High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs
In Arctic ecosystems, increasing temperatures are driving the expansion of nitrogen (N) fixing shrubs across tundra landscapes. The implications of this expansion to the biogeochemistry of Arctic ecosystems are of critical importance and more work is needed to better understand the form, availabilit...
Published in: | The Cryosphere |
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Language: | English |
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Copernicus Publications
2022
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Online Access: | https://doi.org/10.5194/tc-16-1889-2022 https://doaj.org/article/2d3d55796ce04f9a93855b6fd08410e4 |
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ftdoajarticles:oai:doaj.org/article:2d3d55796ce04f9a93855b6fd08410e4 2023-05-15T14:55:49+02:00 High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs R. E. McCaully C. A. Arendt B. D. Newman V. G. Salmon J. M. Heikoop C. J. Wilson S. Sevanto N. A. Wales G. B. Perkins O. C. Marina S. D. Wullschleger 2022-05-01T00:00:00Z https://doi.org/10.5194/tc-16-1889-2022 https://doaj.org/article/2d3d55796ce04f9a93855b6fd08410e4 EN eng Copernicus Publications https://tc.copernicus.org/articles/16/1889/2022/tc-16-1889-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-1889-2022 1994-0416 1994-0424 https://doaj.org/article/2d3d55796ce04f9a93855b6fd08410e4 The Cryosphere, Vol 16, Pp 1889-1901 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/tc-16-1889-2022 2022-12-30T23:31:04Z In Arctic ecosystems, increasing temperatures are driving the expansion of nitrogen (N) fixing shrubs across tundra landscapes. The implications of this expansion to the biogeochemistry of Arctic ecosystems are of critical importance and more work is needed to better understand the form, availability, and transportation potential of N from these shrubs across a variety of Arctic landscapes. To gain insights into the processes controlling N within a permafrost hillslope system, the spatiotemporal variability of nitrate (NO <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="53e1f98be2cdf70dbe180d95894fc6b5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-1889-2022-ie00002.svg" width="9pt" height="16pt" src="tc-16-1889-2022-ie00002.png"/></svg:svg> ) and its environmental controls were investigated at an alder ( Alnus viridis spp. fruticosa ) dominated permafrost tundra landscape in the Seward Peninsula, Alaska, USA. Soil pore water was collected from locations within alder shrubland growing along a well-drained hillslope and was compared to soil pore water collected from locations outside ( upslope , downslope , and between ) the alder shrubland. Soil pore water collected within alder shrubland had an average NO 3 -N (nitrogen from nitrate) concentration of 4.27±8.02 mg L −1 and differed significantly from locations outside alder shrubland ( 0.23±0.83 mg L −1 p <0.05 ). Temporal variation in NO 3 -N within and downslope of alder shrubland co-occurred with precipitation events where NO <math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn ... Article in Journal/Newspaper Arctic permafrost Seward Peninsula The Cryosphere Tundra Alaska Directory of Open Access Journals: DOAJ Articles Arctic The Cryosphere 16 5 1889 1901 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 R. E. McCaully C. A. Arendt B. D. Newman V. G. Salmon J. M. Heikoop C. J. Wilson S. Sevanto N. A. Wales G. B. Perkins O. C. Marina S. D. Wullschleger High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
In Arctic ecosystems, increasing temperatures are driving the expansion of nitrogen (N) fixing shrubs across tundra landscapes. The implications of this expansion to the biogeochemistry of Arctic ecosystems are of critical importance and more work is needed to better understand the form, availability, and transportation potential of N from these shrubs across a variety of Arctic landscapes. To gain insights into the processes controlling N within a permafrost hillslope system, the spatiotemporal variability of nitrate (NO <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn mathvariant="normal">3</mn><mo>-</mo></msubsup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="9pt" height="16pt" class="svg-formula" dspmath="mathimg" md5hash="53e1f98be2cdf70dbe180d95894fc6b5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-1889-2022-ie00002.svg" width="9pt" height="16pt" src="tc-16-1889-2022-ie00002.png"/></svg:svg> ) and its environmental controls were investigated at an alder ( Alnus viridis spp. fruticosa ) dominated permafrost tundra landscape in the Seward Peninsula, Alaska, USA. Soil pore water was collected from locations within alder shrubland growing along a well-drained hillslope and was compared to soil pore water collected from locations outside ( upslope , downslope , and between ) the alder shrubland. Soil pore water collected within alder shrubland had an average NO 3 -N (nitrogen from nitrate) concentration of 4.27±8.02 mg L −1 and differed significantly from locations outside alder shrubland ( 0.23±0.83 mg L −1 p <0.05 ). Temporal variation in NO 3 -N within and downslope of alder shrubland co-occurred with precipitation events where NO <math xmlns="http://www.w3.org/1998/Math/MathML" id="M10" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mi/><mn ... |
format |
Article in Journal/Newspaper |
author |
R. E. McCaully C. A. Arendt B. D. Newman V. G. Salmon J. M. Heikoop C. J. Wilson S. Sevanto N. A. Wales G. B. Perkins O. C. Marina S. D. Wullschleger |
author_facet |
R. E. McCaully C. A. Arendt B. D. Newman V. G. Salmon J. M. Heikoop C. J. Wilson S. Sevanto N. A. Wales G. B. Perkins O. C. Marina S. D. Wullschleger |
author_sort |
R. E. McCaully |
title |
High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
title_short |
High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
title_full |
High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
title_fullStr |
High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
title_full_unstemmed |
High nitrate variability on an Alaskan permafrost hillslope dominated by alder shrubs |
title_sort |
high nitrate variability on an alaskan permafrost hillslope dominated by alder shrubs |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/tc-16-1889-2022 https://doaj.org/article/2d3d55796ce04f9a93855b6fd08410e4 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic permafrost Seward Peninsula The Cryosphere Tundra Alaska |
genre_facet |
Arctic permafrost Seward Peninsula The Cryosphere Tundra Alaska |
op_source |
The Cryosphere, Vol 16, Pp 1889-1901 (2022) |
op_relation |
https://tc.copernicus.org/articles/16/1889/2022/tc-16-1889-2022.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-16-1889-2022 1994-0416 1994-0424 https://doaj.org/article/2d3d55796ce04f9a93855b6fd08410e4 |
op_doi |
https://doi.org/10.5194/tc-16-1889-2022 |
container_title |
The Cryosphere |
container_volume |
16 |
container_issue |
5 |
container_start_page |
1889 |
op_container_end_page |
1901 |
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1766327825023893504 |