Research

Why can we learn something about the deformation of rocks when we deform analog materials?

The answer to this question can be given in one word: scaling. In general, the problem with deforming real rocks is often that we need high pressures and temperatures and sometimes very long timescales to deform a rock at the same conditions that would for example exist in the middle crust at approximately 15 kilometers depth. This means we need heavy machinery and small sample sizes, which in return means that in most cases we cannot directly observe what happens during deformation. At this point scaling comes into play. If we find materials that deform in a similar manner to rocks but, let’s say at lower pressure and temperatures, we can build a deformation apparatus where we can actually observe the deformation while it happens and where we are not restricted by sample size, time, etc. With other words, we choose a material that has a rheology which scales to the rheology of a real rock. However, choosing a material as a rock analog also requires making some compromises. In the materials we are using in the structure lab we, for example, do not take chemical processes into account. This means that our materials are scaled with respect to things like rheology and strain rates but they have a completely different chemistry compared to actual rocks.


Experimental analysis of strain transients in a heterogeneous, semi-brittle system: Tom Birren, M.S. Student

In the experiment we observe the evolution of different fractures and how they impact the deformation dynamics.
In the experiment we observe the evolution of different fractures and how they impact the deformation dynamics.

In addition to earthquakes, the scientific community has now been aware of strain transient-slips for the last decade. These transients manifest in slow-slip events and low frequency earthquakes that transfer stress from plate motions up-fault into seismogenic depths. These transients are detected using seismography, geodetic, and tilt measurements in various settings (i.e. subduction environments and the creeping segment of the San Andreas). Not much is known about the mechanics of strain transients. In the structure lab we conduct experiments to model how strain transients relate to the rheology of semi-brittle systems. We are using a visco-elastic-plastic yield-stress fluid that has properties comparable to at mid-crustal levels. We investigate the impact fractures have on the deformation dynamics and combine our experimental results with numerical models developed by Luc Lavier at UT Austin.

Funding source: NSF Geophysics # 1547492


Experimental analysis of strain transients in bi-modal granular systems and applications to the San Andreas Fault: Jeremy Randolph-Flagg, M.S. Student

Hypothesis of the proposed work where the grain size distribution governs the slip dynamics in a shear zone.
Hypothesis of the proposed work where the grain size distribution governs the slip dynamics in a shear zone.

Faults accommodate displacement through a continuum of aseismic steady slip or creep to earthquake-generating stick-slip events. The mode of slip can change along the length of a single fault, as is the case of the San Andreas Fault. We study what effect the grain size distribution of fault gouge or cataclasite might have on the the mode of slip using a simple shear apparatus and acrylic disks.


Fracture pattern and propagation in materials with complex rheologies: Kyle Bogatz, Undergraduate Research Assistant

Fracture patterns are stronly dependent on teh rheology of the material. a) Fracture in gelatin (elasto-plastic), c) fracture in Carbopol (visco-elasto-plastic)
Fracture patterns are stronly dependent on teh rheology of the material. a) Fracture in gelatin (elasto-plastic), c) fracture in Carbopol (visco-elasto-plastic)

Understanding how rocks fracture is not only vital for risk management concerning earthquakes but it has a large socio-economic impact as it is essential for the extraction of hydrocarbons, geothermal energy, waste disposal, and CO2 sequestration. How a rock may fracture is dependent on the properties of the rock, or with other words on its rheology. Here we are conducting physical experiments investigating what effect the rheology has on the fracture pattern and propagation. We conduct experiments in a Hele-Shaw-Cell where we fracture a variety of materials ranging from powders, to gelatin, to hydrous gels, by injecting pressured air. We monitor the pressure evolution in the experimental cell and document the evolving fracture pattern.


The effect of a liquid phase in a granular system on force distribution during deformation: Chris Ladd, M.S. Student

The force chain pattern changes strongly form a purely granular (a) to a two-phase (b) system
The force chain pattern changes strongly form a purely granular (a) to a two-phase (b) system

We investigate the stress distribution in a two-phase system where one phase is solid and the other fluid. These systems are important geologically – for example as petroleum fluids in reservoir rocks – but have only received limited numerical and experimental investigation. Understanding the stress distribution provides insights into the mechanisms of how such systems deform and fail, which has a large impact on the effective extraction of petroleum. We perform physical experiments on photoelastic uncemented and cemented granular materials with a viscous pore fluid during shear deformation.

Funding source: ACS PRF 57123-DNI8