...
首页> 外文期刊>Global change biology >Drought turns a Central European Norway spruce forest soil from an NO source to a transient NO sink
【24h】

Drought turns a Central European Norway spruce forest soil from an NO source to a transient NO sink

机译:干旱使挪威中部的欧洲云杉林土壤从一氧化碳来源转变为一氧化碳暂时汇

获取原文
获取原文并翻译 | 示例
           

摘要

Based on current climate scenarios, a higher frequency of summer drought periods followed by heavy rainfall events is predicted for Central Europe. It is expected that drying/rewetting events induce an increased matter cycling in soils and may contribute considerably to increased emissions of the greenhouse gas NO on annual scales. To investigate the influence of drying/rewetting events on NO emissions in a mature Norway spruce forest in the Fichtelgebirge area (NE Bavaria, Germany), a summer drought period of 46 days was induced by roof installations on triplicate plots, followed by a rewetting event of 66 mm experimental rainfall in 2 days. Three nonmanipulated plots served as controls. The experimentally induced soil drought was accompanied by a natural drought. During the drought period, the soil of both the throughfall exclusion and control plots served as an NO sink. This was accompanied by subambient NO concentrations in upper soil horizons. The sink strength of the throughfall exclusion plots was doubled compared with the control plots. We conclude that the soil water status together with the soil nitrate availability was an important driving factor for the NO sink strength. Rewetting quickly turned the soil into a source for atmospheric NO again, but it took almost 4 months to turn the cumulative soil NO fluxes from negative (sink) to positive (source) values. NO concentration and isotope analyses along soil profiles revealed that NO produced in the subsoil was subsequently consumed during upward diffusion along the soil profile throughout the entire experiment. Our results show that long drought periods can lead to drastic decreases of NO fluxes from soils to the atmosphere or may even turn forest soils temporarily to NO sinks. Accumulation of more field-scale data on soil NO uptake as well as a better understanding of underlying mechanisms would essentially advance our knowledge of the global NO budget.
机译:根据当前的气候情景,预计中欧夏季干旱发生的频率较高,随后出现强降雨事件。可以预料,干燥/再润湿事件会导致土壤中物质循环的增加,并可能在每年规模上大大增加温室气体NO的排放。为了研究干燥/再润湿事件对Fichtelgebirge地区(德国北巴伐利亚州)成熟的挪威云杉林中NO排放的影响,在三份样地上安装了屋顶,引发了46天的夏季干旱期,随后发生了重新润湿事件2天的66毫米实验降雨量。三个未操纵的地块用作对照。实验诱发的土壤干旱伴随着自然干旱。在干旱期间,贯通降雨排除区和对照区的土壤均作为NO汇。这伴随着较高的土壤层中低于环境中的NO浓度。与对照图相比,穿透瀑布排除图的下沉强度增加了一倍。我们得出的结论是,土壤水分状况以及土壤硝态氮有效性是影响NO沉降强度的重要驱动因素。重新润湿很快使土壤再次成为大气NO的来源,但是花了将近4个月才将累积的土壤NO通量从负(汇)变为正(源)值。沿土壤剖面的NO浓度和同位素分析表明,在整个实验中,沿土壤剖面向上扩散期间,地下土壤中产生的NO随后被消耗掉。我们的结果表明,长期干旱会导致NO从土壤到大气的通量急剧下降,甚至可能使森林土壤暂时变成NO汇。积累更多关于土壤NO吸收的现场规模数据以及更好地了解其潜在机制,将实质上提高我们对全球NO预算的了解。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号