Zhang Lei, Qin Yan-wen, Zheng Bing-hui, Xu De-xing
River and Coastal Environment Research Center, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Huan Jing Ke Xue. 2009 Oct 15;30(10):2884-90.
This study measures the contents of different nitrogen forms in the immerged soils and the soils of water-level-fluctuating zone of the backwater area from input river of Three Gorges Reservoir, and analyzes the relationship between nitrogen forms and environmental parameters. The results indicates that: (1) Content of TN in the surface immerged soils ranged from 436.0 to 921.6 mg/kg, and that in the soils of water-level-fluctuating zone ranged from 1253.5 to 2439.8 mg/kg. Compared with the TN content in surface immerged soils from the shallow lakes in the middle and lower reaches of Yangtze River, content of TN in the surface immerged soils is in the mid-lower level and the TN content in the soils of water-level-fluctuating zone is higher than that in the surface immerged soils. (2) Content of transferable nitrogen in the surface immerged soils ranged from 289.7 to 511.3 mg/kg, and that in the soils of water-level-fluctuating zone ranged from 271.6 to 595.1 mg/kg. Organic matter-sulfide form nitrogen (OSF-N) is the predominant form of the transferable nitrogen, whereas ion-exchangeable form nitrogen (IEF-N) is predominant in the transferable inorganic nitrogen. (3) Correlation coefficients between nitrogen forms and environmental parameters show that OSF-N is the main impact factor to increase the concentrations of total nitrogen and transferable nitrogen in the surface immerged soils and the soils of water-level-fluctuating zone. The increasing of the concentration of the transferable nitrogen is mainly from OSF-N.
本研究测定了三峡水库入库河流回水区淹没土壤及消落带土壤中不同形态氮的含量,并分析了氮形态与环境参数之间的关系。结果表明:(1)表层淹没土壤中总氮(TN)含量范围为436.0~921.6mg/kg,消落带土壤中TN含量范围为1253.5~2439.8mg/kg。与长江中下游浅水湖泊表层淹没土壤中的TN含量相比,表层淹没土壤中TN含量处于中下游水平,消落带土壤中TN含量高于表层淹没土壤。(2)表层淹没土壤中可迁移氮含量范围为289.7~511.3mg/kg,消落带土壤中可迁移氮含量范围为271.6~595.1mg/kg。有机质-硫化物形态氮(OSF-N)是可迁移氮的主要形态,而离子交换态氮(IEF-N)是可迁移无机氮中的主要形态。(3)氮形态与环境参数之间的相关系数表明,OSF-N是增加表层淹没土壤和消落带土壤中总氮和可迁移氮浓度的主要影响因素。可迁移氮浓度的增加主要来自OSF-N。