Title of article
Evaluation of sulfate reduction at experimentally induced mixing interfaces using small-scale push–pull tests in an aquifer–wetland system
Author/Authors
Tara A. Kneeshaw، نويسنده , , Jennifer T. McGuire، نويسنده , , Erik W. Smith، نويسنده , , Isabelle M. Cozzarelli، نويسنده ,
Issue Information
روزنامه با شماره پیاپی سال 2000
Pages
12
From page
2618
To page
2629
Abstract
This paper presents small-scale push–pull tests designed to evaluate the kinetic controls on image reduction in situ at mixing interfaces between a wetland and aquifer impacted by landfill leachate at the Norman Landfill research site, Norman, OK. Quantifying the rates of redox reactions initiated at interfaces is of great interest because interfaces have been shown to be zones of increased biogeochemical transformations and thus may play an important role in natural attenuation. To mimic the aquifer–wetland interface and evaluate reaction rates, image-rich anaerobic aquifer water image was introduced into image-depleted wetland porewater via push–pull tests. Results showed image reduction was stimulated by the mixing of these waters and first-order rate coefficients were comparable to those measured in other push–pull studies. However, rate data were complex involving either multiple first-order rate coefficients or a more complex rate order. In addition, a lag phase was observed prior to image reduction that persisted until the mixing interface between test solution and native water was recovered, irrespective of temporal and spatial constraints. The lag phase was not eliminated by the addition of electron donor (acetate) to the injected test solution. Subsequent push–pull tests designed to elucidate the nature of the lag phase support the importance of the mixing interface in controlling terminal electron accepting processes. These data suggest redox reactions may occur rapidly at the mixing interface between injected and native waters but not in the injected bulk water mass. Under these circumstances, push–pull test data should be evaluated to ensure the apparent rate is actually a function of time and that complexities in rate data be considered.
Journal title
Applied Geochemistry
Serial Year
2000
Journal title
Applied Geochemistry
Record number
740817
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