Le Yua,
Diana N. H. Tranab,
Peter Forwardc,
Martin F. Lambertd and
Dusan Losic*ab
aSchool of Chemical Engineering, The University of Adelaide, Adelaide, SA 5005, Australia. E-mail: dusan.losic@adelaide.edu.au
bARC Graphene Enabled Industry Transformation Hub, The University of Adelaide, Adelaide, SA 5005, Australia
cSA Water, South Australia 5005, Australia
dSchool of Civil, Environmental and Mining Engineering, The University of Adelaide, Adelaide, SA 5005, Australia. E-mail: martin.lambert@adelaide.edu.au
First published on 11th October 2018
Iron oxides and their hydroxides have been studied and analysed with properties of their mutual transformations under different hydrothermal conditions being indicated. Amorphous bacteria nanowires produced from biofilm waste were investigated under the influence of pH at a fixed duration (20 h) and reaction temperature (200 °C). The morphology, structure, and particle size of the transformation of hematite (α-Fe2O3) was obtained and characterised with SEM, XRD, FTIR, and particle sizer. The optimal conditions for the complete conversion of amorphous iron oxide nanowires to crystalline α-Fe2O3 is under acidic conditions where the pH is 1. The flower-like α-Fe2O3 structures have photocatalytic activity and adsorbent properties for heavy metal ions. This one-pot synthesis approach to produce α-Fe2O3 at a low cost would be greatly applicable to the recycling process of biofilm waste in order to benefit the environment.
Iron oxide (such as magnetite, Fe3O4) pigments have numerous desirable attributes as colouring agents, especially in cosmetics, as they can range in colours with high tinting strength. In addition, they are extremely stable (no fading and no bleeding) and are highly resistant. There are two major methods used to produce these iron oxides. One is to oxidize the iron metal with water and the other is to reduce hematite (Fe2O3) with hydrogen (H2) as shown in eqn (1) and (2), respectively:10
Fe + 4Fe2O3 = 3Fe3O4 | (1) |
3Fe2O3 + H2 = 2Fe3O4 + H2O | (2) |
The reduction of Fe2O3 to Fe3O4 needs to be synthesized at both elevated pressure and temperature when it is in the presence of water. Both reactions need to be performed under hydrothermal conditions.
Iron oxides and their hydroxides have been studied and analysed with indicating properties of their mutual transformations under different hydrothermal conditions. Most of their transformations are set examples of a phenomenon called topotaxy.11 This phenomenon signifies the change of one solid crystalline phase to another form. It is believed that both two phases share a fixed structural relationship with one another. Within the iron oxide system, most transformations are well known, which have been examined and analysed in rational crystallochemical methods.12 The major six crystal structures of oxides and hydroxides iron are hematite, magnetite, maghemite, wustite, goethite and lepidocrocite. They are composed of various stackings of oxygen or hydroxyl sheets combined with different arrangement of iron ions in tetrahedral or octahedral spaces.11 Therefore, this structure could impact on the properties of one another within the iron oxide system. When the sheets are stacked differently, the structure will transform and automatically rearrange with a distinct stacking formation, where each sheet will share a strong link associated with each other. For the formation of a particular iron oxide, the annealing temperature and pH during the hydrothermal process is critical as this will affect the crystal structure of the material. Table 1 summarizes the different formation requirements of each oxide and hydroxide of iron under hydrothermal conditions. However, it is unclear where the optimised conditions are for the different iron oxide formation due to the very few and inconclusive available data in the current literature whether it is the time, temperature, or pH.
Iron oxide | Colour | Crystal shape | Source | pH | Temperature | Time of reaction |
---|---|---|---|---|---|---|
Hematite | Red | Hexagonal prisms | Acidic: Fe(III) solution with Fecl3 or Fe(NO3)3 solution base: amorphous iron(III)hydroxides12 | Acidic: 1–2 base: 8–10 | Acidic >100 °C base: 100–200 °C | Acidic: several days base: - |
Goethite | Brownish reddish yellow | Needle, laths | Acidic: Ferrihydrite precursor base: amorphous iron(III)hydroxides12 | Acidic: 1–2 base: 10.5–10.87 | Acidic: room temp base: 70 °C | Acidic: 50 days base: 60 h |
Maghemite | Red to brown | Cubes | Heating synthetic lepidocrocite or synthetic magnetite | — | 250 °C | 2 h |
Magnetic | Black | Cubes | Mixed solution of Fe(III) and Fe(II) with the ratio of 2 | Base: 9–10 | 90 °C | 30–60 min |
Lepidocrocite | Reddish yellow | Laths | Slow hydrolysis of an acidic Fe(III) | Ideal at 6.7–6.9 or <7.5–8 | Room temp | 2–3 h |
To our knowledge there is no study on the hydrothermal reduction of iron oxides from Bac-FeOxs, which we present here. The aim of this work is to demonstrate for the first time the hydrothermal processing of iron oxides from biofilm waste in a ‘one-pot’ synthesis reaction. The conversion of hematite was targeted as it is the most important ore of iron. The temperature and pH of the hydrothermal process were optimised and the changes in structure were analysed. The synthesis method is simple and free of toxic wastes which can be scaled for industry.
Fig. 1 (a) Low resolution SEM image and (b) XRD spectra of purified Bac-FeOxNWs. Inset is a high-resolution SEM of the twisted nanowires indicated by the red arrow (scale bar = 3 μm). |
Fig. 2 Photographs of Bac-FeOxNWs before reaction (control) and as a function of pH (1–10) after the hydrothermal process. |
Fig. 3a displays the XRD spectra of the different crystalline forms of the Bac-FeOxNWs from pH 1 to 10. Among these curves, the sharp and intensity peaks on pH 1 confirm the highly crystalline form of iron oxide.23 The peaks that appear at 2θ = 24.2, 33.2, 35.7, 42.5, 49.5, 54.1 and 64.2° corresponds to the characteristic peaks of α-Fe2O3 (JSPDS card no. 89-2810, Fig. S2a†).15,16 The sharp intensity peaks also suggests the high purity of the iron oxide production.23 The peaks on pH 2 and 3 are slightly less intense than pH 1, but still presents the typical peaks. On the other hand, the spectra of pH 4 and pH 5 weakly displays only four of the typical peaks at 2θ = 33.2, 35.7, 42.5 and 54.1°. The less distinct and weak peaks in pH 6 and 7 (2θ = 33.2, 35.7°) shows that the pH is not ideal for the complete formation of crystalline iron oxides. At pH 8–10 the XRD peaks are also less well-defined, although there is a phase transition occurring. The successful transformation of the amorphous Bac-FeOxNWs to α-Fe2O3 is under acidic conditions at 200 °C for 20 h is greater than in alkaline conditions at the same temperature and duration. The optimal hydrothermal condition of iron oxides production is pH 1 due to the higher crystalline form obtained.
Fig. 3 (a) XRD and (b) FTIR spectra for Bac-FeOxNWs before (control) after the hydrothermal process from pH 1 to 10. |
FTIR spectra shown in Fig. 3b correlates with the findings interpreted from the XRD data. From the purified (control) and synthesised Bac-FeOxNWs curves (pH 1–10), the broad bands at 3400 cm−1 and narrow peaks at 1640 cm−1 correspond to the stretching –OH groups from the angular deformation of water.17 From pH 1–6, two typical bands at 470 cm−1 and 540 cm−1 are observed, which indicate the vibrations of metal and oxide of Fe–O, which is the form of the hematite phase (Fig. S2b†).18–20,23 However, these two peaks in Bac-FeOxNWs-pH 1, 2 and 3 are much sharper and narrower than those at pH 4–10, confirming the partial and weak transformation of the crystal iron phase. In addition, there is a medium and broad band approx. at 1080 cm−1 in both samples that may be attributed to atmospheric CO2, which commonly occurs in 20 h hydrothermal treated nano-particles.16,24 The hydrothermal process performed at pH 1–2 provide greater performance for synthesis of crystalline iron oxides.
SEM images of the synthesised Bac-FeOxNWs taken at low and high magnifications further provide evidence for the difference in the nanostructure of each hydrothermal condition. Fig. 4(a–a′) shows the complete transition from the amorphous structure into high crystalline flower-like structure. These flower-like nanostructures have well-preserved hierarchical patterns of α-Fe2O3.21,22 At high SEM magnification, the exterior of each of the nanostructure is composed of irregular sheets. This flower-like nanostructure is attributed to the presence of HCl in the solution. During the reduction process, iron oxide and HCl react to form iron chloride (FeCl3). The FeCl3 solution is the key factor that contributes to the flower-like formation of α-Fe2O3 under a heating temperature of 200 °C 20–24 h.21 Fig. 4(b–b′) shows clusters of wrinkled nano-sheets starting to form at pH 2, it is due to the fact that loose and irregular clusters occur under this hydrothermal condition. This structure is maintained at pH 3 (Fig. 4(c–c′)) with a similar show of irregular clusters where the breakdown of the structure begins, as observed at pH 4–5 (Fig. 4(d–d′) and (e–e′)). From pH 6 to 10, the structure begins to gather to form irregular and large microparticles, which is the transition from the early stage to the synthesis.25 Under highly alkaline conditions from pH 8–10 these irregular and large clusters become tightly-packed and well-shaped forms, especially in Fig. 4(h–h′).26 Fig. 4(i and j) are the period of transition from the irregular forms into more crystalline structures again. Both pH 1 and pH 10 can provide well crystalline forms of iron oxide, however the acidic condition of pH 1 gives better performance with high crystallization of the flower-like forms.
Particle size distribution of the raw and synthesised materials after the hydrothermal process are present in Fig. 5a. The Bac-FeOxNWs (control) displays a broad PSD ranging from 0.2 to 80.0 μm,27 which is expected due to the presence of many broken nanowires (Fig. 1a). As the nanowires are hydrothermally treated under high temperatures and in an acidic solution their morphology begins to change. The Bac-FeOxNWs synthesised at pH 1 displays a narrow PSD with larger particles (d(50) = 54.5 μm) compared to the broad PSD (twin peaks) at pH 2. With increasing pH from 3 to 4, the flower-like nanostructures break down into small particles from 13.8 to 10.4 μm, respectively. Around pH 5–7, the particle size of the synthesised Bac-FeOxNWs are consistent (d(50) = 17.2 μm) as the broken down particles start to form large clusters (Fig. 4(e–g)). Under the hydrothermal treatment in an alkaline condition, the clusters become well-packed and tightly bound from pH 8 to 10, hence a decrease in the particle size to 12.0 μm. When the powdered dispersions (Fig. 2) were re-examined after 24 h, it was noticed that all the particles at pH 1 had settled down compared to the well-dispersed stable solutions of all the other pHs. This result further confirms the formation of the larger particles at pH 1 (Fig. 5b) and is complemented by the SEM characterisation.
Fig. 5 Particle size distribution (PSD) of the purified (control) and synthesised Bac-FeOxNWs from pH 1–10 after the hydrothermal process. |
The study of Mohapatra and Anand9 shows that the only reaction product formed is hematite in the pH range of 0.8–2.6, however, this is contradictory to the results that claim that the iron product is formed greater under basic pH.14 The difference in results is related to the starting materials used to form α-Fe2O3. Majority of the studies use the iron chemical precursors to form the end product, whereas in this work we start with the natural amorphous iron oxide instead. Considering the XRD, FTIR, SEM and PSD results, the optimal hydrothermal treatment is under acidic conditions for Bac-FeOxNWs at a reaction temperature of 200 °C with pH 1 and a reaction time of 20 h for the complete transformation of α-Fe2O3. The reaction is successfully reduced due to the pink coloured powder that is obtained as illustrated in Fig. 2 than the majority of orange powders achieved for the other pH values. Although, red powders were obtained under alkaline pHs their crystalline structures are weak and are not fully developed.
This ‘nucleation, growth and ostwald ripening’ behaviour is common for the synthesis of iron oxides under different conditions (e.g. time, temperature, environment).28–32 Under hydrothermal conditions, starting at neutral pH 7, by decreasing pH (acidic) the system shows that the particles grew through Ostwald ripening, while at basic pH the particles underwent continuous nucleation and growth to form aggregates,23,25 which confirms the SEM and PSD data.
Fig. 6 (a) UV-Vis spectra of the degradation of RhB at 15 min, and (b) and adsorption capacity (Q) of As(III) and As(V) ions after 90 min. |
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c8ra07061j |
This journal is © The Royal Society of Chemistry 2018 |