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Thermal and Photoinduced Reduction of Ionic Au(III) to Elemental Au Nanoparticles by Dissolved Organic Matter in Water: Possible Source of Naturally Occurring Au Nanoparticles

机译:水中溶解的有机物热和光诱导将离子Au(III)还原为元素Au纳米颗粒:天然存在的Au纳米颗粒的可能来源

摘要

Naturally occurring Au nanoparticles (AuNPs) have been widely observed in ore deposits, coal, soil, and environmental water. Identifying the source of these naturally occurring AuNPs could be helpful for not only the discovery of Au deposits through advanced exploration methods, but also the elucidation of the biogeochemical cycle and environmental toxicity of ionic Au and engineered AuNPs. Here, we investigated the effect of natural/simulated sunlight and heating on the reduction of ionic Au by ubiquitous dissolved organic matter (DOM) in river water. The reductive process probed by X-ray photoelectron spectroscopy revealed that phenolic, alcoholic, and aldehyde groups in DOM act as reductive sites. Long-time exposure with thermal and photoirradiation induced the further fusion and growth of AuNPs to branched Au nanostructure as precipitation. The formation processes and kinetics of AuNPs were Further investigated using humic acid (HA) as the DOM model, with comprehensive characterizing methods. We have observed that HA can reduce ionic Au(III) complex (as chloride or hydroxyl complex) to elemental Au nanoparticles under sunlight or heating. In this process, nearly all of the Au(III) could be reduced to AuNPs, in which HA serves as not only the reductive agent, but also the coating agent to stabilize and disperse AuNPs. The size and stability of AuNPs were highly dependent on the concentration ratio of Au(III) to HA. These results imply that, besides biological processes, this thermal or photochemical reduction process is another possible source of naturally occurring AuNPs in natural environments, which possibly has critical impacts on the transport and transformation of Au and engineered AuNPs.
机译:天然金金纳米颗粒(AuNPs)已在矿床,煤,土壤和环境水中广泛观察到。鉴定这些天然存在的AuNPs的来源不仅有助于通过先进的勘探方法发现Au矿床,而且有助于阐明离子Au和工程AuNPs的生物地球化学循环和环境毒性。在这里,我们研究了自然/模拟阳光和加热对河水中普遍存在的溶解有机物(DOM)还原离子Au的影响。 X射线光电子能谱探测的还原过程表明,DOM中的酚,醇和醛基充当还原位点。长时间暴露于热和光辐照下会诱导AuNPs进一步融合和生长,形成沉淀的分支Au纳米结构。以腐殖酸(HA)为DOM模型,进一步研究了AuNPs的形成过程和动力学,并采用了全面的表征方法。我们已经观察到,HA可以在阳光或加热下将离子性Au(III)络合物(如氯化物或羟基络合物)还原为元素Au纳米颗粒。在此过程中,几乎所有的Au(III)都可以还原为AuNPs,其中HA不仅充当还原剂,而且还充当稳定和分散AuNPs的涂层剂。 AuNPs的大小和稳定性高度依赖于Au(III)与HA的浓度比。这些结果表明,除了生物过程之外,这种热还原或光化学还原过程是自然环境中天然存在的AuNP的另一种可能来源,这可能对Au和工程AuNP的运输和转化产生关键影响。

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