4.7 Article

Stable isotopes provide insight into sources and cycling of N compounds in the Sacramento-San Joaquin Delta, California, USA

期刊

SCIENCE OF THE TOTAL ENVIRONMENT
卷 816, 期 -, 页码 -

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ELSEVIER
DOI: 10.1016/j.scitotenv.2021.151592

关键词

Stable isotopes; Biogeochemical processes; Ammonium; Nitrate; Wastewater

资金

  1. state of California under Delta Science Program [5051]

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River deltas are increasingly impacted by human inputs of nitrogen, which can lead to harmful phenomena. A study on the Sacramento-San Joaquin Delta in California used a multi-tracer approach to examine nitrogen sources and processes. Results showed that the Sacramento River and its distributaries primarily received nitrogen in the form of NH4+ from treated wastewater effluent, and there were significant biogeochemical processes that affected the downstream transport of nitrogen. The study also highlighted the diversity in nitrogen dynamics and the utility of a multi-tracer approach in complex river delta environments.
River deltas and their diverse array of aquatic environments are increasingly impacted by anthropogenic inputs of nitrogen (N). These inputs can alter the N biogeochemistry of these systems and promote undesirable phenomena including harmful algae blooms and invasive aquatic macrophytes. To examine N sources and biogeochemical processes in the Sacramento-San Joaquin Delta, a river delta located in central California, USA, that is fed primarily by the Sacramento River, we utilized a multi-tracer approach that measured N species concentrations and stable isotope valuesmonthly from April 2011 to November 2012 in samples collected from the channelizedmainstemof the Sacramento River, two channelized distributaries of the Sacramento River, and the Cache Slough Complex, a network of Sacramento River tributaries and shallow water wetland habitat. We found that the Sacramento River and its channelized distributaries received N primarily in the form of NH4+ from treated wastewater effluent and that NH4+ was lost rapidly while NO3- was gained more slowly during subsequent downstream transit, driven by an array of biogeochemical processes whose identities could be constrained via examination of stable isotope values. The Cache Slough Complex, which was characterized by lower net flows and higher water residence times than the Sacramento River and its distributaries, received variable inputs of low conductivity water elevated in NH4+ from the Sacramento River and higher conductivity water elevated in NO3- from landward tributaries. Deviations from expected conservative mixing of these sources were spatially variable but broadly indicative of local inputs of treated wastewater effluent NO3-, conversion of Sacramento River NH4+ to NO3- via nitrification, uptake of NH4+ and NO3- by phytoplankton, and remineralization of organic N. These findings highlight both the diversity in N dynamics in anthropogenically impacted river delta environments and the utility of a multi-tracer approach in constraining these processes in such complex systems. Published by Elsevier B.V.

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