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Characterization of metal binding sites onto biochar using rare earth elements as a fingerprint

机译:使用稀土元素作为指纹表征生物炭上金属结合位点

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摘要

The ability of biochar to immobilize metals relies on the amount of functional groups at its surface but the contribution of each functional groups (e.g. carboxylic, phenolic) to metal bonding is poorly known. Using a new approach based on previous works on rare earth element (REE) interactions with humic substances, we aim at elucidating the relative contribution of these binding sites to metal sorption under various conditions (i.e. pH and ionic strengths, IS). Using batch experiments, REE sorption onto biochar was analyzed from pH 3 to 9 and IS 10−1 mol/L to 10−3 mol/L. Rare earth element patterns show a Middle REE (MREE) downward concavity at acidic pH and low ionic strength. These patterns are in good agreement with existing datasets quantifying REE binding with humic substances. Indeed, the MREE downward concavity displayed by REE-biochar complexation pattern compares well with REE patterns with various organic compounds. This similarity in the REE complexation pattern shapes suggests that carboxylic groups are the main binding sites of REE in biochar. Overall, our results indicate that the strength of the metal bonding with biochar increases when pH and IS increase, suggesting that biochar is more efficient for long-term metal immobilization at near neutral pH and high ionic strength.
机译:生物炭固定金属的能力取决于其表面上官能团的量,但是每个官能团(例如,羧基,酚基)对金属键的贡献却知之甚少。我们使用一种基于先前关于稀土元素(REE)与腐殖质相互作用的新方法,旨在阐明这些结合位点在各种条件下(即pH和离子强度,IS)对金属吸附的相对贡献。使用分批实验,分析了REE在生物炭上的吸附,pH值为3至9,IS 10 -1 mol / L至10 -3 mol / L。稀土元素图案在酸性pH和低离子强度下显示中等REE(MREE)向下凹度。这些模式与量化REE与腐殖质结合的现有数据集非常吻合。确实,由REE-生物炭络合模式显示的MREE向下凹度与具有各种有机化合物的REE模式相当。 REE络合模式形状的相似性表明,羧基是生物炭中REE的主要结合位点。总体而言,我们的结果表明,随着pH和IS的增加,金属与生物炭的结合强度也会提高,这表明生物炭对于在接近中性pH和高离子强度的金属长期固定更为有效。

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