0000000000354245

AUTHOR

Eleonora Crisci

0000-0002-5525-5049

showing 7 related works from this author

The Role of Anisotropy on the Volumetric Behaviour of Opalinus Clay upon Suction Change

2017

An experimental investigation to analyse the anisotropic volumetric response of shaly and sandy facies of Opalinus Clay upon suction variations is presented. Obtained results demonstrate the different behaviour of the tested facies to a wetting-drying cycle. The shaly facies exhibits higher water retention capacity and stronger volumetric response than the sandy facies. Anisotropic response is experienced by both facies with the strain perpendicular to bedding higher than in the parallel direction. The sandy facies exhibits a more pronounced anisotropic behaviour in particular during the drying phase. A detailed analysis of the response in the two directions with respect to the bedding orie…

SuctionsuctionSettore ICAR/07 - GeotecnicaBedding0211 other engineering and technologies02 engineering and technology010502 geochemistry & geophysicsopalinus clay01 natural sciencesSoilPhase (matter)FaciesShalesPerpendicularLaboratory TestingGeotechnical engineeringPetrologyAnisotropyGeology021101 geological & geomatics engineering0105 earth and related environmental sciences
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One dimensional consolidation of Opalinus Clay from shallow depth

2017

First experimental results on Opalinus Clay from shallow depth (< 30 m depth) are presented and compared to results on cores from Mont Terri Underground Rock Laboratory (~ 300 m depth). Samples were tested in one dimensional condition using an advanced experimental technique. The samples from the two sites show similar properties in terms of geotechnical characterization and one dimensional compressibility/swelling indexes, despite the different source depths.

Consolidation (soil)MineralogyOverburden pressureVoid ratioPore water pressureSoilParticle-size distributionSoil waterCompressibilityShalesLaboratory TestingMercury intrusion porosimetryOpalinus ClayGeology
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Discussion on “Experimental Deformation of Opalinus Clay at Elevated Temperature and Pressure Conditions: Mechanical Properties and the Influence of …

2021

AbstractThe testing procedure and results on saturated samples of Opalinus Clay in the work of Schuster et al. (Rock Mech Rock Eng https://doi.org/10.1007/s00603-021-02474-3, 2021) were conducted and presented using strain rates two to four orders of magnitudes higher than the rates needed to allow pore pressure equilibrium in the material, both in drained and undrained conditions. This leads to an erroneous estimation of the mechanical properties in saturated conditions. We discuss this aspect in the context of shale testing. We also discuss the effect of drying-induced fissuring on the mechanical properties of geomaterials tested in dry conditions.

Clay rock Desiccation cracks Micro-fissuring Opalinus Clay Pore pressure generation Rate-dependent mechanical behaviour ShaleSettore ICAR/07 - GeotecnicaClay rockGeologyContext (language use)Strain rateGeotechnical Engineering and Engineering GeologyPore water pressureTemperature and pressureGeotechnical engineeringDeformation (engineering)Oil shaleGeologyCivil and Structural EngineeringRock Mechanics and Rock Engineering
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Effect of the mineralogical composition on the elastoplastic hydromechanical response of Opalinus Clay shale

2021

Abstract Opalinus Clay is the shale currently under investigation as the host formation for geological radioactive waste disposal in Switzerland. Its hydromechanical response has been widely studied, and the experimental results show a range of values whose dispersion needs to be clarified. This work aims to explain the dispersion in the literature results by correlating the hydro-mechanical response to the mineralogical variability of the tested specimens . Based on published microstructural studies, the Opalinus Clay shale is herein schematised as a sequence of two kinds of layers: the shaly (high in clay-mineral content) and the sandy (low in clay-mineral content) layers. The mineralogic…

Settore ICAR/07 - Geotecnica0211 other engineering and technologiesMineralogy02 engineering and technologyGeotechnical Engineering and Engineering GeologyDispersion (geology)Mineralogical compositionAnisotropy Composition Elasto-plasticity Mineralogy Opalinus clay ShaleLayered structureTransverse isotropyCompressibilityAnisotropyPorosityOil shaleGeology021101 geological & geomatics engineering021102 mining & metallurgy
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Hydro-mechanical behaviour of shallow Opalinus Clay shale

2019

In Switzerland, Opalinus Clay shale has been selected as the host formation for radioactive waste disposal. The minimum required depth of the repository is related to the long-lasting isolation required for the disposal (1 million years). During this period, possible erosion scenarios affecting the repository need to be analysed. Opalinus Clay from shallow depths (< 70 m) was sourced from a borehole in Northern Switzerland, where the formation was affected by a considerable exhumation process. This work aims to investigate the impact of the mentioned phenomenon on the hydro-mechanical behaviour of Opalinus Clay through one-dimensional consolidation and permeability measurements. Laboratory …

Diagenesi0211 other engineering and technologiesGeochemistryRadioactive wasteOne-dimensional consolidation and hydraulic conductivityGeological exhumationGeology02 engineering and technologyShale010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesDiagenesisDiagenesisErosionAnisotropyEnvironmental scienceOpalinus ClayOil shale021101 geological & geomatics engineering0105 earth and related environmental sciencesEngineering Geology
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Anisotropic volumetric behaviour of Opalinus clay shale upon suction variation

2016

Opalinus clay shale is under consideration to serve as the host geomaterial for the underground storage of nuclear waste in Switzerland. Water retention behaviour and anisotropic behaviour represent two main features of this geomaterial; however, a comprehensive understanding of the interaction between these two features is still lacking. This paper aims to provide a detailed experimental analysis of the coupling between the water retention capacity and the anisotropic behaviour of two facies (shaly and sandy) of the Opalinus clay shale. The response of the tested geomaterials is characterised by an unequal swelling and shrinkage response in directions parallel and perpendicular to the bed…

SuctionsuctionBedding0211 other engineering and technologiesanisotropy02 engineering and technology010502 geochemistry & geophysicsGeotechnical Engineering and Engineering Geology01 natural sciencesWater retentionstrainFaciesEarth and Planetary Sciences (miscellaneous)medicineGeotechnical engineeringWettingmedicine.symptomAnisotropyOil shaleGeology021101 geological & geomatics engineering0105 earth and related environmental sciencesShrinkageGéotechnique Letters
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Anisotropic Volumetric Response of Shales upon Suction Changes

2016

Anisotropic fabric and volumetric response to suction changes represent two main features of shales, which are involved in several engineering applications. However, a comprehensive understanding of the interaction between these two aspects is still missing. The present work aims to provide a detailed analysis of the coupling between the water retention capacity of shales and their anisotropic behaviour through an advanced experimental methodology. Among the various tested facies of the Opalinus Clay Shale (Mont Terri, Switzerland), the results from the shaly facies are presented in this study. The behaviour of the material is characterized by swelling and shrinkage respectively upon wettin…

SuctionanisotropySuctionShalestrainBedmedicineGeotechnical engineeringWettingSwellingmedicine.symptomAnisotropyOil shaleWater contentGeologyShrinkageProceedings
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