T110 Source, Fate, and Roles of Natural Organic Matter in Geochemical Cycling of Metals and Metalloids in Surface and Groundwater Systems

Monday, 11 October 2021
1:30 PM - 5:30 PM
D135

AN XRF STUDY IN MECHANISMS OF CHROMIUM REMOVAL FROM INDUSTRIAL STORM WATER USING PEAT MEDIUM

Paper number: T110-3
Program: Technical Sessions
Time: 1:50 PM – 2:05 PM

Authors

Abstract

Treatment processes for metals in industrial storm water can be cost prohibitive. Therefore, passive remediation strategies using natural materials and microbial processes have the potential to provide affordable solutions for removing metals from aqueous waste streams, which is important from regulatory and environmental quality perspectives. Our research explores the key chemical, biological and physical processes promoting removal of hexavalent chromium (Cr) from an industrial storm water treatment system by association with granular organic peat media. In this installation chromium is primarily in the water soluble and carcinogenic hexavalent form, chromate. Prior to treatment, chromate is converted to Cr(III) via an oxidation-reduction reaction using iron sulfate (Fe(II)SO4). The resulting Cr(III) is less water soluble than chromate (Cr(VI), making Cr precipitation as hydroxides likely. The removal capacity for Cr(III) is much higher than expected for adsorption and filtration alone, suggesting other mechanisms, including microbially mediated attenuation may play a role. In addition to filtration of Cr(III) precipitates, the presence of excess Fe(III) (from the pre-treatment step) could yield Cr(III) co-precipitation with Fe minerals and/or serve as a terminal electron acceptor.

Samples were collected from an industrial-sized installation in Howell, MI USA, where Cr-laden storm water is treated in large, flow-through tank reactors filled with a peat sorbent material. We sampled one reactor in four different locations at four depths for a total of 16 solid-phase peat material samples after 1 and 3.5 years. Chemical digestions show total Cr concentrations ranging from 400-900 mg/kg peat after 3.5 years dependent on depth and location. X-ray Fluorescence Microprobe (XFM) data reveal that Cr is heterogeneously distributed within the remediation media with both diffuse and “hot spot” features on the micron to 10s of micron scale and is highly correlated with Fe and Zn. Additionally, X-ray Absorption Near Edge Structure (XANES) results show both Cr(III) and metallic Cr-bearing particles in the same sample often as rind-like features accumulating on the surface of peat particles over time.

Geological Society of America Abstracts with Programs. Vol. 53, No. 6

doi: 10.1130/abs/2021AM-371283

© Copyright 2021 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.