CAS Key Laboratory of Mineralogy and Metallogeny, Guangdong Provincial Key Laboratory of Mineral Physics and Materials, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; CAS Center for Excellence in Deep Earth Science, Guangzhou 510640, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Macau University of Science and Technology, State Key Laboratory of Lunar and Planetary Sciences, Avenida Wai Long, Taipa, Macau, China.
Sci Total Environ. 2022 Sep 10;838(Pt 1):155835. doi: 10.1016/j.scitotenv.2022.155835. Epub 2022 May 10.
The surface interactions of iron (hydr)oxides with various environmental chemicals play a vital role in controlling their environmental transport and fate. As a bioessential element, phosphorus and its biogeochemical cycling are usually controlled by its adsorption on iron (hydr)oxides. Photoreductive dissolution of iron (hydr)oxides can change their surface structure and properties, but its influence on the adsorption of phosphate remains unknown. Here, an enhanced removal of phosphate during the photoreductive dissolution of ferrihydrite (Fh) was investigated. The K value of phosphate adsorption on Fh under light irradiation is evidently larger than that in the dark (21 vs 13 L/g). Zeta potential determination in combination with X-ray photoelectron spectroscopy analysis suggested that the released Fe from Fh surface during photoreductive dissolution can be oxidized to Fe, which then co-adsorb with phosphate back to Fh surface, enhancing the immobilization of phosphate on Fh. In situ ATR-FTIR results disclosed that light irradiation could further facilitate the formation of ternary complexes and surface precipitation on Fh, even after the increment of phosphate adsorption becoming negligible in the dark, and the relative content of surface precipitation increased evidently. The desorption ratio of phosphate from the irradiated Fh sample was reduced, which should be attributed to a high content of surface precipitation that can tightly bind phosphate on Fh. The findings of this study highlight an important yet previously unappreciated pathway that light irradiation can enhance the immobilization of phosphate on iron (hydr)oxides.
铁(氢)氧化物与各种环境化学物质的表面相互作用在控制其环境传输和归宿方面起着至关重要的作用。作为一种生物必需元素,磷及其地球化学循环通常受其在铁(氢)氧化物上的吸附控制。铁(氢)氧化物的光还原溶解会改变其表面结构和性质,但它对磷酸盐吸附的影响尚不清楚。本研究考察了在 Fh 的光还原溶解过程中,磷酸盐的去除得到增强。在光照下 Fh 上吸附磷酸盐的 K 值明显大于黑暗中的 K 值(21 比 13 L/g)。结合 X 射线光电子能谱分析的动电电位测定表明,Fh 表面在光还原溶解过程中释放的 Fe 可以被氧化为 Fe,然后与磷酸盐一起重新吸附到 Fh 表面,从而增强了磷酸盐在 Fh 上的固定。原位衰减全反射傅里叶变换红外光谱结果表明,即使在黑暗中磷酸盐吸附增加可忽略不计后,光照仍可以进一步促进三元配合物和表面沉淀的形成,并且表面沉淀的相对含量明显增加。从辐照 Fh 样品中解吸的磷酸盐比例降低,这归因于表面沉淀含量高,可以将磷酸盐紧密结合在 Fh 上。本研究的结果强调了一个重要但以前未被重视的途径,即光照可以增强铁(氢)氧化物对磷酸盐的固定。