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首页> 外文期刊>Chemical speciation and bioavailability >Transformation of cadmium in soils treated with Cd-enriched sewage sludge and cadmium chloride under field capacity and flooding moisture regimes
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Transformation of cadmium in soils treated with Cd-enriched sewage sludge and cadmium chloride under field capacity and flooding moisture regimes

机译:田间持水量和淹水条件下富镉污泥和氯化镉处理土壤中镉的转化

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A laboratory incubation study was conducted to examine the long-term (16 m) dynamics of transformation of Cd in soils polluted by Cd-enriched sewage sludge or cadmium chloride under field capacity (1/3 bar) and flooding moisture regimes. Cadmium transformation was investigated by determining: (i) different operationally defined chemical fractions of Cd ; (ii) DTPA extractable and (iii) 1M CaCl_2 extractable Cd. Under field capacity moisture regime, Cd added through cadmium chloride transformed into NaOAc extractable and residual Cd fractions while Cd added through Cd-enriched sludge was transformed from water soluble + exchangeable fraction into the NaOAc extractable, and organically bound, fractions in all soils and also into the residual fraction in neutral soil. Under a flooding moisture regime, Cd added through cadmium chloride transformed from water soluble + exchangeable Cd fraction into the residual fraction in acidic soil and into NaOAc extractable, and residual, fractions in alkaline soil. However, in neutral soil, residual Cd fraction underwent a small decrease to cause a minor increase in the water soluble + exchangeable, and organically bound, Cd fractions. With Cd-enriched sludge as the Cd source under a flooding moisture regime, water soluble + exchangeable Cd transformed into NaOAc extractable fraction in acidic and alkaline soils but into an organically bound fraction in neutral soil. Flooding decreased DTPA, and 1M CaCl_2 extractable, Cd in soils polluted through cadmium chloride or Cd-enriched sewage sludge as compared to the field capacity moisture regime.
机译:进行了一项实验室孵化研究,以研究在田间持水量(1/3巴)和水汽条件下,土壤中被富Cd污水污泥或氯化镉污染的土壤中Cd的长期转化动力学(16 m)。通过确定以下因素来研究镉的转化:(i)不同操作定义的Cd化学分数; (ii)可萃取的DTPA和(iii)1M CaCl_2可萃取的Cd。在田间持水量条件下,通过氯化镉添加的Cd转化为NaOAc可提取和残留的Cd馏分,而通过富含Cd的污泥添加的Cd从水溶性+可交换馏分转化为NaOAc可提取且有机结合的馏分,在所有土壤中以及进入中性土壤的残留部分。在水淹条件下,Cd通过从水溶性+可交换Cd馏分转化为氯化镉的方式添加到酸性土壤中的残留馏分中,并转化为NaOAc可提取的碱性土壤中的残留馏分。但是,在中性土壤中,残留的Cd分数略有下降,从而导致水溶性+可交换和有机结合的Cd分数略有增加。在洪水条件下,以富含Cd的污泥作为Cd来源,水溶性+可交换Cd在酸性和碱性土壤中转化为NaOAc可萃取级分,而在中性土壤中转化为有机结合级分。与田间持水量相比,淹水减少了通过氯化镉或富含镉的污水污泥污染的土壤中的DTPA和1M CaCl_2可提取的Cd。

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