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Stephen Hedan

Researcher at University of Poitiers

Publications -  46
Citations -  443

Stephen Hedan is an academic researcher from University of Poitiers. The author has contributed to research in topics: Digital image correlation & Displacement field. The author has an hindex of 10, co-authored 41 publications receiving 355 citations. Previous affiliations of Stephen Hedan include École Normale Supérieure.

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Digital Image Correlation Development for the Study of Materials Including Multiple Crossing Cracks

TL;DR: In this article, an improvement of the digital image correlation (DIC) procedure was proposed to solve the uncertainty problems at the vicinity of the junction of two cracks, which was used to perform an evaluation of the displacement when multiple cracks are present in the subset.
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New routes for complete regeneration of coked zeolite

TL;DR: In this article, the active species responsible for catalyst regeneration are the short-lived oxygenated species and not ozone, and a simple way to increase their concentration consists to substitute N2 by a noble gas as He.
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Investigation of the damage induced by desiccation and heating of Tournemire argillite using digital image correlation

TL;DR: In this paper, a set of samples taken from the Tournemire site was submitted to a desaturation process in an oven at different temperature levels of 40, 50, 60, 80, 90, 105, 120, 150, and 200°C.
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One-year monitoring of desiccation cracks in Tournemire argillite using digital image correlation

TL;DR: In this article, the authors used a digital image correlation (DIC) method to monitor desiccation cracks during an annual climatic cycle, and the results demonstrate the ability of the non-invasive DIC technique to monitor clay-rock strains for at least four months and to monitor the opening and closing of cracks for more than one year.
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Multi-scale study on the deformation and fracture evolution of clay rock sample subjected to desiccation

TL;DR: In this paper, the authors compared and discussed the values of desiccation cracks at different scales (micrometer to decimeter) and found that cracks at the macroscopic scale (centimeter) exhibit a phase of opening and closure, followed by gradual closure, and finally, a final phase in which the cracks closed.