Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains.
There is a growing understanding of the role that bedrock weathering can play as a source of nitrogen (N) to soils, groundwater and river systems. The significance is particularly apparent in mountainous environments where weathering fluxes can be large. However, our understanding of the relative co...
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Public Library of Science (PLoS)
2021-01-01
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| Series: | PLoS ONE |
| Online Access: | https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0247907&type=printable |
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| author | Taylor Maavara Erica R Siirila-Woodburn Fadji Maina Reed M Maxwell James E Sample K Dana Chadwick Rosemary Carroll Michelle E Newcomer Wenming Dong Kenneth H Williams Carl I Steefel Nicholas J Bouskill |
| author_facet | Taylor Maavara Erica R Siirila-Woodburn Fadji Maina Reed M Maxwell James E Sample K Dana Chadwick Rosemary Carroll Michelle E Newcomer Wenming Dong Kenneth H Williams Carl I Steefel Nicholas J Bouskill |
| author_sort | Taylor Maavara |
| collection | DOAJ |
| description | There is a growing understanding of the role that bedrock weathering can play as a source of nitrogen (N) to soils, groundwater and river systems. The significance is particularly apparent in mountainous environments where weathering fluxes can be large. However, our understanding of the relative contributions of rock-derived, or geogenic, N to the total N supply of mountainous watersheds remains poorly understood. In this study, we develop the High-Altitude Nitrogen Suite of Models (HAN-SoMo), a watershed-scale ensemble of process-based models to quantify the relative sources, transformations, and sinks of geogenic and atmospheric N through a mountain watershed. Our study is based in the East River Watershed (ERW) in the Upper Colorado River Basin. The East River is a near-pristine headwater watershed underlain primarily by an N-rich Mancos Shale bedrock, enabling the timing and magnitude of geogenic and atmospheric contributions to watershed scale dissolved N-exports to be quantified. Several calibration scenarios were developed to explore equifinality using >1600 N concentration measurements from streams, groundwater, and vadose zone samples collected over the course of four years across the watershed. When accounting for recycling of N through plant litter turnover, rock weathering accounts for approximately 12% of the annual dissolved N sources to the watershed in the most probable calibration scenario (0-31% in other scenarios), and 21% (0-44% in other scenarios) when considering only "new" N sources (i.e. geogenic and atmospheric). On an annual scale, instream dissolved N elimination, plant turnover (including cattle grazing) and atmospheric deposition are the most important controls on N cycling. |
| format | Article |
| id | doaj-art-9b32cacdb54841509a709c4c1497a598 |
| institution | OA Journals |
| issn | 1932-6203 |
| language | English |
| publishDate | 2021-01-01 |
| publisher | Public Library of Science (PLoS) |
| record_format | Article |
| series | PLoS ONE |
| spelling | doaj-art-9b32cacdb54841509a709c4c1497a5982025-08-20T02:17:56ZengPublic Library of Science (PLoS)PLoS ONE1932-62032021-01-01163e024790710.1371/journal.pone.0247907Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains.Taylor MaavaraErica R Siirila-WoodburnFadji MainaReed M MaxwellJames E SampleK Dana ChadwickRosemary CarrollMichelle E NewcomerWenming DongKenneth H WilliamsCarl I SteefelNicholas J BouskillThere is a growing understanding of the role that bedrock weathering can play as a source of nitrogen (N) to soils, groundwater and river systems. The significance is particularly apparent in mountainous environments where weathering fluxes can be large. However, our understanding of the relative contributions of rock-derived, or geogenic, N to the total N supply of mountainous watersheds remains poorly understood. In this study, we develop the High-Altitude Nitrogen Suite of Models (HAN-SoMo), a watershed-scale ensemble of process-based models to quantify the relative sources, transformations, and sinks of geogenic and atmospheric N through a mountain watershed. Our study is based in the East River Watershed (ERW) in the Upper Colorado River Basin. The East River is a near-pristine headwater watershed underlain primarily by an N-rich Mancos Shale bedrock, enabling the timing and magnitude of geogenic and atmospheric contributions to watershed scale dissolved N-exports to be quantified. Several calibration scenarios were developed to explore equifinality using >1600 N concentration measurements from streams, groundwater, and vadose zone samples collected over the course of four years across the watershed. When accounting for recycling of N through plant litter turnover, rock weathering accounts for approximately 12% of the annual dissolved N sources to the watershed in the most probable calibration scenario (0-31% in other scenarios), and 21% (0-44% in other scenarios) when considering only "new" N sources (i.e. geogenic and atmospheric). On an annual scale, instream dissolved N elimination, plant turnover (including cattle grazing) and atmospheric deposition are the most important controls on N cycling.https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0247907&type=printable |
| spellingShingle | Taylor Maavara Erica R Siirila-Woodburn Fadji Maina Reed M Maxwell James E Sample K Dana Chadwick Rosemary Carroll Michelle E Newcomer Wenming Dong Kenneth H Williams Carl I Steefel Nicholas J Bouskill Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. PLoS ONE |
| title | Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. |
| title_full | Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. |
| title_fullStr | Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. |
| title_full_unstemmed | Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. |
| title_short | Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains. |
| title_sort | modeling geogenic and atmospheric nitrogen through the east river watershed colorado rocky mountains |
| url | https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0247907&type=printable |
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