Longitudinal distribution of nitrate δ15N and δ18O in two contrasting tropical rivers: implications for instream nitrogen cycling View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2009-09

AUTHORS

Toshihiro Miyajima, Chikage Yoshimizu, Yoshie Tsuboi, Yoshiyuki Tanaka, Ichiro Tayasu, Toshi Nagata, Isao Koike

ABSTRACT

The longitudinal variations in the nitrogen (δ15N) and oxygen (δ18O) isotopic compositions of nitrate (NO3−), the carbon isotopic composition (δ13C) of dissolved inorganic carbon (DIC) and the δ13C and δ15N of particulate organic matter were determined in two Southeast Asian rivers contrasting in the watershed geology and land use to understand internal nitrogen cycling processes. The became higher longitudinally in the freshwater reach of both rivers. The also increased longitudinally in the river with a relatively steeper longitudinal gradient and a less cultivated watershed, while the gradually decreased in the other river. A simple model for the and the that accounts for simultaneous input and removal of NO3− suggested that the dynamics of NO3− in the former river were controlled by the internal production by nitrification and the removal by denitrification, whereas that in the latter river was significantly affected by the anthropogenic NO3− loading in addition to the denitrification and/or assimilation. In the freshwater-brackish transition zone, heterotrophic activities in the river water were apparently elevated as indicated by minimal dissolved oxygen, minimal δ13CDIC and maximal pCO2. The δ15N of suspended particulate nitrogen (PN) varied in parallel to the there, suggesting that the biochemical recycling processes (remineralization of PN coupled to nitrification, and assimilation of NO3−-N back to PN) played dominant roles in the instream nitrogen transformation. In the brackish zone of both rivers, the displayed a declining trend while the increased sharply. The redox cycling of NO3−/NO2− and/or deposition of atmospheric nitrogen oxides may have been the major controlling factor for the estuarine and , however, the exact mechanism behind the observed trends is currently unresolved. More... »

PAGES

243-260

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/s10533-009-9334-8

DOI

http://dx.doi.org/10.1007/s10533-009-9334-8

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1016167771


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