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dc.contributor.authorDolph, Christine L.
dc.contributor.authorBoardman, Evelyn
dc.contributor.authorDanesh‐Yazdi, Mohammad
dc.contributor.authorFinlay, Jacques C.
dc.contributor.authorHansen, Amy T.
dc.contributor.authorBaker, Anna C.
dc.contributor.authorDalzell, Brent
dc.date.accessioned2021-02-24T15:25:36Z
dc.date.available2021-02-24T15:25:36Z
dc.date.issued2019-10-24
dc.identifier.citationDolph, C. L., Boardman, E., Danesh‐Yazdi, M., Finlay, J. C., Hansen, A. T., Baker, A. C., & Dalzell, B. (2019). Phosphorus Transport in Intensively Managed Watersheds. Water Resources Research, 55, 9148– 9172. https://doi.org/10.1029/2018WR024009en_US
dc.identifier.urihttp://hdl.handle.net/1808/31473
dc.descriptionAn edited version of this paper was published by AGU. Copyright 2019 American Geophysical Union.en_US
dc.description.abstractUnderstanding controls of P movement through watersheds are essential for improved landscape management in intensively managed regions. Here, we analyze observational data from 104 gaged river sites and 176 nongaged river sites within agriculturally dominated watersheds of Minnesota, USA, to understand the role of landscape features, land use practices, climate variability, and biogeochemical processes in total, dissolved and particulate P dynamics at daily to annual scales. Our analyses demonstrate that factors mediating P concentration‐discharge relationships varied greatly across watersheds and included near‐channel sediment sources, lake and wetland interception, assimilation by algal P, and artificial land drainage. The majority of gaged sites exhibited mobilizing behavior for all forms of P at event (i.e., daily) timescales and chemostatic behavior at annual timescales. The large majority of watershed P export (>70%, on average) occurred during high flow conditions, suggesting that more frequent large storm events arising from climate change will drive increased P losses from agricultural watersheds without substantial management changes. We found that P export could be dominated by dissolved P, particulate P, or an even mix of the two forms, depending on watershed attributes. Implementation of management practices to control P losses must be guided by understanding of how local landscapes interact with current and future climate conditions. Managing for both dissolved and particulate P is required to reduce overall P load in many agricultural watersheds.en_US
dc.publisherAmerican Geophysical Unionen_US
dc.rights© 2019. American Geophysical Union. All Rights Reserved.en_US
dc.titlePhosphorus Transport in Intensively Managed Watershedsen_US
dc.typeArticleen_US
kusw.kuauthorHansen, Amy T.
kusw.kudepartmentCivil, Environmental, and Architectural Engineeringen_US
dc.identifier.doi10.1029/2018WR024009en_US
dc.identifier.orcidhttps://orcid.org/0000-0003-3667-7809en_US
dc.identifier.orcidhttps://orcid.org/0000-0003-2918-7713en_US
dc.identifier.orcidhttps://orcid.org/0000-0002-7968-7030en_US
dc.identifier.orcidhttps://orcid.org/0000-0002-6152-9595en_US
dc.identifier.orcidhttps://orcid.org/0000-0001-8194-7535en_US
dc.identifier.orcidhttps://orcid.org/0000-0001-9710-6562en_US
kusw.oaversionScholarly/refereed, publisher versionen_US
kusw.oapolicyThis item meets KU Open Access policy criteria.en_US
dc.rights.accessrightsopenAccessen_US


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