2022
DOI: 10.1016/j.engfracmech.2022.108722
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Analytical investigation on the unstable fracture toughness of fine-grained quartz-diorite rock considering the size effect

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Cited by 16 publications
(19 citation statements)
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“…Since energy release rate is uniquely related to stress intensity, G also provides a single-parameter description of crack-tip conditions, and Gc (such as šŗ in mode I fracture) is an alternative measure of toughness, which is also called critical energy release rate. In linear elastic conditions, šŗ and š¾ are correlated with each other by Equations (3) and ( 4) [2]: šŗ = š¾ /šø for plane stress (3) or šŗ = (1 āˆ’ š‘£ )š¾ /šø for plane strain (4) However, many materials such as rock, concrete and ceramics are not linear elastic [9][10][11] and a large number of experimental data have shown that šŗ and š¾ do not conform to the relation in Equation (2) [9,10,[12][13][14]. For example, it was found that as the length of a crack increases, šŗ and š¾ /E show a different relation from Equation ( 2), e.g., when a/w is 0-0.1 (a is the length of the crack and w is the width of the specimen), šŗ and š¾ /E show a power function relation, and when a/w is 0.1-0.85, they are linearly related [15].…”
Section: Introductionmentioning
confidence: 99%
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“…Since energy release rate is uniquely related to stress intensity, G also provides a single-parameter description of crack-tip conditions, and Gc (such as šŗ in mode I fracture) is an alternative measure of toughness, which is also called critical energy release rate. In linear elastic conditions, šŗ and š¾ are correlated with each other by Equations (3) and ( 4) [2]: šŗ = š¾ /šø for plane stress (3) or šŗ = (1 āˆ’ š‘£ )š¾ /šø for plane strain (4) However, many materials such as rock, concrete and ceramics are not linear elastic [9][10][11] and a large number of experimental data have shown that šŗ and š¾ do not conform to the relation in Equation (2) [9,10,[12][13][14]. For example, it was found that as the length of a crack increases, šŗ and š¾ /E show a different relation from Equation ( 2), e.g., when a/w is 0-0.1 (a is the length of the crack and w is the width of the specimen), šŗ and š¾ /E show a power function relation, and when a/w is 0.1-0.85, they are linearly related [15].…”
Section: Introductionmentioning
confidence: 99%
“…However, many materials such as rock, concrete and ceramics are not linear elastic [ 9 , 10 , 11 ] and a large number of experimental data have shown that and do not conform to the relation in Equation (2) [ 9 , 10 , 12 , 13 , 14 ]. For example, it was found that as the length of a crack increases, and show a different relation from Equation (2), e.g., when a/w is 0ā€“0.1 (a is the length of the crack and w is the width of the specimen), and show a power function relation, and when a/w is 0.1ā€“0.85, they are linearly related [ 15 ].…”
Section: Introductionmentioning
confidence: 99%
“…(2020) found that the unstable fracture toughness was approximately 1.5 times of mode I fracture toughness via testing notched semicircular bending (NSCB) specimens of granite. The unstable fracture toughness and initial fracture toughness converged to a constant as the specimen depth was sufficiently large (Wu et al., 2022; X. Zhang et al., 2007). In addition, the doubleā€K parameters varied with material heterogeneity.…”
Section: Introductionmentioning
confidence: 99%
“…When we have obtained the parameters (i.e., P ini , P max , a 0 , and a c ) from cracking tests, KIcini ${K}_{Ic}^{\mathit{ini}}$ and KIcun ${K}_{Ic}^{un}$ can be calculated using the LEFM formula. For the threeā€point bending (TPB) specimen, the mode I fracture toughness is (Wu et al., 2022): KI(P,a)=3PSa2H12BF(Ī±) ${K}_{I}(P,a)=\frac{3PS\sqrt{a}}{2{{H}_{1}}^{2}B}F(\alpha )$ where P is the applied load; a is the effective crack length; H 1 , B , and S are the sample geometries shown in Figure 3; Ī± = a / H 1 ; and F ( Ī± ) is the dimensionless stress intensity factor, which depends on the spanā€toā€depth ratio S / H 1 . For S / H 1 = 4: F4(Ī±)=1.99āˆ’Ī±(1āˆ’Ī±)()2.15āˆ’3.93Ī±+2.7Ī±2Ļ€1/2(1+2Ī±)false(1āˆ’Ī±false)3/2 ${F}_{4}(\alpha )=\frac{1.99-\alpha (1-\alpha )\left(2.15-3.93\alpha +2.7{\alpha }^{2}\right)}{{\pi }^{1/2}(1+2\alpha ){(1-\alpha )}^{3/2}}$ …”
Section: Introductionmentioning
confidence: 99%
“…Rock masses in deep underground projects are usually subjected to dynamic loads caused by excavation, blasting, and drilling [ 1 , 2 , 3 , 4 , 5 , 6 , 7 , 8 , 9 , 10 ]. Since local tensile failure often occurs under dynamic loads, many scholars have been attracted to conduct research on the dynamic tensile properties and fracture mechanism of rock materials [ 11 , 12 , 13 , 14 ]. The test methods for rock tensile strength include direct stretching and indirect stretching, i.e., the Brazilian disc [ 15 , 16 ].…”
Section: Introductionmentioning
confidence: 99%