T34 A Showcase of Undergraduate Research in Hydrogeology (Posters)

Sunday, 4 November 2018
9:00 AM - 5:30 PM
Halls J-K


INVESTIGATING THE ROLE OF MONTMORILLONITE CLAY ON THE TRANSPORT OF CAFFEINE, BISPHENOL A, SULFAMETHOXAZOLE, AND CARBAMAZEPINE IN GROUNDWATER

Paper number: T34-21
Program: Technical Sessions
Time: 9:00 AM – 5:30 PM


Authors


Abstract

Results from this study indicate the presence of montmorillonite clays can disproportionately affect the transport of wastewater contaminants in groundwater. Caffeine, pharmaceuticals, and other household products can enter groundwater from septic tanks, wastewater treatment facilities, and farm runoff and experience varying amounts of sorption or degradation depending on the nature of the specific chemicals and the substrate. Household chemicals are useful as tracers for identifying anthropogenically-influenced groundwater, but also have potential to pollute groundwater in populated areas.

In this study, laboratory column and batch experiments were conducted with four household products commonly found in groundwater (caffeine, bisphenol A, sulfamethoxazole, and carbamazepine) using an artificial soil composed of quartz playground sand and montmorillonite clay at varying concentrations (0%, 0.1%, 0.2%, 0.5% and 1.0%). Caffeine was significantly impacted by the montmorillonite, with adsorption coefficients ranging from 1.9 L/kg in the playground sand (0% clay) to 11.5 L/kg with 1% clay. Experiments with natural soils demonstrate that even minute levels of montmorillonite could make caffeine a less reliable tracer of anthropogenic activity than previously thought. Montmorillonite had less impact on bisphenol-A and carbamazepine and no significant impact on sulfamethoxazole transport.


Geological Society of America Abstracts with Programs. Vol. 50, No. 6

doi: 10.1130/abs/2018AM-318080

© Copyright 2018 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.