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间歇性水流和土地利用对地中海流域有机物分解的相反影响。

Contrary effects of flow intermittence and land uses on organic matter decomposition in a Mediterranean river basin.

机构信息

Department of Evolutionary Biology, Ecology and Environmental Sciences, Universitat de Barcelona, Barcelona, Catalonia, Spain.

Department of Evolutionary Biology, Ecology and Environmental Sciences, Universitat de Barcelona, Barcelona, Catalonia, Spain; IdRA, The Water Research Institute, Universitat de Barcelona, Barcelona, Catalonia, Spain.

出版信息

Sci Total Environ. 2022 Mar 15;812:151424. doi: 10.1016/j.scitotenv.2021.151424. Epub 2021 Nov 4.

Abstract

Flow interruption in intermittent rivers (IRs) generates a mosaic of terrestrial and aquatic habitats across the river network affecting ecosystem processes, as organic matter (OM) decomposition. Water use for farming in arid and semi-arid climates intensifies the dry conditions and affects local river characteristics. In that way, flow intermittence and the distribution of land uses may affect the OM processing along the river. To understand the role of IRs in global OM dynamics and how global change affecting water flow regimes determines these dynamics, it is important to estimate OM-processing rates at a basin scale. The aim of this study was to evaluate the effect of the intensity of flow intermittence on OM processing, and how this effect was modulated by local environmental factors related to land uses across a Mediterranean river basin. To do this, wood decomposition (mass loss and fungal biomass) was selected as a functional indicator. Drying duration and frequency were measured to characterize flow intermittence in different reaches along the river, as well as local environmental factors. Linear models stablished the role of factors on decomposition. The results showed that differences in decomposition rates across the river network were negatively related to the duration of flow interruption. Dissolved inorganic nitrogen associated with agriculture counteracted the negative effect of intermittence on mass loss (increasing by up to three times); but with a higher duration of dry conditions, its effect was insignificant. An increase of 20% of canopy (higher in natural areas) resulted in increases of up to 5% of mass loss. Overall, our study is relevant to understanding the interaction between flow intermittence and land uses on OM processing, especially considering the intensification of flow intermittence and its increased distribution to other regions, which is expected to be a consequence of climate warming and human activities.

摘要

间歇性河流(IRs)中的水流中断会在整个河流网络中产生陆地和水生栖息地的镶嵌体,从而影响生态系统过程,如有机质(OM)分解。在干旱和半干旱气候下,农业用水会加剧干旱条件,并影响当地河流的特征。因此,水流间歇性和土地利用的分布可能会影响沿河流的 OM 处理。为了了解 IR 在全球 OM 动态中的作用,以及影响水流状况的全球变化如何决定这些动态,在流域尺度上估计 OM 处理速率是很重要的。本研究的目的是评估水流间歇性强度对 OM 处理的影响,以及这种影响如何被与土地利用有关的当地环境因素所调节,研究范围是一个地中海河流流域。为此,选择木材分解(质量损失和真菌生物量)作为功能指标。测量干燥时间和频率,以描述河流不同河段的水流间歇性,以及当地环境因素。线性模型确定了这些因素对分解的作用。结果表明,网络中分解速率的差异与水流中断的持续时间呈负相关。与农业相关的溶解无机氮抵消了间歇性对质量损失的负面影响(增加高达三倍);但随着干燥条件持续时间的增加,其影响变得微不足道。冠层增加 20%(自然区域更高)会导致质量损失增加高达 5%。总的来说,我们的研究对于理解水流间歇性和土地利用对 OM 处理的相互作用是有意义的,特别是考虑到水流间歇性的加剧及其在其他地区的分布增加,这预计将是气候变暖和人类活动的后果。

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