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  • 1
    ISSN: 1435-1528
    Keywords: Polymer ; extrusion ; ship ; surface energy ; distorsions elimination
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Physics
    Notes: Abstract An overview is given of extrudate distortions, flow fields and flow curves observed for flexible polymer melts, when they are extruded using axisymmetric or two-dimensional dies. Die walls with high surface energy and low-energy slippery surfaces are considered, as well as the influence of wall roughness. The connection between flow curves and the flow field structure is explained. Details of the extrudate distortions are given, focusing on the physical phenomena common to all polymer chemical species. A description of the second oscillating flow regime is included. Recent results on ideal and on slippery surfaces are reviewed. An application of slippery surface extrusion to several commercial polyethylenes is presented. It is shown that cracks and flow oscillation distortions can be completely eliminated, and very significant quality and productivity improvements can be obtained using slippery surfaces.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1435-1528
    Keywords: Adhesion ; peel ; master curves ; mechanisms ; elongation ; surface energy
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Physics
    Notes: Abstract We consider the adhesion of a pressure sensitive adhesive on different substrates (Pyrex, stainless steel, Plexiglas). First, we characterize the rheological properties of the adhesive material and compare it with the predictions of Lodge's model. Then we investigate the adhesive properties using a special machine which enables us to peel at 90° with a fixed peeling front and we construct peeling master curves on different substrates. The mechanisms of peeling are analyzed by looking at the peeling front using a video camera. We realize that the flow within the filaments and ribs observed is mainly of elongational type. Also, by looking at the shape of the backing, we find out that most of the energy is spent within the ribs or filaments. To understand the effect of rheology on adhesion, we propose a simple model to predict peeling curves, by assuming that the flow is mainly of elongational type. This explains the high energy regions. At low velocities, surface energies become important and their effect is also analyzed. To conclude, we propose different dimensionless equations which explain the importance of the relevant parameters, via dimensionless numbers. Thus the peeling energy is investigated, as well as the condition which predicts the transition from cohesive to adhesive peeling.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2015-07-24
    Description: Large earthquakes on mid-ocean ridge transform faults are commonly preceded by foreshocks1, 2, 3 and changes in the seismic properties of the fault zone3. These seismic precursors could be linked to fluid-related processes2, 3. Hydrothermal fluids within young, hot crust near the intersection of oceanic transform faults are probably in a supercritical condition4. At constant temperature, supercritical fluids become significantly more compressible with decreasing pressure, with potential impacts on fault behaviour. Here we use a theoretical model to show that oceanic transform faults can switch from dilatant and progressive deformation to rupture in response to fluid-related processes. We assume that the fault core material behaves according to a Cam-clay-type5 constitutive law, which is commonly used to account for the behaviour of clays. According to our model, we find that the fault is initially stable, with stresses gradually increasing over a timescale of years in response to tectonic loading. The fault evolves into a metastable phase, lasting a few days, during which the fault rocks dilate and pore pressures decrease, causing the compressibility of the supercritical fluids to increase. This in turn triggers fault-slip instability that creates foreshock swarms. In the final phase, the fault fails in the mainshock rupture. Our results imply that seismic precursors are caused by changes in fluid pressure which result in variations in fluid compressibility, in response to rock deformation just before rupture.
    Type: Article , PeerReviewed
    Format: text
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