University of Natural Resources and Life Sciences Vienna (BOKU), Institute of Soil Research, Peter Jordan-Straße 82, 1190, Vienna, Austria; Mazingira Centre, International Livestock Research Institute, Box 30709, Old Naivasha Road, 00100, Nairobi, Kenya.
Environment Agency Austria, Department for Ecosystem Research and Environmental Information Management, Spittelauer Lände 5, 1090, Vienna, Austria.
J Environ Manage. 2020 May 15;262:110338. doi: 10.1016/j.jenvman.2020.110338. Epub 2020 Feb 28.
With climate change the occurrence of summer droughts is expected to increase in Central Europe. This could lead to increased nitrate (NO) leaching when water scarcity affects the N-uptake capacity of trees and increases soil N availability due to early leaf senescence and higher litter input. In the present study, we used 16 years of ecological monitoring data from the LTER research site "Zöbelboden" in Austria. The monitoring site is a mixed Spruce-Sycamore-Ash-Beech forest on karst, which is representative for many watersheds that supply drinking water in Austria. We found that in the year after a summer drought, NO leaching via soil water seepage was significantly elevated compared to the long-term mean. While in normal years, NO leaching was primarily affected by soil water seepage volume, after a summer drought these controls changed and NO leaching was controlled by NO input via precipitation, tree N uptake, and vapor-pressure deficit. Furthermore, higher aboveground litter input during dry years was correlated with increased NO leaching in the following year. Our findings show that NO leaching from temperate mountain forests on karst is susceptible to summer drought, which could affect drinking water quality in the Central European Alps in the future, especially in combination with forest disturbances like bark beetle outbreaks, which are often a direct consequence of drought damage to trees.
随着气候变化,中欧夏季干旱的发生预计将会增加。这可能会导致硝酸盐(NO)淋失增加,因为水分短缺会影响树木的氮吸收能力,并由于早期叶片衰老和更高的凋落物输入而增加土壤氮的有效性。在本研究中,我们使用了奥地利 LTER 研究站“Zöbelboden”的 16 年生态监测数据。该监测站是一个混合云杉-梧桐-白蜡-山毛榉森林,位于喀斯特地貌上,这代表了奥地利许多供应饮用水的流域。我们发现,在夏季干旱后的一年中,通过土壤水渗漏的 NO 淋失明显高于长期平均值。而在正常年份,NO 淋失主要受土壤水渗漏量的影响,但在夏季干旱后,这些控制因素发生了变化,NO 淋失受降水、树木氮吸收和蒸气压亏缺带来的 NO 输入控制。此外,干旱年份地上凋落物输入量的增加与下一年 NO 淋失的增加有关。我们的研究结果表明,喀斯特地区温带山地森林的 NO 淋失容易受到夏季干旱的影响,这可能会影响中欧阿尔卑斯山未来的饮用水质量,特别是与森林干扰(如树皮甲虫爆发)相结合时,而这些干扰往往是树木干旱损害的直接后果。