ABSTRACT
For the first time, the dual isotope approach was applied to trace the sources of impacts and to identify the governing biogeochemical processes in a river network in the tropical deltaic region of the Red River (Vietnam). Our long term surveys concluded that water in this river network was severely impacted by anthropogenic activities. Analysis has shown strong spatio-temporal variation of nitrate isotopes; ranges of δ15N– and δ18O–
were from −5 to 15 ‰ and from −10 to 10 ‰, respectively. Average values of δ15N–
and δ18O–
in the dry season, when fertilizer is applied, were 3.54 and 3.15 ‰, respectively. In the rainy season, the values changed to 6.41 and −2.23 ‰, respectively. Denitrification and biological assimilation were active throughout the year, but were especially enhanced during fertilization time. Mineralization of domestic organic matter and consequent nitrification of mineralized
were the dominant processes, particularly during the rainy period.
Acknowledgements
Special gratitude is sent to Assoc. Prof. Nishida Kei (ICRE, University of Yamanashi, Japan) for help in the stable isotope analysis. We also thank the two anonymous reviewers for the valuable advice to improve the discussion. Appreciation is sent to Prof. Alexander Scheeline, University of Illinois, for editing this paper.
Disclosure statement
No potential conflict of interest was reported by the authors.
Notes
* Originally presented at the IAEA International Symposium on Isotope Hydrology: Revisiting Foundations and Exploring Frontiers, 11–15 May 2015, Vienna, Austria.