Assessment of Reservoir Quality and Potential Impact of Sequestered
Carbon
Dioxide in Reservoir Units of Diverse Lithologies in South-Central, Mississippi, USA
Degny, Assonman D.; Kirkland, Brenda L.; Schmitz, Darrel W.
The objective of this study is to determine the impact of
carbon
dioxide on mineralogy, porosity, permeability, and fractures in hydrocarbon reservoirs in southern Mississippi with emphasis on the Heidelberg Field, Jasper County. Eight samples, two from the Eutaw Formation, one from the Tuscaloosa Formation, one from the Rodessa Formation, three from the Smackover Formation, and one from the Salem Formation (selected as control based on mineralogical homogeneity), were studied in a laboratory setting. Samples were placed in a carbonic acid solution, sealed into steel chambers, and heated. Pre- and Post-
carbon
dioxide analyses include: standard petrography, X-ray diffraction, and scanning electron microscopy. Potentially reactive minerals include: feldspars, glauconite, siderite, kaolinite, and calcite. In the pre-
carbon
dioxide samples porosity types identified are interparticle, intraparticle, voggy, and microfracture, with percent porosity ranging from 0.0114% to 29.318%. The first post-
carbon
dioxide sample was held for three months at an average temperature of 30 to 35 degrees Celsius. This sample from the Salem Formation showed limited evidence of dissolution. The other post-
carbon
dioxide samples were held for six months at an average temperature of 80 to 90 degrees Celsius. The significance of this study is that it contributes to the understanding of the behavior of reservoir rocks undergoing enhanced oil recovery with
carbon
dioxide or serving as
carbon
sequestration sites.
AAPG Search and Discovery Article #90163©2013AAPG 2013 Annual Convention and Exhibition, Pittsburgh, Pennsylvania, May 19-22, 2013