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自然过程和人为压力的沉积物源指纹:有助于管理受 B1 尾矿坝溃坝影响的帕拉奥佩巴河流域。

Sediment source fingerprints of natural processes and anthropogenic pressures: A contribution to manage the Paraopeba River basin impacted by the B1 tailings dam collapse.

机构信息

University of Vigo, Agroforestry Group, School of Forestry Engineering, 36005, Pontevedra, Spain; Inov4Agro/Centro de Investigação e Tecnologias Agroambientais e Biológicas, Universidade de Trás-os-Montes e Alto Douro, Ap 1013, 5001-801, Vila Real, Portugal.

Instituto Federal do Triângulo Mineiro, Campus Uberaba, Laboratório de Geoprossessamento, Uberaba, MG, 38064-790, Brazil.

出版信息

J Environ Manage. 2024 Apr;356:120590. doi: 10.1016/j.jenvman.2024.120590. Epub 2024 Mar 23.

DOI:10.1016/j.jenvman.2024.120590
PMID:38522281
Abstract

Understanding the origins of sediment transport in river systems is crucial for effective watershed management, especially after catastrophic events. This information is essential for the development of integrated strategies that guarantee water security in river basins. The present study aimed to investigate the rupture of the B1 tailings dam of the Córrego do Feijão mine, which drastically affected the Brumadinho region (Minas Gerais, Brazil). To address this issue, a confluence-based sediment fingerprinting approach was developed through the SedSAT model. Uncertainty was assessed through Monte Carlo simulations and Mean Absolute Error (MAE). Estimates of the overall average contributions of each tributary were quantified for each station and annually during the period 2019-2021. It was observed that the sampling point PT-09, closest to the dam breach, contributed to almost 80% of the Paraopeba River in 2019. Despite the dredging efforts, this percentage increased to 90% in 2020 due to the need to restore the highly degraded area. Additionally, the main tributaries contributing to sediment increase in the river are Manso River "TT-03" (almost 36%), associated with an area with a high percentage of urban land use, and Cedro stream "TT-07" (almost 71%), whose geology promotes erosion, leading to higher sediment concentration. Uncertainties arise from the limited number of available tracers, variations caused by dredging activities, and reduced data in 2020 due to the pandemic. Parameters such as land use, riparian vegetation degradation, downstream basin geology, and increased precipitation are key factors for successfully assessing tributary contributions to the Paraopeba River. The obtained results are promising for a preliminary analysis, allowing the quantification of key areas due to higher erosion and studying how this disaster affected the watershed. This information is crucial for improving decision-making, environmental governance, and the development of mitigating measures to ensure water security. This study is pioneering in evaluating this methodology in watersheds affected by environmental disasters, where restoration efforts are ongoing.

摘要

了解河流系统中泥沙输移的成因对于有效的流域管理至关重要,特别是在灾难性事件发生之后。这些信息对于制定综合战略至关重要,这些战略可确保流域的水安全。本研究旨在调查巴西米纳斯吉拉斯州布鲁马迪纽地区的铁矿尾矿坝 B1 溃坝事件。为了解决这个问题,我们通过 SedSAT 模型开发了一种基于汇流的泥沙示踪剂方法。通过蒙特卡罗模拟和平均绝对误差(MAE)评估了不确定性。量化了每个支流在每个站点和每年(2019-2021 年)对整个流域的平均贡献。结果表明,最接近坝口的采样点 PT-09 在 2019 年对帕拉奥佩巴河的贡献近 80%。尽管进行了疏浚,但由于需要恢复高度退化的区域,这一比例在 2020 年增加到 90%。此外,导致河流中泥沙增加的主要支流是曼索河“TT-03”(近 36%),与城市土地利用比例较高的地区相关,以及塞德罗河“TT-07”(近 71%),其地质促进了侵蚀,导致更高的泥沙浓度。不确定性源于可用示踪剂数量有限、疏浚活动造成的变化以及 2020 年因大流行导致的数据减少。土地利用、河岸植被退化、下游流域地质和降水增加等参数是成功评估支流对帕拉奥佩巴河贡献的关键因素。获得的结果对于初步分析是有希望的,可以量化由于侵蚀加剧的关键区域,并研究这场灾难如何影响流域。这些信息对于改善决策、环境治理和制定缓解措施以确保水安全至关重要。本研究在评估受环境灾害影响的流域中的这种方法方面具有开创性,这些流域正在进行恢复工作。

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