43 research outputs found

    On the possibly multifractal properties of dissipated energy in brittle materials

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    The paper reports an analytical study on the properties of fracture networks in brittle materials. Micro-deformation gradients are considered random fields and/or scaling fields. Under dynamic crack propagation conditions the possibly fractal properties of the (macro) crack pattern are governed by the interplay of fluctuations and spatial correlations. For "slow" crack propagation they are governed by the kinematic fields in the vicinity of crack or notch tips. The spatial distribution of dissipated energy, due to fracture, is evaluated. It is shown that there is a strong possibility that the dissipated energy is multifractal. Here, its properties are characterized in a fashion similar to the so-called p-model where p herein denotes normalized dissipated energy. For the three cases analyzed -uniaxial tension, pure shear, and dilatation -the dissipated energy under pure shear shows the strongest disorder, the one under dilatation the weakest, and the tension case is always between these two. INTRODUCTION Engineering materials are, in general, heterogeneous due to the presence of microstructure. If interest is in mechanical properties at scales much larger than the atomic, heterogeneity for materials like ceramics, rocks, concretes, composites means several things: size and properties of grains, aggregates, pores, microcracks, interfaces, composite structure, interactions with discontinuities and surfaces. These influence the analysis of such materials substantially, experimentally (in the choice of scales, methods of observation) and theoretically, for example in the limitations of homogenization methods. The fracture behavior of materials is important, so it continues to be the subject of intensive research. Microcracking, crack bridging, crack arrest are some of the many mechanisms that absorb energy during the fracture process. Physical reasoning suggests that these mechanisms are affected by the heterogeneity of the material before (macro) fracture activation. Thus heterogeneity contributes to the energy absorption mechanisms, which then contribute to the tendency of the (macro) crack network to follow a tortuous path. One problem examined herein is the following. Consider a brittle material loaded at a low loading rate, either by controlling the external load or the external displacement. At some point a macrocrack network will form. Does this network form dynamically or quasi-statically? Let us assume, for a moment, that crack propagation is dynamic. Then, there may not be enough time for the stress/strain fields to redistribute to an equilibrium state until the crack propagates further. Of course, this is a heuristic argument that is difficult to verify experimentally. In dynamic fracture mechanics literature, i.e., If the specimen/structure is loaded dynamically, the macrocrack network develops dynamically and several factors influence its characteristics -the waves propagating in the medium influence the crack pattern significantly. Especially near surfaces strong surface waves usually result in disintegration of the material from the surfaces inward. Such problems are difficult to treat analytically. Of course, near boundaries the behavior is expected to be different than in the bulk, i.e. In a recent study, Frantziskonis (1993a, b), it is shown that under certain conditions a statistical approach to material heterogeneity yields results analogous to the so-called gradient theories. These conditions call for small heterogeneity fluctuations allowing a spatial Taylor series expansio

    Surface Effects in Brittle Materials and Internal Length Estimation

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