Geological and Mining Institute of Spain (IGME), Spanish National Research Council (CSIC), Calle Ríos Rosas 23, 28003 Madrid, Spain.
University of the Azores, Faculty of Agricultural and Environmental Sciences, Rua Capitão João d'Ávila, 9700 Angra do Heroísmo, Açores, Portugal.
Sci Total Environ. 2022 Sep 1;837:155789. doi: 10.1016/j.scitotenv.2022.155789. Epub 2022 May 10.
Volcanic lakes in oceanic islands represent extremely important areas for biodiversity and offer exceptional conditions for nature-based tourism as one of the main pillars of economic growth in these regions. Nitrogen and phosphorus fertilizers are being used extensively at the Azores archipelago, similarly to other places in the world, to increase agricultural production and is causing severe pollution and eutrophication of surface freshwater reservoirs. This work concentrates on the evaluation of the efficiency of surface water diversion as a remediation measure to reduce nutrient loading and reverse eutrophication of Furnas crater lake on the island of São Miguel. Nutrient loading was monitored using an extensive water quality monitoring program in the main watershed of the eutrophicated lake that, together with watershed-scale mass balance methods and groundwater and solute transport models, allowed us to identify an average 98% efficiency in the reduction of nitrate loading. However, phosphorus total load in the discharged water to Furnas lake was observed to only be decreased by 33% due to the groundwater origin of phosphorus. Results from modelling suggested that nutrients were emitted from both point (nitrates) and diffuse (phosphorus) sources as surface runoff and as groundwater seepage, respectively. The results obtained recognized a partially successful surface water diversion, since groundwater path was not initially identified, thus highlighting the importance of groundwater flow regime in the design of such remediation measures. This work also provides a perspective on surface water diversion to revert eutrophication under a volcanic formation, where lakes can be naturally more nutrient rich.
大洋岛屿上的火山湖是生物多样性的极其重要区域,为以自然为基础的旅游业提供了极好的条件,而后者是这些地区经济增长的主要支柱之一。与世界其他地方一样,亚速尔群岛广泛使用氮和磷肥来增加农业产量,这导致了地表水水库的严重污染和富营养化。本工作集中评估地表水引水作为一种修复措施的效率,以减少营养物质负荷并逆转圣米格尔岛富营养化的福尔纳斯火山口湖的富营养化。使用富营养化湖泊主要流域的广泛水质监测计划监测营养物质负荷,结合流域尺度的质量平衡方法和地下水和溶质运移模型,我们能够确定硝酸盐负荷减少的平均效率为 98%。然而,由于磷的地下水来源,排入福尔纳斯湖的总磷负荷仅减少了 33%。模型结果表明,养分分别作为地表径流和地下水渗流从点源(硝酸盐)和弥散源(磷)排放。所获得的结果承认了地表水引水在扭转火山地貌下富营养化方面取得了部分成功,因为最初并未识别到地下水路径,因此凸显了地下水流动模式在设计此类修复措施中的重要性。这项工作还提供了一种在火山地貌下通过地表水引水来逆转富营养化的观点,因为在这种地貌下,湖泊可能自然更富含营养物质。