State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen 361005, China.
Sci Total Environ. 2012 Aug 1;431:357-65. doi: 10.1016/j.scitotenv.2012.05.072. Epub 2012 Jun 15.
Rain storms are predicted to increase in the subtropical region due to climate change. However, the effects of storm events on riverine nitrogen (N) dynamics are poorly understood. In this study, the riverine N dynamics and storm effects in a large subtropical river (North Jiulong River, southeastern China) were investigated through continuous sampling of two storm events which occurred in June 2010 and June 2011. The results disclosed a strong linkage between N dynamics and hydrological controls and watershed characteristics. The extreme storm in June 2010 resulted in more fluctuations in N concentrations, loads, and composition, compared with the moderate storm in June 2011. There were contrasting patterns (e.g., the hysteresis effect) between nitrate and ammonium behavior in storm runoff, reflecting their different supply source and transport mechanism. Overall, nitrate supply originated from subsurface runoff and was dominated by within-channel mobilization, while ammonium was mainly from over-land sources and flushed by surface runoff. Extreme storm runoff (2010) caused a four-fold increase in dissolved inorganic N fluxes (DIN), with a greater fraction of ammonium (up to 30% of DIN) compared with the moderate storm and background flow condition (less than 15%). Storm-driven sharp increases of N loads and changes in nutrient stoichiometry (more ammonium) might have been connected with algal blooms in the adjacent estuary and Xiamen Bay. Combined with the background flow measurement of N gradients along the main river and a stream together with anthropogenic N load information, the interactive effect of hydrological and biogeochemical process on riverine N was preliminarily revealed. Current results suggested that storm runoff N was controlled by rainfall, hydrological condition, antecedent soil moisture, spatial variability of land-based N source, and damming. These findings could be used as a reference for future water quality monitoring programs and the development of a pollution mitigation strategy.
由于气候变化,预计亚热带地区的暴雨会增加。然而,暴雨事件对河流氮(N)动态的影响还不太清楚。本研究通过连续采集 2010 年 6 月和 2011 年 6 月发生的两次暴雨事件的样本,研究了中国东南部九龙河这样一个大型亚热带河流的河流水体 N 动态及其对暴雨的响应。结果表明,N 动态与水文控制和流域特征之间存在紧密联系。与 2011 年 6 月的中度暴雨相比,2010 年 6 月的极端暴雨导致 N 浓度、负荷和组成的波动更大。在暴雨径流水体中,硝酸盐和铵态氮的行为表现出明显不同的模式(例如滞后效应),反映了它们不同的供应源和输移机制。总的来说,硝酸盐的供应源自地下径流,主要受河道内部的迁移作用影响,而铵态氮主要来自陆地,被地表径流冲刷。与中度暴雨和背景流情况相比,极端暴雨径流(2010 年)导致了溶解无机 N 通量(DIN)增加了四倍,其中铵态氮的比例更大(DIN 的 30%左右),而非极端暴雨径流的 DIN 中铵态氮的比例小于 15%。暴雨导致 N 负荷急剧增加和营养化学计量比的变化(更多的铵态氮),这可能与相邻河口和厦门湾的藻类大量繁殖有关。结合沿主要河流和一条支流的背景流 N 浓度梯度的测量值以及人为 N 负荷信息,初步揭示了水文和生物地球化学过程对河流 N 的交互作用。目前的研究结果表明,暴雨径流 N 受到降雨、水文条件、前期土壤湿度、陆源 N 源的空间变异性和筑坝的控制。这些发现可以作为未来水质监测计划和污染缓解策略制定的参考。