Li Zhe, Guo Jing-Song, Fang Fang, Chen Jie, Zhang Chao, Tian Guang
Faculty of Urban Construction and Environmental Engineering, Chongqing University, Chongqing 400045, China.
Huan Jing Ke Xue. 2009 Jun 15;30(6):1588-94.
Nitrogen is one of the key nutrients for phytoplankton. Seasonal variation of different forms of nitrogen in Xiaojiang backwater area (XBA) in Three Gorges Reservoir from Mar. 2007 to Mar. 2008 was reported. It was found that average concentration of total nitrogen (TN) during the research period was (1553 +/- 43) microg x L(-1). Although remarkable seasonal variability of TN, it showed a general trend of increase of TN during the research period. Dissolved inorganic nitrogen (DIN) was the major form of nitrogen with an average concentration of (1031 +/- 32) micro x L(-1), amounted up to 66.38% in TN. The relatively high level of nitrate in DIN indicated that XBA remained a strong oxidation environment with a good self-purification generally. Mean value of the concentration of dissolved organic nitrogen (DON) and particulate organic nitrogen (PON) were (273 +/- 23) microg x L(-1) and (249 +/- 23) microg x L(-1), taking up to 26.48% and 24.15% in TN separately. However, the DON/PON ratio was only 3.63 +/- 0.93, which represented the intensive nitrogen cycling and high turnover rates. The amount of DIN in TN decreased from 80% in Mar. 2007 to 60% in Mar. 2008, which showed a trend that forms of nitrogen had been transferring from inorganic forms to organic forms. Compared to the lower slope of DIN-TN log-log linear model, the relatively high slope of TON-TN log-log linear model indicated the contribution of total organic nitrogen (TON) to TN would become significant with the increase of TN. Meanwhile, the positive correlation between NH4(+) -N/NO3(-) -N and TON/TN indicated the increase of TON in TN might contribute to a reductive environment in XBA. Nevertheless, it also showed a close relationship between ammonia and DON, but whether the ammonification of DON existed or might become the controlling process of nitrogen cycling in XBA still needs further study.
氮是浮游植物的关键营养元素之一。本文报道了三峡水库小江回水区(XBA)2007年3月至2008年3月不同形态氮的季节变化。研究发现,研究期间总氮(TN)的平均浓度为(1553±43)μg·L⁻¹。尽管TN存在显著的季节变化,但在研究期间呈现出总体上升趋势。溶解无机氮(DIN)是氮的主要形态,平均浓度为(1031±32)μg·L⁻¹,占TN的66.38%。DIN中硝酸盐含量相对较高,表明XBA总体上仍保持强氧化环境和良好的自净能力。溶解有机氮(DON)和颗粒有机氮(PON)的平均浓度分别为(273±23)μg·L⁻¹和(249±23)μg·L⁻¹,分别占TN的26.48%和24.15%。然而,DON/PON比值仅为3.63±0.93,这表明氮循环强烈且周转率高。TN中DIN的含量从2007年3月的80%降至2008年3月的60%,这表明氮的形态已从无机形态向有机形态转变。与DIN-TN对数-对数线性模型的较低斜率相比,总有机氮(TON)-TN对数-对数线性模型的相对较高斜率表明,随着TN的增加,TON对TN的贡献将变得显著。同时,NH₄⁺-N/NO₃⁻-N与TON/TN之间的正相关表明,TN中TON的增加可能有助于XBA形成还原环境。然而,这也表明氨与DON之间存在密切关系,但DON的氨化作用是否存在或可能成为XBA氮循环的控制过程仍需进一步研究。