Jtam-A4.dvi JOURNAL OF THEORETICAL AND APPLIED MECHANICS 52, 3, pp. 617-628, Warsaw 2014 THERMAL STRESSES AROUND TWO UPPER CRACKS PLACED SYMMETRICALLY ABOUT A LOWER CRACK IN AN INFINITE ORTHOTROPIC PLANE UNDER UNIFORM HEAT FLUX Shouetsu Itou Kanagawa University Rokkakubashi, Department of Mechanical Engineering, Kanagawa-ku, Yokohama, Japan e-mail: itous001@kanagawa-u.ac.jp Two upper collinear cracks are placed parallel to a lower crack in an infinite orthotropic plane under uniform heat flux perpendicular to the cracks. The surfaces of the cracks are assumed to be thermally insulated. The mixed boundary value conditions with respect to the temperature field and those with respect to the stress field are reduced to dual integral equations using the Fourier transform technique. In order to satisfy the boundary conditions outside the cracks, the differences in temperature and displacement at each crack surface are expanded in a series of functions that are zero outside the cracks. The unknown coefficients in each series are evaluated using the Schmidtmethod. The stress intensity factors are then calculated numerically for selected crack configurations. Keywords: heat flux, three parallel cracks, stress intensity factor, infinite orthotropic plane 1. Introduction Fiber-reinforced composite materials have been widely used as structural members in airpla- nes, automobiles and high-speed trains because they are both strong and lightweight. In their construction, a matrix is reinforced with fibers, which are stiffer and stronger than the matrix. Therefore, it follows that the composite materials are orthotropic.When thematerials are sub- jected to repeated cycles of stress, some cracks may develop in the matrix material because the fibers are stronger than thematrix. If cracked compositematerials are used in high-temperature or low-temperature environments, heat flows through the materials. In this case, it is useful to evaluate the stress intensity factors that are caused by the disturbance in heat flux around the cracks. The stress intensity factor was first determined for a crack in an infinite plate in which heat flowed perpendicular to the crack by Sih (1962). Later, Sekine (1977) evaluated the stress intensity factor for a crack in a half-plane under heat flux. Sekine (1979) also determined the thermal stresses for two cracks in an infinite plate under heat flux.The two cracks were situated arbitrarily in the infinite plate, and heat flowed perpendicular to one of the two cracks (Sekine, 1979). Itou (1991) evaluated the thermal stresses for a crack in an infinite elastic layer the upper surface of which was heated to maintain a constant temperature T0, and the lower surface of which was cooled to maintain a constant temperature −T0. Itou and Rengen (1993) evaluated the thermal stresses around two parallel cracks in two bonded dissimilar elastic half-planes the upper crack of which lied in the upper half-plane, while the other crack was in the lower half- plane. The stress intensity factors were obtained for a crack in an adhesive layer sandwiched between two dissimilar elastic half-planes under heat flux perpendicular to the cracks by Itou (1993). Later, a similar problemwas also solved for the case in which two collinear cracks were situated in the adhesive layer sandwiched between two dissimilar elastic half-planes by Itou and Rengen (1995). 618 S. Itou As for orthotropic elastic problems that are related to thermal stresses, Tsai (1994) deter- mined the stress intensity factors for a crack in an infinite orthotropic plate under uniform heat flow. Chen and Zhang (1988) evaluated stress intensity factors around two collinear cracks in an orthotropic plate under heat flux. Later, Chen and Zhang (1994, 1995) evaluated stress in- tensity factors caused by a disturbance in heat flux from three coplanar cracks in an infinite orthotropic plate. The stress intensity factors were also evaluated for two parallel cracks in an infinite orthotropic plate under heat flux by Itou (2001). The solutions for an infinite plate are ineffective if a crack exists near the plane surface of a structuralmember.ChenandZhang (1993) determined the thermal stresses around two collinear cracks in an orthotropic strip. In their solution, two cracks were placed in the middle surface of the strip. If the cracks were situated near the stress-free surface, the thermal stress intensity factors would have been affected by the presence of the surface. Itou (2000) estimated the stress intensity factors around a crack in an orthotropic layer the upper surface of which maintained a constant temperature T0, while the lower surfacemaintained a constant temperature −T0. In the paper by Itou (2000) the stress intensity factors were also determined for a crack under heat flux. Since stresses around a crack are very high, a parallel crack may also develop above the original crack in compositematerials. If a tensile stress is applied to thematerial, a stress increase and stress shielding occur around the crack ends due to the position of the upper cracks (Kamei andYokobori, 1974). It is necessary to clarify whether or not the same phenomenon also occurs in a cracked orthotropic material under heat flux. In the present paper, the thermal stresses around three insulated cracks in an infinite orthotropic plate are evaluated under heat flux. Two upper cracks are situated symmetrically on either side of the central crack, and heat flows perpendicular to the cracks. Themixed boundary value conditions concerning the temperature field are reduced to two pairs of dual integral equations. To solve the equations, the differences in temperature at each crack surface are expanded in a series of functions that are zero outside the cracks. The unknown coefficients in the series are determined from the conditions inside the cracks using the Schmidt method (Yau, 1967). Next, the mixed boundary value conditions concerning the stress field are reduced to a set of dual integral equations. The differences in displacement at the upper and lower cracks are also expanded in a series of functions that are zero outside the cracks. The Schmidtmethod is used to solve for the unknown coefficients so as to satisfy the conditions inside the cracks, and the stress expressions are represented by infinite integrals. From the character of the integrands, the stress intensity factors are defined in the usual manner and are computed for steel and ceramic-fiber-reinforced ceramic (Tyrannohex) infinite planes. 2. Fundamental equations With respect to rectangular coordinates (x,y), as shown in Fig. 1, a crack is situated along the x-axis from −c to c at y=−h, and two collinear cracks are situated along the x-axis from −b to −a and from a to b at y =0. For convenience, we refer to −h¬ y ¬ 0 as layer (1), 0¬ y as upper half-plane (2), and y¬−h as lower half-plane (3). The fundamental equations for an orthotropic material were derived by Nowinski (1978). For convenience, the basic equations are shown here. If a state of plane stress is assumed, the stresses can be expressed by τxx =Q11εxx+Q12εyy−β1T τyy =Q12εxx+Q22εyy−β2T τxy =Q66γxy (2.1) with Q11 = Exx 1−νyxνxy Q22 = Eyy 1−νyxνxy Q12 = Eyyνxy 1−νyxνxy = Exxνyx 1−νyxνxy Q66 =Gxy β1 =Q12αyy +Q11αxx β2 =Q12αxx+Q22αyy (2.2) Thermal stresses around two upper cracks placed symmetrically... 619 Fig. 1. Coordinate system and three parallel cracks where Exx, Eyy are Young’s moduli, Gxy is the shear modulus, νxy, νyx are Poisson’s ratios, and αxx,αyy are the coefficients of linear expansion. The relationships between the strains and displacements are given as follows εxx = ∂u ∂x εyy = ∂v ∂y γxy = ∂u ∂y + ∂v ∂x (2.3) In equation (2.1), the temperature T satisfies ∂2T ∂x2 +k2 ∂2T ∂y2 =0 (2.4) with k2 = ky kx (2.5) where ky, kx are the thermal conductivities. Substituting equation (2.1) into the equations of equilibrium for the forces reduces these equations to the forms Q11 ∂2u ∂x2 +Q66 ∂2u ∂y2 +L ∂2v ∂x∂y −β1 ∂T ∂x =0 Q66 ∂2v ∂x2 +Q22 ∂2v ∂y2 +L ∂2u ∂x∂y −β2 ∂T ∂y =0 (2.6) with L=Q12+Q66 (2.7) 3. Boundary conditions Uniform heat flow (heat flux) q is applied perpendicular to the three cracks as shown in Fig. 1. Stresses are caused when the heat flow is disturbed by the insulating effect of the cracks. The temperature field can be provided using the following boundary conditions 620 S. Itou ∂T1 ∂y =                      ∂T2 ∂y at y=0, |x| ¬∞ −t at y=0, a¬ |x| ¬ b ∂T3 ∂y at y=−h, |x| ¬∞ −t at y=−h, 0¬ |x| ¬ c (3.1) T1 = { T2 at y=0, 0¬ |x| ¬ a, b¬ |x| ¬∞ T3 at y=−h, c¬ |x| ¬∞ (3.2) with t= q ky1 (3.3) The variables with the subscript “1” are for layer (1). The variables for upper half-plane (2) and lower half-plane (3) are denoted with the subscripts “2” and “3”, respectively. The stress field can be evaluated using the following boundary conditions τyy1 =            τyy2 at y=0, |x| ¬∞ 0 at y=0, a¬ |x| ¬ b τyy3 at y=−h, |x| ¬∞ 0 at y=−h, 0¬ |x| ¬ c (3.4) τxy1 =            τxy2 at y=0, |x| ¬∞ 0 at y=0, a¬ |x| ¬ b τxy3 at y=−h, |x| ¬∞ 0 at y=−h, 0¬ |x| ¬ c (3.5) u1 = { u2 at y=0, 0¬ |x| ¬ a, b¬ |x| ¬∞ u3 at y=−h, c¬ |x| ¬∞ (3.6) v1 = { v2 at y=0, 0¬ |x| ¬ a, b¬ |x| ¬∞ v3 at y=−h, c¬ |x| ¬∞ (3.7) 4. Analysis 4.1. Fundamental equations in Fourier domain To find the solutions, the Fourier transforms are introduced as f(ξ)= ∞ ∫ −∞ f(x)exp(iξx) dx f(x)= 1 2π ∞ ∫ −∞ f(ξ)exp(−iξx) dξ (4.1) Applying equation (4.1)1 to equation (2.6) results in Q66 d2u dy2 − ξ2Q11u− iLξ dv dy +iβ1ξT =0 Q22 d2v dy2 − ξ2Q66v− iLξ du dy −β2 ∂T ∂y =0 (4.2) Thermal stresses around two upper cracks placed symmetrically... 621 Eliminating u or v from equation (4.2), the ordinary differential equations are obtained as ζ1 d4u dy4 + ζ2 d2u dy2 + ζ3u= iη1 d2T dy2 +iη2T ζ1 d4v dy4 + ζ2 d2v dy2 + ζ3v= η3 d3T dy3 +η4 dT dy (4.3) with ζ1 = Q22Q66 L ζ2 =−(Q266+Q11Q22−L2) ξ2 L ζ3 =Q11Q66 ξ4 L η1 = ξ ( β2− β1Q22 L ) η2 =β1Q66 ξ3 L η3 = Q66β2 L η4 = ξ 2 ( β1− β2Q11 L ) (4.4) The Fourier-transformed stresses are found to be τxx =Q11(−iξ)u+Q12 dv dy −β1T τyy =Q12(−iξ)u+Q22 dv dy −β2T τxy =Q66 du dy − iξQ66v (4.5) Equation (2.4) can now be expressed in the Fourier domain as d2T dy2 − (ξ k )2 T =0 (4.6) 4.2. Temperature field The solutions for equation (4.6) have the following forms for layer (1), upper half-plane (2), and lower half-plane (3), respectively T1 =A1 sinh |ξ|y k +B1cosh |ξ|y k T2 =A2exp ( − |ξ|y k ) T3 =A3exp (|ξ|y k ) (4.7) where A1,B1,A2, and A3 areunknowncoefficients.Boundaryconditions (3.1)1,3,whicharevalid for −∞