptical hole.
qx − iq y = −k
Y(ς)
ω(ς)
qρ − iq θ= ςω(ς)
where q x and q y denote the heat flux components in the x- and y-axes, respectively,
qρ and q θ represent these in the orthogonal curvilinear coordinates generated by
ω(ς), and k signifies the thermal conductivity of the material Also the heat flux
boundary condition is given as follows:
−k[Y (σ ) − Y (σ)] = 2i
where σ and q n denote a value of ς and the normal heat flux component on the
boundary, respectively, and the integration is carried out along the boundary From
(5), the adiabatic condition (q n= 0) along the boundary is:
3.2 Thermal stress field
Employing complex functions φ(ς) and ψ(ς), the stresses in the elastic body are
(Muskhelishvili, 1963):
σx + σ y= 4Re
φ(ς)
ω(ς)
σy − σ x + 2iτ xy= 2
ω(ς)
φ(ς)
ω(ς)
+ ψ(ς)
Trang 5
σθ + σ ρ = σ x + σ y , (9)
σθ − σ ρ + 2iτ ρθ= ς2ω(ς)
The stress boundary condition is written as:
φ(σ ) + ω(σ )
ω(σ ) φ
(σ ) + ψ(σ ) = i
where p x and p y denote external force components applied to the boundary in the
x- and y-directions, respectively.
Using the complex stress functions φ(ς), ψ(ς) and the temperature function Y (ς),
the displacement expression can be put into the following form:
κφ(ς) − ω(ς)
ω(ς) φ
(ς) − ψ(ς) + 2Gα
where G is the shear modulus, κ and α are: κ = 3 − 4v, α= (1 + v)α for plane strain and κ = (3 − v)/(1 + v), α=α for generalized plane stress; v and α are Poisson’s ratio
and the coefficient of thermal expansion, respectively
4 Solution of problem B
4.1 Temperature field
Consider the heat conduction problem shown in Figure 1b, in which q is the inten-sity of the uniform heat flux; δ is the angle between the direction of the heat flux and the x-axis Herein the hole edge and crack faces are assumed to be adiabatic The temperature function YB(ς) of problem B can be broken down into two parts:
where the first function denotes the one induced from the uniform heat flux; the
sec-ond one denotes the complementary part From (3), function Y1B(ς) can be obtained:
Y1B(ς) = − q
k e
Substituting (13) and (14) into (6) yields:
Y2B(σ ) − Y2B(σ ) = q
k e
−iδ ω(σ ) − q
k e
Multiplying (15) by the factor dσ/[2πi(σ − ς)] and carrying out the Cauchy integra-tion along the unit circle, we obtain Y2B(ς) and finally (Hasebe et al., 1988):
YB(ς) = − q
k
e −iδ E0ς + e iδ E¯0
ς
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372 P.C Vinh et al.
4.2 Thermal stress field
The stress function for the thermoelastic problem can be split into two parts: a
non-holomorphic part [φ1B(ς), ψ1B(ς)] and a holomorphic part [φ2B(ς), ψ2B(ς)]:
φB(ς) = φ1B(ς) + φ2B(ς),
The last term of the left-hand side of (12) denotes the thermal displacement This integration contains logarithmic term which represents dislocation in the
thermo-elasticity To remove it, we consider the following stress functions φ1B(ς), ψ1B(ς)
(Florence and Goodier, 1960):
where the constants AB and BB are determined using the conditions that the stress and the displacement components around the hole are single-valued Substituting (17) and (18) into (11), and using the stress single valuedness condition, we have
Next, substitute (17) and (18) into (12) Multiple values of logarithmic terms must
be cancelled due to the single-valuedness of displacement Consequently, the constant
AB is determined as:
AB=αqGR
2k E0
N
k=1
Ek e −iδ+ ¯E0e iδ
where R = (1 + v)/(1 − v) for plane strain and R = (1 + v) for generalized plane stress.
Now we consider the boundary condition to derive the holomorphic functions
φ2B(ς) and ψ2B(ς) The hole edge and crack faces are assumed traction free without
loss of generality, i.e., p x = p y= 0 Substituting (17) into (11) yields
φ2B(σ ) + ω(σ )
ω(ς) φ
2B(σ ) + ψ2B(σ ) = −φ1B(σ ) − ω(σ )
ω(σ ) φ
1B(σ ) − ψ1B(σ ). (21)
Multiplying (21) by the factor dσ/[2πi(σ − ς)] and carrying out the Cauchy integra-tion along the unit circle, we obtain φ2B(ς) as:
φ2B(ς) =
N
k=1
¯
AkBk
ς − ςk+ ¯AB
N
k=1
Bkςk
in which B k ≡ E k/ω(ς k) with ς k≡ 1/ ¯ς k and A k = φ
2B(ς k) Here the real and
imagi-nary values of A k are determined by the simultaneous equations of 2N derived by differentiating (22) and substituting ς = ς k
Thus, the stress function φB(ς) is (Hasebe et al., 1988):
φB(ς) = ABlog ς +
N
k=1
¯
Ak Bk
ς − ςk + ¯AB
N
k=1
Bk ςk
Trang 7The stress function ψB(ς) can be derived by analytic continuation along the
free-traction boundary of the unit circle Indeed, by introducing the following function:
φB(ς) = − ¯ω ω(ς)(1/ς)
¯
φB(1/ς) − ¯ ψB(1/ς), ς ∈ S−= {ς : |ς| < 1} (24)
from (11) with regarding p x = p y= 0 on the unit circle and (24), we have
This means the function φB(ς), ς ∈ S− is a continuation of the function φB(ς), ς ∈
S+={ς : |ς| > 1} from the outside of the unit circle to its inside From (25) it follows:
ψB(ς) = − ¯ φB(1/ς) − ¯ω(1/ς)
ω(ς) φ
5 Solution of problem C
Consider an infinite plane with a cracked hole subjected to distributed tempera-ture dislocations along the line crack surface, as shown in Figure 1c The hole edge and crack faces are assumed to be traction-free and adiabatic As previously said, by means of the principle of superposition, problem C can be reduced to
a problem E, in which the cracked hole subjected to a temperature point
dislo-cation placed at some point z0(= ω(ς0), ς0 is a point in the ζ -plane correspond-ing to z0) on the line AB To solve problem E, we need to find the Green’s function for the temperature field, as well as the stress field of the cracked hole under a temperature point dislocation After problem E is solved, the solution
of problem C can be obtained by integrating the Green’s function along the line AB
It is not difficult to verify that, for the temperature field, the Green’s function of problem E for a couple temperature dislocation is (Hasebe and Han, 2001):
YE(ς) =
2πk
e iϑ
ω(ς0)(ς − ς0)− e −iϑ ς
2
p
ω(ς0)(ς − ςp)
where k is thermal conductivity of the material, β is the angle between the line AB and the x-axis, denotes the magnitude of the couple temperature dislocation, and
ς0= ω−1(z0), ςp ≡ 1/ ¯ς0
Next, for the stress field, the stress functions φE(ς) and ψE(ς) for problem E can
be expressed in the following form:
φE(ς) = φ1E(ς) + φ2E(ς),
where φ2E(ς) and ψ2E(ς) are holomorphic in S+; φ1E(ς) and ψ1E(ς) are expressed as
φ1E(ς) = − 2π C log(ς − ς0) + AElog ς,
ψ1E(ς) = − 2π C log(ς − ς0) + 2π C ω(ς0)
ω(ς )(ς−ς ) + BElog ς
(29)
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with C = k(κ+1) 2Gα e iϑ and AElog ς and BElog ς are functions to cancel the dislocation
of both stress and displacement around the hole Substituting (28) and (29) into (11), and moving around the unit circle once, the requirement that the stress are single val-ued around the hole gives
Substituting (28), (29) and (30) into the displacement expression (12), after mov-ing around the unit circle, the displacements must recover their initial values This
requirement fixes the constant AE in the following expression:
AE= C
2π
N
k=1
Ek
ω(ς0)(ς0− ς k)2+ ¯C
2π
E0ς p2
On account of (28), the traction-free boundary condition (11) is of the form:
φ2E(σ ) + ω(σ )
ω(ς) φ
2E(σ ) + ψ2E(σ ) = −φ1E(σ ) − ω(σ )
ω(σ ) φ
1E(σ ) − ψ1E(σ ). (32)
For obtaining φ2E(ς), we substitute (29) into (32), multiply both sides of the resulting
equation by the factor dσ/[2πi(σ − ς)], (ς ∈ S+), and carry out the Cauchy
integra-tion along the unit circle Using the following:
(i) The function (ω(ς)/ ¯ ω(1/ς)) ¯ φ2E (1/ς) is holomorphic in S− except the points
ςk (k = 1, , N), which are poles with the principal parts: E k
ς k −ς φ
2E(ς k)
ω(ς k)
(ii) The function (ω(ς)/ ¯ ω(1/ς)) ¯ φ1E (1/ς) is holomorphic in S− except the points
ςk (k = 1, , N) and ςp, which are poles with the principal parts, respectively, being:
Ek
ω(ς k)(ς − ςk)
¯C
2π
ςpςk
ςp − ς k− ¯AEςk
and ¯C 2π
ω(ςp)
ω(ς0)
ς p2
and taking φ2E(∞) = 2π C log(−ς0), we obtain the function φ2E(ς) as:
φ2E(ς) = C
2π log
1
ς − ς0
+
N
k=1
Ek
ω(ς k)(ς − ςk)
φ2E (ς k) + ¯ AEςk− ¯C
2π
ςpςk
ςp − ς k
+ ¯C
2π
ω(ς0) − ω(ςp) ς2
p
It is noted that the real and the imaginary values of φ2E (ς k) in (34) are determined by
solving the simultaneous equations of 2N derived by differentiating (34) and substi-tuting ς = ς k Thus, the function φE(ς) is:
φE(ς) = C
2π log
1
ς − ς0
+
N
k=1
Ek
ω(ς k)(ς − ςk )
φ2E (ς k) + ¯ AEςk− ¯C
2π
ςpςk
ςp − ς k
+ ¯C
2π
ω(ς0) − ω(ςp) ς p2
ω(ς0)(ς − ςp ) − C
2π log(ς − ς0) + AElog ς. (35)
Trang 9Similar to Section 4, the stress function ψE(ς) can be derived directly by analytic
continuation along the traction-free boundary as:
ψE(ς) = − ¯ φE(1/ς) − ¯ω(1/ς)
ω(ς) φ
As previously stated, by means of the principle of the superposition, after problem E
is solved, the solution of problem C is obtained by using the Green’s functions YE(ς),
and φE(ς) and ψE(ς), respectively, along the line AB (see Equations (45) and (48)).
6 Solution of problem D
Problem D is shown in Figure 1d, in which an infinite plane having a hole with
an edge crack is under distributed edge dislocations along the line crack AB The hole edge and crack surfaces are traction-free Naturally, by means of the principle
of superposition, problem D can be reduced to a problem F, in which an edge point
dislocation with magnitude D is placed at a point z0 (= ω(ς0)) on the line AB
Simi-lar to the previous sections, the Green’s function of problem F: φF(ς) and ψF(ς) can
be found in the form:
φF(ς) = φ1F(ς) + φ2F(ς),
where φ2F(ς) and ψ2F(ς) are functions holomorphic in S+ and (Hasebe and Chen, 1996):
φ1F(ς) = − D
2π log(ς − ς0),
(38)
ψ1F(ς) = − D¯
2π log(ς − ς0) +
D
2π
ω(ς0)
ω(ς0)(ς − ς0) .
From (37), the traction-free boundary condition (11) for problem F is of the form:
φ2F(σ ) + ω(σ )
ω(ς) φ
2F(σ ) + ψ2F(σ ) = −φ1F(σ ) − ω(σ )
ω(σ ) φ
1F(σ ) − ψ1F(σ ). (39)
Multiplying both sides of (39) by the factor dσ/[2πi(σ − ς)], (ς ∈ S+), and carrying
out the Cauchy integration along the boundary yield the result of φ2F(ς) Similar to
the procedures used in the section 5, we obtain:
φ2F(ς) = D
2π log
1
ς − ¯ς0
+
N
k=1
Ek
ω(ς k)(ς − ςk ) φ
2F(ς k) + D¯
2π
1
¯ς0− ¯ς
k
+D¯
2π
ω(ς0) − ω(ςp) ς p2
It should be noted that the real and imaginary parts of φ2F (ς k) in (40) are
deter-mined by solving the simultaneous equations of 2N derived by differentiating (40)
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and substituting ς = ς k Taking into account (37), (38) and (40), the function φF(ς)
is obtained
φF(ς) =
N
k=1
Ek
ω(ς k)(ς − ςk ) φ
2F(ς k) + D¯
2π
1
¯ς0− ¯ς
k
+D¯
2π
ω(ς0) − ω(ςp) ς p2
ω(ς0)(ς − ςp) − D
2π log(ς − ς0) +
D
2π log
1
ς − ¯ς0
The stress function ψF(ς) is derived directly by analytic continuation along the
traction-free boundary of the unit circle as:
ψF(ς) = − ¯ φF(1/ς) − ¯ω(1/ς)
ω(ς) φ
By means of the principle of superposition, the solution of problem D can be
obtained by using φF(ς) and ψF(ς), respectively, along the line AB (see Equation
(48))
7 Solution of problem A: Integral equations
The original problem A can be reduced to the superposition of three subproblems
B, C and D which have been studied in Sections 4–6, respectively Thus, from these results, the solution of problem A is derived as follows:
Temperature function:
where YB(ς) is defined by (17) and YC(ς) is obtained by integrating YE(ς) with
corresponding density along the line AB
Stress functions:
φ(ς) = φB(ς) + φC(ς) + φD(ς),
where φB(ς) and ψB(ς) are defined by (23), (26); φC(ς) and ψC(ς), and φD(ς) and
ψD(ς) are obtained by integrating the Green’s functions φE(ς) and ψF(ς), and φF(ς)
and ψF(ς), respectively, along the line AB.
It should be noted that in (43) and (44), there are still two unknown functions
(t) and D(t) Therefore, in order to calculate the solution of problem A, we need
to find equations (singular integral equations) for the unknown functions: the
distri-bution density of the temperature dislocation γ (t)dt = d(t) and the density of edge dislocation D(t) From the adiabatic condition along the crack faces expressed by (6) and (43), the following singular integral equation for γ (t) is derived:
Im
b
−b
γ (t)YE(s, t)dt −
b
−b
γ (t)YE(s0, t)]dt
=−Im [YB(s) − YB(s0)] , |s| ≤ b, (45)
where s0 is an arbitrary point (standard point) on the crack face AB, Y E is expressed
by (27) with = 1 Function γ (t) can be further reduced to the following form for a
crack problem:
... which an infinite plane having a hole withan edge crack is under distributed edge dislocations along the line crack AB The hole edge and crack surfaces are traction-free Naturally, by means...
where φB(ς) and ψB(ς) are defined by (23), (26); φC(ς) and ψC(ς), and φD(ς) and< /i>
ψD(ς)...
ψD(ς) are obtained by integrating the Green’s functions φE(ς) and ψF(ς), and φF(ς)
and ψF(ς),