Lake–Groundwater Biogeochemical Interactions in a River‐Delimited System: The Groundwater and Lakes Urban Observatory (GLUO)

地下水 生物地球化学循环 环境科学 低角膜缘 漫滩 水文学(农业) 生态系统 湿地 湖沼学 生物多样性 水生生态系统 地表水 自然(考古学) 湖泊生态系统 环境化学 矿化(土壤科学) 生物地球化学 溶解有机碳 稳定同位素比值 微粒 生态学 水位
作者
Marlene Dordoni,Andréas Musolff,Kay Knöeller,Luisa Coder,Martin Krauß,Yvonne Rosenlöcher,Olaf Büttner,Jörg Tittel
出处
期刊:International Review of Hydrobiology [Wiley]
卷期号:110 (2): 135-150 被引量:1
标识
DOI:10.1002/iroh.70025
摘要

ABSTRACT Preservation of urban aquatic ecosystems is of primary importance for human well‐being, biodiversity protection and the future of society. Lake–groundwater–river interactions within urban floodplains harbour intrinsic fragility, yet remain largely understudied. Appropriate environmental management can help assure the conservation of these sites through strategies that are based on physical, chemical and isotope constraints. Here we present the example of the Groundwater and Lakes Urban Observatory (GLUO) in Magdeburg, Germany, where monitoring has been carried out since 2022. Our database for the year 2023 includes data from the Elbe River, two lakes named Lake Salbker South and Lake Salbker North, and two groundwater wells. Major ion patterns point to the Elbe River and Lake Salbker South as the end‐members for water compositions within the system, although contributions from the former appear less significant. Stiff plots suggest the existence of a more saline end‐member that may receive inputs from the Zechstein Formation and drives the geochemistry of Lake Salbker South. Dissolved oxygen (DO) concentrations in Lake Salbker South during stratification show a marked depletion in the hypolimnion with values down to 1.8 mg L −1 that we attribute to mineralization of organic matter as well as oxidation of sulphur compounds. This feature acknowledges Lake Salbker South as a natural hydrogen sulphide (H 2 S) reactor. Water stable isotope compositions (δ 2 H H2O and δ 18 O H2O ) of the water bodies within the GLUO outline a trend that is compatible with moderate evaporation. We discuss that dissolution of saline deposits may also play a role. These findings emphasize the need to implement the study of lake–groundwater–river interactions within floodplains, especially when hypertrophic or sulphur‐rich water bodies are involved. Due to the inherent vulnerability and potential hazards associated to these environments, we stress the importance of establishing a multidisciplinary monitoring framework to evaluate their geochemical fluxes and ecological integrity.
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