T52 Characteristics, Reactivity and Role of Natural Organic Matter (NOM) in Elemental Cycling in the Environment
Sunday, 15 October 2023
1:30 PM - 5:30 PM
333
GEOCHEMICAL MECHANISMS OF TRACE ELEMENT MOBILIZATION AND ATTENUATION IN A CRUDE-OIL CONTAMINATED AQUIFER
Paper number: T52-3
Program: Technical Sessions
Time: 1:50 PM – 2:05 PM
Authors
-
Brady ZieglerTrinity University, San Antonio, TX
-
Ann OjedaAuburn University, Auburn, AL
-
Isabelle CozzarelliGeology, Energy & Minerals Science Center, Reston, VA
Abstract
We used sequential extractions of sediment from geochemical zones along the plume path to elucidate the sediment phase origins of 30 trace elements and provide insight into attenuation mechanisms. Extractions targeted elements in surface exchangeable, carbonate, (hydr)oxide, and organic phases, which were then analyzed with inductively coupled plasma-mass spectrometry (ICP-MS) and -optical emission spectroscopy. Pairwise Wilcoxon tests of resulting data identified statistically significant differences between zones for each element. Principal component analyses examined elemental relationships for each phase.
Lead, manganese, and Fe, which were mobilized into groundwater by the reductive dissolution of (hydr)oxides, precipitated as carbonates in the Fe-reducing zone. Arsenic (As), boron, and chromium (Cr) were elevated in the organic fraction from Fe-reducing zone sediment, suggesting metalloorganic complexing with the oxyanions. Ultraviolet-visible spectroscopy, size exclusion-high-performance liquid chromatography, and ICP-MS showed the presence of organic complexes of As, Cr, and calcium in the interface zone. Further understanding the behavior of geogenic contaminants following an oil spill aids efforts to remediate secondary contaminants and protect groundwater resource quality.
Geological Society of America Abstracts with Programs. Vol. 55, No. 6
doi: 10.1130/abs/2023AM-395440
© Copyright 2023 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.