National hydrologic connectivity classification links wetlands with stream water quality
Wetland hydrologic connections to downstream waters influence stream water quality. However, no systematic approach for characterizing this connectivity exists. Here using physical principles, we categorized conterminous US freshwater wetlands into four hydrologic connectivity classes based on strea...
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| Veröffentlicht in: | Nature water 2023-04, Vol.1 (4), p.370-380 |
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| creator | Leibowitz, Scott G Hill, Ryan A Creed, Irena F Compton, Jana E Golden, Heather E Weber, Marc H Rains, Mark C Jones, Jr, Chas E Lee, E Henry Christensen, Jay R Bellmore, Rebecca A Lane, Charles R |
| description | Wetland hydrologic connections to downstream waters influence stream water quality. However, no systematic approach for characterizing this connectivity exists. Here using physical principles, we categorized conterminous US freshwater wetlands into four hydrologic connectivity classes based on stream contact and flowpath depth to the nearest stream: riparian, non-riparian shallow, non-riparian mid-depth and non-riparian deep. These classes were heterogeneously distributed over the conterminous United States; for example, riparian dominated the south-eastern and Gulf coasts, while non-riparian deep dominated the Upper Midwest and High Plains. Analysis of a national stream dataset indicated acidification and organic matter brownification increased with connectivity. Eutrophication and sedimentation decreased with wetland area but did not respond to connectivity. This classification advances our mechanistic understanding of wetland influences on water quality nationally and could be applied globally. |
| doi_str_mv | 10.1038/s44221-023-00057-w |
| format | Article |
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However, no systematic approach for characterizing this connectivity exists. Here using physical principles, we categorized conterminous US freshwater wetlands into four hydrologic connectivity classes based on stream contact and flowpath depth to the nearest stream: riparian, non-riparian shallow, non-riparian mid-depth and non-riparian deep. These classes were heterogeneously distributed over the conterminous United States; for example, riparian dominated the south-eastern and Gulf coasts, while non-riparian deep dominated the Upper Midwest and High Plains. Analysis of a national stream dataset indicated acidification and organic matter brownification increased with connectivity. Eutrophication and sedimentation decreased with wetland area but did not respond to connectivity. This classification advances our mechanistic understanding of wetland influences on water quality nationally and could be applied globally.</description><identifier>ISSN: 2731-6084</identifier><identifier>EISSN: 2731-6084</identifier><identifier>DOI: 10.1038/s44221-023-00057-w</identifier><identifier>PMID: 37389401</identifier><language>eng</language><publisher>England: Nature Publishing Group</publisher><subject>Acidification ; Biogeochemistry ; Classification ; Connectivity ; Creeks & streams ; Drainage ; Environmental restoration ; Eutrophication ; Floods ; High plains ; Nitrogen ; Organic matter ; Stream water ; Streams ; Surface water ; Water ; Water quality ; Watersheds ; Wetlands</subject><ispartof>Nature water, 2023-04, Vol.1 (4), p.370-380</ispartof><rights>This is a U.S. Government work and not under copyright protection in the US; foreign copyright protection may apply 2023. This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c220w-2234225b243c6859a16f3fd2520a393e10853de68c9b161def4a21e325e0b3163</citedby><cites>FETCH-LOGICAL-c220w-2234225b243c6859a16f3fd2520a393e10853de68c9b161def4a21e325e0b3163</cites><orcidid>0000-0001-5501-9444 ; 0000-0003-0066-8919 ; 0000-0001-8199-1472 ; 0000-0002-9955-9503 ; 0000-0002-9742-4744 ; 0000-0003-4961-6132 ; 0000-0002-7124-3937 ; 0000-0002-8103-475X ; 0000-0001-9583-0426 ; 0000-0001-9833-8664 ; 0000-0002-6089-2608 ; 0000-0002-5619-4161</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.proquest.com/docview/3041695943?pq-origsite=primo$$EHTML$$P50$$Gproquest$$H</linktohtml><link.rule.ids>315,781,785,21393,21394,21395,21396,23261,27929,27930,33535,33536,33708,33709,33749,33750,34010,34011,34319,34320,43664,43792,43810,43958,44072,64390,64392,64394,72474</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/37389401$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Leibowitz, Scott G</creatorcontrib><creatorcontrib>Hill, Ryan A</creatorcontrib><creatorcontrib>Creed, Irena F</creatorcontrib><creatorcontrib>Compton, Jana E</creatorcontrib><creatorcontrib>Golden, Heather E</creatorcontrib><creatorcontrib>Weber, Marc H</creatorcontrib><creatorcontrib>Rains, Mark C</creatorcontrib><creatorcontrib>Jones, Jr, Chas E</creatorcontrib><creatorcontrib>Lee, E Henry</creatorcontrib><creatorcontrib>Christensen, Jay R</creatorcontrib><creatorcontrib>Bellmore, Rebecca A</creatorcontrib><creatorcontrib>Lane, Charles R</creatorcontrib><title>National hydrologic connectivity classification links wetlands with stream water quality</title><title>Nature water</title><addtitle>Nat Water</addtitle><description>Wetland hydrologic connections to downstream waters influence stream water quality. However, no systematic approach for characterizing this connectivity exists. Here using physical principles, we categorized conterminous US freshwater wetlands into four hydrologic connectivity classes based on stream contact and flowpath depth to the nearest stream: riparian, non-riparian shallow, non-riparian mid-depth and non-riparian deep. These classes were heterogeneously distributed over the conterminous United States; for example, riparian dominated the south-eastern and Gulf coasts, while non-riparian deep dominated the Upper Midwest and High Plains. Analysis of a national stream dataset indicated acidification and organic matter brownification increased with connectivity. Eutrophication and sedimentation decreased with wetland area but did not respond to connectivity. This classification advances our mechanistic understanding of wetland influences on water quality nationally and could be applied globally.</description><subject>Acidification</subject><subject>Biogeochemistry</subject><subject>Classification</subject><subject>Connectivity</subject><subject>Creeks & streams</subject><subject>Drainage</subject><subject>Environmental restoration</subject><subject>Eutrophication</subject><subject>Floods</subject><subject>High plains</subject><subject>Nitrogen</subject><subject>Organic matter</subject><subject>Stream water</subject><subject>Streams</subject><subject>Surface water</subject><subject>Water</subject><subject>Water 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hydrologic connectivity classification links wetlands with stream water quality</title><author>Leibowitz, Scott G ; Hill, Ryan A ; Creed, Irena F ; Compton, Jana E ; Golden, Heather E ; Weber, Marc H ; Rains, Mark C ; Jones, Jr, Chas E ; Lee, E Henry ; Christensen, Jay R ; Bellmore, Rebecca A ; Lane, Charles R</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c220w-2234225b243c6859a16f3fd2520a393e10853de68c9b161def4a21e325e0b3163</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Acidification</topic><topic>Biogeochemistry</topic><topic>Classification</topic><topic>Connectivity</topic><topic>Creeks & streams</topic><topic>Drainage</topic><topic>Environmental restoration</topic><topic>Eutrophication</topic><topic>Floods</topic><topic>High plains</topic><topic>Nitrogen</topic><topic>Organic matter</topic><topic>Stream water</topic><topic>Streams</topic><topic>Surface 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Water</addtitle><date>2023-04-06</date><risdate>2023</risdate><volume>1</volume><issue>4</issue><spage>370</spage><epage>380</epage><pages>370-380</pages><issn>2731-6084</issn><eissn>2731-6084</eissn><abstract>Wetland hydrologic connections to downstream waters influence stream water quality. However, no systematic approach for characterizing this connectivity exists. Here using physical principles, we categorized conterminous US freshwater wetlands into four hydrologic connectivity classes based on stream contact and flowpath depth to the nearest stream: riparian, non-riparian shallow, non-riparian mid-depth and non-riparian deep. These classes were heterogeneously distributed over the conterminous United States; for example, riparian dominated the south-eastern and Gulf coasts, while non-riparian deep dominated the Upper Midwest and High Plains. Analysis of a national stream dataset indicated acidification and organic matter brownification increased with connectivity. Eutrophication and sedimentation decreased with wetland area but did not respond to connectivity. 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| subjects | Acidification Biogeochemistry Classification Connectivity Creeks & streams Drainage Environmental restoration Eutrophication Floods High plains Nitrogen Organic matter Stream water Streams Surface water Water Water quality Watersheds Wetlands |
| title | National hydrologic connectivity classification links wetlands with stream water quality |
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