Trevor P.
Almeida
,
Michael W.
Fay
,
Yanqiu
Zhu†
* and
Paul D.
Brown
*
Division of Materials, Mechanics and Structures, & Department of Mechanical, Materials and Manufacturing Engineering, Faculty of Engineering, Nottingham Nanotechnology and Nanoscience Centre, University of Nottingham, University Park, Nottingham, NG7 2RD, UK. E-mail: yanqiu.zhu@nottingham.ac.uk; paul.brown@nottingham.ac.uk
First published on 12th July 2010
The hydrothermal growth mechanism of α-Fe2O3 nanorods has been investigated using a novel valve-assisted pressure autoclave. This approach has facilitated the rapid quenching of hydrothermal suspensions into liquid nitrogen, providing ‘snapshots’ representative of the near in situ physical state of the synthesis reaction products as a function of known temperature. Examination of the acquired samples using complementary characterisation techniques of transmission electron microscopy, X-ray photoelectron spectroscopy and Fourier transform infrared spectroscopy (FT-IR) has provided fundamental insight into the anisotropic crystal growth mechanism of the lenticular α-Fe2O3 nanorods. An intermediate β-FeOOH phase was observed to precipitate alongside small primary α-Fe2O3 nanoparticles. Dissolution of the β-FeOOH phase with increasing temperature, in accordance with Ostwald's rule of stages, led to the release of Fe3+ anions back into solution to supply the growth of α-Fe2O3 nanoparticles, which in turn coalesced to form lenticular α-Fe2O3 nanorods. The critical role of the PO43− surfactant on mediating the lenticular shape of the α-Fe2O3 nanorods is emphasised. Strong phosphate anion absorption on α-Fe2O3 crystal surfaces stabilised the primary α-Fe2O3 nanoparticle size to < 10 nm. FT-IR investigation of the quenched reaction products provided evidence for PO43− absorption on the α-Fe2O3 nanoparticles in the form of mono or bi-dentate (bridging) surface complexes on surfaces normal and parallel to the crystallographic α-Fe2O3 c-axis, respectively. Mono-dentate PO43− absorption is considered weaker and hence easily displaced during growth, as compared to absorbed PO43− bi-dentate species, which implies the α-Fe2O3 c-planes are favoured for the oriented attachment of primary α-Fe2O3 nanoparticles, resulting in the development of filamentary features which act as the basis of growth, defining the shape of the lenticular α-Fe2O3 nanorods.
To date, α-Fe2O3 nanostructures have been produced using a variety of techniques including sol–gel processing,12 microemulsion,13 forced hydrolysis,14 hydrothermal synthesis (HS)15 and chemical precipitation.16 In particular, HS offers effective control over the size and shape of nanoparticles at relatively low reaction temperatures and short reaction times, providing for well-crystallized reaction products with high homogeneity and definite composition.17 Indeed, the technique of continuous and high throughput HS has become a viable method for the commercial synthesis of nanoparticles.18–21 However, there is still much speculation concerning the fundamental mechanisms of hydrothermal reaction and nanoparticle growth. The use of reaction vessels under conditions of high temperature and pressure generally creates an aspect of inaccessibility which limits direct investigation. Indeed, even the exception of in situ synchrotron and energy dispersive X-ray diffraction methods are sensitive only to bulk crystal phase transformations.22–24In situ X-ray absorption spectroscopy, for example, allows time-resolved experiments under specific reaction conditions to provide the structural and electronic properties around a specific atom,25,26 but does not offer direct information on the morphological development and kinetics involved in the growth of nanostructures. Consequently, the analysis of HS nanoparticles on the localised scale has been restricted to post-synthesis reaction products isolated following cool down under equilibrium conditions, with possibility of loss of in situ constituent evidence demonstrating the specific mechanistics of growth.
Aqueous iron (III) chloride (FeCl3) solution is well established as a simple precursor for the formation of monodispersed α-Fe2O3 nanoparticles,27,28 and needle-shaped β-FeOOH nanoparticles are known to form as an intermediate phase which gradually diminishes as the α-Fe2O3 nanoparticles develop.29–31 Further, a small addition of phosphate anions has been shown to mediate the anisotropic growth of α-Fe2O3, leading to the development of lenticular nanorods.31–33Ex situ investigations of the phase transformation of β-FeOOH to α-Fe2O3 to date, along with α-Fe2O3 shape control within phosphate environments, have provided valuable insights into the α-Fe2O3 nanorod growth mechanism.34 However, improved understanding of the in situ mechanistics of α-Fe2O3 nanorod growth is required in order to control fully the functional properties of these 1D nanostructures.
In this context, we have reported previously on the development of a novel, valve-assisted, Teflon-lined, hydrothermal pressure vessel which allows for the rapid quenching of hydrothermal products.35 It is considered that the reaction products obtained from this autoclave are closely representative of the in situ physical state of the developing iron oxide nanostructures due to the large thermal gradient experienced during quenching. This novel investigative approach restricts possible atom/ion transport, thereby locking-in the morphology of the nanostructures to reveal the intricate details of the hydrothermal growth. Indeed, our initial experiments have demonstrated the viability of this ‘snapshot’ approach to provide detailed insight into the localised development of lenticular α-Fe2O3 nanorods, as a function of reaction time.35 We now report on a more detailed investigation of the development of 1D α-Fe2O3 nanostructures, as a function of reaction temperature, using this valve-assisted hydrothermal pressure vessel, recognising that thorough understanding of the temperature response of each reaction vessel is needed to fully appraise the growth. It is considered that detailed analysis of near in situ hydrothermal reaction solutions, acquired at known reaction temperatures, provides for better understanding of the development process of α-Fe2O3 nanorods. In particular, emphasis is given to the critical role of the PO43− surfactant mediating their lenticular shape.
Snapshot Sample | Temperature/°C | Phase and morphology | Size (length/width) |
---|---|---|---|
S100 | 100 | β-FeOOH nanorods Small α-Fe2O3 nanoparticles | < 50/15 nm < 10 nm in diameter |
S120 | 120 | β-FeOOH nanorods Small α-Fe2O3 nanoparticles | < 50/15 nm < 10 nm in diameter |
S140 | 140 | β-FeOOH nanorods Small α-Fe2O3 nanoparticles Lenticular α-Fe2O3 nanorods | < 50/15 nm < 10 nm in diameter ∼ 150/50 nm |
S160 | 160 | Few β-FeOOH nanorods Small α-Fe2O3 nanoparticles Lenticular α-Fe2O3 nanorods | < 40/15 nm < 10 nm in diameter ∼ 350/60 nm |
S180 | 180 | Small α-Fe2O3 nanoparticles Lenticular α-Fe2O3 nanorods | < 10 nm in diameter ∼ 420/65 nm |
S200 | 200 | Lenticular α-Fe2O3 nanorods | ∼ 450/80 nm |
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Fig. 1 Hydrothermal reaction solution temperature plotted as a function of reaction time. |
Tiny frozen droplets of the synthesised reaction product were deposited straight onto lacey carbon/copper mesh support grids (Agar Scientific Ltd, UK) and allowed to melt at room temperature prior to transmission electron microscopy (TEM) investigation. Conventional diffraction contrast bright field (BF) and phase contrast imaging were performed using Jeol 2000fx and 2100F electron microscopes. Selected area electron diffraction (SAED) patterns allowed for phase identification and an appraisal of the relationship between nanorod morphology and crystallographic orientation. X-ray photoelectron spectroscopy (XPS) (Kratos AXISULTRA configured with a monochromated AlK X-ray source) was utilized to investigate the surface chemistries of the nanoparticles. Further, Fourier transform infrared (FT-IR) transmittance spectroscopy (Bruker Tensor, Germany; OPUS Spectroscopy Software) provided information on the covalent bonding present. Frozen droplets were allowed to melt in a pipette at room temperature and deposited directly onto the FT-IR diamond sensor, where it was dried at 80 °C using the heating stage and subsequently clamped. CasaXPS was used to analyze the XPS and FT-IR spectra.
The bright field, diffraction contrast TEM images of Fig. 2a-f illustrate the varied β-FeOOH and α-Fe2O3 reaction products, as a function of increasing HS temperature (Samples S100 to S200). The phases present were identified from associated SAED patterns (Fig. 2a-f inset and summarised in Table 1). Sample S100 (Fig. 2a) showed the presence of β-FeOOH needle-shaped nanorods (< 50 nm long, 15 nm wide) and small α-Fe2O3 nanoparticles (< 10 nm in diameter). The same phases and particle morphologies were observed in Sample S120 (Fig. 2b), with the presence of slightly more of the small α-Fe2O3 nanoparticles. Conversely, Sample S140 (Fig. 2c) exhibited additional darker α-Fe2O3 nanorods (∼ 200 long, ∼ 50nm wide, as arrowed) amongst the previously observed β-FeOOH and α-Fe2O3 nanostructures. Further, Sample S160 (Fig. 2d) demonstrated an increased presence of the small isotropic α-Fe2O3 nanoparticles (< 10 nm in diameter), along with the development of larger α-Fe2O3 lenticular nanorods (∼ 350 nm long, ∼ 60 nm wide) and a correspondingly marked reduction in the presence of the intermediate β-FeOOH phase. The proportion and size of α-Fe2O3 nanorods (∼ 420 nm long, ∼ 65 nm wide) was even greater in Sample S180 (Fig. 2e), without any noticeable evidence for the presence of the intermediate β-FeOOH phase amongst the remaining small α-Fe2O3 nanoparticles. Sample S200 exhibited the largest, most well-defined, crystalline lenticular α-Fe2O3 nanorods (∼ 450 nm long, ∼ 80 nm wide) (Fig. 2f).
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Fig. 2 Bright field TEM images of ‘quenched’ hydrothermal products after 80 min of processing, having achieved temperatures of (a) 100, (b) 120, (c) 140, (d) 160, (e) 180 and (f) 200 °C, respectively (Samples S100 to S200), with corresponding SAED patterns (inset – (a) and (f) are indexed to β-FeOOH and α-Fe2O3, respectively). |
Phase contrast imaging of Sample S100 revealed details of the initial development of β-FeOOH nanostructures, as identified by characteristic lattice fringes corresponding to {110} and {200} planes (Fig. 3a and 3b, respectively). An embryonic β-FeOOH nanoparticle is shown in Fig. 3a, whilst Fig. 3b is representative of the first stages of development of a β-FeOOH nanorod, with characteristic {110} planes (d110 = 7.47Å) lying parallel to the nanorod growth axis (Fig. 3b).
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Fig. 3 Phase contrast TEM images of the hydrothermal products synthesised at 100 °C (Sample S100). (a) Small β-FeOOH nanoparticle (∼ 15 nm in diameter); and (b) small developing β-FeOOH nanorod (∼ 50 nm long, ∼ 15 nm wide); both identified by lattice fringes. |
The bright field and phase contrast TEM images of Fig. 4 present details of the initially formed α-Fe2O3 nanoparticles, as identified in Sample S160. Lattice fringes consistent with the development of crystalline α-Fe2O3 were identified (Fig. 4d), and confirmed by associated Fast Fourier Transform (FFT) patterns (Fig. 4e). The initially formed α-Fe2O3 nanoparticles were all isotropic in shape and < 10 nm in diameter.
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Fig. 4 Bright field and phase contrast TEM images of the first stages of development of α-Fe2O3 nanoparticles, synthesised at 160 °C (Sample S160). (a) Small α-Fe2O3 nanoparticles (< 10 nm in diameter); (b) & (c) small α-Fe2O3 nanoparticles on the edge of the lacey carbon support; (d) an individual α-Fe2O3 nanoparticle identified by lattice fringes and (e) corresponding FFT. |
TEM investigation of Samples S160 and S180 (Fig. 5a-d) demonstrated the close association between the initially formed α-Fe2O3 nanoparticles and the development of single crystalline α-Fe2O3 nanorods. Fig. 5a shows a small crystalline α-Fe2O3 nanorod (∼ 40 nm long, ∼ 12 nm wide), as identified by lattice fringe spacings and associated FFT. Fig. 5b illustrates a slightly larger α-Fe2O3 nanorod (∼ 120 nm long, ∼ 25 nm wide), with an irregular surface. The developing tips of such α-Fe2O3 nanorods exhibited filamentary features, comprising α-Fe2O3 nanoparticles of similar size to those shown in Fig. 4, with lattice fringes aligned with the nanorod bulk (Fig. 5c, inset). Associated SAED patterns (Fig. 5c inset) demonstrated the α-Fe2O3 nanorod growth axis to be parallel to <006>. It is considered that the TEM image of Fig. 5d reveals details of the initial stages of attachment of crystalline α-Fe2O3 nanoparticles to a developing α-Fe2O3 nanorod, prior to their crystallographic alignment with the bulk nanorod.
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Fig. 5 Bright field and phase contrast TEM images of the hydrothermal products processed at (a–c) 160 °C and (d) 180 °C, respectively. (a) Initially formed α-Fe2O3 nanorod (∼ 40 nm long, ∼ 12 nm wide), as identified by lattice fringes and associated FFT (both inset); (b) α-Fe2O3 nanorod (∼ 120 nm long, ∼ 25 nm wide) with corresponding SAED pattern (inset); (c) tip of an α-Fe2O3 nanorod, as identified by lattice fringes and SAED pattern (both inset), exhibiting filamentary features crystallographically aligned with the bulk nanorod (inset); and (d) tip of a developing α-Fe2O3 nanorod, as identified by lattice fringes (inset), with an irregular surface and uneven distribution of α-Fe2O3 nanoparticles attached to the tip (inset). |
Complementary XPS data from samples S100 and S160, showing details of Fe 2p and P 2p peaks are presented in Fig. 6a and 6b, respectively (with additional survey scans given in the Supplementary materials). In our previous investigation,36 it was reported that Fe 2p and P 2p signatures from iron oxide and iron hydroxide grown by HS in a phosphate environment were nearly identical, limiting ease of discrimination between the surfaces of these phases using the technique of XPS. However, subtle differences in the near surface chemistries of these β-FeOOH and α-Fe2O3 nanostructures are revealed by the present data set.
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Fig. 6 XPS data showing (a) Fe 2p and (b) P 2p signatures from Samples S100, S160 & S200. |
Fig. 6a shows Fe 2p3/2 binding energy peaks at 711.8 eV and 711.0 eV for samples S100 and S160, consistent with the presence of β-FeOOH and α-Fe2O3, respectively.37 Satellite peaks characteristic of Fe3+ were evident within both spectra, with differences in the binding energies between satellite and Fe 2p3/2 peaks being 7.60 eV and 4.50 eV for α-Fe2O3 and β-FeOOH, respectively. This observation is consistent with a recent report of an 8.0 eV separation between satellite peak and the Fe 2p3/2 binding energy for bulk α-Fe2O3.38 Further, Fig. 6b showing P 2p peaks centred at 134.0 eV, 133.0 eV and 133.1 eV (Samples S100, 160 and S200, respectively) is consistent with the presence of phosphate species on the surfaces of both β-FeOOH and α-Fe2O3 nanostructures.39,40
The nature of the covalent bonding of the surface phosphate species was investigated using FT-IR spectroscopy. Phosphate stretching modes41 were identified typically in the range of 900–1200 cm−1. Fig. 7a presents FT-IR spectra obtained from Samples S100, S160 and S200, as well as an additional spectrum from acetone cleaned S200 (labelled S200C). It is clear that the signal from Sample 200C is relatively small compared to Samples S100, S160 and S200. For this reason, the signal from the original snapshot samples can be assigned to emission from surface species, as opposed to signal from the crystal bulk. Deconvolution of the S100 and S160 spectra into the individual spectral constituents was performed using CasaXPS software (Fig. 7b and 7c/d, respectively). Sample S100 demonstrated peaks at 1111, 1056 and 987 cm−1 (Fig. 7b) whilst Sample S160 showed peaks at 898, 934, 970, 1004, 1036, 1071 and 1149 cm−1 (Fig. 7d).
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Fig. 7 (a) FT-IR spectra of phosphate species from Samples S100, S160, S200 and S200C; (b) deconvolution of S100 showing labelled individual spectral constituents; (c) deconvolution of S160 showing individual spectral constituents; and (d) labelled individual peaks (Sample S160). |
β-FeOOH has been described as being slightly metastable and therefore kinematically accessible when precipitated from aqueous solution.42 However, due to the very small (< 50 nm) β-FeOOH nanoparticle and nanorod sizes, with positive surface energies by implication, the easily hydrated particle surfaces reduce their effective surface enthalpies by up to 0.1 J/m2.43 Consequently, β-FeOOH nanoparticles become partially thermodynamically stabilized. The Ostwald rule of stages concerns the competition between kinetics, irreversible thermodynamics and equilibrium thermodynamics.44 A decrease in total surface energy is considered to be the driving force for the crystal growth kinetics of β-FeOOH and α-Fe2O3. As the more thermodynamically stable α-Fe2O3 primary particles nucleate and grow, driven by the enthalpy for bond formation at increasing hydrothermal temperatures, the equilibrium Fe3+ concentration at the surface of α-Fe2O3 becomes lower than that of β-FeOOH. The resulting concentration gradient leads to Fe3+ ions flowing from β-FeOOH to the newly formed α-Fe2O3 nanoparticles, prompting β-FeOOH dissolution to restore the equilibrium Fe3+ concentration at the β-FeOOH surface. An illustration of β-FeOOH dissolution and α-Fe2O3 crystal growth based on the Ostwald rule of stages is shown in Fig. 8a.44
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Fig. 8 Schematic representation showing: (a) dissolution of intermediate β-FeOOH nanostructures (grey shading) alongside precipitation of α-Fe2O3 nanoparticles (lined shading), based on the Ostwald rule of stages; and (b) agglomeration, rotation (arrowed) and coarsening of α-Fe2O3 primary particles into an α-Fe2O3 nanorod, based on the oriented attachment mechanism. |
Further, it is considered that phosphate absorption on the α-Fe2O3 nanoparticle surfaces acts to stabilise the < 10 nm particle sizes,45,46 being distinct from the larger (< 150 nm) isotropic α-Fe2O3 nanoparticles which form under surfactant-free conditions.36 These primary α-Fe2O3 nanoparticles may be considered as ‘building blocks’ that collide and coalesce in an oriented fashion to form the single crystalline lenticular α-Fe2O3 nanorods. It is suggested that preferential phosphate absorption on specific α-Fe2O3 crystal faces is consistent with acting to promote the oriented attachment (OA) mechanism47,48 (Fig. 8b). If the α-Fe2O3 nanoparticles are not initially in compatible orientations at the point of coalescence (Fig. 5d), they are still free to rotate to achieve structural coherence at a common interface (Fig. 5a and 5c). It is considered that this grain-rotation-induced grain coalescence (GRIGC) mechanism49,50 acts to minimize the area of high energy interfaces, allowing low-energy configurations to become established, eliminating misoriented grain boundaries and forming coherent grain-grain boundaries in accordance with the model proposed by Zhang et al.47 This OA mechanism appears to be equally applicable to the initial development of α-Fe2O3 nanorods (Fig. 5a), as to the attachment of α-Fe2O3 primary nanoparticles to well-defined crystalline α-Fe2O3 nanorods, creating the filamentary features observed at the nanorod tips (Fig. 5c).
These two distinct stages of crystal growth will be now discussed in more detail, with emphasis on the pivotal role of the phosphate surfactant on the development of the lenticular shape of the α-Fe2O3 nanorods.
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Fig. 9 Schematic representation of the tetragonal β-FeOOH crystal structure showing: projections along the (a) <010> and (b) <110> zone axes; and (c) scaffold-like face normal to the c-axis revealing large channels. Small (red) and large (blue) atoms denote iron and oxygen, respectively. Terminal hydrogen atoms are not shown. |
Further, the FT-IR evidence presented here is consistent with the absorption of phosphate species on the iron atoms at the α-Fe2O3 surfaces, in the form of either mono or bi-dentate complexes. Hence, the form and the role of the phosphate ions attached to α-Fe2O3 needs to be considered in more detail. Assignment of the peaks in the FT-IR spectra of Fig. 7 is made with reference to established literature.56–62 For example, Arai et al.56 applied FT-IR spectroscopy to investigate surface phosphate complexes on FeOOH surfaces at low pH values, whilst Rose et al.57 and Wilhelmy et al.58 both suggested mono-dentate phosphate complexation with ferric ions at pH < 2 when using ferric chloride precursors under specific conditions. In this context, the single broad FT-IR peak (Fig. 7b) for Sample S100 at ∼ 1050 cm−1 can be deconvoluted into peaks at 997, 1056 and 1111 cm−1 and these ν3 bands, consistent with C2ν symmetry or lower,53 are in good agreement with the three ν3 band (see *Footnote) splitting signatures of mono or bi-protonated mono-dentate mononuclear phosphate complexes (FeHPO42+ or FeH2PO42+, both with C1 symmetry).58 The additional peak at ∼ 850 cm−1 is characteristic of the β-FeOOH phase.59
In particular, the FT-IR spectra from Samples S160 and S200 (Fig. 7) provide valuable clues as to the nature of the phosphate complexes on the surfaces of both the α-Fe2O3 nanoparticles and nanorods. Elzinga et al.60 reported on IR spectra of phosphate complexes bonding in a bi-dentate (bridging) fashion with hematite surfaces at low pH values. Accordingly, it is considered that the hematite rich reaction products examined here (Samples S160 to S200, pH ∼1) exhibited similar phosphate bi-dentate surface complexes. Deconvolution of the IR spectrum of Sample S160 revealed strong peaks at 898 934, 970, 1004, 1036, 1071 and 1149 cm−1, (Fig. 7d) which are all consistent with ν3 bands, with the exception of one ν1 band at 898 cm−1 (see *Footnote). The three ν3 bands at 934, 1036 and 1071 cm−1 are assigned to the presence of H2PO42− surface species with C2ν symmetry or lower.58 According to Borgnino et al.,61 this group of shifted H2PO42− vibrations are indicative of ‘inner-sphere surface complexes,’ attributable to the initial formation of the bi-dentate complex (FeO)2PO2.62 It is reasonable to assume this complex becomes protonated ((FeO)2P(OH)2 with C2ν symmetry,60 at the low pH conditions associated with the HS system examined here. However, the three ν3 bands at 970, 1004 and 1136 cm−1, also indicative of C2ν symmetry or lower, are attributable either to a mono-protonated bi-dentate complex (FeO)2(OH)PO or protonated mono-dentate surface complex (FeO)(OH)2PO (both with C1 symmetry).60–62
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Fig. 10 Schematic diagram of the tetragonal α-Fe2O3 crystal lattice showing (a) monodentate phosphate adsorption on the c-plane; and (b) bidentate phosphate adsorption on a faces parallel to the c-axis (Red (small), blue (large) and green (smallest) spheres correspond to iron, oxygen and phosphorus, respectively). |
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Fig. 11 Schematic diagram summarising the HS growth mechanism for α-Fe2O3 nanorods, as a function of increasing temperature: (1) precipitation of β-FeOOH nanoparticles and nanorods (grey), and α-Fe2O3 nanoparticles (brown); (2) nucleation of additional α-Fe2O3 nanoparticles; (3) dissolution of β-FeOOH nanorods alongside oriented α-Fe2O3 nanoparticle attachment; (4) dissolution of β-FeOOH nanorods into nanoparticles and growth of α-Fe2O3 nanorods; (5) growth and coarsening of α-Fe2O3 nanorods; and (6) large, single crystalline α-Fe2O3 nanorods. |
Footnote |
† Present address: College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, EX4 4QF. E-mail: yanqiu.zhu@exeter.ac.uk |
This journal is © The Royal Society of Chemistry 2010 |