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Immobilization of heavy metals in the saturated zone by sorption and in situ bioprecipitation processes

机译:通过吸附和原位生物重建方法固定饱和区中的重金属

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An ex-mining site located in Katowice, Poland, where silver, zinc and lead mining along with other activities took place for decades is now heavily contaminated with heavy metals. Especially the Quaternary and Triassic aquifers and surface water in the surrounding area are polluted. One serious risk is the threat of the contamination to drinking water, since the Triassic aquifer provides drinking water for more than 300 000 inhabitants. The main pollutants of concern are B, Ba, Zn, Cd, Cu, As and Sr. Remediation measures proposed for the Quaternary aquifer include a combination of natural attenuation, sorption barriers and in situ bioprecipitation. Dolomites, fly ash, and peat are considered as suitable adsorbent materials for removing barium and strontium from the contaminated groundwater. However, no adsorbent has been found to efficiently remove B. In situ bioprecipitation (ISBP), a process during which sulphate reducing bacteria are stimulated by the addition of various C-sources and sulphate is reduced to sulphides that concomitantly precipitate the heavy metals, has been tested on both clay and sand aquifer taken from the site. Zn and Cu, and sulphate were removed more quickly in the sandy aquifer material than in clay. In situ bioprecipitation combined with sorption was evaluated over a 150 days time period for the Triassic aquifer. Zeolites in combination with HRC or molasses gave the best results, removing 100 percent of Ba and Sr in less than 2 days and 35 percent of B after 150 days. However, no sulphate was removed under these conditions. In addition, when zeolite was combined with HRC, 100 percent Zn was removed in less than 2 days. Zn was also removed using MRC~R, lactate, and diatomic earth in combination with HRC~R or molasses. A combination of ISBP and sorption offers the potential to contain the metal contamination in this Triassic aquifer.
机译:位于波兰的Katowice的前矿业网站,在那里银,锌和铅开采以及其他活动发生了几十年,现在受重金属严重污染。特别是周围地区的第四纪和三叠纪含水层和地表水被污染。一个严重的风险是污染到饮用水的威胁,因为三叠腹含水层为300 000多名居民提供饮用水。关注的主要污染物是B,Ba,Zn,Cd,Cu,As和Sr.对于季疗管提出的修复措施包括天然衰减,吸附屏障和原位生物沉淀的组合。白云岩,粉煤灰和泥炭被认为是用于从污染地下水中除去钡和锶的合适吸附材料。然而,未发现吸附剂有效地除去B.原位生物沉淀(ISBP),通过添加各种C源和硫酸盐来刺激硫酸盐还原细菌的方法,将致癌重金属的硫化物还原为硫化物在两种粘土和砂含水层上进行了测试。在砂质含水层材料中比粘土更快地除去Zn和Cu,硫酸盐被除去。原位生物沉淀在三叠系含水层的150天时间内相结合吸附。沸石与HRC或糖蜜组合产生了最佳效果,在150天后除去少于2天,35%的Ba和Sr中的100%。但是,在这些条件下没有除去硫酸盐。另外,当沸石与HRC结合时,在少于2天内除去100%Zn。使用MRC〜R,乳酸盐和硅藻土以及HRC〜R或糖蜜组合除去Zn。 ISBP和吸附剂的组合提供了含有该三叠系含水层中的金属污染的可能性。

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