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The synergistic effect of calcium on organic carbon sequestration to ferrihydrite

机译:钙对有机碳螯合至水铁矿的协同作用

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摘要

Sequestration of organic carbon (OC) in environmental systems is critical to mitigating climate change. Organo-mineral associations, especially those with iron (Fe) oxides, drive the chemistry of OC sequestration and stability in soils. Short-range-ordered Fe oxides, such as ferrihydrite, demonstrate a high affinity for OC in binary systems. Calcium commonly co-associates with OC and Fe oxides in soils, though the bonding mechanism (e.g., cation bridging) and implications of the co-association for OC sequestration remain unresolved. We explored the effect of calcium (Ca2+) on the sorption of dissolved OC to 2-line ferrihydrite. Sorption experiments were conducted between leaf litter-extractable OC and ferrihydrite at pH 4 to 9 with different initial C/Fe molar ratios and Ca2+ concentrations. The extent of OC sorption to ferrihydrite in the presence of Ca2+ increased across all tested pH values, especially at pH ≥ 7. Sorbed OC concentration at pH 9 increased from 8.72 ± 0.16 to 13.3 ± 0.20 mmol OC g−1 ferrihydrite between treatments of no added Ca2+ and 30 mM Ca2+ addition. Batch experiments were paired with spectroscopic studies to probe the speciation of sorbed OC and elucidate the sorption mechanism. ATR-FTIR spectroscopy analysis revealed that carboxylic functional moieties were the primary sorbed OC species that were preferentially bound to ferrihydrite and suggested an increase in Fe-carboxylate ligand exchange in the presence of Ca at pH 9. Results from batch to spectroscopic experiments provide significant evidence for the enhancement of dissolved OC sequestration to 2-line ferrihydrite and suggest the formation of Fe–Ca-OC ternary complexes. Findings of this research will inform modeling of environmental C cycling and have the potential to influence strategies for managing land to minimize OM stabilization.Electronic supplementary materialThe online version of this article (10.1186/s12932-018-0049-4) contains supplementary material, which is available to authorized users.
机译:隔离环境系统中的有机碳(OC)对于缓解气候变化至关重要。有机矿物质的结合,尤其是与铁(Fe)氧化物的结合,驱动了土壤中OC螯合和稳定性的化学反应。短程铁氧化物,例如三水铁矿,对二元体系中的OC具有很高的亲和力。钙通常与土壤中的OC和Fe氧化物共缔合,尽管结合机理(例如阳离子桥联)和共缔合对OC螯合的影响仍未解决。我们探讨了钙(Ca 2 + )对溶解的OC吸附到2线亚铁水合物上的影响。在不同初始碳/铁摩尔比和Ca 2 + 浓度下,在凋落物可提取的OC和水铁矿之间的吸附实验在pH为4至9的条件下进行。在所有测试的pH值下,特别是在pH≥7的情况下,在Ca 2 + 存在下OC对水铁矿的吸附程度增加.pH 9的饱和OC浓度从8.72±0.16增加到13.3±0.20 mmol在不添加Ca 2 + 和添加30mM Ca 2 + 的处理之间,OC g -1 亚铁水合物。批处理实验与光谱研究相结合,以探测所吸收的OC的形态并阐明其吸收机理。 ATR-FTIR光谱分析表明,羧基官能团是主要吸附到三水铝石上的主要吸附OC物种,并表明在pH为9的Ca存在下,Fe-羧酸盐配体交换增加。可以将溶解的OC螯合作用增强为2线亚铁水合物,并建议形成Fe–Ca-OC三元络合物。这项研究的发现将为环境C循环建模提供参考,并有可能影响土地管理策略以最大程度地降低OM稳定性。电子补充材料本文的在线版本(10.1186 / s12932-018-0049-4)包含补充材料,其中适用于授权用户。

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