{"id":{"repo_id":"houston","oai_identifier":"oai:uh-ir.tdl.org:10657/3259"},"canonical_url":"https://search.dev.ndltd.org/etd/houston/oai:uh-ir.tdl.org:10657/3259","repository":{"repo_id":"houston","name":"University of Houston","base_url":"https://uh-ir.tdl.org/server/oai/request"},"display":{"title":"Estimating Seismic Anisotropy: Fluid Substitution Theory, 3D-Printed Inclusion Models, and Multi-Component 3D VSP in the Bakken Shale","abstract":"Understanding seismic anisotropy is one of the most important issues in seismic exploration. In this dissertation, I tried to understand how fluids and lithology influence the elastic properties and seismic anisotropy of rocks, theoretically, experimentally, and in the field. I derived anisotropic fluid-substitution equations for the cases of HTI and orthorhombic media. The derivation was based on the anisotropic Gassmann's equations and linear-slip theory. The results have a similar form as the conventional isotropic Gassmann's equations, but now include two more parameters as normal and tangential weaknesses. To further examine the equations, I created two physical models using 3D-printing methods. The input printing material was thermoplastic with a density of 1.04 g/cc, P-wave velocity of 2167 m/s, and shear-wave velocity of 885 m/s. The first model was a solid-printed cube, and the other was a similarly sized cube, but with many layers of penny-shaped inclusions. Ultrasonic measurements (on the inclusion model) gave P-wave velocities of 1351 m/s and 1706 m/s, and shear-wave velocities of 656 m/s and 812 m/s. A fluid-substitution experiment with water observed 20% to 46% increase in P-wave velocities and 9% to 10% decrease in S-wave velocities. I found that predictions using our equations matched the measurements (within 4%) better than the Hudson's theory (within 10%). I also processed zero-offset, walk-away and walk-around VSP data in the Bakken shale, North Dakota, provided to us by Hess Corporation. I found that there was strong polar anisotropy in evidence from the VSP data in the Mission Canyon, Lodgepole, and Bakken formations. Thomsen’s anisotropy parameters for the Bakken formation were estimated to be 0.27 for ε, and 0.07 for δ. Though the Bakken and its overburden formations exhibited strong polar anisotropy, there was no substantial evidence of azimuthal anisotropy. The equations I have derived, experiments performed, and the VSP results obtained, provide methods to understand and estimate seismic anisotropy. Seismic anisotropy at different scales and complexity can be useful to characterize reservoir fluids and lithology.","abstract_html":"Understanding seismic anisotropy is one of the most important issues in seismic exploration. In this dissertation, I tried to understand how fluids and lithology influence the elastic properties and seismic anisotropy of rocks, theoretically, experimentally, and in the field. I derived anisotropic fluid-substitution equations for the cases of HTI and orthorhombic media. The derivation was based on the anisotropic Gassmann's equations and linear-slip theory. The results have a similar form as the conventional isotropic Gassmann's equations, but now include two more parameters as normal and tangential weaknesses. To further examine the equations, I created two physical models using 3D-printing methods. The input printing material was thermoplastic with a density of 1.04 g/cc, P-wave velocity of 2167 m/s, and shear-wave velocity of 885 m/s. The first model was a solid-printed cube, and the other was a similarly sized cube, but with many layers of penny-shaped inclusions. Ultrasonic measurements (on the inclusion model) gave P-wave velocities of 1351 m/s and 1706 m/s, and shear-wave velocities of 656 m/s and 812 m/s. A fluid-substitution experiment with water observed 20% to 46% increase in P-wave velocities and 9% to 10% decrease in S-wave velocities. I found that predictions using our equations matched the measurements (within 4%) better than the Hudson's theory (within 10%). I also processed zero-offset, walk-away and walk-around VSP data in the Bakken shale, North Dakota, provided to us by Hess Corporation. I found that there was strong polar anisotropy in evidence from the VSP data in the Mission Canyon, Lodgepole, and Bakken formations. Thomsen’s anisotropy parameters for the Bakken formation were estimated to be 0.27 for ε, and 0.07 for δ. Though the Bakken and its overburden formations exhibited strong polar anisotropy, there was no substantial evidence of azimuthal anisotropy. The equations I have derived, experiments performed, and the VSP results obtained, provide methods to understand and estimate seismic anisotropy. Seismic anisotropy at different scales and complexity can be useful to characterize reservoir fluids and lithology.","abstract_has_math":false,"creators":["Huang, Long 1988-"],"institution":"University of Houston","degree_name":"Doctor of Philosophy","degree_level":"Doctoral","degree_discipline":"Geophysics","degree_department":null,"school":null,"contributors":[],"advisors":["Stewart, Robert R."],"committee_chairs":[],"committee_members":["Zhou, Hua-Wei","Zheng, Yingcai","Sil, Samik"],"year":2016,"date_issued":"2016-05","date_published":"2016-05","updated_at":"2026-07-24T02:31:42Z","subjects":["Fluid substitution","Fracture behavior","Bakken shale","Anisotropy"],"languages":["eng"],"rights":["The author of this work is the copyright owner. UH Libraries and the Texas Digital Library have their permission to store and provide access to this work. UH Libraries has secured permission to reproduce any and all previously published materials contained in the work. Further transmission, reproduction, or presentation of this work is prohibited except with permission of the author(s)."],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"http://hdl.handle.net/10657/3259","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.advisor","label":"Advisor","values":["Stewart, Robert R."]},{"key":"dc:contributor.committeemember","label":"Committee Member","values":["Zhou, Hua-Wei","Zheng, Yingcai","Sil, Samik"]},{"key":"dc:creator","label":"Author","values":["Huang, Long 1988-"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2018-07-13T21:05:59Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2018-07-13T21:05:59Z"]},{"key":"dc:date.issued","label":"Date","values":["2016-05"]},{"key":"thesis:degree_discipline","label":"Discipline","values":["Geophysics"]},{"key":"thesis:degree_level","label":"Degree Level","values":["Doctoral"]},{"key":"thesis:degree_name","label":"Degree Name","values":["Doctor of Philosophy"]},{"key":"thesis:institution_name","label":"Thesis Institution Name","values":["University of Houston"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Fluid substitution","Fracture behavior","Bakken shale","Anisotropy"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language.iso","label":"Language (ISO)","values":["eng"]},{"key":"dc:rights","label":"Dc Rights","values":["The author of this work is the copyright owner. UH Libraries and the Texas Digital Library have their permission to store and provide access to this work. UH Libraries has secured permission to reproduce any and all previously published materials contained in the work. Further transmission, reproduction, or presentation of this work is prohibited except with permission of the author(s)."]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.uri","label":"Identifier URI","values":["http://hdl.handle.net/10657/3259"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Understanding seismic anisotropy is one of the most important issues in seismic exploration. In this dissertation, I tried to understand how fluids and lithology influence the elastic properties and seismic anisotropy of rocks, theoretically, experimentally, and in the field. I derived anisotropic fluid-substitution equations for the cases of HTI and orthorhombic media. The derivation was based on the anisotropic Gassmann's equations and linear-slip theory. The results have a similar form as the conventional isotropic Gassmann's equations, but now include two more parameters as normal and tangential weaknesses. To further examine the equations, I created two physical models using 3D-printing methods. The input printing material was thermoplastic with a density of 1.04 g/cc, P-wave velocity of 2167 m/s, and shear-wave velocity of 885 m/s. The first model was a solid-printed cube, and the other was a similarly sized cube, but with many layers of penny-shaped inclusions. Ultrasonic measurements (on the inclusion model) gave P-wave velocities of 1351 m/s and 1706 m/s, and shear-wave velocities of 656 m/s and 812 m/s. A fluid-substitution experiment with water observed 20% to 46% increase in P-wave velocities and 9% to 10% decrease in S-wave velocities. I found that predictions using our equations matched the measurements (within 4%) better than the Hudson's theory (within 10%). I also processed zero-offset, walk-away and walk-around VSP data in the Bakken shale, North Dakota, provided to us by Hess Corporation. I found that there was strong polar anisotropy in evidence from the VSP data in the Mission Canyon, Lodgepole, and Bakken formations. Thomsen’s anisotropy parameters for the Bakken formation were estimated to be 0.27 for ε, and 0.07 for δ. Though the Bakken and its overburden formations exhibited strong polar anisotropy, there was no substantial evidence of azimuthal anisotropy. The equations I have derived, experiments performed, and the VSP results obtained, provide methods to understand and estimate seismic anisotropy. Seismic anisotropy at different scales and complexity can be useful to characterize reservoir fluids and lithology."]},{"key":"dc:format.mimetype","label":"Dc Format Mimetype","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["Estimating Seismic Anisotropy: Fluid Substitution Theory, 3D-Printed Inclusion Models, and Multi-Component 3D VSP in the Bakken Shale"]}]}],"canonical_facts":{"dc:contributor.advisor":["Stewart, Robert R."],"dc:contributor.committeemember":["Zhou, Hua-Wei","Zheng, Yingcai","Sil, Samik"],"dc:creator":["Huang, Long 1988-"],"dc:date.accessioned":["2018-07-13T21:05:59Z"],"dc:date.available":["2018-07-13T21:05:59Z"],"dc:date.issued":["2016-05"],"dc:description.abstract":["Understanding seismic anisotropy is one of the most important issues in seismic exploration. In this dissertation, I tried to understand how fluids and lithology influence the elastic properties and seismic anisotropy of rocks, theoretically, experimentally, and in the field. I derived anisotropic fluid-substitution equations for the cases of HTI and orthorhombic media. The derivation was based on the anisotropic Gassmann's equations and linear-slip theory. The results have a similar form as the conventional isotropic Gassmann's equations, but now include two more parameters as normal and tangential weaknesses. To further examine the equations, I created two physical models using 3D-printing methods. The input printing material was thermoplastic with a density of 1.04 g/cc, P-wave velocity of 2167 m/s, and shear-wave velocity of 885 m/s. The first model was a solid-printed cube, and the other was a similarly sized cube, but with many layers of penny-shaped inclusions. Ultrasonic measurements (on the inclusion model) gave P-wave velocities of 1351 m/s and 1706 m/s, and shear-wave velocities of 656 m/s and 812 m/s. A fluid-substitution experiment with water observed 20% to 46% increase in P-wave velocities and 9% to 10% decrease in S-wave velocities. I found that predictions using our equations matched the measurements (within 4%) better than the Hudson's theory (within 10%). I also processed zero-offset, walk-away and walk-around VSP data in the Bakken shale, North Dakota, provided to us by Hess Corporation. I found that there was strong polar anisotropy in evidence from the VSP data in the Mission Canyon, Lodgepole, and Bakken formations. Thomsen’s anisotropy parameters for the Bakken formation were estimated to be 0.27 for ε, and 0.07 for δ. Though the Bakken and its overburden formations exhibited strong polar anisotropy, there was no substantial evidence of azimuthal anisotropy. The equations I have derived, experiments performed, and the VSP results obtained, provide methods to understand and estimate seismic anisotropy. Seismic anisotropy at different scales and complexity can be useful to characterize reservoir fluids and lithology."],"dc:format.mimetype":["application/pdf"],"dc:identifier.uri":["http://hdl.handle.net/10657/3259"],"dc:language.iso":["eng"],"dc:rights":["The author of this work is the copyright owner. UH Libraries and the Texas Digital Library have their permission to store and provide access to this work. UH Libraries has secured permission to reproduce any and all previously published materials contained in the work. Further transmission, reproduction, or presentation of this work is prohibited except with permission of the author(s)."],"dc:subject":["Fluid substitution","Fracture behavior","Bakken shale","Anisotropy"],"dc:title":["Estimating Seismic Anisotropy: Fluid Substitution Theory, 3D-Printed Inclusion Models, and Multi-Component 3D VSP in the Bakken Shale"],"thesis:degree_discipline":["Geophysics"],"thesis:degree_level":["Doctoral"],"thesis:degree_name":["Doctor of Philosophy"],"thesis:institution_name":["University of Houston"]},"updated_at":"2026-07-24T02:31:42Z"}