The Geomaterials research group currently works on the following projects:
Localisation of deformation
This topic uses a combination of experimental methods with different resolution and sensitivity to study localisation (e.g. shear and compaction bands, fracturing) in rock samples and synthetic rocks, and characterises the operative micro-processes by full-volume investigations such as: (1) acoustic emission locations and their mechanism types; (2) acoustic tomography; (3) x-ray tomography; (4) neutron tomography; and (5) post-experiment destructive sampling to obtain optical thin sections and SEM images.
Experimental methods are carried out before, during and after the occurrence of localised deformation. We use differencing techniques applied to sequential images to document the onset and evolution of the deformation mechanisms. Moreover, we experimentally investigate the impact of such mechanisms on the spatio-temporal fluid flow within natural and synthetic rock samples (the latter takes place through EU-funded projects performed in European research facilities).
Numerical simulation of faulting
This topic investigates how permanent strain accumulates, and especially how that strain distribution reveals both compactional and dilational volumetric strains, along with highly variable shear strains. The outputs of the simulation have been transformed into predictions of other (emergent) properties, such as permeability and relative permeabilities, as well as acoustic properties. We have been able to directly relate the simulations with experimental outcomes in some cases, as well as applying the knowledge gained to the interpretation of real faults.
This topic is examining the validity of common methods used to assess the impacts of wellbore construction, and how that prior state affects other operations such as stimulation.
This topic is joint research with colleagues from School of Engineering and Physical Sciences, and focuses on developing nano-sensors that will be introduced into rock samples, or placed into synthetic rocks, to report local states to the experimenter.
This work deals with developing ways to construct controlled rock samples that will allow us to examine porosity, cementation, and grain-arrangements in terms of their impact of deformation responses. It can mix, for example, natural sand grains with synthetic cements and also include nano-sensors in that cement.
Synthetic and experimental diagenesis
This research makes use of methods that have been developed in the Pore-Scale Modelling research group to calculate rock properties as a consequence of diagenetic changes. This strategy has been applied to backstrip observed diagenetic sequences, and to estimate property evolution during burial.
Numerical simulation of flexural-slip and its role in creating fractures
This research is focused on the important role of bedding interfaces as potential mechanical discontinuities. The work has a long history of outcrop investigations, experimental studies, and now, simulations. The simulations require the development of methods to down-scale the continuum responses into probable fracture arrays. The work is associated with fractured reservoirs, and thus has links with the Carbonate Reservoirs research group.
Rock mechanics testing
This topic is pursued with our suite of lab apparatus. We operate two stiff presses into which we can install Hoek cells of SMART cells, which impose radially-differential confining pressures. We also have a large-sample direct-shear machine, with capability of measuring fluid flow both parallel and normal to a shear plane. There is also a soil mechanics rig. We are also completing development of a large-sample enhanced version of the SMART cells, jointly with University of Edinburgh and University of Göttingen.
Geomechanics at high pore pressure
This work examines, and challenges, classical ideas about the interaction of fluids and mechanics at extreme conditions. It has developed an energy-based reformulation that has proven useful for deriving new understanding of the responses of caprocks, and in situations of natural or induced hydraulic fracturing.
Please contact the institute to discuss.