2018
DOI: 10.1111/1365-2478.12720
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Static and dynamic stiffness measurements with Opalinus Clay

Abstract: In this work, an experimental study was carried out with the aim of reconciling static and dynamic stiffness of Opalinus Clay. The static and dynamic stiffness of core plugs from a shaly and a sandy facies of Opalinus Clay were characterized at two different stress states. The measurements included undrained quasi‐static loading–unloading cycles from which the static stiffness was derived, dynamic stiffness measurement at seismic frequencies (0.5–150 Hz) and ultrasonic velocity measurements (500 kHz) probing t… Show more

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Cited by 26 publications
(28 citation statements)
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“…In general, strain rates below 2 μstrain/h during consolidation were considered sufficiently low to have almost no effect on the shale stiffness. For Opalinus Clay, however, the elastic properties no longer changed in a significant way for a consolidation strain rate below 50 μstrain/h (Lozovyi and Bauer, 2018).…”
Section: Samples and Testing Proceduresmentioning
confidence: 95%
“…In general, strain rates below 2 μstrain/h during consolidation were considered sufficiently low to have almost no effect on the shale stiffness. For Opalinus Clay, however, the elastic properties no longer changed in a significant way for a consolidation strain rate below 50 μstrain/h (Lozovyi and Bauer, 2018).…”
Section: Samples and Testing Proceduresmentioning
confidence: 95%
“…The representative parameters and fluid bulk modulus estimated from known temperature, pressure and salinity using Batzle and Wang equations (Batzle and Wang, 1992) are listed in Table 4. Figure 9 -Figure 18 show a comparison between optimized model and measurements for Jurassic shale sample provided by Hornby (1998), Kimmeridge shale sample provided by Hornby (1998), a shale sample ("Shale 2") provided by Hofmann (2006), Norwegian Sea shale sample provided by Dewhurst et al (2011), Mancos shale sample provided by Sarker and Batzle (2010), Opalinus Clay sample ("Shaly facies 3") provided by Lozovyi and Bauer (2019), Pierre shale sample with water saturation of 0.23 provided by Szewczyk et al (2018), Pierre shale sample with water saturation of 0.7 provided by Szewczyk et al (2018), D2 shale, and B3 shale provided by SINTEF, respectively. Interesting findings are as follows:…”
Section: Model Vs Experimental Datamentioning
confidence: 99%
“…In particular, shales often show strong elastic anisotropy that originates from the alignment and platy nature of its constituent minerals, as underpinned by laboratory measurements provided by many authors (e.g. Vernik and Nur, 1992;Wang, 2002b;Szewczyk et al, 2018;Lozovyi and Bauer, 2019). It has also been recognized that the elastic anisotropy has impact on seismic imaging (e.g., Thomsen, 1986), AVO (Amplitude Variation with Offset) response (e.g.…”
Section: Introductionmentioning
confidence: 98%
“…Estimated Skempton's parameters are compared with existing measurement results. Holt et al (2018b) provided measured values for three shales, while Lozovyi and Bauer (2019) gave results for a shaly facies of Opalinus Clay. Skempton's parameters of the stiffer grain case are consistent with shale "B" and "M" of Holt et al (2018b) and the shaly facies of Lozovyi and Bauer (2019), while the anisotropic grain case is consistent with shale "D" of Holt et al (2018b).…”
Section: Comparison With Existing Measurementsmentioning
confidence: 99%
“…Shales often show strong elastic anisotropy that originates from the alignment and platy habit of its constituent minerals, as underpinned by existing laboratory measurements (e.g. Vernik and Nur 1992;Wang 2002;Szewczyk et al 2018;Lozovyi and Bauer 2019). Shale strength is also anisotropic, with less resistance for failure within the symmetry plane ("weak plane") than in other directions (e.g.…”
Section: Introductionmentioning
confidence: 99%