Patterson, James W.
Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures.
Natural convection of water plays a key role in shaping the thermal structure of the subsurface. As a consequence of water density decreasing with temperature and temperature increasing with depth in the Earth’s crust, an unstable situation develops: cold, dense fluid overlies hot, less dense fluid. Given a sufficiently permeable and vertically extensive host, hot water will buoyantly rise towards the surface as cold water sinks to replace it, forming a convective circulation cell. Rock units with permeability far too low to facilitate convection may, however, contain high- permeability faults or fractures capable of sustaining convective fluid flow. We investigate the effects and emergent behavior of fracture convection by means of numerical simulation using the Complex Systems Modeling Platform (CSMP++).
Despite being confined to a narrow, planar feature, natural convection in a fault or fracture significantly impacts the thermal structure of the subsurface via conduction heat exchange with the host rock and enhances fluid mixing. We compare convection in wide, filled fault zones and narrow, open slots and show that convection patterns within the fracture and the strength of this subsequent thermal perturbation are a function of transmissivity – permeability times thickness – rather than either permeability or thickness alone. Fluid circulation may lead to temperature changes of several tens of degrees in the host up to a distance roughly equal to half the height of the fracture, significantly changing the local geothermal gradient. Above the fracture, these thermal perturbations influence conductive heat flow and take on a diffuse pattern, appearing much wider than the originating fracture or fault. By varying host rock permeability, we show that fluid exchange between fracture and host varies with transmissivity, but has little effect on convection patterns. Conversely, Rayleigh convection within the host rock dominates and overprints convection within the fracture.
We build on these results by investigating convection in five elliptic fractures in an en echelon array. Thermal perturbations arising from convection in each fracture eventually connect and align, thereby imposing mutual feedback of convection in neighboring fractures, despite a lack of hydraulic connectivity between them. This interaction leads to a self-organizing pattern of convection cells, with regions of upflow and downflow aligning with the upflows and downflows in their neighbors, inducing a regular pattern of alternating cooled and heated host rock regions between the fractures that is aligned (sub-) perpendicular to the en echelon fracture array. By varying fracture spacing, we determine that this “synchronization” effect may occur
when fracture spacing is less than convection cell width. Even in fractures with heterogeneous permeability, convection cells continue to self-organize despite zones of low-transmissivity. Fractures which alone cannot facilitate convection may nevertheless host weaker fluid circulation cells in response…
Advisors/Committee Members: Driesner, Thomas, Heinrich, Christoph, Geiger, Sebastian, Valley, Benoit.
to Zotero / EndNote / Reference
APA (6th Edition):
Patterson, J. W. (2019). Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/332673
Chicago Manual of Style (16th Edition):
Patterson, James W. “Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures.” 2019. Doctoral Dissertation, ETH Zürich. Accessed April 22, 2019.
MLA Handbook (7th Edition):
Patterson, James W. “Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures.” 2019. Web. 22 Apr 2019.
Patterson JW. Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures. [Internet] [Doctoral dissertation]. ETH Zürich; 2019. [cited 2019 Apr 22].
Available from: http://hdl.handle.net/20.500.11850/332673.
Council of Science Editors:
Patterson JW. Thermo-Hydro-Mechanical Controls on Natural Convection in Faults and Fractures. [Doctoral Dissertation]. ETH Zürich; 2019. Available from: http://hdl.handle.net/20.500.11850/332673