Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau
The carbon release and transport in rivers are expected to increase in a warming climate with enhanced melting. We present a continuous dataset of DOC in the river, precipitation, and groundwater, including air temperature, discharge, and precipitation in the source region of the Yangtze River (SRYR...
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ftmdpi:oai:mdpi.com:/2071-1050/14/4/2441/ 2023-08-20T04:09:14+02:00 Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau Xiaoni You Xiangying Li Mika Sillanpää Rong Wang Chengyong Wu Qiangqiang Xu agris 2022-02-21 application/pdf https://doi.org/10.3390/su14042441 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/su14042441 https://creativecommons.org/licenses/by/4.0/ Sustainability; Volume 14; Issue 4; Pages: 2441 DOC groundwater precipitation river water Yangtze River Text 2022 ftmdpi https://doi.org/10.3390/su14042441 2023-08-01T04:13:37Z The carbon release and transport in rivers are expected to increase in a warming climate with enhanced melting. We present a continuous dataset of DOC in the river, precipitation, and groundwater, including air temperature, discharge, and precipitation in the source region of the Yangtze River (SRYR). Our study shows that the average concentrations of DOC in the three end-members are characterized as the sequence of groundwater > precipitation > river, which is related to the water volume, cycle period, and river flow speed. The seasonality of DOC in the river is observed as the obvious bimodal structure at Tuotuohe (TTH) and Zhimenda (ZMD) gauging stations. The highest concentration appears in July (2.4 mg L−1 at TTH and 2.1 mg L−1 at ZMD) and the secondary high value (2.2 mg L−1 at TTH 1.9 mg L−1 at ZMD) emerges from August to September. It is estimated that 459 and 6751 tons of DOC are transported by the river at TTH and ZMD, respectively. Although the wet deposition flux of DOC is nearly ten times higher than the river flux, riverine DOC still primarily originates from soil erosion of the basin rather than precipitation settlement. Riverine DOC fluxes are positively correlated with discharge, suggesting DOC fluxes are likely to increase in the future. Our findings highlight that permafrost degradation and glacier retreat have a great effect on DOC concentration in rivers and may become increasingly important for regional biogeochemical cycles. Text permafrost MDPI Open Access Publishing Sustainability 14 4 2441 |
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DOC groundwater precipitation river water Yangtze River |
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DOC groundwater precipitation river water Yangtze River Xiaoni You Xiangying Li Mika Sillanpää Rong Wang Chengyong Wu Qiangqiang Xu Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
topic_facet |
DOC groundwater precipitation river water Yangtze River |
description |
The carbon release and transport in rivers are expected to increase in a warming climate with enhanced melting. We present a continuous dataset of DOC in the river, precipitation, and groundwater, including air temperature, discharge, and precipitation in the source region of the Yangtze River (SRYR). Our study shows that the average concentrations of DOC in the three end-members are characterized as the sequence of groundwater > precipitation > river, which is related to the water volume, cycle period, and river flow speed. The seasonality of DOC in the river is observed as the obvious bimodal structure at Tuotuohe (TTH) and Zhimenda (ZMD) gauging stations. The highest concentration appears in July (2.4 mg L−1 at TTH and 2.1 mg L−1 at ZMD) and the secondary high value (2.2 mg L−1 at TTH 1.9 mg L−1 at ZMD) emerges from August to September. It is estimated that 459 and 6751 tons of DOC are transported by the river at TTH and ZMD, respectively. Although the wet deposition flux of DOC is nearly ten times higher than the river flux, riverine DOC still primarily originates from soil erosion of the basin rather than precipitation settlement. Riverine DOC fluxes are positively correlated with discharge, suggesting DOC fluxes are likely to increase in the future. Our findings highlight that permafrost degradation and glacier retreat have a great effect on DOC concentration in rivers and may become increasingly important for regional biogeochemical cycles. |
format |
Text |
author |
Xiaoni You Xiangying Li Mika Sillanpää Rong Wang Chengyong Wu Qiangqiang Xu |
author_facet |
Xiaoni You Xiangying Li Mika Sillanpää Rong Wang Chengyong Wu Qiangqiang Xu |
author_sort |
Xiaoni You |
title |
Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
title_short |
Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
title_full |
Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
title_fullStr |
Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
title_full_unstemmed |
Export of Dissolved Organic Carbon from the Source Region of Yangtze River in the Tibetan Plateau |
title_sort |
export of dissolved organic carbon from the source region of yangtze river in the tibetan plateau |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2022 |
url |
https://doi.org/10.3390/su14042441 |
op_coverage |
agris |
genre |
permafrost |
genre_facet |
permafrost |
op_source |
Sustainability; Volume 14; Issue 4; Pages: 2441 |
op_relation |
https://dx.doi.org/10.3390/su14042441 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/su14042441 |
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Sustainability |
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14 |
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4 |
container_start_page |
2441 |
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