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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Acid–base and copper-binding properties of three organic matter fractions isolated from a forest floor soil solution
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Acid–base and copper-binding properties of three organic matter fractions isolated from a forest floor soil solution

机译:从林地土壤溶液中分离出的三种有机物组分的酸碱和铜结合特性

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Vast amounts of knowledge about the proton- and metal-binding properties of dissolved organic matter (DOM) in natural waters have been obtained in studies on isolated humic and fulvic (hydrophobic) acids. Although macromolecular hydrophilic acids normally make up about one-third of DOM, their proton- and metal-binding properties are poorly known. Here, we investigated the acid–base and Cu-binding properties of the hydrophobic (fulvic) acid fraction and two hydrophilic fractions isolated from a soil solution. Proton titrations revealed a higher total charge for the hydrophilic acid fractions than for the hydrophobic acid fraction. The most hydrophilic fraction appeared to be dominated by weak acid sites, as evidenced by increased slope of the curve of surface charge versus pH at pH values above 6. The titration curves were poorly predicted by both Stockholm Humic Model (SHM) and NICA-Donnan model calculations using generic parameter values, but could be modelled accurately after optimisation of the proton-binding parameters (pH 6 9). Cu-binding isotherms for the three fractions were determined at pH values of 4, 6 and 9. With the optimised proton-binding parameters, the SHM model predictions for Cu binding improved, whereas the NICA-Donnan predictions deteriorated. After optimisation of Cu-binding parameters, both models described the experimental data satisfactorily. Iron(III) and aluminium competed strongly with Cu for binding sites at both pH 4 and pH 6. The SHM model predicted this competition reasonably well, but the NICA-Donnan model underestimated the effects significantly at pH 6. Overall, the Cu-binding behaviour of the two hydrophilic acid fractions was very similar to that of the hydrophobic acid fraction, despite the differences observed in proton-binding characteristics. These results show that for modelling purposes, it is essential to include the hydrophilic acid fraction in the pool of ‘active’ humic substances
机译:通过对分离的腐殖酸和富里酸(疏水性)酸的研究,已经获得了有关自然水中溶解有机物(DOM)的质子和金属结合特性的大量知识。尽管大分子亲水性酸通常占DOM的约三分之一,但它们的质子和金属结合特性却鲜为人知。在这里,我们研究了从土壤溶液中分离出来的疏水性(富维酸)酸级分和两个亲水性级分的酸碱和铜结合特性。质子滴定显示亲水性酸级分的总电荷高于疏水性酸级分的总电荷。在pH值大于6时,表面电荷与pH的关系曲线的斜率增加,证明亲水性最高的部分主要由弱酸性位点所主导。StockholmHumic Model(SHM)和NICA-Donnan均无法很好地预测滴定曲线使用通用参数值进行模型计算,但可以在优化质子结合参数(pH 6 9)之后进行精确建模。在4、6和9的pH值下确定了这三个馏分的Cu结合等温线。通过优化的质子结合参数,对SH结合的SHM模型预测有所改善,而NICA-Donnan预测却恶化了。在优化Cu结合参数后,两个模型均令人满意地描述了实验数据。铁(III)和铝与铜在pH 4和pH 6的结合位点上都竞争激烈。SHM模型可以很好地预测这种竞争,但是NICA-Donnan模型低估了pH 6的影响。总体而言,铜结合尽管在质子结合特性上存在差异,但两个亲水性酸级分的行为与疏水性酸级分的行为非常相似。这些结果表明,出于建模目的,必须将亲水性酸部分包括在“活性”腐殖质库中

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