2013
DOI: 10.1007/s12665-013-2768-2
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Seismic and mechanical properties of Opalinus Clay: comparison between sandy and shaly facies from Mont Terri (Switzerland)

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Cited by 15 publications
(15 citation statements)
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“…The sedimentary, compaction and burial history of OPA led to a sub-parallel arrangement of clay platelets with respect to macroscopic bedding (Wenk et al 2008). Due to this and the heterogeneity of macro-and microfabric in OPA, hydrological, microstructural, mechanical and transport-related properties exhibit transverse isotropy (e.g., NAGRA 2002;VanLoon et al 2004;Plischke 2010, 2011;Keller et al 2011Keller et al , 2013bSiegesmund et al 2014;Keller and Holzer 2018). Porosity estimates depend on resolution of the respective method, ranging between 4.9 and 19.1vol% with best porosity estimates of 18 vol% and 11.1 vol% for the shaly and sandy facies, respectively.…”
Section: Geological Setting and Materials Descriptionmentioning
confidence: 99%
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“…The sedimentary, compaction and burial history of OPA led to a sub-parallel arrangement of clay platelets with respect to macroscopic bedding (Wenk et al 2008). Due to this and the heterogeneity of macro-and microfabric in OPA, hydrological, microstructural, mechanical and transport-related properties exhibit transverse isotropy (e.g., NAGRA 2002;VanLoon et al 2004;Plischke 2010, 2011;Keller et al 2011Keller et al , 2013bSiegesmund et al 2014;Keller and Holzer 2018). Porosity estimates depend on resolution of the respective method, ranging between 4.9 and 19.1vol% with best porosity estimates of 18 vol% and 11.1 vol% for the shaly and sandy facies, respectively.…”
Section: Geological Setting and Materials Descriptionmentioning
confidence: 99%
“…Our observation that samples taken from the sandy facies are stronger with higher elastic moduli (Figs. 4,12) is consistent with previous studies (cf., Popp and Salzer 2007;Plischke 2010, 2011;Amann et al 2011Amann et al , 2012Vöbel et al 2014;Siegesmund et al 2014;Wild and Amann 2018;Favero et al 2018;Giger et al 2018;Zhang and Laurich 2019;Minardi et al 2020).…”
Section: Damage Initiation Failure and The Influence Of Confining Pressurementioning
confidence: 99%
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“…Many studies at Mont Terri have emphasized the tight relations between various rock properties, lithology and texture. Typical examples include the small-scale heterogeneity of geomechanical properties (Klinkenberg et al, 2009;Kaufhold et al, 2013;Siegesmund et al, 2014), the distribution of micro-porosity (Houben et al, 2013(Houben et al, , 2014Keller et al, 2013;Philipp et al, 2017), sorption processes and radionuclides diffusive transport (Hennig et al, 2020;Hennig and Kühn, 2021), the responses of seismic P-wave velocity (Kneuker et al, 2017;Schuster et al, 2017;Lauper et al, 2018), and more generally, the overall (geochemical, petrophysical and hydro-mechanical) anisotropic behavior of the OPA (Van Loon et al, 2004;Wenk et al, 2008;Favero et al, 2018). Jaeggi and Bossart (2014) provide an overview of the main rock properties (petrophysical, hydrogeological, rock mechanical, thermic, geochemical/pore water composition, and gas entry pressure parameters) of the OPA at Mont Terri and their relationship with lithology.…”
Section: Subfacies Types and Rock Propertiesmentioning
confidence: 99%