Brown Alison M, Bass Adrian M, Skiba Ute, MacDonald John M, Pickard Amy E
UK Centre for Ecology & Hydrology (Edinburgh), Bush Estate, Penicuik, Midlothian, EH26 0QB, UK; University of Glasgow, College of Science and Engineering, School of Geographical and Earth Sciences, University Avenue, Glasgow, G12 8QQ, UK.
University of Glasgow, College of Science and Engineering, School of Geographical and Earth Sciences, University Avenue, Glasgow, G12 8QQ, UK.
Water Res. 2023 Jun 1;236:119969. doi: 10.1016/j.watres.2023.119969. Epub 2023 Apr 12.
There is growing global concern that greenhouse gas (GHG) emissions from water bodies are increasing because of interactions between nutrient levels and climate warming. This paper investigates key land-cover, seasonal and hydrological controls of GHGs by comparison of the semi-natural, agricultural and urban environments in a detailed source-to-sea study of the River Clyde, Scotland. Riverine GHG concentrations were consistently oversaturated with respect to the atmosphere. High riverine concentrations of methane (CH) were primarily associated with point source inflows from urban wastewater treatment, abandoned coal mines and lakes, with CH-C concentrations between 0.1 - 44 µg l. Concentrations of carbon dioxide (CO) and nitrous oxide (NO) were mainly driven by nitrogen concentrations, dominated by diffuse agricultural inputs in the upper catchment and supplemented by point source inputs from urban wastewater in the lower urban catchment, with CO-C concentrations between 0.1 - 2.6 mg l and NO-N concentrations between 0.3 - 3.4 µg l. A significant and disproportionate increase in all GHGs occurred in the lower urban riverine environment in the summer, compared to the semi-natural environment, where GHG concentrations were higher in winter. This increase and change in GHG seasonal patterns points to anthropogenic impacts on microbial communities. The loss of total dissolved carbon, to the estuary is approximately 48.4 ± 3.6 Gg C yr, with the annual inorganic carbon export approximately double that of organic carbon and four times that of CO with CH accounting for 0.03%, with the anthropogenic impact of disused coal mines accelerating DIC loss. The annual loss of total dissolved nitrogen to the estuary is approximately 4.03 ± 0.38 Gg N yr of which NO represents 0.06%. This study improves our understanding of riverine GHG generation and dynamics which can contribute to our knowledge of their release to the atmosphere. It identifies where action could support reductions in aquatic GHG generation and emission.
全球日益关注水体的温室气体(GHG)排放因营养水平与气候变暖之间的相互作用而增加。本文通过对苏格兰克莱德河从源头到入海口进行详细研究,比较了半自然、农业和城市环境,调查了影响温室气体排放的关键土地覆盖、季节和水文控制因素。河流中的温室气体浓度相对于大气一直处于过饱和状态。河流中高浓度的甲烷(CH₄)主要与城市污水处理、废弃煤矿和湖泊的点源流入有关,CH₄-C浓度在0.1 - 44微克/升之间。二氧化碳(CO₂)和氧化亚氮(N₂O)的浓度主要受氮浓度驱动,上游集水区以农业面源输入为主,下游城市集水区由城市污水的点源输入补充,CO₂-C浓度在0.1 - 2.6毫克/升之间,N₂O-N浓度在0.3 - 3.4微克/升之间。与半自然环境相比,夏季城市下游河流环境中所有温室气体都出现了显著且不成比例的增加,而半自然环境中温室气体浓度在冬季较高。温室气体季节性模式的这种增加和变化表明了人为因素对微生物群落的影响。河口总溶解碳的损失约为48.4±3.6吉克碳/年,无机碳的年出口量约为有机碳的两倍,是CO₂的四倍,CH₄占0.03%,废弃煤矿的人为影响加速了溶解无机碳的损失。河口总溶解氮的年损失约为4.03±0.38吉克氮/年,其中N₂O占0.06%。这项研究增进了我们对河流温室气体生成和动态的理解,有助于我们了解它们向大气中的排放情况。它确定了哪些行动可以支持减少水生温室气体的生成和排放。