Identifier
etd-06302011-124114
Degree
Master of Science in Petroleum Engineering (MSPE)
Department
Petroleum Engineering
Document Type
Thesis
Abstract
Geopressured geothermal brines are a vast geothermal resource in the US Gulf of Mexico region. In particular, geopressured sandstones near salt domes are potential sources of geothermal energy because salt diapirs with high thermal conductivities may pierce younger, cooler strata. These characteristics enhance transfer heat from older, hotter strata at the base of the diapir into shallower strata. Moreover, widespread geopressure in the Gulf region tends to preserve permeability, enhancing productivity. As an example, the Camerina A sand of South Louisiana was chosen as a geomodel for a numerical simulation study of effects of CO2 injection and coupled convection as a method of geothermal development. This study presents scenarios for heat harvesting from typical Gulf of Mexico aquifers including Camerina A that take advantage of coupled convection and simultaneous CO2 sequestration. Suites of TOUGH2 numerical simulations demonstrate benefits of introducing CO2 injection wells, varying locations of injection/production wells, and exploiting gravity segregation of the fluids.
Date
2011
Document Availability at the Time of Submission
Release the entire work immediately for access worldwide.
Recommended Citation
Plaksina, Tatyana, "Modeling effects of coupled convection and CO2 injection in stimulating geopressured geothermal reservoirs" (2011). LSU Master's Theses. 626.
https://repository.lsu.edu/gradschool_theses/626
Committee Chair
White, Christopher
DOI
10.31390/gradschool_theses.626