Dirnböck Thomas, Kobler Johannes, Kraus David, Grote Rüdiger, Kiese Ralf
Environment Agency Austria, Department for Ecosystem Research and Data Information Management, Spittelauer Lände 5, 1090, Vienna, Austria.
Environment Agency Austria, Department for Ecosystem Research and Data Information Management, Spittelauer Lände 5, 1090, Vienna, Austria.
J Environ Manage. 2016 Jan 1;165:243-252. doi: 10.1016/j.jenvman.2015.09.039. Epub 2015 Oct 3.
Forest management and climate change, directly or indirectly, affect drinking water resources, both in terms of quality and quantity. In this study in the Northern Limestone Alps in Austria we have chosen model calculations (LandscapeDNDC) in order to resolve the complex long-term interactions of management and climate change and their effect on nitrogen dynamics, and the consequences for nitrate leaching from forest soils into the karst groundwater. Our study highlights the dominant role of forest management in controlling nitrate leaching. Both clear-cut and shelterwood-cut disrupt the nitrogen cycle to an extent that causes peak concentrations and high fluxes into the seepage water. While this effect is well known, our modelling approach has revealed additional positive as well as negative impacts of the expected climatic changes on nitrate leaching. First, we show that peak nitrate concentrations during post-cutting periods were elevated under all climate scenarios. The maximal effects of climatic changes on nitrate concentration peaks were 20-24 mg L(-1) in 2090 with shelterwood or clear-cut management. Second, climate change significantly decreased the cumulative nitrate losses over full forest rotation periods (by 10-20%). The stronger the expected temperature increase and precipitation decrease (in summer), the lesser were the observed nitrate losses. However, mean annual seepage water nitrate concentrations and cumulative nitrate leaching were higher under continuous forest cover management than with shelterwood-cut and clear-cut systems. Watershed management can thus be adapted to climate change by either reducing peak concentrations or long-term loads of nitrate in the karst groundwater.
森林管理和气候变化直接或间接地影响着饮用水资源的质量和数量。在奥地利北部石灰岩阿尔卑斯山的这项研究中,我们选择了模型计算(LandscapeDNDC),以解析管理与气候变化之间复杂的长期相互作用及其对氮动态的影响,以及森林土壤中硝酸盐淋溶到岩溶地下水中的后果。我们的研究突出了森林管理在控制硝酸盐淋溶方面的主导作用。皆伐和渐伐都会在一定程度上扰乱氮循环,导致渗流水出现浓度峰值和高流量。虽然这种影响是众所周知的,但我们的建模方法揭示了预期气候变化对硝酸盐淋溶的额外正面和负面影响。首先,我们表明,在所有气候情景下,采伐后时期的硝酸盐浓度峰值都会升高。到2090年,渐伐或皆伐管理下气候变化对硝酸盐浓度峰值的最大影响为20 - 24毫克/升。其次,气候变化显著降低了整个森林轮伐期内硝酸盐的累积损失(降低了10 - 20%)。预期的温度升高和降水减少(夏季)越强烈,观察到的硝酸盐损失就越少。然而,与渐伐和皆伐系统相比,连续森林覆盖管理下的年均渗流水硝酸盐浓度和硝酸盐累积淋溶量更高。因此,流域管理可以通过降低岩溶地下水中硝酸盐的峰值浓度或长期负荷来适应气候变化。