High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends

<p>Poultry manure is the primary cause of nitrate (NO<sub>3</sub><sup>−</sup>) exceedances in the transboundary Abbotsford–Sumas aquifer (ASA; Canada–USA) based on synoptic surveys two decades apart, but questions remained about seasonal and spatial aspects of agricu...

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Main Authors: M. Suchy, L. I. Wassenaar, G. Graham, B. Zebarth
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/22/4267/2018/hess-22-4267-2018.pdf
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author M. Suchy
L. I. Wassenaar
G. Graham
B. Zebarth
author_facet M. Suchy
L. I. Wassenaar
G. Graham
B. Zebarth
author_sort M. Suchy
collection DOAJ
description <p>Poultry manure is the primary cause of nitrate (NO<sub>3</sub><sup>−</sup>) exceedances in the transboundary Abbotsford–Sumas aquifer (ASA; Canada–USA) based on synoptic surveys two decades apart, but questions remained about seasonal and spatial aspects of agricultural nitrate fluxes to the aquifer to help better focus remediation efforts. We conducted over 700 monthly <i>δ</i><sup>15</sup>N and <i>δ</i><sup>18</sup>O of nitrate assays, focusing on shallow groundwater (&lt;&thinsp;5 years old) over a 5-year period to gain new insight on spatio-temporal sources and controls of groundwater nitrate contamination. NO<sub>3</sub><sup>−</sup> concentrations in these wells ranged from 1.3 to 99&thinsp;mg&thinsp;N&thinsp;L<sup>−1</sup> (<i>n</i> = 1041) with a mean of 16.2±0.4&thinsp;mg&thinsp;N&thinsp;L<sup>−1</sup>. The high-frequency <sup>15</sup>N and <sup>18</sup>O isotope data allowed us to identify three distinctive NO<sub>3</sub><sup>−</sup> source patterns: (i) primarily from synthetic fertilizer, (ii) dynamic changes in nitrate due to changes in land use, and (iii) from a mix of poultry manure and fertilizer. A key finding was that the source(s) of nitrate in recharge could be quickly influenced by short-term near-field management practices and stochastic precipitation events, which ultimately impact long-term nitrate contamination trends. Overall, the isotope data affirmed a subtle decadal-scale shift in agricultural practices from manure increasingly towards fertilizer nitrate sources; nevertheless, poultry-derived N remains a predominant source of nitrate contamination. Because the aquifer does not generally support denitrification, remediation of the Abbotsford–Sumas aquifer is possible only if agricultural N sources are seriously curtailed, a difficult proposition due to longstanding high-value intensive poultry and raspberry and blueberry operations over the aquifer.</p>
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spelling doaj.art-a9f664f153484ff5b64989b44fabfd222022-12-21T19:03:02ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382018-08-01224267427910.5194/hess-22-4267-2018High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trendsM. Suchy0L. I. Wassenaar1G. Graham2B. Zebarth3Environment and Climate Change Canada, 201-401 Burrard St., Vancouver, BC, CanadaInternational Atomic Energy Agency, Vienna International Centre, 1400, Vienna, AustriaEnvironment and Climate Change Canada, 201-401 Burrard St., Vancouver, BC, CanadaFredericton Research and Development Centre, Agriculture and Agri-Food Canada, 850 Lincoln Rd., P.O. Box 20280 Fredericton, NB, E3B 4Z7, Canada<p>Poultry manure is the primary cause of nitrate (NO<sub>3</sub><sup>−</sup>) exceedances in the transboundary Abbotsford–Sumas aquifer (ASA; Canada–USA) based on synoptic surveys two decades apart, but questions remained about seasonal and spatial aspects of agricultural nitrate fluxes to the aquifer to help better focus remediation efforts. We conducted over 700 monthly <i>δ</i><sup>15</sup>N and <i>δ</i><sup>18</sup>O of nitrate assays, focusing on shallow groundwater (&lt;&thinsp;5 years old) over a 5-year period to gain new insight on spatio-temporal sources and controls of groundwater nitrate contamination. NO<sub>3</sub><sup>−</sup> concentrations in these wells ranged from 1.3 to 99&thinsp;mg&thinsp;N&thinsp;L<sup>−1</sup> (<i>n</i> = 1041) with a mean of 16.2±0.4&thinsp;mg&thinsp;N&thinsp;L<sup>−1</sup>. The high-frequency <sup>15</sup>N and <sup>18</sup>O isotope data allowed us to identify three distinctive NO<sub>3</sub><sup>−</sup> source patterns: (i) primarily from synthetic fertilizer, (ii) dynamic changes in nitrate due to changes in land use, and (iii) from a mix of poultry manure and fertilizer. A key finding was that the source(s) of nitrate in recharge could be quickly influenced by short-term near-field management practices and stochastic precipitation events, which ultimately impact long-term nitrate contamination trends. Overall, the isotope data affirmed a subtle decadal-scale shift in agricultural practices from manure increasingly towards fertilizer nitrate sources; nevertheless, poultry-derived N remains a predominant source of nitrate contamination. Because the aquifer does not generally support denitrification, remediation of the Abbotsford–Sumas aquifer is possible only if agricultural N sources are seriously curtailed, a difficult proposition due to longstanding high-value intensive poultry and raspberry and blueberry operations over the aquifer.</p>https://www.hydrol-earth-syst-sci.net/22/4267/2018/hess-22-4267-2018.pdf
spellingShingle M. Suchy
L. I. Wassenaar
G. Graham
B. Zebarth
High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
Hydrology and Earth System Sciences
title High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
title_full High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
title_fullStr High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
title_full_unstemmed High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
title_short High-frequency NO<sub>3</sub><sup>−</sup> isotope (<i>δ</i><sup>15</sup>N, <i>δ</i><sup>18</sup>O) patterns in groundwater recharge reveal that short-term changes in land use and precipitation influence nitrate contamination trends
title_sort high frequency no sub 3 sub sup sup isotope i δ i sup 15 sup n i δ i sup 18 sup o patterns in groundwater recharge reveal that short term changes in land use and precipitation influence nitrate contamination trends
url https://www.hydrol-earth-syst-sci.net/22/4267/2018/hess-22-4267-2018.pdf
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