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首页> 外文期刊>Environmental Monitoring and Assessment >Concentration of essential and toxic elements as a function of the depth of the soil and the presence of fulvic acids in a wetland in Cerrado, Brazil
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Concentration of essential and toxic elements as a function of the depth of the soil and the presence of fulvic acids in a wetland in Cerrado, Brazil

机译:作为土壤深度的浓度和有毒元素的函数以及巴西的湿地在湿地中存在富含紫外酸的存在

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摘要

The protection of wetlands is essential for sustainable development. The particular hydrology of wetlands creates conditions for the formation of hydric soils. Hydric soils are formed in oxide-reducing environments and perform important removal and re-oxidation of Fe and Mn oxides and hydroxides. They are also characterized by the formation of a superficial horizon enriched by the accumulation of organic matter. The objective of this study was to determine the concentration of essential (Co, Cu, Fe, Mn, Ni, Zn) and toxic (Al, Cd, Pb) elements in the soil solution in a wetland, surrounded by an intense agricultural activity area. The concentrations of the elements were evaluated according to the level of hydromorphy (border to the center) and the depth of the soil. The physical fractionation of these elements was also assessed (total and 30 kDa), and the results were compared with the chemical speciation of these elements. Despite the high total concentrations of Al and Fe, the concentration of these elements was very low in the 30 kDa fraction, which suggests that these elements are complexed with organic matter, in the form of hydroxides. Evidence of removal of Fe and Mn from the surface horizon was observed at the center of the wetland, where the highest level of hydromorphy is found. The results showed that the concentration of metals in the fraction 30 kDa is insignificant, suggesting that the mechanisms of precipitation and/or adsorption to soil colloids play an important role in the regulation of this ecosystem.
机译:保护湿地对可持续发展至关重要。湿地的特定水文产生了形成液体土壤的条件。液体土壤形成在氧化物还原环境中,并进行重要的去除和再氧化Fe和Mn氧化物和氢氧化物。它们的特征还在于形成富集的有机物质积累的肤浅的地平线。本研究的目的是确定湿地中土壤溶液中的必需(Co,Cu,Fe,Mn,Ni,Zn)和有毒(Al,Cd,Pb)元素的浓度,被激烈的农业活动区域包围。根据湿润的水平(边界到中心)和土壤深度来评估元素的浓度。还评估了这些元素的物理分离(总和30kDa),并将结果与​​这些元素的化学物质进行了比较。尽管Al和Fe的总浓度高,但这些元素的浓度在&lt中非常低。 30 KDA级分,这表明这些元素以氢氧化物形式与有机物质复杂化。在湿地的中心观察到从表面地平线中除去Fe和Mn的证据,发现最高水平的湿润。结果表明,馏分中的金属浓度& 30 KDA是微不足道的,这表明对土壤胶体的沉淀和/或吸附机制在该生态系统的调节中起着重要作用。

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