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Updated: Feb 3, 2026

Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
Published on: October 29, 2016
Coupling High-Frequency Stream Metabolism and Nutrient Monitoring to Explore Biogeochemical Controls on Downstream
Helen P Jarvie1, Andrew N Sharpley2, Timothy Kresse3
1NERC Centre for Ecology and Hydrology , Wallingford , OX10 8BB , United Kingdom.
Seasonal shifts in stream metabolism drive nitrate retention in rivers. Continuous sensors reveal how assimilation and denitrification remove over 90% of baseflow nitrate, highlighting the role of river biota in nitrogen transport.
Area of Science:
- Environmental Science
- Biogeochemistry
- Ecology
Background:
- Instream biogeochemical process measurements are typically short-term and localized.
- Understanding seasonal nitrate dynamics at the river-reach scale is crucial for water quality management.
Purpose of the Study:
- To quantify the net effects of biogeochemical processes on seasonal baseflow nitrate retention.
- To investigate the role of stream metabolism and biota in nitrogen dynamics using in situ sensors.
Main Methods:
- Utilized dual-station, high-frequency in situ nitrate sensors.
- Coupled nitrate data with high-frequency measurements of stream metabolism and dissolved inorganic carbon.
- Calculated nitrate assimilation from net primary production and estimated nitrification/denitrification using mass-balance.
Main Results:
- Instream processes removed >30-90% of baseflow nitrate load over a 6.5 km reach.
- Observed a seasonal switch from nitrate assimilation (spring/early summer) to denitrification (after midsummer).
- Synchronicity noted between metabolic shifts (autotrophy to heterotrophy) and changes in nitrate processing.
Conclusions:
- Seasonal shifts in metabolic pathways significantly drive instream nitrate retention and downstream delivery.
- Continuous in situ stream sensor networks provide novel opportunities for quantifying nitrogen dynamics in fluvial systems.
- River biota play a critical role in the fate and transport of nitrogen in river networks.
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