Quantifying the Response of Nitrogen Speciation to Hydrology in the Chesapeake Bay Watershed Using a Multilevel Modeling Approach. (26th July 2021)

• Record Type: Journal Article
• Authors: Bertani, Isabella; Bhatt, Gopal; Shenk, Gary W.; Linker, Lewis C.
• Is Part Of: Journal of the American Water Resources Association. Volume 58:Number 6(2022)
• Page Start: 792
• Page End: 804
• Publication Date: 2021-07-26
• Subjects: Chesapeake Bay -- nitrogen loads -- nitrogen speciation -- hydrology -- anthropogenic nitrogen inputs -- hierarchical model; Water-supply -- Periodicals; Hydrology -- Periodicals; Water resources development -- Periodicals; Water resources development -- Environmental aspects -- Periodicals; 333.9100973
• DOI: 10.1111/1752-1688.12951
• Languages: English
• ISSNs: 1093-474X

Abstract

Abstract: Excessive nitrogen (N) inputs to coastal waters can lead to severe eutrophication and different chemical forms of N exhibit varying levels of effectiveness in fueling primary production. Efforts to mitigate N fluxes from coastal watersheds are often guided by models that predict changes in N loads as a function of changes in land use, management practices, and climate. However, relatively little is known on the impacts of such changes on the relative fractions of different N forms. We leveraged a long‐term dataset of N loads from over 100 river stations to investigate how the NO 3 ‐ fraction, that is, the ratio of NO 3 ‐ to total N ( NO 3 ‐ /TN), changes as a function of spatio‐temporal changes in TN loads in the Chesapeake Bay watershed. We built a hierarchical model that separates the response of NO 3 ‐ to changes in TN load occurring at different scales: Across river stations, where differences in TN loads are largely driven by spatial differences in anthropogenic inputs, and within stations, where inter‐annual variability in hydrology is a key driver of changes in TN loads. Results suggest that while increases in TN loads resulting from changes in anthropogenic inputs lead to an increase in the NO 3 ‐ fraction, a decrease in the NO 3 ‐ fraction may occur when increases in TN loads are driven by increased streamflow. These results are especially relevant in watersheds that may experience changes in N loads due to both management decisions and climate‐driven changes in hydrology.