Federal Institute of Triângulo Mineiro (IFTM), Uberaba Campus, Geoprocessing Laboratory, Uberaba, MG 38064-790, Brazil.
Federal Institute of Triângulo Mineiro (IFTM), Uberaba Campus, Geoprocessing Laboratory, Uberaba, MG 38064-790, Brazil.
Sci Total Environ. 2023 Sep 15;891:164426. doi: 10.1016/j.scitotenv.2023.164426. Epub 2023 May 24.
The collapse of B1 dam at the Córrego do Feijão mine of Vale, S.A., located in the Ferro-Carvão stream watershed (Brazil), released 11.7 Mm of tailings rich in iron and manganese, and 2.8 Mm entered the Paraopeba River 10 km downstream. Seeking to predict the evolution of environmental deterioration in the river since the dam break on January 25, 2019, the present study generated exploratory and normative scenarios based on predictive statistical models, and proposed mitigating measures and subsides to ongoing monitoring plans. The scenarios segmented the Paraopeba into three sectors: "anomalous" for distances ≤63.3 km from the B1 dam site, "transition" (63.3-155.3 km), and "natural" (meaning unimpacted by the mine tailings in 2019; >155.3 km). The exploratory scenarios predicted a spread of the tailings until reaching the "natural" sector in the rainy season of 2021, and their containment behind the weir of Igarapé thermoelectric plant located in the "anomalous" sector, in the dry season. Besides, they predicted the deterioration of water quality and changes to the vigor of riparian forests (NDVI index) along the Paraopeba River, in the rainy season, and a restriction of these impacts to the "anomalous" sector in the dry season. The normative scenarios indicated exceedances of chlorophyll-a in the period January 2019-January 2022, but not exclusively caused by the rupture of B1 dam as they also occurred in areas not affected by the accident. Conversely, the manganese exceedances clearly flagged the dam failure, and persist. The most effective mitigating measure is likely the dredging of the tailings in the "anomalous" sector, but currently it represents solely 4.6 % of what has entered the river. Monitoring is paramount to update the scenarios until the system enters a route towards rewilding, and must include water and sediments, the vigor of riparian vegetation, and the dredging.
位于巴西费拉雷东河(Ferro-Carvão 流域)的淡水河谷公司 B1 尾矿坝在科雷戈多菲耶诺(Córrego do Feijão)矿场崩塌,释放了 1170 万吨富含铁和锰的尾矿,其中 280 万吨进入了下游 10 公里处的帕拉奥佩巴河。自 2019 年 1 月 25 日大坝决堤以来,为了预测该河环境恶化的演变情况,本研究基于预测统计模型生成了探索性和规范性情景,并提出了缓解措施和正在进行的监测计划的沉降。这些情景将帕拉奥佩巴河分为三个区域:“异常区”(距离 B1 坝址≤63.3 公里)、“过渡区”(63.3-155.3 公里)和“自然区”(在 2019 年不受尾矿影响;>155.3 公里)。探索性情景预测尾矿将在 2021 年雨季蔓延至自然区,在旱季则被伊加拉佩热电站的堰坝阻挡在异常区。此外,它们预测了雨季帕拉奥佩巴河水质恶化和河岸森林活力(NDVI 指数)变化,以及旱季这些影响仅限于异常区。规范性情景表明,2019 年 1 月至 2022 年 1 月期间叶绿素-a 超标,但不仅仅是由 B1 大坝破裂引起的,因为在未受事故影响的地区也发生了超标现象。相反,锰超标明显标志着大坝的破裂,并持续存在。最有效的缓解措施可能是疏浚异常区的尾矿,但目前仅占进入河流尾矿的 4.6%。监测对于更新情景至关重要,直到系统进入重新野化的路径,监测必须包括水和沉积物、河岸植被活力以及疏浚情况。