Program Minisymposium 2013
Schedule for the day
Presentations take place in room NO E51.1 (E-floor of NO-building).
| Time | Who |
Title |
|---|---|---|
| 09:00 | Erik H. Saenger (ETH Zurich) |
Welcome/Intro |
| 09:15 | David Smeulders (TU Delft) |
Extending the Biot theory for electrokinetic coupling measurements |
| 09:45 | Kathleen Sell (JGU Mainz) |
Gas hydrate distribution on the microscale: A synchrotron based tomography experiment - first results |
| 10:15 | – | Coffee break |
| 10:45 | Stewart Greenhalgh (ETH Zurich) |
A model for determination of effective permeability from acoustic wavespeed and attenuation in a rigid two-phase porous medium |
| 11:15 | Paulina Krakowska (AGH Krakowie) |
Tight formations in Poland - the new challenges |
| 11:45 | Poster authors |
Poster overview |
| 12:15 | – | Lunch |
| 14:00 | – | Poster session |
| 15:00 | – | Coffee break |
| 15:30 | Bastien Dupuy (NTNU Trondheim) |
Frequency-dependent AVO attributes for partially saturated rocks |
| 16:00 | Marcel Frehner (ETH Zurich) |
On Krauklis waves in fluid-saturated fractured rocks |
| 16:30 | – | Final discussion/Closing |
| 17:00 | – | End |
Posters
Posters will be displayed close to our meeting room. There will be a poster overview before lunch, 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 portrait.
| Author | Title |
|---|---|
| Evangelos Moulas (ETH Zurich) |
Transient evolution of porosity waves in non-linear viscous rock |
| Rolf Sidler (Uni Lausanne) |
A pseudo-spectral method for simulating poro-elastic seismic wave propagation in complex borehole environments |
| Erik H. Saenger (ETH Zurich) |
Digital Rock Physics |
| Matteo Lupi (ETH Zurich) |
Liquefaction of deeply buried clays induced by parabolic focusing of seismic energy at Lusi Mud Volcano, Indonesia |
| Claudio Madonna (ETH Zurich) |
The Seismic Wave Attenuation Module |
| Nicola Tisato (ETH Zurich) |
Understanding seismic wave attenuation for dry and partially saturated Berea sandstone as a function of confining pressure and frequency ranging from 1 to 100 Hz |
| Holger Steeb (RU Bochum) |
About the hydro-mechanical response of deformable fractures |
| Mandy Duda (RU Bochum) |
Triaxial deformation of sandstones at different states of internal drainage: Implications from ultrasound velocities and amplitudes |
| Beatriz Quintal (ETH Zurich) |
Seismic attenuation in partially saturated rocks: Laboratory measurements and numerical modeling |
