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    An evaluation of carbon dioxide sequestration potential of the Permian Cedar Mesa Sandstone, northeastern Arizona

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    Author
    Rauzi, S.L.
    Spencer, J.E.
    Issue Date
    2014-03-18
    Keywords
    Arizona Geological Survey Open File Reports
    cretaceous
    Jurassic
    Lower Permian
    Paleozoic
    Mesozoic
    Defiance uplift
    northeastern Arizona
    Colorado Plateau
    Navajo County
    Black Mesa
    Dakota Formation
    Entrada Formation
    Rocky Mountain Carbon Capture and Sequestration
    RMCCS
    geologic sequestration
    National Engineering Technology Laboratory
    NETL
    DOE
    carbon sequestration
    carbon storage
    CO2
    global warming
    greenhouse gas
    climate change
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    Citation
    Rauzi, S.L. and Spencer J.E., 2014, An evaluation of carbon dioxide sequestration potential of the Permian Cedar Mesa Sandstone, northeastern Arizona. Arizona Geological Survey Open File Report, OFR-14-03, 22 p.
    Description
    Northeastern Arizona encompasses the southwestern part of the Colorado Plateau, an area of gently dipping to slightly tilted Paleozoic and Mesozoic strata that include porous and permeable sandstone units. The Lower Permian Cedar Mesa Sandstone was identified for study as a potential target for CO2 sequestration in order to reduce anthropogenic CO2 emissions to the atmosphere. The Cedar Mesa Sandstone is overlain by the impermeable Organ Rock Formation, which is necessary to prevent escape of sequestered CO2. The salinity of groundwater in the Cedar Mesa Sandstone is unknown, but must be determined before CO2 can be sequestered because CO2 sequestration is not permitted in potable groundwater under current regulatory conditions. Well logs for 755 drill holes were used to evaluate the extent, depth, and thickness of subsurface formations. ESRI® ArcMap™ software was then used to calculate the volume of the Cedar Mesa Sandstone where the top of the unit is below 3000 feet (915 meters) depth, which is the minimum depth necessary for CO2 sequestration where the CO2 is under sufficient pressure to remain in a dense, nearliquid state. Well logs were used to evaluate porosity, which was then used to calculate the amount of pore space that is theoretically available for CO2 storage (the effective porosity). We calculate that there are between 30 km3 and 80 km3 of pore space in the Cedar Mesa Sandstone. The fraction of pore-space volume that is accessible to CO2 injection is estimated to be approximately 0.5% to 5%. Applying this storage efficiency to the Cedar Mesa Sandstone indicates that 0.15 km3 to 4.3 km3 of pore space is accessible to injected CO2, and that 0.114 to 3.24 billion tonnes of CO2 could be sequestered in this pore space at a density of approximately 750 kg/m3.
    URI
    http://hdl.handle.net/10150/629497
    Additional Links
    https://library.azgs.arizona.edu/
    Language
    en
    Series/Report no.
    OFR-14-03
    Rights
    Arizona Geological Survey. All rights reserved.
    Collection Information
    Documents in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
    North Bounding Coordinate
    37
    South Bounding Coordinate
    35.3
    West Bounding Coordinate
    -112
    East Bounding Coordinate
    -109
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