Abstract
In this paper, we give an simple but approximate yield surface for single FCC crystals in Hill’s criterion form by Schmid’s law and nonlinear optimization theory. Assuming that all FCC crystallites in a polycrystal have the same (current) critical resolved shear stress for slip, we derive two closed but approximate yield functions through the orientational averaging of all FCC crystallites’ yield surfaces in the polycrystal. The effect of crystallography on the two yield functions are described by the orientation distribution function.
1. Introduction
The studies of plasticity on polycrystals may be divided into two classes: the mathematical theory of plasticity and physical theory of plasticity [1,2,3,4]. The mathematical approach of plasticity is a formalization of known experimental results and does not penetrate deeply into the physical process of plastic yielding. An alternative approach to the mathematical theory of plasticity is the physical approach of plasticity. A polycrystalline material is an aggregate of tiny crystallites separated by grain boundaries. The microstructure of the polycrystal includes grain orientations and the grain boundary structure. Plastic properties of the polycrystal are related to slip mechanisms of crystallites and the microstructure of the polycrystal.
In order to study the properties of the polycrystal, we take a representative volume element (RVE) from the polycrystal. Although the volume of the RVE is small, the RVE contains information of the crystallographic texture on the polycrystal. The earlier study of polycrystalline plasticity was conducted by Sachs [5] and Taylor [6]. Sachs assumed that all crystallites in a RVE have the same stress. Taylor assumed that all crystallites in a RVE experience the same deformation. Bishop and Hill [7,8] adopted Taylor’s model to calculate a yield function for an isotropic aggregate of cubic crystallites. Let denote a critical resolved shear stress. For an isotropic aggregate of FCC (face centered cubic) crystallites, assuming that all slip systems of cubic crystallites in a polycrystal have the same (current) critical resolved shear stress, the uniaxial tensile yield stresses should be under Sachs’ model and under Taylor’s model [9]. Maniatty et al. [10] employed the isotropic plasticity equivalent method, in which the actual stress tensor acting on an anisotropic material is transformed into a new stress tensor acting on an “isotropic plasticity equivalent” material, for obtaining an anisotropic yield function. Houtte [11] presented a method of obtaining the yield locus of textured polycrystals by constructing a data bank of the Taylor factors. Both Maniatty et al. and Houtte did not give closed expressions of yield functions with the effect of the texture coefficients.
The micromechanics of polycrystals is interesting only because one can measure the orientations of crystallites by orientation imaging microscopy or by X-ray diffraction. As we know, using the same manufacturing procedure, one can never make two polycrystalline samples with identical crystalline orientations. One can only make samples which seem macroscopically identical. Since the statistical information on the microstructure of a polycrystal can be described mathematically by the orientation distribution function (ODF) and since the plastic deformation of polycrystals involves slips inside crystallites, we will develop a statistical yield function with the effects of the orientation distribution function (ODF) and the the critical resolved shear stress of crystallites.
In this paper, we provide a simple method to obtain two closed but approximate yield functions with the effect of the texture coefficients for the RVE, where the volume average (i.e., orientational averaging) of all crystallites’ yield surfaces is taken as a (macroscopic) yield function of the RVE. Using the physical approach to FCC crystallites, we derive a yield surface of single FCC crystals in Hill’s criterion form by Schmid’s law and nonlinear optimization theory, give a plastic anisotropy tensor of FCC crystallites with orientation , and obtain the volume average of all crystallites’ yield surfaces in the RVE to obtain two closed but approximate yield functions for the RVE. The two yield functions are based on the assumption that all crystallites in the RVE have the same (current) critical resolved shear stress for slip. The effect of crystallography in the two yield functions is described by the texture coefficients. The first yield function is based on Sachs’ model. The second yield function is based on the assumption that the effect of the ODF on the perturbation stress is, up to the terms, linear in the texture coefficients. Man [12,13,14] found that for orthorhombic aggregates of cubic crystallites, a macroscopic yield function of the RVE, up to terms, is linear in the texture coefficients.Our two yield functions are different to Man’s yield function [12,13] in three aspects: (1) the two yield functions are for an anisotropic aggregate of cubic crystallites, but Man’s yield function is for an orthorhombic aggregate of cubic crystallites; (2) we can determine the relations between two material parameters and the (current) critical resolved shear stress through some physical assumptions, but Man’s yield function contains two unspecified parameters ( and ) and Man’s yield function is independent of the physical model; (3) Man’s yield function includes the effect of the ODF being, up to terms, linear in the texture coefficients, while our second yield function is quadratic texture dependence.
The critical resolved shear stress is related to the crystalline dislocation mechanism, the crystalline size, and the grain boundary structure. In this paper, however, we do not discuss the hardening process of the critical resolved shear stress during plastic deformation. Herein, we only study the constitutive form of the yield function of the FCC polycrystal for the given ODF and the given .
2. Approximate Yield Surface of FCC Crystal in Hill’s Criterion Form
Assume that a fixed spatial Cartesian coordinate system is chosen. To describe the orientation of a FCC crystallite in the RVE, we pick as a reference a FCC crystallite , whose three four-fold axes of rotational symmetry coincide with the Cartesian coordinate axes. The orientation of any crystallite in the RVE is then specified by rotation , which takes the reference crystallite to the configuration of the crystallite.
By Schmid’s law, we know that yielding for the reference crystallite would begin on a slip system (combination of a slip plane and a slip direction) when the resolved shear stress on this slip plane and in the slip direction reaches a critical value , where the unit normal of the slip plane is denoted by and the unit vector of the slip direction is denoted by with . When volume average stress components in the reference crystallite are denoted by , the shear stress on the slip plane and in the slip direction should be . Because the shear stress of the reference crystallite on its slip planes and in its slip direction satisfies , the stress components of the reference crystallite are in space :
where . The yield surface of the reference crystallite should be
The space given in (1) is surrounded by a set of yield functions ( linear in stress components.
Assume that the space in (1) can be surrounded approximately by a yield surface
where SO(3) is the second-order identity tensor for the reference crystallite , is called the plastic anisotropy tensor [4] of the reference crystallite with the minor and major symmetries, is the volume average stress in the reference crystallite . Any hydrostatic stress does not change the shear stress value of the reference crystallite because by for all Hence, we have
which leads to the traceless condition for any pair of indices k and l.
When the reference crystallite and the traction acting on the reference crystallite have a rotation , the stress tensor in the reference crystallite becomes , and the plastic anisotropy tensor becomes with constitutive restriction:
where the three four-fold axes of rotational symmetry of the reference FCC crystallite coincide with the Cartesian coordinate axes. Considering
and , we have in (5). Assuming that all crystallites in the RVE have the same (current) critical resolved shear stress for slip, we have the plastic anisotropy tensor of the crystallites with orientation :
If we use to denote the volume average stress of the crystallites with orientation , the yield surface for the crystallites with orientation can be expressed as
by (5) and (7). Since the reference FCC crystallite has the octahedral symmetry O, the plastic anisotropy tensor should satisfy for each rotation tensor , which with the minor and major symmetries of reads [15]
where is the matrix form of in Voigt’s notation (i.e., indices and in are denoted by indices I and J of with convention ,,, ,,; for instances, , ), , , and are the material parameters of the reference crystallite . The plastic anisotropy tensor in (9) can be decomposed into [16]
where and are the matrix form of the following tensors in Voigt’s notation, respectively
and are isotropic fourth-order tensor bases, is a fourth-order tensor basis for cubic crystals. The traceless condition makes the plastic anisotropy tensor in (10) become
because of which makes that
holds.
Putting (12) into (3), we find a yield surface of the reference crystallite in Hill’s criterion form
because
where and
When , in (12) is an isotropic tensor whose corresponding yield surface is von Mises’ yield criterion.
For the reference FCC crystallite , the slip occurs on {111} planes in <110> directions. The unit normal of the slip planes and the unit vector of the slip directions constitute the 24 slip systems [9]
in which there is for each slip system. Substituting (17) into in (1), one can obtain 24 inequalities that are linear in stress components
which constitute the the stress space .
Now we assume that the stress space in (1) can approximately be surrounded by a function in Hill’s criterion form (14). In order to determine and in (14), we introduce two subspaces of in (1)
and two subspaces in
The maximum and minimum values of and in (20) are defined by
where we determine and in (14) through multi-axial tensions and pure shears, respectively. The proceeding maximum and minimum problems in (21) belong to nonlinear optimization problems. The relations (19) and (20) are used to obtain the best fitting of the FCC crystal yield surface .
We use Microsoft Excel to solve the problems (21) with (20) and (18). Then we obtain the maximum and minimum values of and
Putting and into (14), we find a yield surface of FCC crystals for the reference FCC crystallite
which is just the same as that of Maniatty et al. [10].
Since the goal of the paper is to estimate a macroscopic yield function of the RVE, let us choose and in (14) as follows:
3. Yield Function and Effective Plastic Anisotropy Tensor of RVE
The crystallographic texture of a polycrystal is described by the orientation distribution function (ODF). The ODF is used to describe the probability density of finding a crystallite with orientation in the RVE. The mechanical anisotropy of the RVE is caused mainly by its crystallographic texture and plastic anisotropy of crystallites. Let be the orientation distribution function. If SO is the space of the square-integrable complex-valued functions, SO can be expanded as an infinite series in terms of the Wigner -functions [17,18]
where , are the texture coefficients, denote the complex conjugate of the complex number , . The Wigner D-functions constitute an orthogonal basis in SO. The texture coefficients that we shall need can easily be measured by -ray diffraction. The texture coefficients are related to Roe’s coefficients by formula [19]
The micromechanics of polycrystals becomes interesting only because one can obtain statistical information of the orientations by X-ray diffraction or measure the orientations of pcrystallites, pointwise, by orientation imaging microscopy. For the measurement of X-ray diffraction, one measures the specimen surface’s, depth’s, and depth’s texture coefficients, respectively, by sanding the specimen of sheets. The mean values of the texture coefficients on the surface, depth, and depth of the specimen are taken as the texture coefficients of the specimen. For the measurement of the orientation imaging microscopy, one obtains the orientation (Euler angles ) of each crystallite in the specimen. Since the FCC polycrystal can be taken as an aggregate of cubic crystallites (i.e., ), the texture coefficients of the specimen are given by [20]
with
where and O is the group of cubic crystal symmetry.
Let be the volume average stress components of the RVE. By definition of the ODF, the orientational (volume) average stress can be obtained by
where is the Haar measure on SO with SO is the volume average stress tensor of crystallites with orientation in the RVE. When is defined by Roe’s notation [18], there is .
When all crystallites in the RVE have the same (current) critical resolved shear stress for slip, the yield surface of crystallites with orientation is determined by (26). By the ODF definition, the volume average of all crystallites in the RVE can be expressed as
which can be taken as the macroscopic yield function of the RVE.
If the macroscopic yield function can be expressed as
in Hill’s criterion form, then we call in (34) the effective plastic anisotropy tensor of the RVE. The effective plastic anisotropy tensor gives the relationship between the macroscopic yield function and the volume average stress of the RVE. One recipe to compute the effective plastic anisotropy tensor in (34) is by way of putting (8) into (33)
4. Volume Average of Plastic Anisotropy Tensor
The basic assumption for Sachs’ model [5] is that all crystallites in the RVE experience the same state of stress (i.e., SO(3)). Substituting into (35) reads . Since the equation holds for each , the effective plastic anisotropy tensor has to be the volume average plastic anisotropy tensor of the RVE
by (25).
From the results given by Huang and Man [21] and Huang [16,22], we know
because of and being isotropic fourth order tensors and
because of the relation [19]
where is a fourth-order tensor. For an anisotropic aggregate of cubic crystallites, in (38) is totally symmetric (i.e., for any permutation of ) and traceless with non-trivial components [21]:
and
Here and denote the real and imaginary parts of the complex number , respectively. is a real number because of (28)2.
Putting (37) and (38) into (36), we obtain an effective plastic anisotropy tensor of the RVE under the Sachs’ model
with
The texture coefficients above can be measured by the -ray diffraction and inversion of pole figures (Roe, 1965 [18]). Obviously, the effective plastic anisotropy tensor satisfies the traceless condition because of . Substituting (42) and (15)1,2 into (34), we obtain a macroscopic yield function of the RVE
where
The macroscopic yield function of the RVE with a group of texture symmetry can be obtained from the constraints imposed by on the texture coefficients. For instance, if the coordinate axes are the two-fold axes of orthorhombic symmetry of the texture, then for odd m and for all m. Substituting these restriction into (44) and (41), we obtain the macroscopic yield function of the RVE in the Hill’s criterion form
for an orthorhombic aggregate of FCC crystallites, where
and in (41) are determined by the texture coefficients. and in (45) are dependent on the (current) critical resolved shear stress . The formula (46) is the same as that of Man [12,13] in form. However, Man’s yield function is independent of the physical model; hence and for Man’s yield function are two unspecified material parameters.
5. Yield Function with Quadratic Texture Dependence
Under Sachs’ model, the effective plastic anisotropy tensor is the volume average plastic anisotropy tensor of the RVE. Man’s yield function [12,13] and the yield function (46) contain the effect of the ODF only being, up to terms, linear in the texture coefficients, which may not suffice for strongly textured polycrystals [20]. In this section, we will establish a new physical model for deriving a macroscopic yield function of the RVE. The macroscopic yield function delineates the effect of the crystallographic texture on the plastic anisotropy up to terms quadratic in the texture coefficients.
Considering the collection of crystallites with orientation in the RVE and using to denote the volume average stress in these crystallites, we have the average perturbation stress of these crystallites
where is given in (32). We assume that the average perturbation stress of crystallites with orientation are governed by a constitutive relation of the form
with constraint
Similar to the process of deriving the HV-V model given by Huang and Man [21], the average perturbation stress of the crystallites with orientation can approximately be expressed as
where we consider the effect of the ODF to being, up to terms, linear in the texture coefficients,
and is an unspecified material parameter. From (37) and (38), we know that in (52) satisfy the relation (51).
By means of the relations (37) and (38), we can complete the following integrations and obtain the volume average value on (55)
Substituting (36), (42), (57), and (58) into (54), we obtain the effective plastic anisotropy tensor for anisotropic aggregates of FCC crystallites with quadratic texture dependence
with
where because of (43). Substituting (59) into (34), we obtain a macroscopic yield function of the RVE
where we discard terms in (59) and
The effective plastic anisotropy tensor in (59) satisfies the traceless condition .
6. Discussion and Example
When the yield function is in Hill’s criterion form, the Taylor factor for an orthorhombic weakly textured aggregate of FCC crystallites can be expressed as [14]
where is a uniaxial tensile yield stress.
Under Sachs’ model, we obtained the macroscopic yield function (46) for an aggregate of FCC crystallites. For uniaxial tensile problems, the yield function in (46) becomes or
from (47). When the RVE is an orthorhombic aggregate of FCC crystallites, there are and (Roe, 1965 [18]) in (41). From (41), (45) and (29), we rewrite (64) into
which is close to the result (63). However, the derivation of (65) is much simpler than that of (63) because the computation of the Taylor factor for a textured polycrystal is very complicated and time consuming.
The parameter in (62) can be determined by an experiment. For instance, from the relation of an isotropic polycrystal (aluminum) stress–strain curve and a single crystal stress–strain curve, Taylor [6] found that agrees with the experimental data very well. Taking we obtain by solving (62)1 and then get and from (62)2,3. For an orthorhombic weakly textured aggregate of FCC crystallites, if we discard the terms of the texture coefficients in (61), similar to the procedure of deriving (46) and (64) from (44), we obtain the yield stress of uniaxial tension
The formula above is almost the same as (63). To check the form of the expression (66), we give one example as follows.
Example of yield stress under uniaxial tension of sample :
Take an example from a metal sheet with the rolling direction as shown in Figure 1. To obtain the expression of the uniaxial yield stress and the rolling direction , we give the stress tensor of a uniaxial stress on as follows
where , . Similar to the derivation of (66), for an orthorhombic weakly textured aggregate of FCC crystallites, putting in (67) and in (29) into (61) and after discarding the terms of the texture coefficients, we obtain the yield stress of the uniaxial tension sample as follows:
Figure 1.
Samples of metal sheet.
Yu Xiang [23] in the doctoral dissertation gave the experimental data on two aluminum alloys (AA5754 hot band, AA3105 O-temper). As shown in Figure 1, uniaxial test samples were cut with tensile axis with the rolling direction (RD) . For each tensile direction, measurements were made on two samples to obtain the flow stress at 4% longitudinal plastic strain. The experimental results are listed in Table 1, where the data and of Xiang’s Experiment 1 and Experiment 2 are labeled with superscripts (1) and (2), respectively, and the subscript indicates a sample with tensile axis making an angle with the rolling direction (RD) shown in Figure 1. The texture coefficients of the two alloys were measured by X-ray diffraction as shown in Table 2.
Table 1.
Flow stresses (MPa) of two aluminum alloys.
Table 2.
Texture coefficients of two aluminum alloys.
To determine in (68) for the aluminum alloys from Xiang’s experimental data, we introduce an objective function as follows:
By the method of least squares, we solve the equation and obtain the critical resolved shear stress of the FCC crystals for the two aluminum alloys
Putting the fitted values in (70) and the texture coefficients in Table 2 for the two alloys into (68), we plot the fitting results of the yield stress on the uniaxial tension sample as shown in Figure 2. The expression (68) of the yield stress on the uniaxial tension sample can fit Xiang’s experimental data on two aluminum alloys (AA5754 and AA3105) very well.
Figure 2.
Experimental data of Xiang and fitting results of (68).
7. Conclusions
In this paper, we provide a simple method to obtain two closed but approximate yield functions with the effect of the texture coefficients for the RVE, where the volume average (i.e., orientational averaging) of all crystallites’ yield surfaces is taken as a (macroscopic) yield function of the RVE. Through theoretical analysis, we draw the following important conclusions:
- Assuming that all crystallites in the RVE have the same (current) critical resolved shear stress for slip and employing Schmid’s law and the nonlinear optimization theory, we give a plastic anisotropy tensor of the FCC crystals with orientation and obtain the volume average of all crystallites’ yield surfaces in the RVE.
- By the Microsoft Excel, we solve nonlinear optimization problems and obtain an approximate plastic anisotropy tensor and a yield surface of FCC crystallites with orientation.
- For an orthorhombic weakly textured aggregates of FCC crystallites, we obtain two yield stresses of uniaxial tension, respectively.
- Through an example, we obtain the yield stress under the uniaxial tension on sample . We find that the expression of the yield stress can fit Xiang’s experimental data very well.
Author Contributions
Conceptualization, L.Z.; software, T.Z.; formal analysis, L.Z. and G.M.; investigation, G.M.; resources, Z.L.; data curation, M.H.; writing—original draft preparation, L.Z. and M.H.; writing—review and editing, T.Z. and Z.L.; project administration, Z.L. All authors have read and agreed to the published version of the manuscript.
Funding
This research was funded by the Jiangxi Graduate Education and Teaching Reform Research Project (Awards Nos. JXYJG-2021-057) and the National Natural Science Foundation of China (Awards Nos. 51568046).
Data Availability Statement
The data of this study are available from the corresponding author upon request.
Conflicts of Interest
The authors declare no conflict of interest.
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