GEOCHEMICAL MECHANISMS OF TRACE ELEMENT MOBILIZATION AND ATTENUATION IN A CRUDE-OIL CONTAMINATED AQUIFER
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.