The Liao River Basin is one of seven primary river Basins in China. The concentration of dissolved inorganic N (DIN), dual isotopes of NO3- using the denitrifier method, the N isotopes of NH4+ and the N flux in the basin were determined to identify the sources of N and their transformation. The results show that NO3- ranges from 0.3 mu mol/L to 1316 mu mol/L. In general, NO3- is the dominant inorganic N species during both flow seasons, but the fraction of NO3/DIN is variable and high NH4+ is present in some waters. Samples collected from the up-stream portion of the Liao River typically had N isotope values of <+8 parts per thousand, while those from the middle and lower portions had values of >+8 parts per thousand during the high flow season. Most water samples had O isotope values of <+10 parts per thousand during the high flow season. During the low flow season, the ranges of N and O isotopic values were limited, with average values of +10.3 parts per thousand and +4.9 parts per thousand, respectively. There is a wider isotopic range of NO3- during the high flow season than the low flow season. The isotopic pattern of NO3- suggests that wastewater and soil organic N are the sources of NO4+ during the high flow season, while wastewater is the main source during low flow season. It appears that no intense denitrification occurs in the river according to the isotopic and chemical data. The N flux of the Liao River system entering the Liao Dong Bay annually is nearly 7.0 x 10(4) tons, which amounts to 5.0% of the N from chemical fertilizers used in this basin. (C) 2013 Elsevier Ltd. All rights reserved.

Publication name	APPLIED GEOCHEMISTRY Volume: 36 Pages: 1-9 Published: SEP 2013
Author(s)	Yue Fu-Jun; Li Si-Liang; Liu Cong-Qiang; Zhao Zhi-Qi; Jian, Hu
Corresponding author	LI Siliang  lisiliang@vip.skleg.cn   Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Peoples R China.

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