DepartmentSchool of the Environment, Geography, and Geosciences
February and October
Applications accepted all year round
The work on this project will:
- Prepare fractured granite samples by subjecting them to elevated HDR environments
- Measure primary permeability of the thermally treated samples using high pressure rock physics equipment combined with 3D microseismic arrays
- Develop new frictional thermo-physics models to provide new links between laboratory and field scale processes
Permeability is the most important property of geothermal reservoirs and the subject of numerous studies (e.g. Sass and Götz, 2012; Luviano et al., 2015; Brehme et al., 2016; Bär et al., 2017).
While all rocks contain inherent porosity and permeability, the development of a secondary permeability (fracture related) is gaining renewed interest as a means to develop Enhanced Geothermal Systems (EGS), by injecting new tensile fracture networks in hot but relatively impermeable rocks as a source of deep sustainable geothermal energy.
The permeability of EGS will be simulated in a controlled laboratory environment to link Acoustic Emission or AE (the laboratory analogue of tectonic seismicity) to field scale geophysical methods, which have seen an increased application for geothermal sciences, and significant promise in this area.
On this project, a suite of fractured granite samples will be prepared by subjecting them to elevated HDR environments, with thermal damage controlled and monitored using a tube furnace equipped with a waveguide system for measuring passive and active seismicity (Acoustic Emission, AE).
Thermal stressing temperature - which generates a primary microfracture fabric via the differential expansion of component minerals in the granite – will be increased stepwise from 100°C to 600°C to induce a network of cracks. To calibrate the method, samples will be scanned pre- and post-treatment using high resolution X-Ray Computed Tomography.
Primary permeability of the thermally treated samples will be determined using high-pressure rock physics equipment capable of measuring active/passive seismicity and permeability at a range of simulated burial conditions to 4 km depth, and to temperatures of 200°C to simulate geothermal reservoir conditions.
Once primary permeability has been established, the equipment will deform and fracture selected samples in both compression and tension to test the associated secondary permeability, and to thus evaluate improvements in permeability and heat flow resulting from secondary stimulation of Hot Dry Rocks.
Finally, to understand the interplay and relationship between permeability and the heat transfer and thermal conductivity of the rock/fluid system, a range of post-test frictional thermo-physics models will be developed to provide new links between laboratory and field scale processes. An additional output of this link will be to better use the natural seismicity as a tool to both monitor and understand fracturing in EGS for risk mitigation and optimisation purposes.
- You'll need a good first degree from an internationally recognised university (minimum second class or equivalent, depending on your chosen course) or a Master’s degree in Geophysics or Geology
- In exceptional cases, we may consider equivalent professional experience and/or Qualifications
- English language proficiency at a minimum of IELTS band 6.5 with no component score below 6.0
We’d welcome applications from candidates with experience in basic modeling software such as MatLab.
When you are ready to apply, please follow the 'Apply now' link on the Earth and Environmental Sciences PhD subject area page and select the link for the relevant intake. Make sure you submit a personal statement, proof of your degrees and grades, details of two referees, proof of your English language proficiency and an up-to-date CV. Our ‘How to Apply’ page offers further guidance on the PhD application process.
Please note, to be considered for this self-funded PhD opportunity you must quote project code SEES4830219 when applying.