| Literature DB >> 36132886 |
Mario Alberto Gomez1,2, Ruonan Jiang1, Miao Song3, Dongsheng Li3, Alan Scott Lea4, Xu Ma5, Haibo Wang1, Xiuling Yin5, Shaofeng Wang5, Yongfeng Jia5.
Abstract
The biotic or abiotic reduction of nano-crystalline 2-line ferrihydrite (2-line FH) into more thermodynamically stable phases such as lepidocrocite-LP, goethite-GT, magnetite-MG, and hematite-HT plays an important role in the geochemical cycling of elements and nutrients in aqueous systems. In our study, we employed the use of in situ liquid cell (LC) and semi in situ analysis in an environmental TEM to gain further insights at the micro/nano-scale into the reaction mechanisms by which Fe(ii)(aq) catalyzes 2-line FH. We visually observed for the first time the following intermediate steps: (1) formation of round and wire-shaped precursor nano-particles arising only from Fe(ii)(aq), (2) two distinct dissolution mechanisms for 2 line-FH (i.e. reduction of size and density as well as breakage through smaller nano-particles), (3) lack of complete dissolution of 2-line FH (i.e. "induction-period"), (4) an amorphous phase growth ("reactive-FH/labile Fe(iii) phase") on 2 line-FH, (5) deposition of amorphous nano-particles on the surface of 2 line-FH and (6) assemblage of elongated crystalline lamellae to form tabular LP crystals. Furthermore, we observed phenomena consistent with the movement of adsorbate ions from solution onto the surface of a Fe(iii)-oxy/hydroxide crystal. Thus our work here reveals that the catalytic transformation of 2-line FH by Fe(ii)(aq) at the micro/nano scale doesn't simply occur via dissolution-reprecipitation or surface nucleation-solid state conversion mechanisms. Rather, as we demonstrate here, it is an intricate chemical process that goes through a series of intermediate steps not visible through conventional lab or synchrotron bulk techniques. However, such intermediate steps may affect the environmental fate, bioavailability, and transport of elements of such nano-particles in aqueous environments. This journal is © The Royal Society of Chemistry.Entities:
Year: 2020 PMID: 36132886 PMCID: PMC9417501 DOI: 10.1039/d0na00643b
Source DB: PubMed Journal: Nanoscale Adv ISSN: 2516-0230
Fig. 1In situ LC-TEM measurement of the dissolution of 2-line FH in 10 mM Fe(ii)(aq) at pH ∼ 6 with reaction time. The scale bar on all images is 100 nm. Refer to Movie 1† for real-time dissolution events.
Fig. 2The reacted 2-line FH in 10 mM Fe(ii)(aq) at pH ∼ 6 showing the amorphous layer on the surface of the reacted particle as determined by ED and its corresponding chemical composition via EDX.
Fig. 3(a) Shows a diffuse cloud (“aura”) of nano-particles around the reacted 2-line FH with 0.2 mM Fe(ii)(aq) at pH ∼ 6 after 48 and 96 hours. Also displayed is a selected diffuse region of the reacted particle after 48 hours. (b) Illustrates the deposition/attachment of an amorphous phase to the 2-line FH when it is reacted with 10 mM Fe(ii)(aq) at pH ∼ 6.
Fig. 4Semi in situ measurement of the dissolution of 2-line FH in (a) 10 mM Fe(ii)(aq) at pH ∼ 6 and various reaction times. The images display the dissolution process occurring through the breakage of the particles into smaller nano-particles through pores and hollow channels. (b) 0.2 mM Fe(ii)(aq) at pH ∼ 6 and various reaction times. The images display the dissolution process occurring through the breakage of the particles into smaller nano-particles as well as nano-wires and nano-whiskers coming from the surface of the reacted particles and been released.
Fig. 5The formation of lepidocrocite tabular-like crystals from small lamellae of elongated crystals after the reaction of 2-line FH with 10 mM Fe(ii)(aq) at pH ∼ 6 for 6 hours.
Fig. 6A proposed revised conceptual model for the catalytic transformation of 2-line FH by Fe(ii)(aq) at a pH ∼ 6 that includes the intermediate steps observed in this work.