Time | Who |
Title |
---|---|---|
09:00 | Organizers | Welcome / Intro |
09:10 | Yder Masson (Institut national de recherche en sciences du numérique, France) |
Wave propagation modeling in poroelastic media using the distributional finite-difference method |
09:50 | All poster authors | Poster overview presentation (3 slides-3 minutes) |
10:20–11:10 | Posters & Coffee break | |
11:10 |
Nicolas Barbosa (University of Geneva, Switzerland) |
Fracture unclogging: a mechanism of seismically induced permeability changes. |
11:50 | Leonardo Meireles, Chuangxin Lyu, Thomas Ingeman-Nielsen (Technical University of Danemark) |
Impact of sub-zero temperature changes on P and S-wave velocities in a permafrost sample undergoing cyclical loading |
12:30–13:40 | Lunch & Posters | |
13:40 | Yury Alkhimenkov (University of Lausanne, Switzerland), Ludovic Räss (Stanford University, USA), Ludmila Khakimova (Skolkovo Institute of Science and Technology, Russia), Beatriz Quintal and Yury Podladchikov (University of Lausanne, Switzerland) |
High-resolution 3D modeling of the elastodynamic Biot's equations using multiple GPU graphics cards |
14:20 | Samuel Chapman, Jan V. M. Borgomano, Jerome Fortin (ENS Paris), Beatriz Quintal (University of Lausanne) and Sally Benson (Stanford University) |
Seismic wave attenuation and modulus dispersion due to partial saturation by CO2 gas exsolution |
15:00–15:50 | Posters & Coffee break | |
15:50 | Jacques M. Huyghe and Jingqian Ding (University of Limerick, Ireland) |
Step wise progression of Mode I cracks in porous media: Experiment and XFEM-simulation |
16:30 | Matthias Ruf and Holger Steeb (University of Stuttgart, Germany) |
Effects of heat treatments in Carrara marble based on ultrasonic tests and µXRCT investigations |
17:10 | End |
Posters will be displayed close to our meeting room. There will be a poster overview before the first coffee break, where all poster authors are asked to quickly present their poster to stimulate the discussions during the poster session. The poster format should be A0.