巴西铁四合院流域河流沉积物中金属的流动性

L. Marques, D. Reis, Laura Pereira do Nascimento, E. G. Oliveira, A. Santiago, H. Roeser
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引用次数: 5

摘要

近年来,淡水环境中金属行为的动力学一直是环境监测的主要焦点之一。本研究调查了Santa Bárbara河流域(巴西米纳斯吉拉斯)河流沉积物中重金属的分布。研究区域面临着与采矿和一些高影响活动有关的问题,如农业、林业和木炭生产的重新造林。在Conceição河、Caraça河和Santa Bárbara河的四个点收集了表层沉积物。通过欧洲共同体参考局(BCR)提出的顺序提取程序,分析了这些沉积物的交换性、可还原性、可氧化性和残留部分。结果表明,Cd和Pb主要存在于可还原部分,而Fe、Ni、Cr和Zn主要存在于残余部分,Mn和Cu是按比例呈现更多可交换部分和更大迁移率的元素。pH和氧化还原电位等因素会影响几种改变金属迁移率的过程,如吸附和络合。这些参数的值表明采样点具有还原性和酸性特征。通过识别沉积物中金属的地球化学阶段,可以理解介质中的污染并识别可能的来源。这使得能够评估所研究流域的沉积物质量,并可作为监测人类对环境影响的参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mobility of metals in river sediments from a watershed in the Iron Quadrangle, Brazil
The dynamics of the behavior of metals in freshwater environments has been one of the main focuses of environmental monitoring in the last years. The present study investigated the distribution of heavy metals in the river sediments of the Santa Bárbara River Watershed (Minas Gerais, Brazil). The study area suffered from problems related to mining and several high impact activities, such as farming, forestry, and reforestation for charcoal production. Surface sediments were collected at four points in the Conceição, Caraça, and Santa Bárbara rivers. These sediments were analyzed for exchangeable, reducible, oxidizible, and residual fractions through the sequential extraction procedure that was proposed by the European Community Bureau of Reference (BCR). The results indicate that the Cd and Pb are mostly present in the reducible fraction, while Fe, Ni, Cr, and Zn were predominantly found in the residual fraction, Mn and Cu are the elements that proportionally present more exchangeable fractions and greater mobility. Factors such as pH and redox potential influence several processes which alter the mobility of metals, such as adsorption and complexation. The values of these parameters have shown that the sampled points have reducing and acidic characteristics. The identification of the geochemical stages of metals in sediments allowed for the comprehension of the contamination in the medium and the identification of possible sources. This enables the assessment of the quality of the sediments in the studied watershed and serves as a reference for the monitoring of the anthropic effect to the environment.
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