Tian Haoting, Guo Yong, Pan Bo, Gu Cheng, Li Hui, Boyd Stephen A
†State Key Laboratory of Pollution Control and Resource Reuse, School of the Environment, Nanjing University, Nanjing 210023, P.R. China.
‡Faculty of Environmental Science and Engineering, Kunming University of Science and Technology, Kunming 650500, P.R. China.
Environ Sci Technol. 2015 Jul 7;49(13):7784-92. doi: 10.1021/acs.est.5b01026. Epub 2015 Jun 12.
A new photoreduction pathway for nitro-aromatic compounds (NACs) and the underlying degradation mechanism are described. 1,3-Dinitrobenzene was reduced to 3-nitroaniline by the widely distributed aromatic molecule indole; the reaction is facilitated by montmorillonite clay mineral under both simulated and natural sunlight irradiation. The novel chemical reaction is strongly affected by the type of exchangeable cation present on montmorillonite. The photoreduction reaction is initiated by the adsorption of 1,3-dinitrobenzene and indole in clay interlayers. Under light irradiation, the excited indole molecule generates a hydrated electron and the indole radical cation. The structural negative charge of montmorillonite plausibly stabilizes the radical cation hence preventing charge recombination. This promotes the release of reactive hydrated electrons for further reductive reactions. Similar results were observed for the photoreduction of nitrobenzene. In situ irradiation time-resolved electron paramagnetic resonance and Fourier transform infrared spectroscopies provided direct evidence for the generation of hydrated electrons and the indole radical cations, which supported the proposed degradation mechanism. In the photoreduction process, the role of clay mineral is to both enhance the generation of hydrated electrons and to provide a constrained reaction environment in the galley regions, which increases the probability of contact between NACs and hydrated electrons.
本文描述了一种新的硝基芳香族化合物(NACs)光还原途径及其潜在的降解机制。广泛分布的芳香分子吲哚可将1,3-二硝基苯还原为3-硝基苯胺;在模拟阳光和自然阳光照射下,蒙脱石粘土矿物均可促进该反应。蒙脱石上存在的可交换阳离子类型对这种新的化学反应有很大影响。光还原反应由1,3-二硝基苯和吲哚在粘土夹层中的吸附引发。在光照下,受激的吲哚分子产生水合电子和吲哚自由基阳离子。蒙脱石的结构负电荷可能稳定了自由基阳离子,从而防止电荷复合。这促进了活性水合电子的释放,以进行进一步的还原反应。硝基苯的光还原也观察到了类似结果。原位辐照时间分辨电子顺磁共振和傅里叶变换红外光谱为水合电子和吲哚自由基阳离子的产生提供了直接证据,支持了所提出的降解机制。在光还原过程中,粘土矿物的作用是增强水合电子的产生,并在层间区域提供一个受限的反应环境,这增加了NACs与水合电子接触的概率。