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外源铬在土壤中的形态转化
Transformations of fortified Cr in soils
【摘要】 本试验用逐级提取方法,研究了外源铬进入土壤后的形态转化,结果表明:添加到土壤小的Cr(Ⅵ)很快还以为Cr(Ⅲ)而失去其活动性,水溶态和交换态铬含量在培育6周后已恢复到对照水平,添加的Cr(Ⅲ)很快被土壤吸附和沉淀而固定,难以被H_2O和NH_4Ac提取。添加的有机结合态铬能显著提高土壤中水溶态和交换态铬含量,并能在较长时间内稳定存在于土壤中,添加污泥形式的铬进入土壤主要以残渣态、沉淀态和有机紧结合态铬为主。
【Abstract】 Abstract Cr(Ⅵ)add to soil was rapidly reduced into Cr(Ⅲ)and then convertedinto less mobile precipitation and organic-bound Cr。Cr(Ⅲ)add to soils wasrapidly absorbed and precipitated,and then converted gradually into organic-bound and residual Cr as incubation time increased。Treatment with Cr(Ⅲ)raised Cr(Ⅲ)solubility in soils following the order of EPTA-Cr>citric-Cr>fulvic-Cr>humic-Cr. Organic complexed Cr(Ⅲ)might exist in a long per-iod in soil solution, because it could not easily adsorbed and precipitatedby soils.Sludge-amended soil contained very little watersoluble and NH4Acextractable Cr. Residues,precipitation and organic-bound Cr predominatedin the soil, together accounting for about 99%or even more of the totalCr. In the incubation process, residual Cr became Organic-bound and preci-pitated gradually.
- 【文献出处】 农业环境保护 ,AGRO-ENVIRONMENTAL PROTECTION , 编辑部邮箱 ,1995年03期
- 【分类号】X53
- 【被引频次】57
- 【下载频次】549