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通过XAFS光谱和等温滴定量热法分析质子和铜与腐殖酸的结合

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

作者信息

Xu Jinling, Koopal Luuk K, Fang Linchuan, Xiong Juan, Tan Wenfeng

机构信息

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.

出版信息

Environ Sci Technol. 2018 Apr 3;52(7):4099-4107. doi: 10.1021/acs.est.7b06281. Epub 2018 Mar 21.

Abstract

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.

摘要

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)模型,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,Cu与HA结合时发生了双齿和单齿络合。通过结合ITC测量和NICA计算获得的位点类型特异性热力学参数表明,铜与去质子化羧基型位点的结合是由熵驱动的,而与去质子化酚基型位点的结合是由熵和焓驱动的。铜与HA的结合很大程度上取决于位点类型和配位环境,但对于所研究的不同HA,铜与特定位点类型结合的热力学结合机制相似。通过比较HA-Cu络合的位点类型特异性热力学参数与低摩尔质量有机酸的参数,可以进一步明确铜的配位情况。双齿羧基-Cu络合物对铜与HA的结合起主要作用。本研究不仅揭示了离子与HA羧基和酚基型位点结合的分子尺度机制,还提供了新的见解,即位点类型特异性热力学数据的普遍性能够定量估计重金属离子与腐殖质的结合结构。

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