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dc.contributor.advisorCole, David
dc.contributor.advisorWelch, Sue
dc.contributor.advisorSheets, Julie
dc.creatorAdamaitis, Chandler
dc.date.accessioned2017-12-12T22:55:38Z
dc.date.available2017-12-12T22:55:38Z
dc.date.issued2017-12
dc.identifier.urihttp://hdl.handle.net/1811/81634
dc.description.abstractHydraulic fracturing of shale generates brines with complex chemistries. As such, these fluids have trace metal constituents that can be rendered valuable if concentrated. This project used samples of hydraulic fracturing flowback fluid from the Utica/Point Pleasant formations in Ohio to analyze how different additives of acids and bases could influence precipitation and sequester trace metals. Flowback fluids were treated with sulfuric acid (H2SO4), phosphoric acid (H3PO4), hydrochloric acid (HCl), and sodium carbonate (Na2CO3), each in a high and low concentration. The fluids were allowed to react over several weeks and then the precipitates and the solutions were analyzed using scanning electron microscopy (SEM) and x-ray diffraction (XRD), and inductively coupled plasma optical emission spectrometry (ICP-OES) and inductively coupled plasma mass spectrometry (ICP-MS), respectively. Reacting hydraulic fracturing fluid with these acids and bases in different concentrations allowed for the precipitation of different minerals with variable elemental compositions. For example, low concentrations of H2SO4 resulted mainly in barite (BaSO4) precipitation, while high H2 SO4 resulted in precipitates of celestite (SrSO4) and gypsum (CaSO4 ·2H2O). Additionally, akaganeite (Fe^(3+) O(OH,Cl)) was found in the precipitates of the control sample and the high H3PO4 sample. This suggests that further research should focus on akaganeite as another phase that could sequester trace elements, because its crystal structure has large spaces that could accommodate such trace metals.en_US
dc.description.sponsorshipShell Exploration and Production Companyen_US
dc.description.sponsorshipOhio Water Resource Center of the Office of Energy and Environmenten_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. School of Earth Sciences Undergraduate Research Theses; 2017en_US
dc.subjectHydraulic fracturingen_US
dc.subjectFlowback fluiden_US
dc.subjectBariteen_US
dc.subjectCelestiteen_US
dc.subjectAkaganeiteen_US
dc.subjectMineral precipitationen_US
dc.titleFracking the Code on Flowback Fluiden_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US
dc.description.academicmajorAcademic Major: Earth Sciencesen_US


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