Geothermal Fluid Equilibrium Modeling: Comparison of Wellhead Fluid Samples to Deep Samples in the Reykjanes System, Iceland

dc.contributor.advisorReed, Marken_US
dc.contributor.authorSeward, Ryanen_US
dc.date.accessioned2014-06-17T19:45:41Z
dc.date.available2014-06-17T19:45:41Z
dc.date.issued2014-06-17
dc.description.abstractSingle phase geothermal fluids sampled in 2007 from 1500m depth in Well RN-12 of the Reykjanes geothermal system in Iceland show large differences in dissolved copper, zinc and iron concentrations when compared with fluid sampled from the wellhead. Equilibrium modeling of the samples taken at depth indicate that the fluid was supersaturated in sulfide minerals even at moderately acidic pH values, suggesting that the deep samples, as collected, are out of equilibrium. Wellhead sample reconstructions indicate a well-bottom pH of about 5.5 at 295°C, but a pH of 3.6 at saturation with chalcopyrite, bornite, pyrite and sphalerite would be required to account for the large concentrations of Cu, Zn and Fe in the down-well samples. This acidic value needed for the high metal concentrations is not realistic in this naturally buffered system, likely indicating contamination in the downhole analysis.en_US
dc.identifier.urihttps://hdl.handle.net/1794/17933
dc.language.isoen_USen_US
dc.publisherUniversity of Oregonen_US
dc.rightsAll Rights Reserved.en_US
dc.subjectEquilibriaen_US
dc.subjectGeothermalen_US
dc.subjectThermodynamicsen_US
dc.titleGeothermal Fluid Equilibrium Modeling: Comparison of Wellhead Fluid Samples to Deep Samples in the Reykjanes System, Icelanden_US
dc.typeElectronic Thesis or Dissertationen_US
thesis.degree.disciplineDepartment of Geological Sciencesen_US
thesis.degree.grantorUniversity of Oregonen_US
thesis.degree.levelmastersen_US
thesis.degree.nameM.S.en_US

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