氧阴离子
针铁矿
成核
铁酸盐
赤铁矿
内球面电子转移
化学
结晶学
小角X射线散射
纳米颗粒
化学工程
无机化学
透射电子显微镜
散射
材料科学
矿物学
纳米技术
物理化学
有机化学
吸附
催化作用
离子
物理
光学
工程类
作者
Alireza Namayandeh,Wei Zhang,Steven K. Watson,Olaf J. Borkiewicz,Nefeli Bompoti,Maria Chrysochoou,R. Lee Penn,F. Marc Michel
标识
DOI:10.1021/acs.est.3c09955
摘要
The presence of oxyanions, such as nitrate (NO3–) and phosphate (PO43–), regulates the nucleation and growth of goethite (Gt) and hematite (Hm) during the transformation of ferrihydrite (Fh). Our previous studies showed that oxyanion surface complexes control the rate and pathway of Fh transformation to Gt and Hm. However, how oxyanion surface complexes control the mechanism of Gt and Hm nucleation and growth during the Fh transformation is still unclear. We used synchrotron scattering methods and cryogenic transmission electron microscopy to investigate the effects of NO3– outer-sphere complexes and PO43– inner-sphere complexes on the mechanism of Gt and Hm formation from Fh. Our TEM results indicated that Gt particles form through a two-step model in which Fh particles first transform to Gt nanoparticles and then crystallographically align and grow to larger particles by oriented attachment (OA). In contrast, for the formation of Hm, imaging shows that Fh particles first aggregate and then transform to Hm through interface nucleation. This is consistent with our X-ray scattering results, which demonstrate that NO3– outer-sphere and PO43– inner-sphere complexes promote the formation of Gt and Hm, respectively. These results have implications for understanding the coupled interactions of oxyanions and iron oxy-hydroxides in Earth-surface environments.
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