Soil Erosion as a Driver of Eutrophication: An Analysis of European Lakes Using Sentinel-2 Satellite Data

IF 12 1区 环境科学与生态学 Q1 BIODIVERSITY CONSERVATION
Surya Gupta, Simon Scheper, Pasquale Borrelli, Panos Panagos, Christine Alewell
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Abstract

Soil erosion by water is a critical factor contributing to eutrophication in water bodies, acting as a significant source of nitrogen and phosphorus from land. Many models predict soil erosion and sediment transport into lakes and rivers, and the connection between soil erosion triggering eutrophication is considered textbook knowledge. However, limited data-based scientific evidence exists on the consequences of soil erosion and sediment fluxes on eutrophication. This study examines the impact of soil erosion on eutrophication, considering other covariates such as slope, elevation, phosphorus, nitrogen, flow accumulation and temperature, by analyzing zones of varying sizes around lakes in six different countries of Europe covering an area of 1596 km2: Austria (81 lakes), France (310), Germany (266), Hungary (73), Poland (465), and the United Kingdom (316). We utilized multispectral Sentinel-2 satellite remote sensing data at 20-m spatial resolution for 2021 and 2022 to estimate the Floating Algae Index (FAI) of lakes. FAI allowed us to quantify bloom occurrence (BO)—the frequency of detected algal blooms—and maximum bloom extent (MBE)—the total area affected by blooms during the study period. The MBEs were then correlated with the aforementioned covariates within zones of 100 m, 200 m, 500 m, and 1 km distance from the lakes using machine learning algorithms to identify the most significant and thus driving factors within these areas. Our results prove quantitatively that soil erosion is indeed a key driver of eutrophication for all the selected European regions except Austria. Water temperature, nutrient input, and slope are additional important drivers of lake eutrophication.

Abstract Image

土壤侵蚀是富营养化的驱动因素:基于Sentinel-2卫星数据的欧洲湖泊分析。
土壤侵蚀是水体富营养化的关键因素,是土壤氮磷的重要来源。许多模型预测了土壤侵蚀和沉积物进入湖泊和河流,土壤侵蚀引发富营养化之间的联系被认为是教科书知识。然而,关于土壤侵蚀和沉积物通量对富营养化的影响的基于数据的科学证据有限。本研究考察了土壤侵蚀对富营养化的影响,考虑了坡度、高程、磷、氮、流量积累和温度等其他共变量,通过分析欧洲六个不同国家1596平方公里的湖泊周围不同大小的区域:奥地利(81个湖泊)、法国(310个)、德国(266个)、匈牙利(73个)、波兰(465个)和英国(316个)。利用2021年和2022年20 m空间分辨率的Sentinel-2卫星多光谱遥感数据估算湖泊浮藻指数(FAI)。FAI使我们能够量化藻华发生(BO)——检测到的藻华频率——和最大华度(MBE)——研究期间受藻华影响的总面积。然后,使用机器学习算法将MBEs与距离湖泊100米、200米、500米和1公里范围内的上述协变量关联起来,以确定这些区域内最重要的驱动因素。我们的结果定量地证明,土壤侵蚀确实是除奥地利以外所有选定的欧洲地区富营养化的关键驱动因素。水温、养分输入和坡度是湖泊富营养化的重要驱动因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Global Change Biology
Global Change Biology 环境科学-环境科学
CiteScore
21.50
自引率
5.20%
发文量
497
审稿时长
3.3 months
期刊介绍: Global Change Biology is an environmental change journal committed to shaping the future and addressing the world's most pressing challenges, including sustainability, climate change, environmental protection, food and water safety, and global health. Dedicated to fostering a profound understanding of the impacts of global change on biological systems and offering innovative solutions, the journal publishes a diverse range of content, including primary research articles, technical advances, research reviews, reports, opinions, perspectives, commentaries, and letters. Starting with the 2024 volume, Global Change Biology will transition to an online-only format, enhancing accessibility and contributing to the evolution of scholarly communication.
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