Sources and transformations of nitrate in Qixiangcuo Lake and its inflow rivers in the northern Tibetan Plateau

被引:5
|
作者
Shang, Yankai [1 ,2 ]
Wang, Fang [1 ,2 ]
Sun, Shichun [1 ]
Zhu, Boshan [1 ,2 ]
Wang, Pengfei [1 ]
机构
[1] Ocean Univ China, Key Lab Mariculture, Minist Educ, 5 Yushan Rd, Qingdao 266003, Shandong, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Funct Lab Marine Fisheries Sci & Food Prod Proc, 1 Wenhai Rd, Qingdao 266003, Shandong, Peoples R China
关键词
The Qinghai-Tibetan Plateau; Saline lake; Nitrate source; Dual nitrate isotopes; Bayesian model; Atmospheric deposition; CLIMATE-CHANGE; NITROGEN DEPOSITION; GROUND-WATER; OXYGEN; DENITRIFICATION; TEMPERATURE; SURFACE; CLASSIFICATION; FRACTIONATION; GRASSLAND;
D O I
10.1007/s11356-022-22542-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Human activities and climate change input more reactive nitrogen into alpine lakes. Alpine saline lakes are usually located in endorheic watersheds at high-altitude areas, with no other drainage methods than evaporation, and are prone to accumulate nutrients. Meanwhile, alpine saline lakes are usually oligotrophic and sensitive to reactive nitrogen inputs, and even modest reactive nitrogen inputs may have significant effects on them, such as eutrophication. Nitrate is the main form of reactive nitrogen in lakes; therefore, clarifying the sources and transformations of nitrate in alpine saline lakes is important to prevent or mitigate eutrophication in alpine saline lakes. In this study, the sources and transformations of nitrate in Qixiangcuo Lake and its inflow rivers in the northern Tibetan Plateau were identified using dual nitrate isotopes and hydrochemistry. The results show that (1) the ranges of NO3- concentrations, delta N-15-NO3, and delta O-18-NO3- values were 3.6 similar to 26.1 mu g/L, - 10.5 to + 6.0 parts per thousand, and - 10.4 to + 9.2 parts per thousand in Qixiangcuo Lake and 194.4 similar to 728.1 mu g/L, + 5.8 similar to +8.8 parts per thousand, and - 1.9 to +2.4 parts per thousand in its inflow rivers, respectively. The NO3- concentrations and delta N-15-NO3- values were significantly lower in Qixiangcuo Lake than in its inflow rivers (P < 0.05). (2) The main sources of nitrate in both surface water and bottom water of Qixiangcuo Lake were ammonium in atmospheric deposition (mean probability estimate (MPE) 41.0% and 32.2%, respectively) and livestock manure (MPE 28.9% and 21.7%, respectively). The main sources of nitrate in the inflow rivers of Qixiangcuo Lake were domestic sewage (MPE 35.7%) and livestock manure (MPE 29.6%). (3) The main nitrogen transformation process in Qixiangcuo Lake was nitrification. The conservative mixing of multiple sources controlled the nitrate concentration and isotopic composition of Qixiangcuo Lake. Improvement in grazing area planning and the installation of sewage treatment facilities are effective measures to prevent eutrophication in Qixiangcuo Lake and its inflow rivers.
引用
收藏
页码:4245 / 4257
页数:13
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