Geologic characterization and modeling for quantifying CO₂ storage capacity of the High Island 10-L field in Texas state waters, offshore Gulf of Mexico

dc.contributor.advisorChuchla, Richard J. (Richard Julian)
dc.contributor.advisorMeckel, Timothy Ashworth
dc.creatorRamirez Garcia, Omar
dc.date.accessioned2019-09-17T15:14:56Z
dc.date.available2019-09-17T15:14:56Z
dc.date.created2019-08
dc.date.issued2019-09-12
dc.date.submittedAugust 2019
dc.date.updated2019-09-17T15:14:56Z
dc.description.abstractCarbon dioxide capture and storage (CCS) is a promising technology for mitigating climate change by reducing CO₂ emissions to the atmosphere and injecting captured industrial emissions into deep geologic formations. Deep subsurface storage in geologic formations is similar to trapping natural hydrocarbons and is one of the key components of CCS technology. The quantification of the available subsurface storage resource is the subject of this research project. This study focuses on site-specific geologic characterization, reservoir modeling, and CO₂ storage resource assessment (capacity) of a depleted oil and gas field located on the inner continental shelf of the Gulf of Mexico, the High Island 10L field. lower Miocene sands in the Fleming Group beneath the regional transgressive Amphistegina B shale have extremely favorable geologic properties (porosity, thickness, extent) and are characterized in this study utilizing 3-D seismic and well logs. Key stratigraphic surfaces between maximum flooding surfaces (MFS-9 to MFS-10) demonstrate how marine regression and transgression impact the stacking pattern of the thick sands and overlying seals, influencing the overall potential for CO₂ storage. One of the main uncertainties when assessing CO₂ storage resources at different scales is to determine the fraction of the pore space within a formation that is practically accessible for storage. The goal of the modeling section of this project is to address the uncertainty related to the static parameters affecting calculations of available pore space by creating facies and porosity geostatistical models based on the spatial variation of the available data. P50 values for CO₂ storage capacity range from 37.56 to 40.39 megatonnes (Mt), showing a narrow distribution of values for different realizations of the geostatistical models. An analysis of the pressure build-up effect on storage capacity was also performed, showing a reduction in capacity. This research further validates the impact of the current carbon tax credit program (45Q), applied directly to the storage resources results for the High Island field 10L using a simple NPV approach based on discounted cash flows. Several scenarios are assessed, where the main variables are the duration of the applicability of the tax credit, number of injection wells, and total storage capacity. Results are measured in terms of the cost of capture required for a project to be economic, given previous assumptions.
dc.description.departmentEnergy and Earth Resources
dc.format.mimetypeapplication/pdf
dc.identifier.urihttps://hdl.handle.net/2152/75869
dc.identifier.urihttp://dx.doi.org/10.26153/tsw/2971
dc.language.isoen
dc.subjectSubsurface
dc.subjectCarbon capture and storage
dc.subjectCCS
dc.subjectGeological modeling
dc.subjectSeismic
dc.subjectStratigraphy
dc.subjectFinance
dc.titleGeologic characterization and modeling for quantifying CO₂ storage capacity of the High Island 10-L field in Texas state waters, offshore Gulf of Mexico
dc.typeThesis
dc.type.materialtext
thesis.degree.departmentEnergy and Earth Resources
thesis.degree.disciplineEnergy and Earth Resources
thesis.degree.grantorThe University of Texas at Austin
thesis.degree.levelMasters
thesis.degree.nameMaster of Science in Energy and Earth Resources

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