Congratulations Alejandro Cardona Ramirez

27 May, 2020

Congratulations to EGEL group member, Alejandro Cardona Ramirez who successfully defended his Ph.D thesis, Fluid Transport in Fractured Carbonate Rocks on May 21. Alejandro is supervised by Professor J. Carlos Santamarina.His Committee members included Dr. Hussein Hoteit (chair), Dr. Shuyu Sun, Dr. Thomas Finkbeiner, Dr. Maurice Dusseualt (University of Waterloo, Canada) and Dr. Santamarina.

Dissertation Abstract - Fluid Transport in Fractured Carbonate Rocks

Carbonate rocks store approximately half of the world’s proven oil reserves. Whereas the rock matrix controls storativity, natural and induced fractures control the overall flow in fractured carbonate reservoirs and lead to complex hydromechanical processes. This thesis combines novel experimental devices, test protocols, and numerical methods to advance the understanding of flow-related phenomena in a variety of geological materials.

Genesis and postdepositional diagenetic processes define the porous network topology and the matrix permeability. The underlying predictor for permeability is pore size; however, all prediction models have one order of magnitude uncertainty. The use of permeability measurements with simple data acquisition and interpretation overcome these limitations and provide the true value of permeability rather than correlation estimate.

Fractures in the subsurface localize flow and deformations and also pose inherent numerical challenges when modeling fractured rock behavior. Roughness, matedness, and strength all control hydromechanical responses at the fracture level. Physics-inspired, data-driven transmissivity models and robust numerical methods help to identify and predict salient coupled processes.

Although the fundamental laws of capillarity are well understood, complexities arise in fractured systems as add impose multi-scale geometric effects. Fractures and matrices display inherent characteristic velocities and capillary behavior. The invasion morphologies depend on the velocity during immiscible displacement and are a visible manifestation of the balance between the fracture viscous drag and the matrix capillary suction forces.