{"id":{"repo_id":"buffalo","oai_identifier":"oai:ubir.buffalo.edu:10477/78084"},"canonical_url":"https://search.dev.ndltd.org/etd/buffalo/oai:ubir.buffalo.edu:10477/78084","repository":{"repo_id":"buffalo","name":"Buffalo","base_url":"https://ubir.buffalo.edu/oai/request"},"display":{"title":"Hydrologic Process Parameterization of Electrical Resistivity Imaging of Solute Plumes Using POD MCMC","abstract":"M.S.","abstract_html":"M.S.","abstract_has_math":false,"creators":["Awatey, Michael"],"institution":"State University of New York at Buffalo","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":["Oware, Erasmus","Geology"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2018,"date_issued":"2018-06-28T20:33:48Z","date_published":"2018-06-28T20:33:48Z","updated_at":"2026-07-27T19:05:07Z","subjects":["environmental geology","geophysics","hydrologic sciences"],"languages":["eng"],"rights":["Users of works found in University at Buffalo Institutional Repository (UBIR) are responsible for identifying and contacting the copyright owner for permission to reuse. University at Buffalo Libraries do not manage rights for copyright-protected works and cannot assist with permissions.","Copyright retained by author."],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"http://hdl.handle.net/10477/78084","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["Oware, Erasmus","Geology"]},{"key":"dc:creator","label":"Author","values":["Awatey, Michael"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["2018-06-28T20:33:48Z","2018","2018-05-17 21:09:49"]},{"key":"dc:publisher","label":"Institution","values":["State University of New York at Buffalo"]},{"key":"dc:type","label":"Dc Type","values":["Text","Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["environmental geology","geophysics","hydrologic sciences"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["eng"]},{"key":"dc:rights","label":"Dc Rights","values":["Users of works found in University at Buffalo Institutional Repository (UBIR) are responsible for identifying and contacting the copyright owner for permission to reuse. University at Buffalo Libraries do not manage rights for copyright-protected works and cannot assist with permissions.","Copyright retained by author."]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["http://hdl.handle.net/10477/78084"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["M.S.","Markov chain Monte Carlo (MCMC) techniques have attracted wide attention in geophysical estimation of hydrogeological properties due to their ability to recover multiple, equally probable solutions that enable uncertainty assessment. Standard MCMC methods, however, become computationally intractable in high dimensional problems. This research has developed a MCMC method that operates in the reduced-dimensional space, thereby enabling the estimation of a small number of inversion parameters while incorporating knowledge of the physics of the target process. First, we generate training images (TIs) from Monte Carlo simulation of the hydrologic process of interest. We then used proper orthogonal decomposition (POD) to extract a small number of optimal basis vectors that capture most of the variability in the TIs, leading to dimensionality reduction. The basis vectors were subsequently used to constrain the inversion problem to reconstruct the target field. We demonstrate the performance of the algorithm with synthetic electrical resistivity imaging of unimodal and bimodal solute plumes. The unimodal plume was consistent with the hypothesis underlying the generation of the TIs whereas bimodality in the target plume morphology was not theorized. The same set of TIs were, however, employed in both reconstructions. We achieved 90% reduction in the dimensionality of the MCMC problem while being able to retrieve multiple plausible results for uncertainty analysis. Additionally, although bimodality was not captured in the prior conceptualization, the algorithm was able to flexibly adapt towards the geophysical data to yield reasonable results."]},{"key":"dc:format","label":"Dc Format","values":["application/pdf"]},{"key":"dc:title","label":"Title","values":["Hydrologic Process Parameterization of Electrical Resistivity Imaging of Solute Plumes Using POD MCMC"]}]}],"canonical_facts":{"dc:contributor":["Oware, Erasmus","Geology"],"dc:creator":["Awatey, Michael"],"dc:date":["2018-06-28T20:33:48Z","2018","2018-05-17 21:09:49"],"dc:description":["M.S.","Markov chain Monte Carlo (MCMC) techniques have attracted wide attention in geophysical estimation of hydrogeological properties due to their ability to recover multiple, equally probable solutions that enable uncertainty assessment. Standard MCMC methods, however, become computationally intractable in high dimensional problems. This research has developed a MCMC method that operates in the reduced-dimensional space, thereby enabling the estimation of a small number of inversion parameters while incorporating knowledge of the physics of the target process. First, we generate training images (TIs) from Monte Carlo simulation of the hydrologic process of interest. We then used proper orthogonal decomposition (POD) to extract a small number of optimal basis vectors that capture most of the variability in the TIs, leading to dimensionality reduction. The basis vectors were subsequently used to constrain the inversion problem to reconstruct the target field. We demonstrate the performance of the algorithm with synthetic electrical resistivity imaging of unimodal and bimodal solute plumes. The unimodal plume was consistent with the hypothesis underlying the generation of the TIs whereas bimodality in the target plume morphology was not theorized. The same set of TIs were, however, employed in both reconstructions. We achieved 90% reduction in the dimensionality of the MCMC problem while being able to retrieve multiple plausible results for uncertainty analysis. Additionally, although bimodality was not captured in the prior conceptualization, the algorithm was able to flexibly adapt towards the geophysical data to yield reasonable results."],"dc:format":["application/pdf"],"dc:identifier":["http://hdl.handle.net/10477/78084"],"dc:language":["eng"],"dc:publisher":["State University of New York at Buffalo"],"dc:rights":["Users of works found in University at Buffalo Institutional Repository (UBIR) are responsible for identifying and contacting the copyright owner for permission to reuse. University at Buffalo Libraries do not manage rights for copyright-protected works and cannot assist with permissions.","Copyright retained by author."],"dc:subject":["environmental geology","geophysics","hydrologic sciences"],"dc:title":["Hydrologic Process Parameterization of Electrical Resistivity Imaging of Solute Plumes Using POD MCMC"],"dc:type":["Text","Thesis"]},"updated_at":"2026-07-27T19:05:07Z"}