Abstract
In a recent contribution, Kumar et al. (J Mech Phys Solids 142:104027, 2020) have introduced a comprehensive macroscopic phase-field theory for the nucleation and propagation of fracture in linear elastic brittle materials under arbitrary quasistatic loading conditions. The theory can be viewed as a natural generalization of the phase-field approximation of the variational theory of brittle fracture of Francfort and Marigo (J Mech Phys Solids 46:1319–1342, 1998) to account for the material strength at large. This is accomplished by the addition of an external driving force—which physically represents the macroscopic manifestation of the presence of inherent microscopic defects in the material—in the equation governing the evolution of the phase field. The main purpose of this paper is to continue providing validation results for the theory by confronting its predictions with direct measurements from three representative types of experimentally common yet technically challenging problems: (i) the indentation of glass plates with flat-ended cylindrical indenters and the three-point bending of (ii) U-notched and (iii) V-notched PMMA beams.
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Notes
By strength we refer to the general definition of strength introduced by Kumar et al. (2020), which we recall here for the reader’s convenience. When any piece of the elastic brittle material of interest is subjected to a state of monotonically increasing uniform but otherwise arbitrary stress, fracture will nucleate from one or more of its inherent defects at a critical value of the applied stress. The set of all such critical stresses defines a surface in stress space. In terms of the Cauchy stress tensor \(\varvec{\sigma }\), we write \({\mathcal {F}}(\varvec{\sigma })=0\). This definition generalizes the various notions of ‘tensile’ and ‘shear’ strength that were proposed on the heels of the introduction of the stress tensor (Cauchy 1823)by numerous pioneers of continuum mechanics including Lamé, Clapeyron, Tresca, and Mohr; see, e.g., the historical account on rupture of solids in the classic monograph by Love (Love 1906; Section 83). We also note that it has long been recognized that a Griffith criterion alone cannot predict nucleation in general. Attempts to model nucleation of fracture near a notch front in terms of a “tensile” strength at a critical distance from the front combined with a critical energy release rate can be found, for instance, in (Leguillon 2002).
“Large” refers to large relative to the characteristic size of the underlying heterogeneities in the material under investigation. By the same token, “small” refers to sizes that are of the same order or just moderately larger than the sizes of the heterogeneities.
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Support for this work by the National Science Foundation through the grant CMMI–2132528 and the collaborative Grants CMMI–1901583 and CMMI–1900191 is gratefully acknowledged.
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Appendix: sample results showcasing the independence of the phase-field theory (4)–(5) on the localization length \(\varepsilon \)
Appendix: sample results showcasing the independence of the phase-field theory (4)–(5) on the localization length \(\varepsilon \)
In this appendix, as a complement to the results reported in Section 4.3 in (Kumar et al. 2020), we report sample results for each of the three classes of boundary-value problems investigated in the main body of the text that showcase the independence of the phase-field theory (4)–(5) on the localization length \(\varepsilon \).
Figure 14 provides a comparison between the result presented in Fig. 4a for the phase field v predicted by the theory for localization length (13) and that obtained for the different localization length
The calibration of the coefficient \(\delta ^\varepsilon \) for the values (20) renders \(\delta ^\varepsilon =60\) and \(\delta ^\varepsilon =6\), respectively, which result in an actual regularized size of the cracks given by \(\varepsilon ^\star =\varepsilon /\sqrt{1+\delta ^\varepsilon }=1.9\) \(\mu \)m. This is about three times smaller than the size of the cracks obtained for the localization length (13). Yet, it is evident that the results in Figs. 14a and b are essentially the same.
Next, Fig. 15 presents a comparison between the critical force \(P_{cr}\) in Fig. 9 predicted by the theory for notch depth \(A=5\) mm when using a localization length \(\varepsilon =12.5\) \(\mu \)m (solid line) and the corresponding result (dashed line) when using the smaller localization length \(\varepsilon =5\) \(\mu \)m. In the latter case, the calibrated value of the coefficient \(\delta ^\varepsilon \) turns out to be \(\delta ^\varepsilon =1.15\), which results in a regularized crack size of \(\varepsilon ^\star =\varepsilon /\sqrt{1+\delta ^\varepsilon }=3.4\) \(\mu \)m. This is about two times smaller than the regularized crack size that ensues from \(\varepsilon =12.5\) \(\mu \)m. Clearly, the results in Fig. 15 for the two different localization lengths are largely similar to one another.
Finally, Fig. 16 presents a comparison between the critical force \(P_{cr}\) in Fig. 13b predicted by the theory for notch angle \(\gamma =90^{\circ }\) when using a localization length \(\varepsilon =12.5\) \(\mu \)m (solid line) and the corresponding result (dashed line) when using the smaller localization length \(\varepsilon =9\) \(\mu \)m. The calibrated value of the coefficient \(\delta ^\varepsilon \) for the latter case is \(\delta ^\varepsilon =35\), which results in a regularized crack size \(\varepsilon ^\star =\varepsilon /\sqrt{1+\delta ^\varepsilon }=1.5\) \(\mu \)m that is about six times smaller than the regularized crack size that is obtained for \(\varepsilon =12.5\) \(\mu \)m. Consistent with the two preceding comparisons, a quick glance at Fig. 16 suffices to recognize that the two theoretical predictions based on different localization lengths are practically the same.
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Kumar, A., Ravi-Chandar, K. & Lopez-Pamies, O. The revisited phase-field approach to brittle fracture: application to indentation and notch problems. Int J Fract 237, 83–100 (2022). https://doi.org/10.1007/s10704-022-00653-z
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DOI: https://doi.org/10.1007/s10704-022-00653-z