IVL Swedish Environmental Research Institute, Box 53021, SE-40014, Gothenburg, Sweden; Global Change Research Institute CAS, Bělidla 986/4a, 603 00, Brno, Czech Republic.
IVL Swedish Environmental Research Institute, Box 53021, SE-40014, Gothenburg, Sweden.
Environ Pollut. 2018 Nov;242(Pt A):367-374. doi: 10.1016/j.envpol.2018.06.093. Epub 2018 Jul 2.
Chronic high deposition of nitrogen (N) to forest ecosystems can lead to increased leaching of inorganic N to surface waters, enhancing acidification and eutrophication. For 26 years nitrogen has been added as ammonium nitrate (NHNO) at 40 kg N ha yr to a whole forested catchment ecosystem at Gårdsjön, Sweden, to experimentally simulate the transition from a N-limited to N-rich state. Over the first 10 years of treatment there was an increasing amount of nitrate (NO) and to a lesser extent ammonium (NH) lost in runoff, but then N leaching stabilised, and for the subsequent 16 years the fraction of N added lost in runoff remained at 9%. NO concentrations in runoff were low in the summer during the first years of treatment, but now are high throughout the year. High frequency sampling showed that peaks in NO concentrations generally occurred with high discharge, and were enhanced if high discharge coincided with occasions of N addition. Approximately 50% of the added N has gone to the soil. The added N is equivalent to 140 years of ambient N deposition. At current ambient levels of N deposition there thus appears to be no immediate risk of N saturation at this coniferous forest ecosystem, and by inference to other such N-limited forests in Scandinavia.
慢性高浓度氮(N)在森林生态系统中的沉积会导致更多的无机 N 淋溶到地表水中,从而加剧酸化和富营养化。在瑞典的加德松,26 年来,人们一直以硝酸铵(NHNO)的形式向整个森林流域生态系统添加 40 公斤/公顷/年的氮,以实验模拟从 N 限制状态向 N 丰富状态的转变。在处理的最初 10 年内,径流水流失的硝酸盐(NO)和氨(NH)的数量不断增加,但随后氮淋溶稳定下来,在随后的 16 年里,径流水流失的添加氮的比例保持在 9%。在处理的最初几年,夏季径流水的硝酸盐浓度较低,但现在全年都很高。高频采样显示,NO 浓度峰值通常与高流量同时出现,如果高流量与氮添加的时间吻合,浓度峰值会更高。大约 50%的添加氮进入土壤。添加的氮相当于 140 年的自然氮沉积。因此,在当前的自然氮沉积水平下,这个针叶林生态系统似乎没有立即达到氮饱和的风险,由此推断,斯堪的纳维亚其他类似的氮限制森林也没有这种风险。