The hydrochemical signatures of (in) congruent weathering in Iceland

dc.contributor.advisorTorres, Mark
dc.creatorCole, Trevor L.
dc.date.accessioned2020-04-23T16:38:49Z
dc.date.available2020-11-01T05:01:10Z
dc.date.created2020-05
dc.date.issued2020-04-21
dc.date.submittedMay 2020
dc.date.updated2020-04-23T16:38:49Z
dc.description.abstractSilicate weathering is often invoked as the dominant mechanism for sequestering CO2 over geologic timescales, where extrusive lithologies are assumed to disproportionately contribute to global silicate weathering fluxes due to their higher reactivity relative to intrusive substrate. While Iceland is largely considered monolithologic (i.e. basaltic), compiled bedrock and solute measurements herein suggest that river water is enriched in Ca and Na relative to a bedrock array which ranges from basaltic to rhyolitic. To explore this relationship, we evaluate environmental factors that could explain the solute trends including clay precipitation (type-I incongruent weathering), variable dissolution rates of primary minerals (type-II incongruent weathering), and rhyolite dissolution/ groundwater contributions. Through forward models we conclude that the precipitation of high-Mg smectite exerts the most control on solute movement relative to type-II incongruency or dissolution of rhyolite. However, more direct measurements of clay mineralogy and rhyolitic ash dissolution are necessary to better constrain this dataset.
dc.embargo.terms2020-11-01
dc.format.mimetypeapplication/pdf
dc.identifier.citationCole, Trevor L.. "The hydrochemical signatures of (in) congruent weathering in Iceland." (2020) Master’s Thesis, Rice University. <a href="https://hdl.handle.net/1911/108351">https://hdl.handle.net/1911/108351</a>.
dc.identifier.urihttps://hdl.handle.net/1911/108351
dc.language.isoeng
dc.rightsCopyright is held by the author, unless otherwise indicated. Permission to reuse, publish, or reproduce the work beyond the bounds of fair use or other exemptions to copyright law must be obtained from the copyright holder.
dc.subjectIceland
dc.subjectsilicate weathering
dc.titleThe hydrochemical signatures of (in) congruent weathering in Iceland
dc.typeThesis
dc.type.materialText
thesis.degree.departmentEarth Science
thesis.degree.disciplineNatural Sciences
thesis.degree.grantorRice University
thesis.degree.levelMasters
thesis.degree.majorFluvial geochemistry
thesis.degree.nameMaster of Science
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