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Proton and Copper Binding to Humic Acids Analyzed by XAFS Spectroscopy and Isothermal Titration Calorimetry

机译:XAFS光谱和等温滴定量热法分析质子和铜与腐殖酸的结合

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摘要

Proton and copper (Cu) binding to soil and lignite-based humic acid (HA) was investigated by combining X-ray absorption fine structure (XAFS) spectroscopy, isothermal titration calorimetry (ITC), and nonideal-competitive-adsorption (NICA) modeling. NICA model calculations and XAFS results showed that bidentate and monodentate complexation occurred for Cu binding to HA. The site-type-specific thermodynamic parameters obtained by combining ITC measurements and NICA calculations revealed that copper binding to deprotonated carboxylic-type sites was entropically driven and that to deprotonated phenolic-type sites was driven by entropy and enthalpy. Copper binding to HA largely depended on the site-type and coordination environment, but the thermodynamic binding mechanisms for Cu binding to the specific site-types were similar for the different HAs studied. By comparing the site-type-specific thermodynamic parameters of HA–Cu complexation with those of low molar mass organic acids, the Cu coordination could be further specified. Bidentate carboxylic–Cu complexes made the dominating contributions to Cu binding to HA. The present study not only yields molecular-scale mechanisms of ion binding to carboxylic- and phenolic-type sites of HA but also provides the new insight that the universal nature of site-type-specific thermodynamic data enables quantitative estimation of the binding structures of heavy metal ions to humic substances.
机译:通过结合X射线吸收精细结构(XAFS)光谱,等温滴定量热法(ITC)和非理想竞争吸附(NICA)建模研究了质子和铜(Cu)与土壤和褐煤基腐殖酸(HA)的结合。 NICA模型计算和XAFS结果表明,铜与HA的结合发生了双齿和单齿络合。通过结合ITC测量和NICA计算获得的特定于位点类型的热力学参数表明,铜与去质子化的羧基型位点的结合是熵驱动的,而与去质子化的酚型位点的结合是由熵和焓驱动的。铜与HA的结合主要取决于位点类型和配位环境,但是对于不同的HA,Cu与特定位点类型结合的热力学结合机理相似。通过比较HA-Cu配合物与低摩尔质量有机酸的位点特异性热力学参数,可以进一步指定Cu配位。二元羧酸-铜络合物对铜与HA的结合起主要作用。本研究不仅产生了离子结合到HA的羧基和酚型位点的分子尺度机制,而且还提供了新的见解,即特定于位点类型的热力学数据的普遍性质使得能够定量估算重质化合物的结合结构。金属离子到腐殖质。

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  • 来源
    《Environmental Science & Technology》 |2018年第7期|4099-4107|共9页
  • 作者单位

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and the Ministry of Water Resources, Yangling, Shaanxi Province 712100, P. R. China,University of Chinese Academy of Sciences, Beijing, 100049, P. R. China;

    College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, P. R. China,Physical Chemistry and Soft Matter, Wageningen University and Research, Stippeneng 4, 6708 WE Wageningen, The Netherlands;

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and the Ministry of Water Resources, Yangling, Shaanxi Province 712100, P. R. China;

    College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, P. R. China;

    State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and the Ministry of Water Resources, Yangling, Shaanxi Province 712100, P. R. China,College of Resources and Environment, Huazhong Agricultural University, Wuhan 430070, P. R. China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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