Long‐Term Nitrate Trajectories Vary by Season in Western European Catchments

Human alteration of nutrient cycles has caused persistent and widespread degradation of water quality around the globe. In many regions, including Western Europe, elevated nitrate (NO3−) concentration in surface waters contributes to eutrophication and noncompliance with environmental legislation. D...

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Veröffentlicht in:Global biogeochemical cycles 2021-09, Vol.35 (9), p.n/a
Hauptverfasser: Ebeling, Pia, Dupas, Rémi, Abbott, Benjamin, Kumar, Rohini, Ehrhardt, Sophie, Fleckenstein, Jan H., Musolff, Andreas
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container_issue 9
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container_title Global biogeochemical cycles
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creator Ebeling, Pia
Dupas, Rémi
Abbott, Benjamin
Kumar, Rohini
Ehrhardt, Sophie
Fleckenstein, Jan H.
Musolff, Andreas
description Human alteration of nutrient cycles has caused persistent and widespread degradation of water quality around the globe. In many regions, including Western Europe, elevated nitrate (NO3−) concentration in surface waters contributes to eutrophication and noncompliance with environmental legislation. Discharge, NO3− concentrations and the vulnerability of the aquatic ecosystems to eutrophication often exhibit a distinct seasonality. Understanding spatial patterns and long‐term trends in this seasonality is crucial to improve water quality management. Here, we hypothesized that NO3− concentrations during high‐flow periods would respond faster to changes in nutrient inputs than low‐flow concentrations because of greater connectivity of shallow diffuse NO3− sources with the river network. To test this hypothesis, we compiled long‐term NO3− and discharge time series from 290 Western European catchments. To characterize the long‐term trajectories of seasonal NO3− concentration, we propose a novel hysteresis approach comparing low‐ and high‐flow NO3− concentration in the context of multi‐decadal N input changes. We found synchronous winter maxima of NO3− and discharge in 84% of the study catchments. However, contrary to our hypothesis, there were surprisingly diverse long‐term trajectories of seasonal NO3− concentration. Both clockwise (faster high‐flow NO3− response) and counterclockwise hysteresis (faster low‐flow NO3− response) occurred in similar proportions, potentially due to a high complexity in the underlying processes. Spatial variability of seasonality in NO3− concentration across the catchments was more pronounced and better predictable than its long‐term variability. This work demonstrates the value of seasonal and inter‐annual hydrochemical analysis and provides new tools for water quality monitoring and management. Plain Language Summary Nitrogen is an essential element of all living organisms and has thus often been used excessively as fertilizer to secure food production. However, surface waters can suffer from elevated nutrients inputs, causing toxic algal blooms and impairing drinking water quality, especially during summer low flows. To manage water quality, it is crucial to understand these seasonal variations of nitrogen and discharge and the underlying processes. We used data from 290 catchments in France and Germany to characterize average seasonality patterns and their long‐term evolution across the variety of landscapes and human influences
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In many regions, including Western Europe, elevated nitrate (NO3−) concentration in surface waters contributes to eutrophication and noncompliance with environmental legislation. Discharge, NO3− concentrations and the vulnerability of the aquatic ecosystems to eutrophication often exhibit a distinct seasonality. Understanding spatial patterns and long‐term trends in this seasonality is crucial to improve water quality management. Here, we hypothesized that NO3− concentrations during high‐flow periods would respond faster to changes in nutrient inputs than low‐flow concentrations because of greater connectivity of shallow diffuse NO3− sources with the river network. To test this hypothesis, we compiled long‐term NO3− and discharge time series from 290 Western European catchments. To characterize the long‐term trajectories of seasonal NO3− concentration, we propose a novel hysteresis approach comparing low‐ and high‐flow NO3− concentration in the context of multi‐decadal N input changes. We found synchronous winter maxima of NO3− and discharge in 84% of the study catchments. However, contrary to our hypothesis, there were surprisingly diverse long‐term trajectories of seasonal NO3− concentration. Both clockwise (faster high‐flow NO3− response) and counterclockwise hysteresis (faster low‐flow NO3− response) occurred in similar proportions, potentially due to a high complexity in the underlying processes. Spatial variability of seasonality in NO3− concentration across the catchments was more pronounced and better predictable than its long‐term variability. This work demonstrates the value of seasonal and inter‐annual hydrochemical analysis and provides new tools for water quality monitoring and management. Plain Language Summary Nitrogen is an essential element of all living organisms and has thus often been used excessively as fertilizer to secure food production. However, surface waters can suffer from elevated nutrients inputs, causing toxic algal blooms and impairing drinking water quality, especially during summer low flows. To manage water quality, it is crucial to understand these seasonal variations of nitrogen and discharge and the underlying processes. We used data from 290 catchments in France and Germany to characterize average seasonality patterns and their long‐term evolution across the variety of landscapes and human influences. This allowed classifying catchment behavior and linking them to controls. As expected, both nitrogen and discharge peak during winter in most catchments (84%). However, there are well explainable deviations, for example, in mountainous regions. The long‐term evolution of seasonality was more diverse than expected suggesting a complex interplay of various processes with the long input history from fertilization and wastewater being part of the controls. We found that the differences among catchments were greater than the long‐term changes of seasonality within most catchments. By identifying catchment typologies, our study increases the understanding of nitrate seasonality patterns across a large extent and thus supports ecological water quality management. Key Points Spatial patterns of nitrate and discharge seasonality are linked to topography and hydroclimate with winter maxima dominating for both After decreasing nutrient inputs, cases with decreases in river nitrate preceding during low‐ and high‐flow seasons occurred equally often Spatial variability of nitrate seasonality is greater and more predictable from catchment characteristics than its long‐term variability</description><identifier>ISSN: 0886-6236</identifier><identifier>EISSN: 1944-9224</identifier><identifier>EISSN: 1944-8224</identifier><identifier>DOI: 10.1029/2021GB007050</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Algal blooms ; Aquatic ecosystems ; Biodegradation ; Biological fertilization ; Catchment area ; catchment hydrology ; Catchments ; Complexity ; controls ; Discharge ; Drinking water ; Environment and Society ; Environmental degradation ; Environmental law ; Environmental legislation ; Environmental Sciences ; Eutrophication ; Evolution ; Fertilization ; Fertilizers ; Food production ; Human influences ; Hydrochemical analysis ; Hydrochemicals ; Hypotheses ; Hysteresis ; Legislation ; long‐term trends ; Low flow ; Mountain regions ; nitrate seasonality ; Nitrates ; Nitrogen ; Nutrient concentrations ; Nutrient cycles ; Nutrients ; Quality management ; Regions ; River networks ; Seasonal variation ; Seasonal variations ; Seasonality ; Seasons ; Spatial variability ; Spatial variations ; Surface water ; Variability ; Vulnerability ; Wastewater ; Water monitoring ; Water quality ; Water quality management ; Water quality monitoring ; Winter</subject><ispartof>Global biogeochemical cycles, 2021-09, Vol.35 (9), p.n/a</ispartof><rights>2021. 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In many regions, including Western Europe, elevated nitrate (NO3−) concentration in surface waters contributes to eutrophication and noncompliance with environmental legislation. Discharge, NO3− concentrations and the vulnerability of the aquatic ecosystems to eutrophication often exhibit a distinct seasonality. Understanding spatial patterns and long‐term trends in this seasonality is crucial to improve water quality management. Here, we hypothesized that NO3− concentrations during high‐flow periods would respond faster to changes in nutrient inputs than low‐flow concentrations because of greater connectivity of shallow diffuse NO3− sources with the river network. To test this hypothesis, we compiled long‐term NO3− and discharge time series from 290 Western European catchments. To characterize the long‐term trajectories of seasonal NO3− concentration, we propose a novel hysteresis approach comparing low‐ and high‐flow NO3− concentration in the context of multi‐decadal N input changes. We found synchronous winter maxima of NO3− and discharge in 84% of the study catchments. However, contrary to our hypothesis, there were surprisingly diverse long‐term trajectories of seasonal NO3− concentration. Both clockwise (faster high‐flow NO3− response) and counterclockwise hysteresis (faster low‐flow NO3− response) occurred in similar proportions, potentially due to a high complexity in the underlying processes. Spatial variability of seasonality in NO3− concentration across the catchments was more pronounced and better predictable than its long‐term variability. This work demonstrates the value of seasonal and inter‐annual hydrochemical analysis and provides new tools for water quality monitoring and management. Plain Language Summary Nitrogen is an essential element of all living organisms and has thus often been used excessively as fertilizer to secure food production. However, surface waters can suffer from elevated nutrients inputs, causing toxic algal blooms and impairing drinking water quality, especially during summer low flows. To manage water quality, it is crucial to understand these seasonal variations of nitrogen and discharge and the underlying processes. We used data from 290 catchments in France and Germany to characterize average seasonality patterns and their long‐term evolution across the variety of landscapes and human influences. This allowed classifying catchment behavior and linking them to controls. As expected, both nitrogen and discharge peak during winter in most catchments (84%). However, there are well explainable deviations, for example, in mountainous regions. The long‐term evolution of seasonality was more diverse than expected suggesting a complex interplay of various processes with the long input history from fertilization and wastewater being part of the controls. We found that the differences among catchments were greater than the long‐term changes of seasonality within most catchments. By identifying catchment typologies, our study increases the understanding of nitrate seasonality patterns across a large extent and thus supports ecological water quality management. Key Points Spatial patterns of nitrate and discharge seasonality are linked to topography and hydroclimate with winter maxima dominating for both After decreasing nutrient inputs, cases with decreases in river nitrate preceding during low‐ and high‐flow seasons occurred equally often Spatial variability of nitrate seasonality is greater and more predictable from catchment characteristics than its long‐term variability</description><subject>Algal blooms</subject><subject>Aquatic ecosystems</subject><subject>Biodegradation</subject><subject>Biological fertilization</subject><subject>Catchment area</subject><subject>catchment hydrology</subject><subject>Catchments</subject><subject>Complexity</subject><subject>controls</subject><subject>Discharge</subject><subject>Drinking water</subject><subject>Environment and Society</subject><subject>Environmental degradation</subject><subject>Environmental law</subject><subject>Environmental legislation</subject><subject>Environmental Sciences</subject><subject>Eutrophication</subject><subject>Evolution</subject><subject>Fertilization</subject><subject>Fertilizers</subject><subject>Food production</subject><subject>Human influences</subject><subject>Hydrochemical analysis</subject><subject>Hydrochemicals</subject><subject>Hypotheses</subject><subject>Hysteresis</subject><subject>Legislation</subject><subject>long‐term trends</subject><subject>Low flow</subject><subject>Mountain regions</subject><subject>nitrate seasonality</subject><subject>Nitrates</subject><subject>Nitrogen</subject><subject>Nutrient concentrations</subject><subject>Nutrient cycles</subject><subject>Nutrients</subject><subject>Quality management</subject><subject>Regions</subject><subject>River networks</subject><subject>Seasonal variation</subject><subject>Seasonal variations</subject><subject>Seasonality</subject><subject>Seasons</subject><subject>Spatial variability</subject><subject>Spatial variations</subject><subject>Surface water</subject><subject>Variability</subject><subject>Vulnerability</subject><subject>Wastewater</subject><subject>Water monitoring</subject><subject>Water quality</subject><subject>Water quality management</subject><subject>Water quality monitoring</subject><subject>Winter</subject><issn>0886-6236</issn><issn>1944-9224</issn><issn>1944-8224</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp9kEFLwzAYhoMoOKc3f0DAk2D1S5qkzXErcxPKPDj1GNIsdR1bO5NO2c2f4G_0l5hREU-evpePh5eHF6FzAtcEqLyhQMl4CJAAhwPUI5KxSFLKDlEP0lREgsbiGJ14vwQgjHPZQ9O8qV--Pj5n1q3xtGqdbi2eOb20pm1cZT1-0m6Hix1-sNo3Na5q_Gx9a12NR1vXbKyucaZbs1jbuvWn6KjUK2_Pfm4fPd6OZtkkyu_Hd9kgj0ycpDKKaQEsLoo5F5IXvOTa0CJYl4aUWpCQ0tRQXs4JM3KeUqoJWCM0sZwBEyTuo8uud6FXauOqdZBUja7UZJCr_Q_iJHQk8LZnLzp245rXbXBXy2br6qCnKE-EYDGkIlBXHWVc472z5W8tAbVfV_1dN-C0w9-rld39y6rxMKOEJDL-BrKHeYE</recordid><startdate>202109</startdate><enddate>202109</enddate><creator>Ebeling, Pia</creator><creator>Dupas, Rémi</creator><creator>Abbott, Benjamin</creator><creator>Kumar, Rohini</creator><creator>Ehrhardt, Sophie</creator><creator>Fleckenstein, Jan H.</creator><creator>Musolff, Andreas</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>24P</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7TG</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0001-7213-9448</orcidid><orcidid>https://orcid.org/0000-0002-5080-5275</orcidid><orcidid>https://orcid.org/0000-0002-5932-4056</orcidid><orcidid>https://orcid.org/0000-0002-4396-2037</orcidid><orcidid>https://orcid.org/0000-0001-5861-3481</orcidid><orcidid>https://orcid.org/0000-0003-4166-5597</orcidid><orcidid>https://orcid.org/0000-0002-0115-1359</orcidid></search><sort><creationdate>202109</creationdate><title>Long‐Term Nitrate Trajectories Vary by Season in Western European Catchments</title><author>Ebeling, Pia ; 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Geoastrophysical Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Global biogeochemical cycles</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ebeling, Pia</au><au>Dupas, Rémi</au><au>Abbott, Benjamin</au><au>Kumar, Rohini</au><au>Ehrhardt, Sophie</au><au>Fleckenstein, Jan H.</au><au>Musolff, Andreas</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Long‐Term Nitrate Trajectories Vary by Season in Western European Catchments</atitle><jtitle>Global biogeochemical cycles</jtitle><date>2021-09</date><risdate>2021</risdate><volume>35</volume><issue>9</issue><epage>n/a</epage><issn>0886-6236</issn><eissn>1944-9224</eissn><eissn>1944-8224</eissn><abstract>Human alteration of nutrient cycles has caused persistent and widespread degradation of water quality around the globe. In many regions, including Western Europe, elevated nitrate (NO3−) concentration in surface waters contributes to eutrophication and noncompliance with environmental legislation. Discharge, NO3− concentrations and the vulnerability of the aquatic ecosystems to eutrophication often exhibit a distinct seasonality. Understanding spatial patterns and long‐term trends in this seasonality is crucial to improve water quality management. Here, we hypothesized that NO3− concentrations during high‐flow periods would respond faster to changes in nutrient inputs than low‐flow concentrations because of greater connectivity of shallow diffuse NO3− sources with the river network. To test this hypothesis, we compiled long‐term NO3− and discharge time series from 290 Western European catchments. To characterize the long‐term trajectories of seasonal NO3− concentration, we propose a novel hysteresis approach comparing low‐ and high‐flow NO3− concentration in the context of multi‐decadal N input changes. We found synchronous winter maxima of NO3− and discharge in 84% of the study catchments. However, contrary to our hypothesis, there were surprisingly diverse long‐term trajectories of seasonal NO3− concentration. Both clockwise (faster high‐flow NO3− response) and counterclockwise hysteresis (faster low‐flow NO3− response) occurred in similar proportions, potentially due to a high complexity in the underlying processes. Spatial variability of seasonality in NO3− concentration across the catchments was more pronounced and better predictable than its long‐term variability. This work demonstrates the value of seasonal and inter‐annual hydrochemical analysis and provides new tools for water quality monitoring and management. Plain Language Summary Nitrogen is an essential element of all living organisms and has thus often been used excessively as fertilizer to secure food production. However, surface waters can suffer from elevated nutrients inputs, causing toxic algal blooms and impairing drinking water quality, especially during summer low flows. To manage water quality, it is crucial to understand these seasonal variations of nitrogen and discharge and the underlying processes. We used data from 290 catchments in France and Germany to characterize average seasonality patterns and their long‐term evolution across the variety of landscapes and human influences. This allowed classifying catchment behavior and linking them to controls. As expected, both nitrogen and discharge peak during winter in most catchments (84%). However, there are well explainable deviations, for example, in mountainous regions. The long‐term evolution of seasonality was more diverse than expected suggesting a complex interplay of various processes with the long input history from fertilization and wastewater being part of the controls. We found that the differences among catchments were greater than the long‐term changes of seasonality within most catchments. By identifying catchment typologies, our study increases the understanding of nitrate seasonality patterns across a large extent and thus supports ecological water quality management. Key Points Spatial patterns of nitrate and discharge seasonality are linked to topography and hydroclimate with winter maxima dominating for both After decreasing nutrient inputs, cases with decreases in river nitrate preceding during low‐ and high‐flow seasons occurred equally often Spatial variability of nitrate seasonality is greater and more predictable from catchment characteristics than its long‐term variability</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2021GB007050</doi><tpages>19</tpages><orcidid>https://orcid.org/0000-0001-7213-9448</orcidid><orcidid>https://orcid.org/0000-0002-5080-5275</orcidid><orcidid>https://orcid.org/0000-0002-5932-4056</orcidid><orcidid>https://orcid.org/0000-0002-4396-2037</orcidid><orcidid>https://orcid.org/0000-0001-5861-3481</orcidid><orcidid>https://orcid.org/0000-0003-4166-5597</orcidid><orcidid>https://orcid.org/0000-0002-0115-1359</orcidid><oa>free_for_read</oa></addata></record>
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subjects Algal blooms
Aquatic ecosystems
Biodegradation
Biological fertilization
Catchment area
catchment hydrology
Catchments
Complexity
controls
Discharge
Drinking water
Environment and Society
Environmental degradation
Environmental law
Environmental legislation
Environmental Sciences
Eutrophication
Evolution
Fertilization
Fertilizers
Food production
Human influences
Hydrochemical analysis
Hydrochemicals
Hypotheses
Hysteresis
Legislation
long‐term trends
Low flow
Mountain regions
nitrate seasonality
Nitrates
Nitrogen
Nutrient concentrations
Nutrient cycles
Nutrients
Quality management
Regions
River networks
Seasonal variation
Seasonal variations
Seasonality
Seasons
Spatial variability
Spatial variations
Surface water
Variability
Vulnerability
Wastewater
Water monitoring
Water quality
Water quality management
Water quality monitoring
Winter
title Long‐Term Nitrate Trajectories Vary by Season in Western European Catchments
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