Wetland water quality patterns and anthropogenic pressure associations across the continental USA

• Published in: Wetlands (Wilmington, N.C.) N.C.), 2023-12, Vol.43 (8), p.1-19, Article 107
• Main Authors: Trebitz, Anett S., Herlihy, Alan T.
• Format: Article
• Language: English
• Subjects: Acidic lakes; Anthropogenic factors; Biogeography; Biomedical and Life Sciences; Catchment scale; Catchments; Check lists; Chlorides; Chlorophyll; Chromatography; Coal mining; Coastal Sciences; Dissolved organic carbon; Ecology; Environmental Management; Flats (landforms); Freshwater & Marine Ecology; General Wetland Science; Human influences; Hydrogeology; Ionic strength; Laboratories; Lakes; Landscape Ecology; Life Sciences; Nutrients; Organic acids; Pressure; Road salt; Site selection; Streams; Sulfates; Surface water; Turbidity; Urban agriculture; Water analysis; Water quality; Water sampling; Wetlands
• ISSN: 0277-5212; 1943-6246
• DOI: 10.1007/s13157-023-01754-8

Anthropogenic impacts on lake and stream water quality are well established but have been much less studied in wetlands. Here we use data from the 2016 National Wetland Condition Assessment to characterize water quality and its relationship to anthropogenic pressure for inland wetlands across the conterminous USA. Water samples obtained from 525 inland wetlands spanned pH from  9 and 3 to 5 orders of magnitude in ionic strength (chloride, sulfate, conductivity), nutrients (total N and P), turbidity, planktonic chlorophyll, and dissolved organic carbon (DOC). Anthropogenic pressure levels were evaluated at two spatial scales – an adjacent scale scored from field checklists, and a catchment scale indicated by percent agricultural plus urban landcover. Pressure at the two spatial scales were uncorrelated and varied considerably across regions and wetland hydrogeomorphic types. Both adjacent- and catchment-scale pressure were associated with elevated ionic-strength metrics; chloride elevation was most evident in road-salt using states, and sulfate was strongly elevated in a few sites with coal mining nearby. Nutrients were elevated in association with catchment-scale pressure but concomitant changes were not seen in planktonic chlorophyll. Acidic pH and high DOC occurred primarily in upper Great Lakes and eastern seaboard sites having low anthropogenic pressure, suggesting natural organic acid sources. Ionic strength and nutrients increased with increasing catchment-scale pressure even in Flats and closed Depression and Lacustrine sites, which indicates connectivity to rather than isolation from upland anthropogenic landuse even for wetlands lacking inflowing streams.