The presence of cracks and fractures in geomaterials makes their mechanical behaviour difficult to predict, this is particularly true for fluid saturated rocks [1]. Fluids spread through pores and cracks of rocks and have significant effects on the rock mechanics. The continuous interest in this hydromechanical coupling in geomaterials reflects the need to rationalize empirical practices in fields of applications as diverse as earthquake forecasting or mine pit stability. The description of the fluid transport and hydromechanical coupling in fractured rocks is a non-trivial physics problem encountered in many research fields. Our ability to overcome current challenges in the domain relies on a better fundamental and experimental understanding of the behaviour of rocks having heterogeneous pore structures and complex interconnected fracture morphologies (see picture).
Recent advances in X-ray micro-computed tomography (micro-CT) enable 3D observations of the inner structure of rocks and offer new avenues to carry out mechanical studies on fractured geomaterials at the laboratory scale. The two groups at the Australian National University and Ghent University have developed world-class in-situ (e.g., inside the scanner) micro-mechanical instruments that enable 3D study of the hydromechanical coupling and fluid transport in a rock as it deforms, fails or even fragments [2-5]. The PhD student will join this collaborative research activity tackling difficult questions such as:
How does the failure and fracturing of a rock depend on its level of fluid saturation? Can we quantify the impact of different loading paths and fragmentation level on pores connectivity to better predict fractured rock permeability? Can we characterise the 3D structure of hydraulically cracked rocks at different description level from local fracture morphology to the connectivity of the fracture network? What is the response of a fracture with a complex morphology to cyclic changes in fluid pressure?
Those questions will be explored by carrying out tomography-based experiments on actual rock cores and on model synthetic solids to try rationalising key factors and mechanisms underlying our observations; an important aspect of the work will be the frequent interactions with geotechnical engineers with expertise in empirical field practices.
[1] Gueguen Y. and Bouteca M., Mechanics of Fluid-saturated Rocks (Elsevier Academic Press, 2004). [2] Francois, N., et al., Review of Scientific Instruments, 93(8): p. 083704 (2022). [3] Bultreys, T., et al. 34, 042008 Phys. Fluids (2022). [4] Bultreys, T., et al. 121 (12) PNAS (2024). [5] Francois, N., et al. arXiv:2206.12763, (2022).
Candidate profile
We are looking for candidates having a curious mind, creative thinking, some grit and determination. He/She will help developing a set of advanced experimental set-ups to explore the hydromechanical coupling in geomaterials.
Work environment
What we offer
To Apply
To be considered for this position, please apply online via:
https://docs.google.com/forms/d/1qmy6touHyw8vvy4ocPl6kiSWft_4jhAjNr0A22hczx0/edit?ts=66dee5a0
Applications by email will NOT be processed. Applications close on 1st March 2025 and will be evaluated on a bi-weekly rolling basis. The starting date of the position will be in 2025 and is to be determined together with the selected candidate.
Questions can be directed to A/Prof. Nicolas Francois (nicolas.francois@anu.edu.au) Experimental Mechanics Lab at ANU and Prof. Tom Bultreys (Tom.Bultreys@UGent.be) at Centre for X-ray Tomography (UGCT), Ghent University.
Links to our labs
Experimental Mechanics Lab is part of the M3D Training centre (https://m3d.edu.au/) and ANU CT-Lab (https://ctlab.anu.edu.au/). Geomaterials research group at Ghent University, Belgium (PProgress, https://pprogress.ugent.be/ and https://www.youtube.com/watch?v=SZo-StQtAYs )