Hydrate systems in geologic media are multiple phase systems, in which the potential for both mobile and immobile phases occupy the same pore space, with the potential mobile phases being aqueous, gas, and nonaqueous liquid, and the potential immobile phases being ice and hydrate. Gas hydrates form at high pressures and low temperatures, and the stability envelope for natural gas hydrates span the triple-point of water, complicating the thermodynamics of hydrate systems via phase transitions, appearances, and disappearances. For example, a hydrate bearing formation, stable at temperatures above freezing, could yield ice formations with strong depressurization, resulting in hydrate dissociation and cooling. Hydrate structures vary across their host geologic settings, from large concretions in suboceanic muds to connected, pore-filling bodies in subarctic sandstones. The geomechanical reaction of a hydrate-bearing formation to the dissociation process depends on the contribution of the hydrate structure to the mechanical properties of the formation. Production of natural gas hydrates from geologic reservoirs is controlled by coupled processes, each with inherent complexities.
This project will investigate the numerically and experimentally coupled hydrologic, thermodynamic, and geomechanical processes that dominate the production of natural gas hydrates from geologic accumulations. Production technologies will include both conventional (such as depressurization, thermal stimulation, and inhibitor injection) and unconventional (such as nitrogen injection, air injection, and former swapping). Production of natural gas hydrates from geologic reservoirs is controlled by coupled processes, each with inherent complexities.