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评估磷石膏对廷托河(西班牙西南部)盐沼的影响:自然衰减过程的作用。

Assessment of phosphogypsum impact on the salt-marshes of the Tinto river (SW Spain): role of natural attenuation processes.

机构信息

Institute of Environmental Assessment and Water Research, CSIC, Jordi Girona 18, 08034 Barcelona, Spain.

出版信息

Mar Pollut Bull. 2011 Dec;62(12):2787-96. doi: 10.1016/j.marpolbul.2011.09.008. Epub 2011 Oct 10.

Abstract

About 120 Mton of phosphogypsum from the fertiliser industry were stack-piled on the salt-marshes of the Tinto river (Spain). This paper investigates the capacity of salt-marshes to attenuate contamination due to downward leaching from phosphogypsum. Solids and pore-waters were characterized at different depths of the pile to reach the marsh-ground. In superficial zones, metals were highly mobile, and no reduced sulphur was found. However, pollutant concentration decreased in the pore-water in deeper oxygen-restricted zones. Metal removal occurred by precipitation of newly formed sulphides, being this process main responsible for the contamination attenuation. Pyrite-S was the main sulphide component (up to 2528 mg/kg) and occurred as framboids, leading to high degrees of pyritization (up to 97%). The sulphidization reaction is Fe-limited; however, excess of acid-volatile sulphide over other metals cause precipitation of other sulphides, mainly of Cu and As. This decrease in metal mobility significantly minimises the impact of phosphogypsums on the salt-marshes.

摘要

约 120 万吨磷石膏来自肥料工业,被堆积在西班牙廷托河的盐沼上。本文研究了盐沼通过向下沥滤从磷石膏中减轻污染的能力。在磷石膏堆的不同深度对固体和孔隙水进行了特征描述,以到达沼泽地。在表层区域,金属具有很高的移动性,且未发现还原态硫。然而,在更深的缺氧限制区,污染物浓度在孔隙水中降低。金属的去除是通过新形成的硫化物的沉淀来实现的,这一过程是污染衰减的主要原因。黄铁矿-S 是主要的硫化物成分(高达 2528 毫克/千克),呈莓球状,导致高程度的黄铁矿化(高达 97%)。硫化反应受铁限制;然而,酸可挥发硫超过其他金属的过剩会导致其他硫化物的沉淀,主要是铜和砷。金属迁移率的这种降低显著减少了磷石膏对盐沼的影响。

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