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Hexavalent Chromium Extraction from Soils: A Comparison of Five Methods

机译:从土壤中提取六价铬:五种方法的比较

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A quantitative extraction method for total Cr(Ⅵ) (soluble and insoluble forms) in soils is needed to assess potential hazards from this heavy metal to humans and ecological systems. A laboratory study was Conducted to measure native levels of Cr(Ⅵ) and recovery percentages of soluble and insoluble CrO_4~(2-) matrix spikes in four diverse soil materials following equilibration with commonly used extractants: distilled water (pH 5.7), phosphate buffer (5 mM K_2HPO_4/5 mM KH_2PO_4, pH 7.0), carbonate-hydroxide extractant (0.28 M Na_2CO_3/0.5 M NaOH; pH ≈ 11.8) with and without heating, and hydroxide solution (0.1 M NaOH; pH 13) with sonication. The heated carbonate-hydroxide solution was the most effective extractant for operationally defining total Cr(Ⅵ) in soils that contained native Cr(Ⅵ) or in soils that had a sufficiently high redox status to maintain Cr as Cr(Ⅵ). More than 90% of a soluble K_2CrO_4 spike [1.0 g of Cr(Ⅵ) kg~(-1)] was recovered using the heated carbonate-hydroxide extraction method on a redox-inert quartz sand, loamy-textured A horizon soil (Ultic Hapludalf), and chromite ore processing residue-enriched soil (HighHex COPR) containing 29% of its total Cr(Ⅵ) (1.4 g kg~(-1)) in insoluble forms. Mo Cr(Ⅵ) was recovered by any of the methods after spiking an anoxic sediment, as predicted by the reducing sonditions of this soil for Cr(Ⅵ). Lead chromate [K_(sp) 1.8 x 10~(-14)) was completely recovered by the heated carbonate-hydroxide extractant in the absence of a soil matrix, after being spiked into the loam soil containing no native Cr(Ⅵ), and after being spiked into another COPR soil (LowHex COPR) with 61% of its lative Cr(Ⅵ) in insoluble forms. In contrast, BaCrO_4 (K_(sp) 1.6 x 10~(10)) was completely recovered by the carbonate-hydroxide extractant in the absence of a soil matrix, but 63 and 78% recoveries were measured after spiking into the loam and LowHex COPR soils, respectively. Method-induced reduction of soluble Cr(Ⅵ) was not observed under the conditions of the heated alkaline extraction.
机译:需要一种定量提取土壤中总Cr(Ⅵ)(可溶和不可溶形式)的方法,以评估这种重金属对人类和生态系统的潜在危害。进行了一项实验室研究,以测量在用常用的萃取剂平衡后的四种不同土壤材料中的天然Cr(Ⅵ)水平以及可溶性和不溶性CrO_4〜(2-)基质钉的回收率:蒸馏水(pH 5.7),磷酸盐缓冲液(5 mM K_2HPO_4 / 5 mM KH_2PO_4,pH 7.0),碳酸盐-氢氧化物萃取剂(0.28 M Na_2CO_3 / 0.5 M NaOH; pH≈11.8)和超声处理的氢氧化物溶液(0.1 M NaOH; pH 13)。加热的碳酸盐-氢氧化物溶液是在操作上确定含有天然Cr(Ⅵ)的土壤或具有足够高的氧化还原状态以保持Cr为Cr(Ⅵ)的土壤中总Cr(Ⅵ)的最有效萃取剂。使用加热的碳酸盐-氢氧化物萃取方法,在氧化还原惰性石英砂,质壤密实的地平线土壤(Ultic)上回收了90%以上的可溶性K_2CrO_4峰[1.0 g Cr(Ⅵ)kg〜(-1)]。 Hapludalf)和铬铁矿矿石处理后的富残渣土壤(HighHex COPR),其不溶形式的总Cr(Ⅵ)(1.4 g kg〜(-1))占29%。如该土壤对Cr(Ⅵ)的还原态所预测的那样,在添加缺氧沉积物后,可通过任何一种方法回收Mo Cr(Ⅵ)。将铬酸铅[K_(sp)1.8 x 10〜(-14))掺入不含天然Cr(Ⅵ)的壤土中,然后在不存在土壤基质的情况下,用加热的碳酸盐-氢氧化物萃取剂完全回收。掺入另一种COPR土壤(LowHex COPR)后,其相对应的Cr(Ⅵ)的61%为不溶形式。相反,在不存在土壤基质的情况下,碳酸盐-氢氧化物萃取剂可完全回收BaCrO_4(K_(sp)1.6 x 10〜(10)),但掺入壤土和LowHex COPR后,回收率分别为63%和78%土壤。在加热的碱萃取条件下未观察到方法诱导的可溶性Cr(Ⅵ)还原。

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