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University of Illinois at Urbana-Champaign

Sediment-water interactions in three Holocene saline, alkaline playas, south-central Oregon: Mineralogy and geochemistry

Abstract

dc:description

Mineralogical, chemical, and isotopic analyses of clay minerals from outcrops and playa sediments, as well as chemical and isotopic analyses of groundwater and interstitial playa pore waters, have been used to improve understanding of the nature of sediment/water reactions in playa environments. Outcrop samples and 5 to 7 m deep playa cores were studied from three closed basins in south-central Oregon. Al-rich dioctahedral smectite dominates outcrop samples from the Alkali and Abert basins, whereas Al- and Fe-rich dioctahedral smectite is most abundant in the Alvord basin. The composition of smectite from outcrop samples reflects the composition of parent rock in each basin. In Alkali and Abert playas, randomly interstratified Mg-rich trioctahedral kerolite/smectite (Ke/Sm) formed, whereas in the Alvord playa Mg-smectite did not form, due to a lower degree of evaporative concentration. Thus, mineral authigenesis in playa sediments is controlled by the composition of pore waters. Although the pore waters from all three playas plot in the stability field for trioctahedral Mg-smectite, progressive evaporation reaction-path calculations of dilute playa pore waters predict that Mg-silicate minerals should not precipitate from Alvord pore waters until the maximum extent of evaporative concentration observed at Alvord. In contrast, calculations predict precipitation of Mg-silicates at Alkali and Abert playas after little evaporative concentration. Additional reactions in playa sediments are formation of clinoptilolite $(\pm$ searlesite) at 2 to 4 m depth in the Alkali playa, probably reflecting an influx of volcanic ash and K$\sp+$-fixation within collapsed smectite interlayers at the Alvord playa. Authigenic illite was not found.

Degree

thesis:*
Name thesis:degree_name
Ph.D.
Level thesis:degree_level
Dissertation
Discipline thesis:degree_discipline
Geology
Grantor
University of Illinois at Urbana-Champaign
Year dc:date
2011

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Matthews, James Coert
Contributors dc:contributor
  • Altaner, Stephen P.

Subjects

dc:subject × 2

Rights

dc:rights
Statement dc:rights
  • Copyright 1992 Matthews, James Coert
Language dc:language
eng

Identifiers

dc:identifier.*
Identifier
AAI9305616
(UMI)AAI9305616
OAI identifier oai:identifier
oai:www.ideals.illinois.edu:2142/22463

Chain of custody

source
Harvested from
University of Illinois - Urbana-Champaign
Base URL
www.ideals.illinois.edu/oai-pmh
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Matthews, James Coert. Sediment-water interactions in three Holocene saline, alkaline playas, south-central Oregon: Mineralogy and geochemistry. Dissertation thesis, University of Illinois at Urbana-Champaign, 2011. http://hdl.handle.net/2142/22463