1. Introduction
One of the biggest challenges in material sensitive design is to accurately and reliably predict the fundamental mechanical properties of materials. However, the physical properties such as tensile strength
ft and fracture toughness
KIC are not fixed or deterministic, and fluctuate in certain range, which has been well recognized recently [
1,
2,
3].
The inevitable variation in mechanical property of materials is mainly due to the heterogeneity of microstructure, defects like pores and the activation of various fracture mechanisms during the crack-microstructure interactions [
4]. For polycrystalline brittle materials such as fine-grained ceramics [
5,
6,
7] and coarse-grained rocks [
8,
9,
10], the average grain size
G has a profound influence on material properties including
ft and
KIC. For composites and 3D-printed scaffolds [
11], their unit cells have a similar role as that of
G.
Nonlinear elastic fracture of those solids initiated from shallow defects comparable to their grain sizes can bring out significant information on the inherent relationship between microstructure and material properties. Besides separate influence on
ft and
KIC, the effect of
G on the combined parameter 0.25*(
KIC/
ft)
2, commonly known as characteristic crack size
a*
ch indicating the transition from
ft-controlled to
KIC-controlled fracture of brittle solid [
12,
13], is becoming increasingly important. Taylor has done numerous studies on characteristic length
lch, proportional to
a*
ch, and proposed the world-renowned theory of critical distance (TCD) [
14,
15,
16,
17,
18,
19]. It has been found that the
lch varies from 1 to 10 times of grain size
G depending on the materials. Generally speaking,
lch = (3–4)
G can be adopted for various fine-grained ceramics. More recently, we reanalysed the fracture measurements data on four fine-grained ceramics with
G from 2 to 20 μm and on two coarse-grained rocks with
G = 2.5 and 10 mm, and also found a semi-quantitative relation of
a*
ch ≥ 3
G [
7,
10].Therefore, an explicit relationship between
a*
ch and
G is an urgency need not only for the fundamental knowledge of microstructure-driven material research, but also for the safe design application.
For fracture data analysis methods, the common practice is that fracture strength is first obtained from experiment and then fitted by various fracture models, and the scatters are usually indicated by the maximum and minimum values but rarely described with a specified reliability [
20,
21,
22,
23,
24,
25,
26]. The problem is that the models cannot describe the scatter of physical properties or fracture strength with specified reliability. In addition, many parameters in the models are fitting parameters which carry little physical significance.
In this study, five groups of fracture measurements on ceramics specimens with
G from 2 to 20 μm and containing different initial defects from 100 nm to 800 μm [
27,
28] were reanalyzed to determine the relative characteristic crack size
C =
a*
ch/
G. Based on this, a non- linear elastic fracture mechanics (non-LEFM) analytical model is proposed to predict
ft and
KIC of ceramics as function of grain size
G from common fracture measurements, and to predict fracture strength of specimens with and without small defects if
ft or
KIC are available. Instead of curve fitting, the common normal distribution was used to analyse the fracture behaviour of ceramics to consider the scatters of physical and mechanical properties.
2. Determination of the Relative Characteristic Crack Size in Non-LEFM Model
Based on our previous work [
7], fracture strength of ceramic specimens containing small flaws/cracks can be assessed by the following formula,
where the combined parameter
C⋅
G =
a*
ch = 0.25(
KIC/
ft)
2 is a material constant defined by the intersection of two fracture criteria
KIC and
ft, and
σN is the engineering stress without consideration of the influence of initial crack size
a.
Although Weibull distribution has been widely used to determine the fracture behavior of materials, its role has usually been confined to fit experimental data rather than providing predictive insight into material properties (e.g.,
ft and
KIC) and their experimental scatters [
4]. In our previous study [
7,
10], another common statistical analysis method of normal distribution has been used to analyze experimental data of ceramic fracture after roughly assessing the relative characteristic crack size
C (=
a*
ch/
G) at intervals of 0.25. In this study, we accurately determine the
C value by continuously changing its value instead of interval.
The average grain size G is the microstructure characteristic of a polycrystalline material which can be statistically measured separately.If the C is a fixed value, Equation (1a) can be linearized by considering σN and 1/[1 + a/(C⋅G)]0.5 as ordinate and abscissa respectively, then it can be used in conjunction with the common normal distribution to make probabilistic analysis on ft with 96% reliability. That is, if an experimental data (σN, a) is measured, the ft from Equation (1a) becomes a single parameter after giving C a fixed value. Having numerous pairs of values of original crack a and engineering stress σN obtained from specimens with different α ratio (= a/W, W is the beam/specimen height), the data points (σN, 1/[1 + a/(C⋅G)]0.5) obtained can be plotted with these quantities considered as ordinate and abscissa respectively. Using Equation (1a), a group of ft values can be easily statistically analysed by normal distribution mehthodology.
Similarly, the following equation can be obtained by substituing the relation
C⋅
G = 0.25(
KIC/
ft)
2 into Equation (1a), which is used to calculate
KIC value from fracture measurement (
σN,
a). Similarly, Equation (1b) combined with normal distribution can be used to do statistical analyses of
KIC values from experimental measurements data if the
C is a fixed value.
Therefore, a determined value of
C urgently needs to be included in the two formulas of Equation (1). For this reason, the ralative characteristic crack size
C (=
a*
ch/
G) independent of grain size
G is assessed based on the experimental data (
σN,
a) on five ceramics with different
G from 2 to 20 μm. In total, 14 experimental data points (
σN,
a) of the Sialon with average grain size
G = 2 μm, 29 points of the SiC with
G = 3 μm, 25 points of Si
3N
4 with
G = 3 μm, 16 points of Si
3N
4 with
G = 4 μm, and 42 points of Al
2O
3 with
G = 20 μm, were digitized from the reference [
28].
Based on the fracture measurements (σN, a) of the five ceramics considered in this study, each group of ft values from Equation (1a) and KIC values from Equation (1b) was analyzed using two ways respectively to ensure reliability of analyzed results.
Figure 1 illustrates the evolution of standard deviation
σf of tensile strength
ft from Equation (1) as the relative characteristic crack size
C (=
a*
ch/
G) varies continuously.
C0 is defined as the critical value of
C signifying the
σf transitioned from decrease to increase. That is the
C0 value is determined by the condition that the
σf value is minimum. When the relative characteristic crack size
C gradually deviates from the
C0 value,
σf increases accordingly. According to the analyzed results of the five ceramics with different
G from 2 to 20 μm, it can be found that
C0 value is not dependent on grain size and fluctuates in a range from 2.8 to 4.7.
The largest number of experimental data points selected in this analysis is 42 from Al2O3 fracture, and the minimum number is mere 14 from Sialon. Considering the effect of the fewer number of data points (14 to 42 points) in each group of fracture measurements, we take the average of C0 values (i.e., 3.380 in this analysis) obtained from the fracture measurements of the five ceramics as the determined value of C, which at least should be one of the accepted and reasonable ways.
For the analysis of
ft distribution in
Figure 1,
ft is derived from fracture measurement data (
σN,
a) through Equation (1a), in which
σN and 1/[1 +
a/(
C⋅
G)]
0.5 follow a linear relation and
ft in MPa is the slope of the straigth line through the origin. For each data point (
σN,
a), the angle between the abscissa and the straight line through the origin and the considered point approaches 90° because the tangent of angle indicating
ft value is usually around several hundred. Therefore, any tiny error in the degitization of data point (
a,
σN) can result in significant fluctuation in the corresponding
ft value.
For this reason, we tried another statistic method to determine the
C value based on the same five groups of ceramic fracture measurements.
Figure 2 illustrates the evolution of the sum of distances of all the experimental points to the mean line indicating the average of
ft values from Equation (1a) as
C varies continuously.
C0 value is determined by the condition that the sum of distances by normal to the mean line is minimum. It is evident that the sum of the distances gradually increases when the
C deviates from
C0. It can also be found that
C0 value is not dependent on the grain size
G and flucturates in a range from 2.6 to 4.3. Again, we took the average of
C0 values obtained from the five different ceramics fracture as the determined
C value, i.e., 3.1788 in this analysis.
Figure 3 illustrates the evolution of standard deviation
σk of
KIC from Equation (1b) determined by normal distribution as the relative characteristic crack size
C (=
a*
ch/
G) varies continuously for the five ceramics, and the
C0 value is determined by the condition the
σk is minimum. The same as above,
C0 value is not dependent on the grain size
G and flucturates in narrower range from 2.7 to 4.1 in comparison to the results of
ft distribution. The average of
C0 values obtained from the five different ceramics fracture is 3.1426 in this analysis.
Figure 4 illustrates the evolution of the range of (
KIC)
max–(
KIC)
min from Equation (1b) as the relative characteristic crack size
C (=
a*
ch/
G) varies continuously for the five ceramics, and the
C0 value is determined by the condition the range is minimum. Again, the
C0 value is not dependent on the grain size
G and flucturates in narrower range from 2.6 to 4.0 in comparison to the results of
ft distribution. The average of
C0 values obtained from the five different ceramics fracture is 3.1288 in this analysis.
According to the above analyses based on the fracture measurements of the five ceramic with largely different G, the relative charateristic crack C (= a*ch/G) value is indeed not dependent on the grain size G, and is eaual to 3.380 and 3.1788 obtained from ft distribution, and 3.1426 and 3.1288 from KIC distribution. It should be noted that the characteristic crack size a*ch = C⋅G is a specified crack indicating the transition from ft-controlled fracture to KIC-controlled fracture. Furthermore, the dominant non-LEFM mechanism of brittle materials such as ceramic should have relation to the defects in solids, which may be linked to microstructure characteristic G. If one quantitatively links the specified crack length a*ch to the material microstructure characteristic G, from the perspectives of mathematics and physics the relation of a*ch = π⋅G between the two should be a good choice under condition of C ≈ 3.1–3.4 from the above ft and KIC distribution analyses. In addtion, the C values from KIC distribution is more stable than those from ft distribution, which will be proved in the following section. For simplicity and consistency between ft distribution and KIC distribution, C0 = a*ch/G = π is selected in this study.
3. Probabilistic Strength and Fracture Toughness Analyses
Following the determination of the relative characteristic crack size
C = π based on the fracture behaviour of five ceramics with
G from 2 to 20 μm, Equation (1) can now be rewritten as follows.
The dimensionless
η(
a,
G) and equivalent length
Le (
a,
G) in Equation (2) are wholly determined for a specified sample. For any group of ceramic specimens, the seemingly randomly varied fracture measurements data (
σN,
a) can be used to obtain a group of
ft value using Equation (2a) and
KIC values using Equation (2b) which can be easily analysed by normal distribution to get corresponding mean and standard deviation. With the mean
μf and standard deviation
σf of
ft distribution, Equation (2a) can be rewritten to include the mean and upper and lower bounds with 96% reliability indicating
ft scatter during fracture behaviour.
Similarly, Equation (2b) can be rewritten as follows.
The problem of the most existing probabilistic models is that they do not consider the scatters of
ft,
KIC and fracture strength
σN prior to experimental measurements [
4]. After determinations of the corresponding mean and standard deviation, three
σN–
η(
a,
G) linear relations from
ft distribution and three
σN–
Le(
a,
G) straight lines based on
KIC distribution, can be plotted together including the mean line and upper and lower bounds indicating both
ft and
KIC scatters.
In
Figure 5,
Figure 6,
Figure 7,
Figure 8 and
Figure 9, we take the five ceramic-fracture cases as examples to illustrate the combined application of the non-LEFM model Equation (3) and the normal distribution, and to check the validity and reliability of the
C = π. For each group of ceramic fracture,
ft normal distribution illustrated in
Figure 5a–
Figure 9a and
KIC normal distribution in
Figure 5b–
Figure 9b are evaluated from the same experimental measurements (
σN,
a). Then the three predicted linear relations from Equation (3a) using
μf and
σf of
ft distribution are shown in
Figure 5c–
Figure 9c, and the three predicted straight lines from Equation (3b) with the
μk and
μk ± 2
σk from
KIC distribution are illustrated in
Figure 5d–
Figure 9d.
Obviously, both ft and KIC with 96% reliability can be successfully deduced from the seemingly randomly varied experimental data points (σN, a). It can also be seen that the middle straight lines indicating the mean values of ft or KIC are almost the same as the corresponding fitted curves respectively. As we all know, the commonly used curve fitting methodology cannot describe the experimental scatter of fracture behaviour, but the proposed model can provide more scientific descriptions. This adds a significant understanding for the fracture of ceramic with and without small defects. Similarly, the scatters of fracture strength σN due to the stochastic characteristic of microstructure and the activation of various fracture mechanisms during the crack-microstructure interaction cannot be identified by the common curve fitting methodology.
Because the
μf and
σf values are constants, the corresponding slopes of the three straight lines of
σN–
η(
a,
G) relation indicating mean and upper and lower bounds are kept as constants as
η(
a,
G) increases in
Figure 5c–
Figure 9c, leading to more
σN scatter, which matches very well the experimental results reported in the literature [
27,
28]. This indicates that a specimen with higher
η(
a,
G) value will have larger fluctuation of
σN during fracture. That is larger specimen has larger
σN scatter which is absolutely reasonable in physics concept. Here, it should be noted that the percentage of
σN variation keeps constant in theory for various specimens with different
η(
a0,
G) as the mean and standard deviation are constant. The same conclusions can also be observed from the corresponding results obtained from
KIC distribution in
Figure 5d–
Figure 9d.
It should be noted that the two linear relations of
σN–
η(
a,
G) and
σN–
Le (
a,
G) pass through their respective origins, which are fixed points from perspectives of mathematics and physics. During the process of application, this is very useful to helping determine the slopes of the linear relations, which indicate the
ft or
KIC values. In addition, it can be seen that
KIC normal distribution is better than the
ft normal distribution from the histograms for Sialon, SiC and Al
2O
3 cases, and
KIC and
ft normal distribution are similar for the other two cases. Thus, it is reasonable that the determination of
C value (=π) in
Section 2 thought more of the
KIC analyses.
4. Probabilistic Prediction of Ceramic Facture
By employing the two concepts of dimensionless η(a, G) and equivalent length Le (a, G), the nonlinear relation in Equation (1) for assessing the fracture strength of ceramic specimen is linearized in relation as listed in Equation (2). The non-LEFM model combined with the common normal distribution can easily deduce ceramic’s ft and KIC with a specified reliability from the seemingly randomly varied fracture measurements (σN, a) as shown in Equation (3).
In fact, the linearized non-LEFM model with a specified reliability or Equation (3) can be conveniently transformed to an application model in nor-linear relation of
σN–
a for finally predicting the fracture strength
σN. If corresponding mean and standard deviation of material strength
ft or fracture toughness
KIC are available, the fracture strength of notched specimens with and without small defects can be easily predicted with a specified reliability through Equation (3). Using the values of
ft property obtained and shown in
Figure 5a–
Figure 9a, here we take Equation (3a) as an example to show how to apply the model in nonlinear relation for predicting
σN with a specified reliability.
The three predicted
σN–
a curves with mean and upper and lower bounds are shown in
Figure 10 together with the experimental data points. For comparison, the fitted curves for the nonlinear relationship of
σN–
a using Equation (3a) are also added to the figure. A direct comparison between the experimental results and the predicted curves shows that the non-LEFM model or Equation (3a) can reliably predict the fracture of notch ceramics as the predicted curves with 96% reliability cover all the data points. In addition, the middle curve indicating the mean of
ft value is more appropriate than the best fitted curve in each case. More importantly, those
σN variations are inevitable for ceramic fracture. The proposed model can describe the
σN scatter with a specified reliability, which is beyond the job of common curve fitting.
5. Discussion
In most of the existing probabilistic models, the fracture measurements data (a,σN) is usually first obtained from experiment and then fitted by linearized formula to get ft and KIC values. The problem of the most existing models is that they do not allow the scatters of ft and KIC data to be predicted before the experimental testing. As we all known, it is easy to establish a normal distribution for a group of data (e.g., ft or KIC values) with a specified reliability if a group of samples without defects or cracks are tested. But such a practical application soon becomes impractical for a wide crack range from the ft-controlled fracture over non-LEFM to finally the KIC-controlled fracture. The non-LEFM model in Equation (3) removes the need of curve fitting for fracture measurements data, and considers the scatters of mechanical properties ft and KIC through the upper and lower bounds with 96% reliability.
In the model, the microstructure characteristic
G of ceramic is explicitly linked to both
ft and
KIC. In the present study, the five ceramics, Sialon, SiC, Si
3N
4 with
G = 3 μm, Si
3N
4 with
G = 4 μm and Al
2O
3, were considered, and they have hugely different grain size
G ranged from 2 to 20 μm. Since
a*
ch = 0.25(
KIC/
ft)
2, they also have different characteristic crack size
a*
ch values due to obvious difference in material properties
ft and
KIC. Most recently, we studied the relative characteristic crack size
C =
a*
ch/
G at an interval of 0.25 from 2 to 4.5, and found
C ≥ 3.0 [
7,
10]. Following the conclusion, the present study further found the
C = π (or
a*
ch = π⋅
G) is appropriate to consider the effect of microstructure characteristic
G on the
a*
ch value indicating the transition from
ft-controlled fracture to
KIC-controlled fracture.
Equation (3) can be easily used in either linear relations [σN–η(a, G), σN–Le (a, G)] or nonlinear relations (σN–a) as required. It should be noted that the predicted results (e.g., ft, KIC and σN) with 96% reliability do not change with the different forms of non-LEFM model, which makes the combined use of the proposed model and normal distribution more meaningful and easier in practical applications and data analysis. Furthermore, the σN–η(a, G) and σN–L(a, G) linear relations through the respective origins make the non-LEFM model easier to determine ft and KIC values as the origin is absolutely fixed.
Substituting Equation (1a) into Equation (1b), the mechanical properties
ft and
KIC can be linked together through the average grain size
G and the relative characteristic crack size
C = π as shown in Equation (4). In another word, the microstructure characteristic
G has direct influence on
ft and
KIC of ceramic.
To have a better understanding, the
σN–
η(
a,
G) linear relations in
Figure 5c–
Figure 9c were plotted together to show the influnce of microstructure characteristic
G on
ft value. To make it clearer, three different ceramics with different
G are shown in
Figure 11a, and two types of Si
3N
4 ceramic with slightly different
G are illustrated in
Figure 11b in which only mean lines are given because the experimental points get close each other due to that the two materials are Si
3N
4 and have similar
G values. Obviously, both
ft and
KIC have been explicitly linked together through the average grain size, in which the fracture toughness
KIC is determined from Equation (4) based on the
ft value and
G value. Grain size
G has significant influence on
ft and
KIC, and can explicitly link the two properties.
In this study, five groups of fracture data on ceramics with average grain size
G from 2 to 20 μm have been analyzed. Using the fracture data, it has been proven the proposed non-LEFM model and normal distribution can be combined used to (i) deduce both
ft and
KIC with a specified reliability from the seeming randomly varied fracture measurement and (ii) probabilistic predict
σN of ceramic specimens with and without defects if
ft or
KIC values (corresponding mean and standard deviation) are available. The predictions including mean and upper and lower bounds can be either linear relation as shown in
Figure 5,
Figure 6,
Figure 7,
Figure 8 and
Figure 9, or nonlinear relation in
Figure 10 as required.