From fluid flow to coupled processes in fractured rock: Recent advances and new frontiers
HS Viswanathan, J Ajo‐Franklin… - Reviews of …, 2022 - Wiley Online Library
Quantitative predictions of natural and induced phenomena in fractured rock is one of the
great challenges in the Earth and Energy Sciences with far‐reaching economic and …
great challenges in the Earth and Energy Sciences with far‐reaching economic and …
A review of techniques for measuring the biot coefficient and other effective stress parameters for fluid-saturated rocks
HA Kasani, APS Selvadurai - Applied …, 2023 - asmedigitalcollection.asme.org
Predicting the behavior of a saturated rock with variations in pore fluid pressure during geo-
energy production and storage, deep geological disposal of nuclear wastes, etc. with …
energy production and storage, deep geological disposal of nuclear wastes, etc. with …
Experimental study of Young's modulus dispersion and attenuation in fully saturated sandstones
L Pimienta, J Fortin, Y Guéguen - Geophysics, 2015 - library.seg.org
Although seismic wave dispersion and attenuation have been found to occur in sedimentary
rocks, it remains challenging to experimentally observe these effects. A new experimental …
rocks, it remains challenging to experimentally observe these effects. A new experimental …
Elastic and inelastic deformation of fluid-saturated rock
RY Makhnenko, JF Labuz - Philosophical Transactions of …, 2016 - royalsocietypublishing.org
In situ rock is often saturated with fluid, the presence of which affects both elastic parameters
and inelastic deformation processes. Techniques were developed for testing fluid-saturated …
and inelastic deformation processes. Techniques were developed for testing fluid-saturated …
Anisotropic behaviour of opalinus clay through consolidated and drained triaxial testing in saturated conditions
This paper investigates the anisotropic hydro-mechanical behaviour of Opalinus Clay shale,
the host material currently being considered for the construction of a nuclear waste …
the host material currently being considered for the construction of a nuclear waste …
A laboratory investigation on thermal properties of the Opalinus claystone
M Monfared, J Sulem, P Delage… - Rock Mechanics and Rock …, 2011 - Springer
Some aspects of the thermal behavior of the Opalinus claystone are investigated through
laboratory tests conducted on a new hollow cylinder triaxial apparatus specially designed for …
laboratory tests conducted on a new hollow cylinder triaxial apparatus specially designed for …
A laboratory investigation of thermally induced pore pressures in the Callovo-Oxfordian claystone
M Mohajerani, P Delage, J Sulem, M Monfared… - International Journal of …, 2012 - Elsevier
In the framework of research into radioactive waste disposal, it was decided to investigate
the thermally induce pore pressure occurring in the Callovo-Oxfordian claystone (a possible …
the thermally induce pore pressure occurring in the Callovo-Oxfordian claystone (a possible …
Poroelasticity of the Callovo–Oxfordian claystone
This work is devoted to an experimental investigation of the poroelastic behavior of the
Callovo–Oxfordian claystone, a potential host rock for the deep underground repository of …
Callovo–Oxfordian claystone, a potential host rock for the deep underground repository of …
Determination of the continuous stress-dependent permeability, compressibility and poroelasticity of shale
The continuous changes of the stress-dependent permeability, compressibility and
poroelasticity of a tight oil and gas shale were characterized by using the Constant Rate of …
poroelasticity of a tight oil and gas shale were characterized by using the Constant Rate of …
Modelling the drained/undrained transition: Effect of the measuring method and the boundary conditions
The dependence of fluid‐saturated rocks' elastic properties to the measuring frequency is
related to fluid‐flow phenomena at different scales. In the frequency range of [10− 3, 10 6] …
related to fluid‐flow phenomena at different scales. In the frequency range of [10− 3, 10 6] …