Decadal Delays in Groundwater Recovery from Nitrate Contamination Caused by Low O2Reduction Rates

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dc.contributor.authorWild, Lisa M.
dc.contributor.authorMayer, Bernhard
dc.contributor.authorEinsiedl, Florian
dc.date.accessioned2022-09-02T22:14:23Z
dc.date.available2022-09-02T22:14:23Z
dc.date.issued2018-11-13
dc.description.abstractNitrate (NO urn:x-wiley:wrcr:media:wrcr23708:wrcr23708-math-0001) is one of the main pollutants in agriculturally impacted groundwater systems. The availability and reactivity of electron donors control the prevalent redox conditions in aquifers and past nitrate contamination of groundwater can be ameliorated if denitrification occurs. Using aqueous geochemistry data and the stable isotope composition of dissolved nitrate (δ15N and δ18O), we found that nitrate concentrations above the World Health Organization drinking water guideline were caused predominantly by manure and to a lesser extent by synthetic fertilizer applications and that denitrification was not a significant nitrate removal process in an aquifer in southern Germany underlying agricultural land with intensive hog farming. We also applied environmental isotopes (δ2H and δ18O, 3H/3He, and 14C) linked with a lumped parameter approach to determine apparent mean transit times (MTT) of groundwater that ranged from <5 years to >100 years. Furthermore, we determined low reduction rates of dissolved oxygen (O2) of 0.015 1/year for first-order kinetics. By extrapolating the O2 reduction rates beyond the apparent MTT ranges of sampled groundwater, denitrification lag times (time prior to commencement of denitrification) of approximately 114 years were determined. This suggests that it will take many decades to significantly reduce nitrate concentrations in the porous aquifer via denitrification, even if future nitrate inputs were significantly reduced.en_US
dc.description.grantingagencyNatural Sciences and Engineering Research Council (NSERC)en_US
dc.identifier.citationWild, L. M., Mayer, B., & Einsiedl, F. (2018). Decadal Delays in Groundwater Recovery from Nitrate Contamination Caused by Low O2 Reduction Rates. Water Resources Research, 54(12), 9996-10,012. https://doi.org/10.1029/2018WR023396en_US
dc.identifier.doihttp://dx.doi.org/10.1029/2018WR023396en_US
dc.identifier.issn1944-7973
dc.identifier.urihttp://hdl.handle.net/1880/115162
dc.language.isoengen_US
dc.publisherWiley Periodicals, Inc. on behalf of the American Geophysical Unionen_US
dc.publisher.departmentGeoscienceen_US
dc.publisher.facultyScienceen_US
dc.publisher.hasversionpublishedVersionen_US
dc.publisher.institutionUniversity of Calgaryen_US
dc.publisher.policyhttps://www.agu.org/Publish-with-AGU/Publish/Author-Resources/Policies/Permission-policyen_US
dc.rightsUnless otherwise indicated, this material is protected by copyright and has been made available with authorization from the copyright owner. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.en_US
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0en_US
dc.subject15Nen_US
dc.subjectDenitrificationen_US
dc.subjectMean transit time (MTT)en_US
dc.subjectNitrate contaminationen_US
dc.subjectO2 reduction rateen_US
dc.titleDecadal Delays in Groundwater Recovery from Nitrate Contamination Caused by Low O2Reduction Ratesen_US
dc.typejournal articleen_US
ucalgary.item.requestcopyfalseen_US
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