کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
6412379 | 1332898 | 2014 | 11 صفحه PDF | دانلود رایگان |
- NO3â and DON were the major nitrogenous compounds in Songhua Rivers.
- Low contents and isotopic values of nitrate found in rivers covering forest.
- The nitrogen mass balance and isotopic proof confirm denitrification occurring.
- Point pollution should be managed first in the rivers, Northeast China.
SummaryTo understand the sources and transformations of nitrate in the Songhua River basin, which is one of seven largest river basins in China, the concentration of dissolved nitrogenous species, nitrogen and oxygen isotopes of NO3â, nitrogen isotopes of NH4+, and stable isotopes of water were determined in this study. Low NO3â concentrations and a high dissolved organic nitrogen/total dissolved nitrogen ratio (DON/TDN) were observed in the Nen River and other rivers originating from the mountains, which are covered by forest. NO3â and DON were the major nitrogenous compounds in aquatic systems, accounting for the TDN being about 90% during high flow season and about 85% during low flow season, respectively. The nitrogen efflux for the entire basin was estimated to be approximately 1.17 Ã 105 tons/yr, which represents an annual N output of 0.21 ton/(km2 yr). The majority of the δ18O-NO3â values were between â4â° and 4â°, reflecting nitrification. During the high flow season, the isotopic compositions of NO3â and the water chemistry suggest that NO3â in the Nen River was mainly derived from soil organic nitrogen (SON), whereas NO3â in the Songhua River originated from organic nitrogen, nitrogenous fertilizers and sewage waters. NO3â in the low flow season samples generally originates from SON and sewage waters. Moreover, the calculated loss of nitrate via the mass budget in rivers, together with isotopic values and water chemistry confirm that denitrification occurs during the high flow season, especially in the Songhua River. This study suggests that the mass calculation and isotopic proof provide a better understanding for riverine N budget and biogeochemical processes.
Journal: Journal of Hydrology - Volume 519, Part A, 27 November 2014, Pages 329-339