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dc.contributor.advisorGermanovich, Leonid N.
dc.contributor.authorSmith, Joshua Eric
dc.date.accessioned2018-01-22T21:09:35Z
dc.date.available2018-01-22T21:09:35Z
dc.date.created2017-12
dc.date.issued2017-08-29
dc.date.submittedDecember 2017
dc.identifier.urihttp://hdl.handle.net/1853/59215
dc.description.abstractFluid flow influences mechanical processes in the earth's crust, but many aspects of these processes remain poorly understood; in large part, because of a scarcity of controlled field experiments or measurements at appropriate scales. For example, advective heat transfer data from hydrothermal sites are necessary for understanding the geochemical and nutrient fluxes to seafloor biological communities and for constraining subsurface models at mid-ocean ridges. Yet, such data are limited or lacking. This work provides the most comprehensive database currently available for fluid flow and heat output from seafloor hydrothermal systems. We describe 120 new measurements on the Juan de Fuca ridge (North Pacific), Lau Basin (South Pacific), and East Pacific Rise (Equatorial Pacific) collected on the seafloor with submersibles Alvin and Jason. The second topic of this work is concerned with monitoring fluid flow in geologic formations. Specifically, there is significant concern on how to monitor fluid migration during carbon storage and petroleum operations. During fluid injection, pressure redistribution and formation properties affect the deformation pattern, and this effect is possible to interpret from field measurements of the strain tensor. Modern borehole strainmeters are now capable of measuring multiple components of strain and tilt in the shallow subsurface, and these measurements can be used to interpret processes at much greater depths. The first field test of this technique will occur during a waterflooding operation at the North Avant oil field in Osage County, OK. This field is a representative example of geological formations proposed for carbon storage. To design the field test, we developed a model of the poroelastic response to fluid injection and determined zones of deformation optimal for measurements. Currently, two boreholes have been drilled for instrument installation based on this modeling. The model is based on our geologic analysis of the North Avant field site, but it can be applied elsewhere. The model shows it is indeed possible to use monitoring wells at significantly shallower depths than the reservoir for measuring strain signals generated by waterflooding or carbon sequestration operations. Additionally, permeability is likely to vary within reservoirs, but boundaries are challenging to identify. We show that it is feasible to identify channels of high permeability in deep formations using the strain tensor measured in shallow boreholes. This is significant as such channels are common in petroleum formations consisting of fluvial deposits and strongly affect the fluid flow pattern.
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.publisherGeorgia Institute of Technology
dc.subjectHydrothermal venting
dc.subjectHeat flux
dc.subjectDischarge
dc.subjectCarbon storage
dc.subjectFluid injection
dc.subjectMeasuring in situ strain
dc.titleGeophysical fluid flow during hydrothermal venting and carbon sequestration
dc.typeDissertation
dc.description.degreePh.D.
dc.contributor.departmentCivil and Environmental Engineering
thesis.degree.levelDoctoral
dc.contributor.committeeMemberFrost, James D.
dc.contributor.committeeMemberHuang, Haiying
dc.contributor.committeeMemberDai, Sheng
dc.contributor.committeeMemberLowell, Robert P.
dc.contributor.committeeMemberMurdoch, Lawrence C.
dc.date.updated2018-01-22T21:09:35Z


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