Predicting opening mode fracture patterns through stress corrosion cracking

OpenFrac will develop a new fundamental model to quantify the evolution of opening mode fractures – such as economically important joints and veins – through the diagenetic evolution of sedimentary rocks. We will measure the growth of single sub-critical fractures in sandstone and limestone as a function of the chemical composition of pore water, temperature, and pressure. Our new understanding of the physico-chemical processes of sub-critical fracture in rocks will provide parameters for numerical models designed to explore the evolution of more complex patterns of multiple fractures in space and time.