Compaction Band Formation and Propagation Behavior in Closed Cell Aluminum Foam David Brush1 and Kathleen Issen2 Department of Mechanical and Aeronautical Engineering Aluminum foam is a porous, lightweight alternative to solid aluminum, which is relatively new to the market. As such, not much is known about the material, despite its possible applications in sound and vibration damping devices, a light weight construction, and impact energy absorbers. Further understanding of the material, and specifically its tendency to form regions of high local strain during compressive deformation, is the goal of this research. Compaction bands, or strain C5a15 Stress Strain Curve 8 localizations, are defined as regions of high 7 local strain within a material being 6 compressed. These bands are an apparently 5 (MPa) Stress common failure mode among highly porous 4 3 solids, including aluminum foams (Bastawros 2 et al. 2000; Bart-Smith et al. 1998), sandstone 1 (Olsson 2001), Steel Foam (Park & Nutt 2001), 0 0 0.005 0.01 0.015 0.02 0.025 0.03 Axial Strain (Crosshead) 0.035 0.04 0.045 0.05 and polycarbonate honeycombs (Papka & Figure 1: Stress-strain plot (with unloading loops) of the foam sample Kyriakides 1998). The formation of these referenced in this paper. Note the stress drop and subsequent plateau bands occurs in two stages. In the first stage, region. band formation, a single void, or cell, fails, due to load concentration and/or weak cell geometry. The collapse of this cell leads to the collapse of surrounding cells, thus causing the failure to propagate across the material until a complete layer of crushed cells forms (Daxner et al. 1999). During this failure, there is unloading of the surrounding cells in the material, and therefore a drop in the applied load, corresponding to an overall stress drop in the material. This phenomenon can be thought of as a series of three springs. Up until the beginning of band formation, these springs all have a constant elastic modulus, and act as a single spring. However, when the band forms, the middle spring’s modulus gradually decreases, thereby causing the middle spring to 1 2 Class of 2005, Mechanical Engineering, Clarkson University, Honors Program; Oral Presentation Associate Professor, MAE Department, Clarkson University 83 take up some of the displacement of the surrounding springs, and also lessening the load required to keep the springs compressed. The second, longer stage (band propagation) is when this original band propagates not across the material, but along it (parallel to the loading). Not all materials that form bands will exhibit propagation, however, many form multiple discrete bands instead. No matter whether a material propagates or forms multiple bands, this stage is characterized by a largely constant stress within the material, indicated by a “plateau region” on stress-strain plots. Similar research has been performed regarding the localization behavior of sandstone regarding propagation behavior (Olsson 2001). Linking of his results and those gathered from this research would make excellent progress toward a unified theory for compaction band formation in many, if not all porous solids. Of particular interest is the equation relating band propagation speed and overall deformation rate to change in porosity Where vr and vp are the rate of band thickening and overall specimen shortening, respectively, and P and Po are the band and original material porosities. The relation between relative propagation rate and energy absorption is also of interest, and is given by Where E - Eo is the change in strain energy, and σ is the plateau stress of the material. This second relation is of special interest due to the great potential aluminum foam has as an impact energy absorption material. Understanding this failure mechanism better is important for bringing porous materials into widespread use. Porous metals, such as aluminum foam, are already known to have many uses, including lightweight construction/filler material, sound damping, heat exchange, and impact energy absorbers (Sugimura et al. 1997; Bastawros et al. 1998; Daxner et al. 1999; Park & Nutt 2001). In construction materials, it is imperative that the material not be loaded past its peak stress, as doing this would lead to a massive compressive failure. Compression fractures in persons with osteoporosis may be looked at as such a failure. Also, as foam metals do not exhibit a fully elastic initial deformation, pre-loading of structural foam may be desired. Impact energy absorption applications, however, make full use of this same phenomenon, the plateau region of foam failure providing excellent energy absorption over a large strain at a nearly constant stress. The focus of research thus far has been to analyze the behavior of aluminum foam down the stress drop, when the band first forms. This was done using surface images of aluminum foam samples compacted in the course of previous experimentation. By processing these images using an image correlation software package, Vic2D, a 2 dimensional “map” of surface strain can be produced (strain 84 being calculated from one image to another) One very interesting trend appears when looking at these local strain maps. By taking a one dimensional “slice” of data coincident with the loading of the specimen, one can get a sort of band strain profile, as seen below. The data points on such a profile, when shifted slightly, correspond extremely well to an exponential plot defined by the equation Where A is the maximum local strain Strains down central pixels (x=493) across the band region, and B is a constant 0.01 0 0 100 200 300 400 500 600 700 800 900 1000 which scales the width of the plot. B does not appear to change much, if at all, throughout the -0.02 stress drop, indicating that the width of the -0.03 band does not change at all throughout the -0.04 drop, indicating a formation event with little or -0.05 no propagation, as was expected. This curve, strain -0.01 interestingly enough, is in the same family of -0.06 Y-axis location curves as the bell probability curve. Taking two derivatives of this relation, we then find an expression for the value of x at inflection, and plugging this value back into the equation, we find that the inflection point of this curve is located at 37 percent of the maximum strain. Since inflection in this plot represents where the local strain increases the fastest, this point gives us a good approximation of where the band “front” would be located. If this phenomenon were ideal, the strain would instantaneously jump from a low, non-localized, to a much higher band strain (think of the spring example from above, each of the springs would have its own constant strain throughout it, but the middle spring’s strain would be much higher due to a lower elastic modulus). Thus, at the band front, an infinite slope would be observed in the strain plot. In research to come, this definition of band strain will be used to analyze the propagation of the compaction band beyond its initial formation, and comparison of the behavior of aluminum foam and Olsson’s sandstone will be made. 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