长江流域资源与环境 >> 2021, Vol. 30 >> Issue (9): 2227-2235.doi: 10.11870/cjlyzyyhj202109016

• 生态环境 • 上一篇    下一篇

洱海罗时江河口湿地沉积物净氮矿化与硝化速率

李瑞琳,侯磊,袁海英,梁启斌*   

  1. (西南林业大学生态与环境学院,云南 昆明 650224)
  • 出版日期:2021-09-20 发布日期:2021-09-27

Net Nitrogen Mineralization and Nitrification Rate of Luoshijiang Estuarine Wetland Sediments in Erhai Basin

LI Rui-lin, HOU Lei, YUAN Hai-ying, LIANG Qi-bin   

  1. (College of Ecology and Environment, Southwest Forestry University, Kuming 650224, China)
  • Online:2021-09-20 Published:2021-09-27

摘要: 为探究高原湖泊河口湿地氮循环过程,以洱海罗时江河口湿地沉积物为研究对象,布设8个监测点按季度开展现场调查,分析沉积物无机氮的时空分异特征,采用PVC顶盖原位培育法分别在夏、秋季开展沉积物净氮矿化与硝化速率实验研究。结果表明:(1)湿地沉积物氨氮(NH4+ -N)、硝氮(NO 3- -N)和总氮(TN)含量分别为5.92±6.31、14.49±20.89和1 408.98±625.29 mg·kg-1,NH4+-N含量沿进水口到出水口方向呈递减趋势,且冬季显著高于其他季(P<0.05)。湿地西侧沉积物NO3- -N含量高于东侧,NO3- -N含量存在极显著的季节性差异,春季显著高于夏秋冬季(P<0.01)。(2)沉积物净氮矿化和硝化速率的变化范围分别为-0.244~0.256和-0.085~0.084 mg·kg-1·d-1,湿地进水口两个培养期的净氮矿化速率和培养期II的硝化速率显著低于其他监测点(P<0.05),而培养期I的硝化速率在湿地中部较高。净氮矿化速率大于硝化速率并形成NH4+ -N累积。河口湿地沉积物培养后的无机氮主要以NH4+-N形式存在(占NH 4+ -N和NO3--N总量的55.37%)。(3)Pearson相关分析表明,净氮矿化速率与含水率显著负相关(P<0.05),硝化速率与培养前的NO3--N含量呈极显著的正相关关系(P<0.01),而与培养前的NH 4 +-N含量显著负相关(P<0.05)。

Abstract: In order to explore the nitrogen cycle process in estuarine wetland of plateau lake, the sediments in Luoshijiang estuarine wetland of Erhai Lake was taken as the research object, and the quarterly field investigation involving 8 monitoring sites was conducted to analyze the spatial and temporal distribution of sediment nitrogen. An in-situ incubation approach with top-closed PVC tubes was carried out to study the net mineralization and nitrification rate of sediment nitrogen in summer and autumn. The results showed that: (1) The contents of ammonia nitrogen (NH4+ -N), nitrate nitrogen (NO 3--N) and total nitrogen (TN) in Luoshijiang estuarine wetland sediments were 5.92±6.31, 14.49±20.89 and 1 408.98±625.29 mg·kg-1, respectively. The content of NH4+-N showed a decreasing trend from the inlet to the outlet, and was significantly higher in winter than in others seasons (P<0.05). The contents of NO3--N in sediments showed a decreasing trend from the west to the east side of the wetland. There was a significant seasonal difference in NO 3--N content (P<0.01), which showed much higher content in spring than in other seasons. (2) The net nitrogen mineralization and nitrification rates in sediments varied from -0.244 to 0.256 and from -0.085 to 0.084 mg·kg-1·d-1, respectively. The net nitrogen mineralization rates of both cultivation period and nitrification rate of cultivation period Ⅱ at the inlet of the wetland were significantly lower than that at other monitoring sites (P<0.05). The nitrification rate of cultivation period I was higher in the middle of the wetland. The net nitrogen mineralization rate was greater than the nitrification rate and NH4+-N accumulation was formed. After the cultivation, the inorganic nitrogen mainly existed as NH4+-N in estuarine wetland sediments (i.e., 55.37% of the total amount of NH4+-N and NO3--N). (3) Pearson correlation analysis showed that the net nitrogen mineralization rate was significantly negatively correlated with water content (P<0.05). There was a highly significant positive correlation between nitrification rate and NO 3--N content before cultivation (P < 0.01), while a negative correlation between nitrification rate and NH4+-N content before cultivation (P < 0.05).

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