铁
粒子(生态学)
氯化物
X射线光电子能谱
粒径
化学
无机化学
傅里叶变换红外光谱
腐植酸
水解
表面电荷
胶体
化学工程
纳米颗粒
铁酸盐
铁质
有机化学
吸附
地质学
物理化学
工程类
海洋学
肥料
作者
Joseph E. Goodwill,Yanjun Jiang,David A. Reckhow,Joseph G. Gikonyo,John E. Tobiason
标识
DOI:10.1021/acs.est.5b00225
摘要
Studies were conducted evaluating the nature of particles that result from ferrate reduction in a laboratory water matrix and in a natural surface water with a moderate amount of dissolved organic carbon. Particle characterization included size, surface charge, morphology, X-ray photoelectron spectroscopy, and transmission Fourier transform infrared spectroscopy. Characteristics of ferrate resultant particles were compared to particles formed from dosing ferric chloride, a common water treatment coagulant. In natural water, ferrate addition produced significantly more nanoparticles than ferric addition. These particles had a negative surface charge, resulting in a stable colloidal suspension. In natural and laboratory matrix waters, the ferrate resultant particles had a similar charge versus pH relationship as particles resulting from ferric addition. Particles resulting from ferrate had morphology that differed from particles resulting from ferric iron, with ferrate resultant particles appearing smoother and more granular. X-ray photoelectron spectroscopy results show ferrate resultant particles contained Fe2O3, while ferric resultant particles did not. Results also indicate potential differences in the mechanisms leading to particle formation between ferrate reduction and ferric hydrolysis.
科研通智能强力驱动
Strongly Powered by AbleSci AI