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Titel |
Impact of human activities on organic carbon transport in the Yellow River |
VerfasserIn |
L. J. Zhang, L. Wang, W.-J. Cai, D. M. Liu, Z. G. Yu |
Medientyp |
Artikel
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Sprache |
Englisch
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ISSN |
1726-4170
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Digitales Dokument |
URL |
Erschienen |
In: Biogeosciences ; 10, no. 4 ; Nr. 10, no. 4 (2013-04-15), S.2513-2524 |
Datensatznummer |
250018200
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Publikation (Nr.) |
copernicus.org/bg-10-2513-2013.pdf |
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Zusammenfassung |
Using data from four field investigations between 2003 and 2009 along the
Yellow River mainstream, we examined the transport features and seasonal
variations of organic carbon, with a focus on contrasting the impacts of
human activities with those of natural processes. Particulate organic carbon
(POC) in the Yellow River originated mainly from the Loess Plateau, and thus
the POC content in suspended sediments was much lower than in the
world's other large rivers. Owing to both natural and human influences,
dissolved organic carbon (DOC) has only a weak correlation with discharge.
DOC varied as a result of human activities such as agricultural irrigation
and pollution in the whole basin except for the upstream Qinghai–Tibetan
Plateau. Our study also suggested that while reservoirs are a POC sink over
short periods, a long-term POC storage flux cannot be easily estimated as
discharge and sediment regulations have completely changed the relationship
between the fluxes of water, sediments, and rainfall. However, this carbon
sink can be obtained reliably through high-frequency sampling over long time
periods. In addition, the annual water and sediment regulation (WSR) scheme
has imposed an extremely severe human disturbance on the transport pattern
of river organic carbon. Our study demonstrated for the first time that in a
WSR event of less than 20 days, large proportions of the annual DOC (35%)
and POC (56%) fluxes of the Yellow River were transported to the
estuarine and coastal zone, potentially influencing estuarine and coastal
geochemistry and ecosystems profoundly. |
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