{"id":{"repo_id":"woods-hole","oai_identifier":"oai:darchive.mblwhoilibrary.org:1912/66540"},"canonical_url":"https://search.dev.ndltd.org/etd/woods-hole/oai:darchive.mblwhoilibrary.org:1912/66540","repository":{"repo_id":"woods-hole","name":"Woods Hole Oceanographic Institute","base_url":"https://darchive.mblwhoilibrary.org/server/oai/request"},"display":{"title":"Joule heating and pore pressure evolution, magmatic intrusions at continental rifts, and microseisms in Yellowstone Lake","abstract":"The goal of this thesis is to investigate research topics related to geothermal resources. Chapter 1 introduces the thesis and motivates the need to study research topics in relevant geothermal environments, and develop new technologies to economically extract heat from these resources. In Chapter 2, microseism events in Yellowstone National Park are studied. Yellowstone is located in one of the most seismically active volcanic calderas in the world and is a widely studied area for investigating physical (e.g., faulting) and chemical (e.g., hydrothermal venting) relationships in geothermal systems. Chapter 3 describes dike intrusion modeling research I conducted early in my graduate studies including the feedback mechanisms between magma injection at plate spreading centers and topographic development. Chapter 4 represents a shift in my research interests from science to engineering problems relevant for geothermal heat extraction. In this chapter, I describe the design process for developing a novel experimental approach to study the effects of applying a high-voltage to saturated rock specimens under in-situ states of stress. This novel “Electric Rock Fracturing” experimental set-up is used in Chapter 5, the final chapter of this thesis, to study the effects of high-voltage application on the temperature, electrical conductivity, and permeability of brine saturated Berea Sandstone rock specimens.","abstract_html":"The goal of this thesis is to investigate research topics related to geothermal resources. Chapter 1 introduces the thesis and motivates the need to study research topics in relevant geothermal environments, and develop new technologies to economically extract heat from these resources. In Chapter 2, microseism events in Yellowstone National Park are studied. Yellowstone is located in one of the most seismically active volcanic calderas in the world and is a widely studied area for investigating physical (e.g., faulting) and chemical (e.g., hydrothermal venting) relationships in geothermal systems. Chapter 3 describes dike intrusion modeling research I conducted early in my graduate studies including the feedback mechanisms between magma injection at plate spreading centers and topographic development. Chapter 4 represents a shift in my research interests from science to engineering problems relevant for geothermal heat extraction. In this chapter, I describe the design process for developing a novel experimental approach to study the effects of applying a high-voltage to saturated rock specimens under in-situ states of stress. This novel “Electric Rock Fracturing” experimental set-up is used in Chapter 5, the final chapter of this thesis, to study the effects of high-voltage application on the temperature, electrical conductivity, and permeability of brine saturated Berea Sandstone rock specimens.","abstract_has_math":false,"creators":["Smalls, Paris T."],"institution":"Massachusetts Institute of Technology and Woods Hole Oceanographic Institution","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":["Einstein, Herbert"],"committee_chairs":[],"committee_members":[],"year":2023,"date_issued":"2023-09","date_published":"2023-09","updated_at":"2026-07-27T22:05:19Z","subjects":["Thermal pore pressure","Permeability","Joule heating"],"languages":["en_US"],"rights":["©2023 Paris Smalls. This work is licensed under a CC BY-SA 2.0. The author hereby grants to MIT a nonexclusive, worldwide, irrevocable, royalty-free license to exercise any and all rights under copyright, including to reproduce, preserve, distribute and publicly display copies of the thesis, or release the thesis under an open-access license."],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier.doi","label":"DOI","values":["10.1575/1912/66540"],"render_values":[{"text":"10.1575/1912/66540","href":"https://doi.org/10.1575/1912/66540","code":true}]}]},"links":{"outbound_url":"https://hdl.handle.net/1912/66540","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.advisor","label":"Advisor","values":["Einstein, Herbert"]},{"key":"dc:creator","label":"Author","values":["Smalls, Paris T."]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2023-08-02T14:06:29Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2023-08-02T14:06:29Z"]},{"key":"dc:date.issued","label":"Date","values":["2023-09"]},{"key":"dc:publisher","label":"Institution","values":["Massachusetts Institute of Technology and Woods Hole Oceanographic Institution"]},{"key":"dc:type","label":"Dc Type","values":["Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Thermal pore pressure","Permeability","Joule heating"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language.iso","label":"Language (ISO)","values":["en_US"]},{"key":"dc:rights","label":"Dc Rights","values":["©2023 Paris Smalls. 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Chapter 1 introduces the thesis and motivates the need to study research topics in relevant geothermal environments, and develop new technologies to economically extract heat from these resources. In Chapter 2, microseism events in Yellowstone National Park are studied. Yellowstone is located in one of the most seismically active volcanic calderas in the world and is a widely studied area for investigating physical (e.g., faulting) and chemical (e.g., hydrothermal venting) relationships in geothermal systems. Chapter 3 describes dike intrusion modeling research I conducted early in my graduate studies including the feedback mechanisms between magma injection at plate spreading centers and topographic development. Chapter 4 represents a shift in my research interests from science to engineering problems relevant for geothermal heat extraction. In this chapter, I describe the design process for developing a novel experimental approach to study the effects of applying a high-voltage to saturated rock specimens under in-situ states of stress. This novel “Electric Rock Fracturing” experimental set-up is used in Chapter 5, the final chapter of this thesis, to study the effects of high-voltage application on the temperature, electrical conductivity, and permeability of brine saturated Berea Sandstone rock specimens."]},{"key":"dc:title","label":"Title","values":["Joule heating and pore pressure evolution, magmatic intrusions at continental rifts, and microseisms in Yellowstone Lake"]}]}],"canonical_facts":{"dc:contributor.advisor":["Einstein, Herbert"],"dc:creator":["Smalls, Paris T."],"dc:date.accessioned":["2023-08-02T14:06:29Z"],"dc:date.available":["2023-08-02T14:06:29Z"],"dc:date.issued":["2023-09"],"dc:description":["Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution September 2023."],"dc:description.abstract":["The goal of this thesis is to investigate research topics related to geothermal resources. 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In this chapter, I describe the design process for developing a novel experimental approach to study the effects of applying a high-voltage to saturated rock specimens under in-situ states of stress. This novel “Electric Rock Fracturing” experimental set-up is used in Chapter 5, the final chapter of this thesis, to study the effects of high-voltage application on the temperature, electrical conductivity, and permeability of brine saturated Berea Sandstone rock specimens."],"dc:identifier.doi":["10.1575/1912/66540"],"dc:identifier.uri":["https://hdl.handle.net/1912/66540"],"dc:language.iso":["en_US"],"dc:publisher":["Massachusetts Institute of Technology and Woods Hole Oceanographic Institution"],"dc:rights":["©2023 Paris Smalls. This work is licensed under a CC BY-SA 2.0. The author hereby grants to MIT a nonexclusive, worldwide, irrevocable, royalty-free license to exercise any and all rights under copyright, including to reproduce, preserve, distribute and publicly display copies of the thesis, or release the thesis under an open-access license."],"dc:subject":["Thermal pore pressure","Permeability","Joule heating"],"dc:title":["Joule heating and pore pressure evolution, magmatic intrusions at continental rifts, and microseisms in Yellowstone Lake"],"dc:type":["Thesis"]},"updated_at":"2026-07-27T22:05:19Z"}