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Effects of organic acids on Cd adsorption and desorption by two anthropic soils

机译:有机酸对两种人类土壤中镉吸附和解吸的影响

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摘要

The objective of this experiment was to study the effects of malic, tartaric, oxalic, and citric acid on the adsorption and desorption characteristics of Cd by two typical anthropic soils (lou soil and irrigation-silted soil) in North-west China. Cadmium adsorption and desorption were studied under a range of temperatures (25℃, 30℃, 35℃, 40℃), organic acid concentrations (0.5-5.0 mmol-L~(-1)), and pH values (2-8). The results showed that the Cd adsorption capacity of the lou soil was significantly greater than that of the irrigation-silted soil. Generally, Cd adsorption increased as the temperature increased. In the presence of NaNO_3, the adsorption of Cd was endothermic with △H values of 31.365 kJ · mol~(-1) for lou soil and 28.278 kJ·mol~(-1) for irrigation-silted soil. The endothermic reaction indicated that H bonds were the main driving force for Cd adsorption in both soils. However, different concentrations of organic acids showed various influences on the two soils. In the presence of citric acid, chemical adsorption and van der Waals interactions were the main driving forces for Cd adsorption rather than H bonds. Although the types of organic acids and soil properties were different, the effects of the organic acids on the adsorption and desorption of Cd were similar in the two soils. The adsorption percentage of Cd generally decreased as organic acid concentrations increased. In contrast, the adsorption percentage increased as the pH of the initial solution increased. The exception was that adsorption percentage of Cd increased slightly as oxalic acid concentrations increased. In contrast, the desorption percentage of Cd increased with increasing concentrations of organic acids but decreased as the initial solution pH increased.
机译:本实验的目的是研究苹果酸,酒石酸,草酸和柠檬酸对中国西北两种典型的人为土壤(娄土壤和灌溉淤积土壤)对镉的吸附和解吸特性的影响。在温度(25℃,30℃,35℃,40℃),有机酸浓度(0.5-5.0 mmol-L〜(-1))和pH值(2-8)范围内研究了镉的吸附和解吸。 。结果表明,the土对镉的吸附能力明显大于灌水淤积土壤。通常,Cd吸附随着温度的升高而增加。在NaNO_3存在下,镉的吸热是吸热的,土壤的△H值为31.365 kJ·mol〜(-1),灌溉淤泥土壤的△H值为28.278 kJ·mol〜(-1)。吸热反应表明,H键是两种土壤中Cd吸附的主要驱动力。但是,不同浓度的有机酸对这两种土壤都有不同的影响。在柠檬酸的存在下,化学吸附和范德华相互作用是Cd吸附而不是H键的主要驱动力。尽管有机酸的类型和土壤性质不同,但两种土壤中有机酸对Cd吸附和解吸的影响相似。 Cd的吸附百分比通常随着有机酸浓度的增加而降低。相反,随着初始溶液的pH值增加,吸附百分比增加。唯一的例外是,随着草酸浓度的增加,Cd的吸附百分比会略有增加。相反,Cd的解吸百分比随有机酸浓度的增加而增加,但随着初始溶液pH值的增加而降低。

著录项

  • 来源
    《Frontiers of environmental science & eng》 |2013年第1期|19-30|共12页
  • 作者单位

    College of Resources and Environment, Northwest A&F University, Yangling 712100, China,Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling 712100, China;

    College of Resources and Environment, Northwest A&F University, Yangling 712100, China,Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling 712100, China;

    College of Resources and Environment, Northwest A&F University, Yangling 712100, China,Key Laboratory of Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling 712100, China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    adsorption; desorption; cadmium; organic acids; temperature; anthropic soil;

    机译:吸附解吸镉;有机酸温度;人类土壤;

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