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Type: | Resource | |
Storage: | The size of this resource is 27.6 KB | |
Created: | Feb 02, 2024 at 8:26 p.m. | |
Last updated: | Feb 05, 2024 at 3:51 p.m. (Metadata update) | |
Published date: | Feb 05, 2024 at 3:51 p.m. | |
DOI: | 10.4211/hs.5d326d1f18aa40738bf8bd7ec6e65eb9 | |
Citation: | See how to cite this resource |
Sharing Status: | Published |
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Views: | 303 |
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Abstract
Groundwater nitrate-N isotopes (δ15N-NO3-) have been used to infer the effects of natural and anthropogenic change on N cycle processes in the environment. Here we report unexpected changes in groundwater δ15N-NO3- for riparian zones affected by relict milldams and salinization. Contrary to natural conditions, groundwater δ15N-NO3- values declined from the upland edge through the riparian zone and were lowest near the stream. Groundwater δ15N-NO3- values increased for low electron donor (dissolved organic carbon and iron) to acceptor (NO3-) ratios but decreased beyond a specific change point. Groundwater δ15N-NO3- values were particularly low for the riparian milldam site subjected to road-salt salinization. We attributed these N isotopic trends to suppression of denitrification, occurrence of dissimilatory nitrate reduction to ammonium (DNRA), and/or road salt salinization. Groundwater δ15N-NO3- can provide valuable insights into process mechanisms and can serve as “imprints” of anthropogenic activities and legacies.
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Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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National Science Foundation | Hydrologic Sciences grant | #1929747 and # 2213855. |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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