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Effect of humic substances on Cu(II) solubility in kaolin-sand soil

机译:腐殖质对高岭土砂土中Cu(II)溶解度的影响

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The type and amount of organic matter present in industrially contaminated soils will influence the risk they pose. Previous studies have shown the importance of humic and fulvic acids (FAs) (important components of soil organic matter) in increasing the solubility of toxic metals but were not carried out using toxic metal levels and the pH range typical of industrially contaminated soils. This study investigated the influence of three humic substances (HSs: humates, fulvates and humins) on the solubility of copper(II) ions in kaolinitic soil spiked with Cu at levels representative of industrially contaminated soil. Humates, fulvates and humin were extracted from Irish moss peat, and controlled pH batch leaching tests were conducted on an artificial kaolin-sand soil that was spiked with each. Further leaching tests were conducted on soil spiked with each HS and copper nitrate. Dissolved organic contents were determined by titration and total and free aqueous copper concentrations in the leachate were measured using AAS and ion selective electrode (ISE) poten-tiometry respectively (dissolved complexed copper levels were determined by difference). It was found that humates and fulvates are partially sorbed by the soil, probably by chemisorption on positively charged gibbsite (Al-hydroxide) sites in the kaolinite. The addition of 340 mg/kg Cu(II) ions did not significantly affect the amount of humate or fulvate sorbed. Dissolved humates and fulvates form soluble complexes with copper over the pH range 3-11. However, in the presence of kaolinite, soluble copper humates and fulvates are unable to compete with the kaolinite for Cu ions at pH 6-7. Above pH 8, humate and fulvate complexes are the only forms of dissolved Cu. Humin is largely insoluble and has little effect on Cu mobility between pH 2 and 12. The implication of this study is that measurement of total soil organic content and water leaching tests should be a standard part of contaminated site investigation.
机译:工业污染土壤中有机物的类型和数量将影响其构成的风险。先前的研究表明,腐殖酸和富里酸(FAs)(土壤有机质的重要成分)在增加有毒金属的溶解度方面的重要性,但并未使用有毒金属水平和工业污染土壤的典型pH范围进行。这项研究调查了三种腐殖质(腐殖酸盐,腐殖酸盐和腐殖质)对铜(II)离子在以工业污染土壤为代表的加标铜的高岭土中的溶解度的影响。从爱尔兰苔藓泥炭中提取腐殖质,腐殖质和腐殖质,并在人工掺加高岭土砂土的土壤上进行受控的pH分批浸出试验。在掺有每种HS和硝酸铜的土壤上进行了进一步的浸出试验。通过滴定法确定溶解的有机物含量,并分别使用AAS和离子选择电极(ISE)电位测定法测量渗滤液中的总铜和游离铜的浓度(通过差异确定溶解的络合铜含量)。已发现腐殖酸盐和富夫酸盐被土壤部分吸附,可能是通过化学吸附在高岭石中带正电的菱铁矿(氢氧化铝)上。添加340 mg / kg的Cu(II)离子不会显着影响所吸收的腐殖酸盐或草酸盐的量。在3-11的pH范围内,溶解的腐殖酸盐和fulvates与铜形成可溶性络合物。但是,在高岭石的存在下,可溶性铜腐殖酸盐和富铝酸盐不能与高岭石竞争pH为6-7的Cu离子。 pH高于8时,腐殖酸盐和富草酸盐络合物是溶解的Cu的唯一形式。腐殖质很大程度上不溶,对pH在2和12之间的Cu迁移率几乎没有影响。这项研究的含义是,土壤总有机物含量的测定和水浸出试验应成为污染场地调查的标准部分。

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