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Characterization and Differentiation of Chemical Heterogeneity in Humic Substances by Continuous Intrinsic Proton Affinity Distribution

机译:通过连续内在质子亲和力分布表征和区分腐殖质中的化学异质性

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摘要

The chemical heterogeneity of proton binding on humic substances was studied via continuous intrinsic proton affinity distributions calculated using the condensation approximation from the master curves for two soil fulvic acids (FAs), one soil humic acid (HA) and one fulvic acid obtained from weathered coal. The master curves, i.e. plots of θ_(T,H) (the overall protonation degree) versus Hs (the proton concentration in the diffuse double layer), were obtained from potentiometric titration curves at three ionic strengths. The value of Hs was calculated using an electrical double-layer model in which the humic substances were considered as rigid impermeable spheres. For all four samples, the proton affinity distributions were characterized by a few peaks with peak positions in the range 4-5.5. The similarities and differences between the samples studied were discussed.
机译:质子结合在腐殖质上的化学非均质性是通过连续的内在质子亲和力分布来研究的,该亲和力分布是使用主曲线通过缩合近似计算出的两种土壤黄腐酸(FAs),一种土壤腐殖酸(HA)和一种风化煤制得的富里酸。从三个离子强度下的电位滴定曲线获得了主曲线,即θ_(T,H)(总质子化度)与Hs(扩散双层中的质子浓度)的关系图。使用双电层模型计算Hs值,其中将腐殖质视为刚性的不渗透球体。对于所有四个样品,质子亲和力分布的特征在于几个峰,其峰位置在4-5.5范围内。讨论了所研究的样本之间的异同。

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