Reservoir characterization using laboratory ultrasonic rock physics: understanding pore fluid effects on elastic properties

dc.contributor.authorShodunke, Ganiyat Oluwaseun
dc.date.accessioned2020-12-08T18:10:00Z
dc.date.available2020-12-08T18:10:00Z
dc.date.graduationmonthMay
dc.date.issued2021-05-01
dc.description.abstractThe quantity of hydrocarbon recovered from a carbonate reservoir varies depending on the quality (i.e., porosity, permeability, reservoir volume) of that reservoir, indirectly characterized from the elastic properties encoded in the seismic reflection data. Due to the complexity of carbonates, they require repeated updating of characterization and modeling during production. This creates added cost to well drilling but provides significant return in terms of decisive field development plans and knowledge of productive and nonproductive hydrocarbon zones. The purpose of this study is to understand the effects of pore-fluid composition on the elastic properties of the Viola formation reservoir found in Kansas, Oklahoma, and Texas, and implications for utilization of seismic data attributes in optimizing reservoir studies and guiding field development efforts. Rock physics experiments such as lab ultrasonic experiments and fluid replacement experiments integrated with seismic fluid replacement modeling were used to pursue a thorough understanding of the carbonate reservoir properties. Brine, oil, and water were injected into the carbonate rock during the fluid replacement experiment and ultrasonic waves were propagated through the rock to obtain Primary P wave velocity, Secondary S wave velocity, and elastic parameters such as Young’s modulus, Shear (Rigidity) modulus, Bulk modulus, and Poisson’s ratio. These parameters were also recorded for the rock under dry conditions, and they provided useful information about the seismic wave’s response to fluids and lithofacies changes in the Viola carbonate rock. There was a noticeable response change in amplitude and some change in velocity and impedance of the wave traveling through the Viola limestone formation with the presence of and type of fluid present. Higher amplitudes and faster velocities were observed for dry rock wave signals, while lower amplitudes and slower velocities were recorded for brine and oil-saturated rock wave signals. The recorded results on the Viola cores were in accordance with previously observed Gassmann fluid replacement modeling results (Cimino, 2020) from the Viola well log data and seismic amplitude analysis (Vohs, 2016) from the Viola seismic data.
dc.description.advisorAbdelmoneam Raef
dc.description.advisorMatthew W. Totten
dc.description.degreeMaster of Science
dc.description.departmentDepartment of Geology
dc.description.levelMasters
dc.identifier.urihttps://hdl.handle.net/2097/41000
dc.language.isoen_US
dc.publisherKansas State University
dc.rights© the author. This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectViola limestone formation
dc.subjectRock physics
dc.subjectFluid replacement experiments
dc.subjectUltrasonic velocity experiment
dc.subjectAttenuation
dc.subjectComanche County, Kansas
dc.titleReservoir characterization using laboratory ultrasonic rock physics: understanding pore fluid effects on elastic properties
dc.typeThesis

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