Clay-Cation Compositions from Groundwater Chemistry as an Indicator of Depositional Environments, Paleoclimates, and Paleo-Groundwater Flow

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dc.contributor.advisorCapuano, Regina M.
dc.contributor.committeeMemberLapen, Thomas J.
dc.contributor.committeeMemberMurphy, Michael A.
dc.contributor.committeeMemberLouie, Stacey M.
dc.creatorJones, Cole R.
dc.creator.orcid0000-0002-7983-4061
dc.date.accessioned2023-01-14T23:45:07Z
dc.date.createdMay 2022
dc.date.issued2022-04-29
dc.date.updated2023-01-14T23:45:08Z
dc.description.abstractNew methods to calculate the cation compositions of clays from equilibrated groundwater are presented and applied in three clay-rich coastal aquifers where significant chemical differences are shown to exist among clays based on their depositional environment and the climate at deposition. River-water analyses show that fluvial deposited sediments are represented by majority XNa≤ 8.0% and marine deposited sediments by majority XNa > 8.0%. In a natural system with fluvial, mixed, and marine environments identified by traditional core, log and paleontological analyses, each depositional environment has a distinguishing range of XNa, XCa and XMg consistent with these criteria. Differences in XNa are related to climate of deposition among clays deposited in a fluvial environment, where a larger portion of the fluvial clays deposited in a semi-arid paleoclimate have elevated XNa compared to those deposited in a humid subtropical paleoclimate. Perturbations in these trends were compared to elements in the groundwater not involved in ion exchange to identify areas of upwelling and halite dissolution. Mass-balance calculations show that the effect of cation exchange on each pore volume of fluid that flows in the aquifer is large, whereas the effect on the clay composition is small, so clays will not only retain the signature of their depositional setting, but changes in the clay exchange composition can be used to identify the aquifer’s past chemical evolution and historical-flow paths. These relationships might be used to aid stratigraphic interpretations based on well logs, sediment samples, and paleontology in distinguishing fluvial, marine, and mixed fluvial-marine depositional environments.
dc.description.departmentEarth and Atmospheric Sciences, Department of
dc.format.digitalOriginborn digital
dc.format.mimetypeapplication/pdf
dc.identifier.citationPortions of this document appear in: Capuano, R.M., and Jones, C.R.(2020) Cation exchange in groundwater-chemical evolution and prediction of paleo-groundwater flow: a natural-system study. Water Resources Research, 56, e2019WR026318. https://doi.org/10.1029/2019WR0
dc.identifier.urihttps://hdl.handle.net/10657/13323
dc.language.isoeng
dc.rightsThe author of this work is the copyright owner. UH Libraries and the Texas Digital Library have their permission to store and provide access to this work. UH Libraries has secured permission to reproduce any and all previously published materials contained in the work. Further transmission, reproduction, or presentation of this work is prohibited except with permission of the author(s).
dc.subjectCation-exchange
dc.subjectClay
dc.subjectDeposition
dc.subjectClimate
dc.subjectGroundwater
dc.titleClay-Cation Compositions from Groundwater Chemistry as an Indicator of Depositional Environments, Paleoclimates, and Paleo-Groundwater Flow
dc.type.dcmiText
dc.type.genreThesis
dcterms.accessRightsThe full text of this item is not available at this time because the student has placed this item under an embargo for a period of time. The Libraries are not authorized to provide a copy of this work during the embargo period.
local.embargo.lift2024-05-01
local.embargo.terms2024-05-01
thesis.degree.collegeCollege of Natural Sciences and Mathematics
thesis.degree.departmentEarth and Atmospheric Sciences, Department of
thesis.degree.disciplineGeology
thesis.degree.grantorUniversity of Houston
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy

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