A VISCOPLASTIC CONSTITUTIVE THEORY FOR MONOLITHIC CERAMICS - II Lesley A. Janosik NASA Lewis Research Center Cleveland, OH 44135 Stephen F. Duffy, PhD, PE Cleveland State University Cleveland, OH 44115 ABSTRACT This paper, which is the second of two in a series, exercises the viscoplastic constitutive model developed by the authors in the previous article (Janosik and Duffy, 1998). The model accounts for time-dependent phenomena (e.g., creep, rate sensitivity, and stress relaxation) in monolithic ceramics. Additionally, the formulation exhibits a sensitivity to hydrostatic stress, and allows different behavior in tension and compression. Here, the constitutive equations formulated for the flow law (i.e., the strain rate) and the evolutionary law have been incorporated into computer algorithms for predicting the multiaxial inelastic (creep) response of a given homogeneous state of stress. Numerically simulated examples illustrate the model’s ability to capture the time-dependent phenomena suggested above. For each imposed service (load) history considered, creep curves and viscoplastic flow surfaces are examined to demonstrate the model’s ability to capture the inelastic creep deformation response. No attempt is made here to assess the accuracy of the model in comparison to experiment. A quantitative assessment is reserved for a later date, after the material constants have been suitably characterized for a specific ceramic material. INTRODUCTION This paper, which is the second of two in a series, exercises the theory developed in the previous manuscript by examining specific time-dependent stress-strain behavior that can be modeled with the viscoplastic constitutive relationship. Here, the constitutive equations formulated for the flow law and the evolutionary law have been incorporated into computer algorithms for predicting the multiaxial inelastic (creep) response of homogeneously stressed elements. Examples are presented to illustrate certain aspects of the constitutive model. Creep curves and viscoplastic flow surfaces are examined to demonstrate the model’s ability to capture the inelastic deformation response in advanced monolithic ceramic materials. In monolithic ceramics, creep deformation and creep rupture are generally controlled by the physical and chemical properties of the grain and grain boundaries. These microstructural phenomena, including the nucleation, growth, and coalescence of cavities, lead eventually to macrocracks which propagate and ultimately lead to component fracture. Much work continues in determining the exact mechanisms responsible for the observed creep deformation and rupture behavior of ceramics. An in-depth discussion of the micromechanical aspects of creep of ceramics is beyond the scope of this work. Here attention will focus on the macromechanical phenomena (specifically, creep deformation) that can be accounted for in the proposed model. Creep rupture is not considered in the model, although incorporating damage mechanics concepts into the present theory could yield a workable creep rupture model. This task is reserved for a future enhancement. Under isothermal conditions, a typical creep test entails abruptly applying a constant stress (or load) to a test specimen. The material response in this type of test is conveniently described in terms of strain vs. time. In a typical creep strain vs. time plot, the material response usually (but not always) exhibits three distinct regions of behavior. The first, denoted primary creep, is identified as the initial period during which the strain rate diminishes with time. Following the primary creep response, the strain rate stabilizes and remains constant for a (relatively) long period of time. This region is denoted as secondary, or steady-state, creep. In the third region, the strain rate accelerates, leading to specimen or component fracture (failure) or rupture. The response in this region is denoted tertiary creep. Many types of monolithic ceramics typically don’t exhibit tertiary creep behavior. Therefore, many constitutive equations formulated for these material systems appropriately describe only the primary and secondary creep regions. This is the case with the proposed model. However, the tertiary creep response (including creep rupture) can be added to the current model by incorporating continuum damage mechanics concepts. This task is reserved for a future enhancement. CONSTITUTIVE THEORY The complete theory was derived in detail in the previous manuscript by the authors (Janosik and Duffy, 1998). For brevity, the derivation of the constitutive theory will only be summarized here. The theory is derived from a scalar dissipative potential function attributed to Robinson (1978), which is identified here as . Under isothermal conditions, this function is dependent upon the applied Cauchy stress (ij) and internal state variable (aij), i.e., , ij ij K 2 1 n R m 2 F dF + H G dG F 1 c ~ 1 2 J2 r ~ 5 i j 3 1/ 2 (2) ~ I 1 parameters , c, and r( ) shown in equation (2) are presented in detail in the previous article (Janosik and Duffy, 1998) and will not be discussed herein. With the functions F and G (and hence ) completely defined, the flow law (i.e., the inelastic strain rate) and the evolutionary law are derived from the potential function. The flow law is derived from the potential function by taking the partial derivative with respect to the applied stress, i.e., (1) In this formulation, ij and ij represent second rank Cartesian tensors. Indicial notation is used with the convention that repeated indices imply summation. The parameters K, , R, H, n, and m are material constants related to viscoplasticity. The authors realize that several of these quantitites identified as material constants in the theory may be strongly temperature-dependent in a non-isothermal environment. However, for simplicity, the present work is restricted to isothermal conditions. A paper by Robinson and Swindeman (1982) provides the approach by which an extension can be made to non-isothermal environments. This task is reserved for a future enhancement to the current model. Specific macroscopic behavior (e.g., different behavior in tension and compression) is readily embedded in the model through the use of invariant theory. A three-parameter yield criterion originally proposed by Willam and Warnke (1975) for concrete serves as the threshold flow criterion, F, for the model ~ ~ ~ I1 , J 2 , J 3 advanced monolithic ceramics in practical engineering applications. Specifically, the proposed formulation permits the constitutive model to exhibit a sensitivity to the hydrostatic component of stress, and allows different behavior in tension and compression. The additional 1 c The functional form of the scalar state function, G, has similar mathematical formulation, following the framework of previously proposed constitutive models based on Robinson’s (1978) viscoplastic law. For frame indifference, the scalar functions F and G (and hence ) must be form invariant under all proper orthogonal transformations. Combining the principal stress invariants ~ ~ ~ ( I 1, J 2, J 3 for the scalar function F, and ^I 1, ^J2, ^J3 for the scalar function G) in an intelligent fashion allows the model to account for the viscoplastic response to general multiaxial loading conditions encountered when utilizing = i j (3) Here, the inelastic strain rate vector is the gradient (directed outward normal) to level surfaces of , similar to the structure encountered in classical plasticity. The evolutionary law is similarly derived from the flow potential. The rate of change of the internal stress with deformation history is expressed as i j = -h i j (4) where h is a scalar hardening function of the inelastic state variable (i.e., the internal stress) only. The complete multiaxial statement of the viscoplastic constitutive theory was presented in the previous manuscript by the authors. The remainder of this paper will focus on applying the theory to account for asymmetric tensile and compressive behavior, as well as sensitivity to hydrostatic stress exhibited by advanced monolithic ceramics. EXAMPLES This section presents theoretical predictions of the multiaxial creep response of homogeneously stressed elements obtained using the viscoplastic constitutive theory. The coupled system of differential equations for the inelastic strain, ij, and the state variable, ij, as expressed in the flow and evolutionary laws (equations (3) and (4), respectively), have been incorporated into computer algorithms. For a full multiaxial creep problem, solution requires integration of twelve coupled differential equations representing the constitutive law, i.e., six equations from the flow law and six equations from the evolutionary law. Three numerical examples are presented below to illustrate various aspects of the constitiutive model. In each of the examples, it is assumed that the material is initially in a virgin state, i.e., the centers of the flow surfaces lie at the origin of stress space. 0.02 0 M Pa 0.03 15 Example 1. Uniaxial Tension vs. Uniaxial Compression—Longitudinal Creep Curves. This example illustrates the model’s ability to qualitatively capture the asymmetric behavior in tension and compression exhibited experimentally by ceramic materials. The William-Warnke threshold stress parameters are chosen as t = 10 MPa (1.450 ksi), c = 100 MPa (14.503 ksi), and bc = 116 MPa (16.824 ksi). Equal magnitude uniaxial tensile and compressive stresses are used to generate the creep curves (longitudinal strain, 11) presented in Figure 1. Notice that the creep curves in this figure exhibit the classical behavior described previously in Example 2. Uniaxial Tension—Multiaxial Creep Curves and Inelastic Flow Surfaces. This example examines both creep curves and viscoplastic flow surfaces to illustrate the constitutive model’s ability to capture the inelastic (creep) deformation response of homogeneously stressed elements. For the uniaxial tensile case of 11 = 125 MPa (18.129 ksi), Figure 2 depicts the multiaxial components of the creep strain tensor, ij, obtained using the William-Warnke model with threshold stress parameters t = 10 MPa (1.450 ksi), c = 100 MPa (14.503 ksi), and bc = 116 MPa (16.824 ksi). Notice that here the entire inelastic creep strain tensor, ij, is represented; the creep curves in the previous figure depicted only the longitudinal strain 11. Here, it is observed that the largest strain is in the direction of the applied uniaxial tensile stress. The transverse strains, 22 = 33, are essentially neglible in comparison, and the other remaining strain components are equal to zero. = These quantities are consistent with stress having units of ksi (1 ksi = 6.895 MPa) and time measured in hours. While these viscoplasticity parameters remain constant throughout each of the examples which follow, those associated with the Willam-Warnke model, i.e., the Willam-Warnke threshold stress parameters t, c, bc, will vary within the limits imposed by the convexity requirement (i.e., 0.5 < rt /rc = 1.0). The permissible Willam-Warnke model parameters impart great flexibility in capturing a wide range of multiaxial material behavior. The examples that follow will demonstrate the ability of the constitutive model to qualitatively capture the essential features of the complex material deformation behavior. No attempt is made here to assess the accuracy of the model in comparison to experiment. It should be noted that the examples presented are intended to show trends only. A quantitative assessment is reserved for a later date, after the material constants have been suitably characterized for a specific ceramic material. 1 (5a) (5b) (5c) (5d) (5e) (5f) 1 = 1 200 M Pa 1 1 = 175 MP a 1 m = 350,000 H = 10,000 R = 3.0x10-4 n=4 m=4 b = 0.75 that they display a primary creep period followed by a region of steady state behavior. Notice also in this figure that the tertiary region is not included in the response generated by the current model, as indicated previously. It is evident in these creep response curves that the duration of primary creep varies inversely with the stress magnitude, i.e., lower stresses produce a longer duration of primary creep, while higher stresses result in a shorter region of primary creep. The asymmetry between the tensile and compressive (longitudinal) creep strain behaviors depicted in Figure 1 is consistent with experimental results reported in the literature. Luecke and Wiederhorn (1994) present findings from several authors who report that at equivalent stress, creep results for a particular ceramic in tension may be up to a hundred or more times greater than those for the same material in compression. Longitudinal Strain, 11 In addition to the Willam-Warnke threshold stress parameters discussed extensively in the development of the model in the previous manuscript, the viscoplastic material parameters m, m, n, b, R, and H, are needed to obtain the inelastic response predictions. Since there is not yet a complete data base for characterizing these material constants for a particular monolithic ceramic material, the following set of material parameters is adopted here: 25 =1 1 1 MP a 0 MPa 11 = 10 0.01 11 = 75 MPa Time (h) 0 0 -0.01 50 100 150 200 250 300 11 = -150 MPa 11 = -175 MPa -0.02 11 = -200 MPa -0.03 Figure 1 Predicted longitudinal creep strain curves (11) for uniaxial tensile and compressive states of stress with t = 10 MPa, c = 100 MPa, and bc = 116 MPa (1 ksi = 6.895 MPa). 0.03 0.03 11 0.02 11 0.02 0.01 0 0 -0.01 50 100 150 200 250 300 22 = 33 Strain, ij Strain, ij 0.01 Time (h) Time (h) 0 0 50 100 12 = 13 =23 = 0 200 250 300 22 = 33 -0.01 -0.02 150 11 =222 = 233 -0.02 12 = 13 =23 = 0 -0.03 -0.03 Figure 2 Predicted multiaxial creep strain curves (ij) for uniaxial tensile state of stress 11 = 125 MPa with t = 10 MPa, c = 100 MPa, and bc = 116 MPa (1 ksi = 6.895 MPa). Both the Willam-Warnke threshold function, F, and the constitutive equations (i.e., the flow and evolutionary laws) degenerate to the “simpler” underlying models (i.e., Drucker-Prager and von Mises, or J2, models) when certain limiting conditions are imposed. Here, specifically, it is illustrative to notice that the constitutive equations reduce to forms consistent with those of Robinson’s J2-dependent (von Mises) model. This is equivalent to assuming insensitivity to hydrostatic stress and identical behavior in tension and compression. Complete details can be obtained in Janosik (1998). Here, the results of implementing these same limiting conditions are presented as they apply to observations of the inelastic response of homogeneously stressed elements. Figure 3 depicts the multiaxial components of the creep strain tensor ij for the same uniaxial tensile stress state, 11 = 125 MPa (18.129 ksi), presented above. However, in this figure, the Willam-Warnke parameters are stipulated as t = c = bc = 10 MPa (1.450 ksi). This formulation is the equivalent of a J2-dependent model. In figure 3, it is again observed that the largest strain is in the direction of the applied uniaxial tensile stress. However, in this case, the transverse strains, 22 = 33, are equal in magnitude to 0.5 times the longitudinal strain 11. This appropriately reflects the effect of the Poisson’s ratio which is approximately equal to 0.5 in a ductile J2-dependent material. Taking a slightly different perspective, the changes in the inelastic state can be viewed with projections of the scalar function F. Figure 4 depicts inelastic flow surfaces projected onto the 11-22 stress space for the uniaxial tensile case 11 = 125 MPa (18.129 ksi) presented above. The load path is indicated in this figure. Here, again, the Willam-Warnke parameters are chosen as t = c = bc = 10 MPa (1.450 ksi) to represent a J2-dependent model. Each surface in this figure is one of a family representing distinct inelastic states. The largest surface represents the virgin state and corresponds to the initial stages of primary creep. Figure 3 Predicted multiaxial creep strain curves (ij) for uniaxial tensile state of stress 11 = 125 MPa with t = c = bc = 10 MPa (1 ksi = 6.895 MPa). Only the member of each family that passes through the stress point 11 = 125 MPa (18.129 ksi) is shown. Corresponding to each surface is an inelastic strain rate vector. As the size of the flow surfaces diminish, the magnitude of the inelastic strain rate vector decreases. Eventually steady state creep is attained where the size of the surface and the magnitude of the inelastic strain rate vector remain unchanged. The elliptical shape of the surfaces depicted in the 11-22 stress space is a result of the limiting assumptions imposed to achieve identical behavior in tension and compression. Figure 5 depicts the inelastic flow surfaces for this same stress state projected onto the -plane. Here, the member of each family that ~ passes through the point r( ) = 2J 2 along the positive 22 (ksi) 50 40 30 Load Path, 20 11 10 11 (ksi) 0 -50 -40 -30 -20 -10 0 -10 10 20 30 40 50 -20 -30 -40 -50 Figure 4 Inelastic states (F = constant) depicted in the 11-22 stress space for uniaxial stress state 11 = 125 MPa with t = c = bc = 10 MPa (1 ksi = 6.895 MPa). 1 1 2 2 3 Figure 5 Inelastic states (F = constant) depicted in the -plane for uniaxial stress state 11 = 125 MPa with t = c = bc = 10 MPa (1 ksi = 6.895 MPa). 1 axis is shown. Recall that the -plane is a deviatoric plane with no hydrostatic component of stress. The circular surfaces produced in the -plane by this formulation would appear as right circular cylinders in the three-dimensional Haigh-Westergaard principal stress space. As indicated in Figure 5, these surfaces would intersect along a line parallel to the hydrostatic axis in this stress space. Figure 6 depicts inelastic flow surfaces projected onto the 11-22 stress space for the uniaxial tensile case 11 = 125 MPa (18.129 ksi) with Willam-Warnke threshold stress parameters t = 10 MPa (1.450 ksi), c = 100 MPa (14.503 ksi), and bc = 116 MPa (16.824 ksi). Again, the member 22 (ksi) 50 11 0 -300 -250 3 -200 -150 -100 -50 (ksi) 0 -50 50 Load Path, 11 -100 -150 -200 -250 -300 Figure 6 Inelastic states (F = constant) depicted in the 11-22 stress space for uniaxial stress state 11 = 125 MPa with t = 10 MPa, c = 100 MPa, and bc = 116 MPa (1 ksi = 6.895 MPa). Figure 7 Inelastic states (F = constant) depicted in the -plane for uniaxial stress state 11 = 125 MPa with t = 10 MPa, c = 100 MPa, and bc = 116 MPa (1 ksi = 6.895 MPa). of each family that passes through the stress point 11 = 125 MPa (18.129 ksi) is shown. Here, the shape of the surfaces in the 11-22 stress space results from the Willam-Warnke threshold stress parameters imposed to achieve the asymmetric behavior in tension and compression. Figure 7 presents the inelastic flow surfaces for this same case in the -plane. These surfaces would appear as right tetrahedrons in the three-dimensional Haigh-Westergaard principal stress space. Example 3. Thin-Wall Pressure Vessel—Multiaxial Creep Curves and Inelastic Flow Surfaces. In this example, the qualitative change in the inelastic deformation response of a thin-wall pressure vessel resulting from incorporating a sensitivity to hydrostatic stress and asymmetric tensile and compressive behavior is presented. With the postulated normality structure, the direction of the inelastic strain rate vector for each inelastic state is directed along the gradient to the respective state’s surface of F = constant. One can easily view this in the predicted structural response of a thin-wall pressure vessel. Specifically, the stress path 11 = 222 = 125 MPa (18.129 ksi) is equivalent to the state of stress in a thin-wall pressure vessel if 11 is taken as the circumferential stress, 22 the axial stress, and 33 the radial stress. Abruptly applying an internal pressure such that F >> 0 and holding the state of stress fixed at the circumferential and axial stress values specified above allows the tube to deform inelastically. Figure 8 shows the multiaxial creep curves obtained for an isotropic material with Willam-Warnke threshold stress parameters t = c = bc = 10 MPa (1.450 ksi). This formulation is the equivalent of a J2-dependent material; it assumes insensitivity to hydrostatic stress and identical behavior in tension and compression. In this figure it is evident that ii 0. That is, 11 = -33 and 22 = 0, indicating inelastic incompressibility. This results from the assumptions of a J2-dependent theory. 22 (ksi) 50 0.02 -300 Strain, ij 0.01 -250 -200 -150 -100 11 0 -50 11 (ksi) 0 50 Load Path, 11 = 2 22 -50 Time (h) 0 -100 0 50 100 150 200 250 300 -150 -0.01 33 11 = -33 22 = 0 -0.02 -200 12 = 13 =23 = 0 -0.03 -250 -300 Figure 11 8 Predicted multiaxial creep strain curves ij) Figure Inelastic states (F = constant) depicted in (the for thin-wall pressure vessel ( = 2 = 125 MPa) 11 22 stress space for thin-wall pressure vessel ( 11 22 11 = t = MPa) = 10 MPa (1 MPa, ksi = 6.895 c = bc with 2with 22 =125 c = MPa). 100 MPa, and t = 10 bc = 116 MPa (1 ksi = 6.895 MPa). The changes in the inelastic state of the thin-wall pressure vessel as it creeps can be illustrated with projections of the scalar function F. Figure 9 depicts the changes in inelastic state for a J2-dependent material. The load path 11 = 222 = 125 MPa (18.129 ksi) is illustrated in this figure. Each surface in Figure 9 is one of a family representing distinct inelastic states. The largest surface represents the virgin state and corresponds to the initial stages of primary creep. Only the member of each family that passes through the stress point 11 = 222 = 125 MPa (18.129 ksi) is shown. Corresponding to each surface is an inelastic strain rate vector. As the size of the flow 22 (ksi) 50 surfaces diminish, the magnitude of the inelastic strain rate vector decreases. Eventually steady state creep is attained where the size of the surface and the magnitude of the inelastic strain rate vector remain unchanged. Note that the inelastic strain rate vectors do not have components. In contrast to the previous two figures obtained by applying the assumptions for an equivalent J2-dependent formulation, the following two figures represent inelastic deformation results for the same thin-wall pressure vessel incorporating both a sensitivity to hydrostatic stress and differing behavior in tension and compression. The Willam-Warnke threshold stress parameters are stipulated as t = 10 MPa (1.450 ksi), c = 100 MPa (14.503 ksi), and bc = 116 MPa (16.824 ksi). The multiaxial creep strain curves corresponding to this example are depicted in Figure 10. Here it is evident that ii 0. This is consistent with the theory developed in this series of manuscipts, since contraction of the flow law yields a nonzero result for the stipulated loading condition. Figure 11 depicts the inelastic flow surfaces projected onto the 11-22 stress space for the pressure vessel presented above. The load path 11 = 222 = 125 MPa (18.129 ksi) is indicated in this figure. Each surface again represents distinct inelastic states as the vessel deforms under an identical internal pressure of 11 = 222 = 125 MPa (18.129 ksi). Whereas the 22 components vanished in the J2-dependent formulation, it is evident that the 0.03 11 0.02 Time (h) 0 -0.01 40 30 Load Path, 11 = 2 22 20 10 -40 -30 -20 -10 0 -10 20 30 40 50 100 150 200 250 300 33 12 = 13 =23 = 0 (ksi) 10 0 -0.02 11 0 -50 22 0.01 Strain, ij 0.03 50 -20 -30 -0.03 Figure 10 Predicted multiaxial creep strain curves (ij) for thin-wall pressure vessel (11 = 222 = 125 MPa) with t = 10 MPa, c = 100 MPa, and bc = 116 MPa (1 ksi = 6.895 MPa). -40 -50 Figure 9 Inelastic states (F = constant) depicted in the 11-22 stress space for thin-wall pressure vessel (11 = 222 =125 MPa) with t = c = bc = 10 MPa (1 ksi = 6.895 MPa). inelastic strain rate vectors would have relatively large 22 components in the current formulation. Thus, the mode of inelastic deformation changes with sensitivity to hydrostatic stress and asymmetric behavior. Eventually, upon reaching steady state, the size of the surface and the magnitude of the inelastic strain rate vectors remain fixed. SUMMARY AND CONCLUSION This paper has presented numerical examples to illustrate the multiaxial viscoplastic constitutive theory developed by the authors in the previous manuscript. The first paper in this series focused on the formulation and derivation of viscoplastic constitutive equations for the flow law (strain rate) and the evolutionary law. The theory was derived based on a threshold function that exhibits a sensitivity to hydrostatic stress and asymmetric behavior in tension and compression. This paper has presented the results obtained after incorporating these constitutive equations into computer algorithms for predicting the multiaxial inelastic (creep) deformation response of homogeneously stressed elements. Three numerically simulated examples were presented with the intent to qualitatively illustrate the model’s ability to capture and predict the inelastic deformation response exhibited by isotropic monolithic ceramics at elevated service temperatures. A quantitative assessment is reserved for a later date, after the material constants have been characterized for a specific ceramic material. Incorporating this model into a non-linear finite element code would provide industry the means to numerically simulate the inherently time-dependent and hereditary phenomena exhibited by these brittle material systems in service. This task is also reserved for a future enhancement. REFERENCES Janosik, L.A., 1998, "A Viscoplastic Constitutive Theory for Monolithic Ceramic Materials," Master's Thesis, Cleveland State University, Cleveland, OH. Janosik, L.A.; and Duffy, Stephen F., 1998, “A Viscoplastic Constitutive Theory for Monolithic Ceramics—I,” Journal of Engineering for gas Turbines and Power, Vol. 120, No. 1, pp. 155-161. (ASME Paper 96–GT–368,). Luecke, W.E., and Wiederhorn, S.M., 1994 “Tension/Compression Creep Asymmetry in Si3N4,” Key Engineering Materials, Vol. 89-91, pp. 587-592. Robinson, D.N., 1978, "A Unified Creep-Plasticity Model for Structural Metals at High Temperature," ORNL/TM-5969. Robinson, D.N., and Swindeman, R.W., 1982, "Unified Creep-Plasticity Constitutive Equations for 2-1/4 CR-1 Mo Steel at Elevated Temperature," ORNL/TM 8444. Willam, K.J., and Warnke, E.P., 1975, "Constitutive Model for the Triaxial Behaviour of Concrete, Int. Assoc. Bridge Struct. Eng. Proc., Vol. 19, pp. 1-30.
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