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An increase in the slope of the concentration-discharge relation for total organic carbon in major rivers in New England, 1973 to 2019

March 2, 2021

The mobilization and transport of organic carbon (OC) in rivers and delivery to the near-coastal ocean are important processes in the carbon cycle that are affected by both climate and anthropogenic activities. Riverine OC transport can affect carbon sequestration, contaminant transport, ocean acidification, the formation of toxic disinfection by-products, ocean temperature and phytoplankton productivity. There have been many studies reporting temporal trends in OC concentrations in comparatively small streams with minimal anthropogenic influences but there have been fewer studies on larger rivers and fewer still that have investigated changes in OC concentration-discharge (C-Q) relations. This study examined changes in C-Q relations for total organic carbon (TOC) from 1973 to 2019 in 8 rivers in New England, USA. TOC concentrations declined in all rivers, and in most rivers, and in most seasons, the slope of the C-Q relation increased between 1973 to 1995 and 1996 to 2019. The increase in C-Q slope between periods may be related to changes in the magnitude of TOC sources. The most likely sources to have changed are wastewater inputs, urban runoff, production through photosynthesis in aquatic systems, and runoff from agricultural and forestry practices. Changes in wetland abundance and changes in sulfate concentrations can be ruled out as drivers of the observed changes in C-Q.

Publication Year 2021
Title An increase in the slope of the concentration-discharge relation for total organic carbon in major rivers in New England, 1973 to 2019
DOI 10.1016/j.scitotenv.2021.146149
Authors Thomas G. Huntington, Michael Wieczorek
Publication Type Article
Publication Subtype Journal Article
Series Title Science of the Total Environment
Index ID 70221790
Record Source USGS Publications Warehouse
USGS Organization New England Water Science Center
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