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2020, Journal of the European Ceramic Society
Numerous investigators have noticed that there is a relationship between the energy of branching and the energy of initiation during a fracture event in materials that fail in a brittle manner. Usually, this is measured in terms of the stress intensities, i.e., K B /K c. The ratio has been reported between 3 and 4, implying a constant value. However, data suggests that it is a constant for a material, but not a universal constant. The fractal dimension of the fracture surface is related to the critical stress intensity factor. It is a measure of the tortuosity of the fracture surface. We show that the K B /K C ratio is directly related to the square root of the fractal dimensional increment, indicating a relationship between the energy of crack propagation and the tortuosity of the fracture surface.
Europhysics Letters (EPL), 1987
The fractal geometry of fracture patterns in materials is explored by means of a simple model which incorporates the equations of elasticity and simple rules for fracture propagation. Different isotropic media and boundary conditions are considered. Self-similar patterns with fractal dimensions nearly independent of the elastic constants are obtained.
The relationship between geometry and energy is discussed as it applies to the fracture of insulators and metals. It was found that the equations related to toughness provided evidence that fundamental spatial coordinates were intimately related to the fracture energy, namely -for insulators 1-20 A and for metals 0.1-20 um . The equations summarizing this behavior are: metals-G=kE L where E is the elastic modulus and L is measured feature on a fracture surface that provided evidence that a 1:1 relationship was present between a fracture surface feature and the energy of fracture.. For insulators the relationship that applies was; G=1/2ED*ao where D* was the fractal dimensional increment and ao was a spacing obtained from statistical correlations. It is suggested that the equations resemble those found in atomic spectroscopy.
Scripta Metallurgica, 1988
Several authors have recently discussed the use of fractals to describe fracture energies and their relationships to fracture surface geometries. A fractal is a self-similar geometric construction with non-integer dimensionality. Self-similarity means that the fractal appears the same under all magnifications. Dimensionalities are described below and more rigorously. Fracture energies (E) are quantified according to the scale of observation (L), e.g., J integrals on the macroscopic scale or interatomic potentials on the lattice scale. Surface geometries have been described by roughness parameters (R) or by the fracture surface dimensionality: D/sub s/ ..cap alpha..ln(R)ln(L). Another fractal dimensionality for fracture has been defined in terms of energy: D ..cap alpha..ln(E)ln(L). A frequently employed assumption is that D/sub s/ is the same for all scales, or that a plot of ln(R) versus ln(L) is linear. However, others have found that this is in general not true for fracture surfa...
Journal of the European Ceramic Society, 2020
A critical part of failure analysis is to understand the fracture process from initiation through crack propagation. Crack propagation in brittle materials can produce crack branching patterns that are fractal in nature, i.e., the crack branching coefficient (CBC). There is a direct correlation between the CBC and strength, σ f : ∝ σ CBC f. This appears to be in conflict with the fractal dimensional increment of the fracture surface, D * , which is independent of strength and related to the fracture toughness of the material, K c : = K E a D c 0 1/2 * 1/2 , where E is the elastic modulus and a 0 , a characteristic dimension. How can D * be constant in one case and CBC be a variable in another case? This paper demonstrates the relationship between D * and CBC in terms of fractographic parameters. Examples of fractal analysis in analyzing field failures, e.g., that involve comminution, incomplete fractures of components, and potential processing problems will be demonstrated.
Physica A-statistical Mechanics and Its Applications, 2001
Fractal geometry is introduced into elastic–plastic fracture mechanics characterizing the morphology of crack surface. It is shown that the rising of the J–R curve is correlated to the ruggedness dimension (Hurst's exponent) of the crack surface. Experimental results are fitted. Our propositions differ from other currently used in the literature compromising the results therein presented.
The fractal geometry is introduced in the dynamic fracture to describe the ruggedness during the crack propagation characterizing the morphology of generated surfaces. It is shown that the fractal dimension has a strong influence about the limit speed of fast crack propagation. It is also shown that the inatingibility of speed of waves Rayleigh by cracks in some materials can be correlated to the ruggedness of fracture surfaces by means of exponent Hurst, H, that measures the ruggedness dimension. The experimental results of Fineberg et al [FINEBERG 1991; FINEBERG 1992] they were adjusted by the model. The unstability coefficient was calculated for Fineberg et al measurements in agreement with the definition proposed by SANDER [1984]. One concluded that exist an intrinsic unstability to the phenomenon that produces the ruggedness of surfaces, limiting this way the maximum of crack propagation speed for a smaller value than the speed of waves Rayleigh in the material.
EPJ Web of Conferences, 2010
The present study is focused on the correlation of scaling properties of crack branching and brittle fragmentation with damage accumulation and a change in the fracture mechanism. The experimental results obtained from the glass fragmentation tests indicate that the size distribution of fragments has a fractal character and is described by a power law.
Physica D: Nonlinear Phenomena, 1989
We discuss some aspects of models developed to investigate the eventual fractal geometry of growing cracks in sohds. The emphasis is placed upon two questions: (i) relationship wilh olher growlh processes, in particular those occurring in scala, fields. and, (ii) praclical implications. As regards the first point, the similaritnes and differences between the different growing patterns are stressed: for instance, it is shown that an analysis of field singularities at the tips leads to fractal dimensions which are alv'a~,s lower for mechanical breakdown than for Laplacian frectals. Recent efforts caned out to connect models w~th ~ctual cracking of materials, which exhibit a rich phenomenology, are commented on. Finally, several implications of the fracml nature of fracture surfaces, having practical significance, are stressed.
International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 1994
Fracturing and fragmentation processes occur on all scales and, hence, may be described in terms of fractals. We examined the fractal dimensions of discontinuity spacing measurements in a fractured rock mass and observed a relation between the fractal dimension and the quality of the rock mass in terms of RQD. RQD tends to increase with a decrease in fractal dimension for a given scanline length. Thus a relatively more-competent fractured rock mass will tend to have a lower fractal dimension and vice versa.
Acta Metallurgica et Materialia, 1990
To examine the usefulness of the fractal concept in quantitative fractography, a series of classical fracture surfaces, namely transgranular cleavage, intergranular fracture, microvoid coalescence, quasicleavage and intergranular microvoid coalescence, are analyzed in terms of fractal geometry. Specifically, the five brittle and ductile fracture modes are studied, from three well characterized steels (a mild steel, a low-alloy steel and a 32 wt% Mn-steel) where the salient microstructural dimensions contributing to the final fracture morphology have been measured. Resulting plots of the mean angular deviation, and Richardson (fractal) plots of the lineal roughness, as a function of the measuring step size, are interpreted with the aid of computer-simulated fracture-surface profiles with known characteristics. It is found that the ranges of resolution, over which the fractal dimension is constant, correspond to the pertinent metallurgical dimensions on the fracture surface, and thus can be related to microstructural size-scales Rrsumr--Afin d'rvaluer l'utilit6 du concept de fractal dans la fractographie quantitative, une srrie de surfaces de rupture classiques--par clivage transgranulaire, rupture intergranulaire, coalescence de microcavitrs, pseudoclivage et coalescence de microcavitrs intergranulaires--sont analysres en fonction de la grom6trie fractale. On &udie plus particuli&ement ces cinq modes de ruptures ductiles et fragiles dans trois aciers bien connus (un acier doux, un acier faiblement alli6 et un acier d 32% en poids de mangand~) o~ l'on a mesur6 les dimensions microstructurales essentielles qui contribuent ~i la morphologie finale de rupture. On interprdte los courbes qui en rrsultent pour la drviation angulaire moyenne, et les courbes de Richardson (de fractal) de la rugosit6 linraire d l'aide de profils de surfaces de rupture simulres par ordinateur d partir des caractrristiques connues. On trouve que les domaines de rrsolution pour lesquels la dimension du fractal est constante correspondent aux dimensions m&allurgiques approprires sur la surface de rupture, et peuvent done 6tre relirs fi des 6chelles de taille microstructurales.
Fcp2003, 2013
It has long been recognized that the fatigue growth behaviour of cracks having a length comparable with the material microstructure size (the so-called short or small cracks) is remarkably different from that of long cracks. In particular, the threshold condition of fatigue crack growth is seen to be correlated to the crack length and the material microstructure. The well-known "Kitagawa diagram" describes the variation of the threshold stress intensity range against the crack length, showing the existence of a transition value of length beyond which the threshold of fatigue crack growth is governed by linear elastic fracture mechanics. In the present paper, the crack surface is firstly treated as a self-similar invasive fractal set (which is characterized by a uniform fractal dimension) and, owing to the fractional physical dimension of the fracture surface, the stress intensity factor is shown to be a function of the crack length. Consequently, the threshold stress intensity range is deduced to be a function of the crack length. Then the fractal dimensional increment is assumed to vary from 0 to 1 since, in the physical reality, the fractal dimension of the crack surface may change with the crack length. This allows us to put forward a new interpretation of the Kitagawa diagram within the framework of the fractal geometry.
Fractal geometry is a non-Euclidean geometry which has been developed to analyze irregular or fractional shapes. In this paper, fracture in ceramic materials is analyzed as a fractal process. This means that fracture is viewed as a selfsimilar process. We have examined the fracture surfaces of six different alumina materials and five glass-ceramics, with different microstructures, to test for fractal behavior. Slit island analysis and Fourier transform methods were used to determine the fractal dimension, D, of successively sectioned fracture surfaces. We found a correlation between increasing the fractional part of the fractal dimension and increasing toughness. In other words, as the toughness increases, the fracture surface increases in roughness. However, more than just a measure of roughness, the applicability of fractal geometry to fracture implies a mechanism for generation of the fracture surface. The results presented here imply that brittle fracture is a fractal process; this means that we should be able to determine processes on the atomic scale by observing the macroscopic scale by finding the generator shape and the scheme for generation inherent in the fractal process. [
Progress in Materials Science, 1994
This paper offers a systematic approach for obtaining the order of stress singularity for different selfsimilar and self-affine fractal cracks. Mode II and Mode III fractal cracks are studied and are shown to introduce the same order of stress singularity as Mode I fractal cracks do. In addition to these three classical modes, a Mode IV is discovered, which is a consequence of the fractal fracture. It is shown that, for this mode, stress has a weaker singularity than it does in the classical modes of fracture when self-affine fractal cracks are considered, and stress has the same order of singularity when self-similar cracks are considered. Considering this new mode of fracture, some single-mode problems of classical fracture mechanics could be mixed-mode problems in fractal fracture mechanics. By imposing a continuous transition from fractal to classical stress and displacement fields, the complete forms of the stress and displacement fields around the tip of a fractal crack are found. Then a universal relationship between fractal and classical stress intensity factors is derived. It is demonstrated that for a Mode IV fractal crack, only one of the stress components is singular; the other stress components are identically zero. Finally, stress singularity for three-dimensional bodies with self-affine fractal cracks is studied. As in the twodimensional case, the fourth mode of fracture introduces a weaker stress singularity for self-affine fractal cracks than classical modes of fracture do.
Theoretical and Applied Fracture Mechanics, 2005
Fractal modeling of the rugged crack geometry is considered for the stable and dynamic fracture mechanics characterizing the morphology of a fracture surface and the influence of its growth. It is shown that the fractal dimension has a strong influence on the rising of the R-curve in brittle materials. For the unstable Griffith–Mott’s approach or dynamical crack growth the fractal dimension has a strong influence on the velocity limit of the crack growth. It is also shown that the limit of crack velocity lowers with increasing surface ruggedness (higher fractal dimension D = 2 − H) explaining the intangibility of the Rayleigh wave velocity by the cracks.
1994
Abstract Experiments aiming at the measurement of the roughness index ζ of “rapid” fracture surfaces are briefly reviewed. For rapid crack propagation, measured values of ζ are close to 0.8, which seems to be a universal exponent. However, it is argued, by re-writing the Griffith criterion for a self-affine crack, that the self-affine correlation length ξ might depend upon the microstructure, and hence on the fracture toughness.
International Journal of Fracture, 1996
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