Forest Dieback Alters Nutrient Pathways in a Temperate Headwater Catchment

IF 3.2 3区 地球科学 Q1 Environmental Science
Andreas Musolff, Larisa Tarasova, Karsten Rinke, José L. J. Ledesma
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Abstract

Forested headwater catchments ensure good water quality for downstream ecosystems and human consumption. Climate change and the exacerbating likelihood of extreme events elevate the risk of severe forest dieback. However, the effects of forest dieback on the quantity and quality of stream water are not fully understood. Here, we analyse high-frequency observations of discharge, electrical conductivity (EC), dissolved organic carbon (DOC) and nitrate (NO3N) obtained before, during and after a drought-induced forest dieback in a headwater stream in the German Harz Mountains. We focus on the characteristics of concentration-discharge (C-Q) relationships at the scale of runoff events to assess the effects of forest dieback on the sources, mobilisation and pathways of EC, DOC and NO3N. When comparing pre- and post-dieback conditions, we found a significant increase in runoff efficiency and a doubling of DOC loads exported from the catchment, while DOC concentrations increased only moderately and their C-Q patterns did not change. EC exhibit no changes in concentrations but a steepening of C-Q dilution patterns. We explain these findings with a dieback-induced decrease in evapotranspiration, which leads to more intensive drainage of the upper organic soil layers in the riparian zone. In contrast, we observed a strong increase in NO3N concentrations and fluxes by a factor of ~5, while C-Q patterns at the event scale changed from enrichment to dilution. We argue that the dieback led to an excess of NO3N on the hillslopes that connect to the stream via surficial flowpaths. In this way, NO3N bypasses the riparian zone, reducing the catchment's efficiency in attenuating this nutrient. Our study emphasises the pivotal role of riparian zones in mediating water quality in headwater streams. Different configurations of the riparian zone and its connection to the hillslopes and the stream network may be a missing piece in explaining differences in water quality responses of catchments to forest dieback.

Abstract Image

森林衰退改变了温带源头汇水区的营养途径
森林覆盖的上游集水区确保了下游生态系统和人类消费的良好水质。气候变化和极端事件的日益加剧增加了森林严重枯死的风险。然而,人们对森林衰退对溪流水量和水质的影响还不完全了解。在此,我们分析了在德国哈尔茨山脉的一条源头溪流中,在干旱引发的森林衰退之前、期间和之后对排水量、导电率(EC)、溶解有机碳(DOC)和硝酸盐(NO3N)进行的高频观测。我们重点研究了径流事件尺度下浓度-排放(C-Q)关系的特征,以评估森林衰退对 EC、DOC 和 NO3N 的来源、移动和路径的影响。在比较森林退缩前后的条件时,我们发现径流效率显著提高,从集水区输出的 DOC 负荷增加了一倍,而 DOC 浓度仅略有增加,其 C-Q 模式也没有变化。EC的浓度没有变化,但C-Q稀释模式变陡。我们对这些发现的解释是,渍背引起的蒸散量减少导致河岸地带上层有机土层的排水更加密集。与此相反,我们观察到 NO3N 浓度和通量大幅增加了约 5 倍,而事件尺度上的 C-Q 模式则从富集变为稀释。我们认为,在通过表层流道与溪流相连的山坡上,土壤退化导致 NO3N 过量。这样,NO3N 就绕过了河岸带,降低了集水区消减这种营养物质的效率。我们的研究强调了河岸带在调节上游溪流水质中的关键作用。河岸带的不同构造及其与山坡和溪流网络的联系可能是解释集水区对森林衰退的水质反应差异的一个缺失部分。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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