Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Falko Bethmann"'
Autor:
Quinn Wenning, Nima Gholizadeh Doonechaly, Alexis Shakas, Francisco Serbeto, Falko Bethmann, Ben Dyer, Raymi Castilla, Peter Meier, Marian Hertrich, Hansruedi Maurer, Domenico Giardini, Stefan Wiemer
Publikováno v:
Proceedings 56th US Rock Mechanics / Geomechanics Symposium.
The Bedretto Underground Laboratory for Geosciences and Geoenergies (BULGG) is located in central Switzerland and serves as a test bed for geothermal energy research. Several boreholes were drilled from the laboratory section (ca. 1.1 km overburden)
Autor:
Hannes Krietsch, Linus Villiger, Francisco Seberto, Domenico Giardini, Morteza Nejati, Marian Hertrich, Philipp Kästli, Hansruedi Maurer, Valentin Gischig, Rebecca Hochreutener, Anne Obermann, Raymi Castilla, Alba Zappone, Stefan Wiemer, Michèle Marti, Antonio Pio Rinaldi, Xiaodong Ma, Barbara Nägeli, Martin O. Saar, Thomas Driesner, Falko Bethmann, Kai Bröker, Quinn Wenning, Peter Meier, Alexis Shakas, Katrin Plenkers, Simon Löw, Nima Gholizadeh Doonechaly, Florian Amann
Publikováno v:
Solid Earth Discussions
The increased interest in subsurface development (e.g., unconventional hydrocarbon, deep geothermal, waste disposal) and the associated (triggered or induced) seismicity calls for a better understanding of the hydro-seismo-mechanical coupling in frac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c91fc8e2b76371431559653714e5256b
https://se.copernicus.org/preprints/se-2021-109/
https://se.copernicus.org/preprints/se-2021-109/
Autor:
Alexis Shakas, David Jordan, Hannes Krietsch, K. Bröker, Francisco Serbeto, Xiaodong Ma, Peter Meier, Marian Hertrich, Simon Löw, Raymi Castilla, P. Guntli, Falko Bethmann
Publikováno v:
Scopus-Elsevier
Summary The Bedretto Underground Laboratory for Geoenergies is an URL (Underground Research Laboratory) developed and managed by ETH Zurich since 2017. It is located in the Bedretto tunnel at about 2 km from the southern entrance, in a 100 m-long enl
Autor:
Valentin S. Gischig, Domenico Giardini, Florian Amann, Marian Hertrich, Hannes Krietsch, Simon Loew, Hansruedi Maurer, Linus Villiger, Stefan Wiemer, Falko Bethmann, Bernard Brixel, Joseph Doetsch, Nima Gholizadeh Doonechaly, Thomas Driesner, Nathan Dutler, Keith F. Evans, Mohammadreza Jalali, David Jordan, Anniina Kittilä, Xiaodong Ma, Peter Meier, Morteza Nejati, Anne Obermann, Katrin Plenkers, Martin O. Saar, Alexis Shakas, Benoît Valley
Publikováno v:
Geomechanics for Energy and the Environment. 24:100190
Autor:
Hannes Hofmann, G. Zimmermann, Arno Zang, Marton Pal Farkas, Ernst Huenges, Ki-Bok Min, Sehyeok Park, Kwang-Il Kim, Peter Fokker, Rob Westaway, Falko Bethmann, Peter Meier, Frederic Guinot, Kern Shin Yoon, Jaiwon Choi, Uijin Jeong, Young Hun Han, Tae Jong Lee, Yoon Ho Song, Myung Sun Kim, Byoung Joon Yoon, Keun Soo Lee, Kwang Yeom Kim
Publikováno v:
Abstracts
12th Euro-conference on Rock Physics and Geomechanics #
12th Euro-conference on Rock Physics and Geomechanics #
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::14ac280d7cbf1fb634f56f34833cb35b
Publikováno v:
Geophysical Journal International. 190:1257-1270
SUMMARY We investigate attenuation (Q−1) of sediments of 2.5–3.5 km thickness underneath the city of Basel, Switzerland. We use recordings of 195 induced events that were obtained during and after the stimulation of a reservoir for a Deep Heat Mi
Autor:
Domenico Giardini, Benjamin Edwards, John Clinton, Falko Bethmann, Bettina P. Goertz-Allmann, Donat Fäh, Nicholas Deichmann
Publikováno v:
Bulletin of the Seismological Society of America. 101:3088-3095
We estimate moment magnitudes M w for earthquakes in Switzerland recorded between 1998 and 2009 using three different spectral methods. The M w estimation in Switzerland is extended to lower magnitudes (local magnitude M L 0.1), and scaling relations
Publikováno v:
Bulletin of the Seismological Society of America. 101:515-534
Theoretical considerations and empirical regressions show that, in the magnitude range between 3 and 5, local magnitude, M L , and moment magnitude, M w , scale 1:1. Previous studies suggest that for smaller magnitudes this 1:1 scaling breaks down. H