Esteban Gioria*a,
Filippo Romeggio
a,
Ruben Bueno Villoro
b,
Ilenia Giarnieri
c,
Patricia Benito
c,
Ib Chorkendorffa and
Christian D. Damsgaard
*abd
aDTU Physics, Technical University of Denmark, Kongens Lyngby, DK-2800, Denmark. E-mail: egagi@dtu.dk; filro@dtu.dk; icho@dtu.dk; cdda@dtu.dk
bVISION, DTU Physics, Technical University of Denmark, Kongens Lyngby, DK-2800, Denmark. E-mail: rbuvi@dtu.dk
cDipartimento Chimica Industriale “Toso Montanari, Università di Bologna, Bologna, 40136, Italy. E-mail: ilenia.giarnieri2@unibo.it; patricia.benito3@unibo.it
dDTU Nanolab, Technical University of Denmark, Kongens Lyngby, DK-2800, Denmark
First published on 8th August 2025
Metal-supported nanoparticles play a crucial role in heterogeneous catalysis, with their activity governed by size, composition, and metal–support interactions. Conventional preparation methods often lack precise control of nanoparticle descriptors or introduce secondary metallic phases, limiting insights into intrinsic catalytic properties. In this study, colloidal iron nanoparticles (FeNPs) were used as pre-formed active sites to investigate CH4 decomposition, a reaction that yields high-purity H2 and carbon nanotubes (CNTs). FeNPs were supported on SiO2, MgO, Si3N4 and MgAl2O4, to systematically assess the influence of support materials on catalytic activity and the nature and morphology of carbon products. Characterization via ex situ TEM, STEM-EDS, SEM, XPS, Raman spectroscopy, and in situ XRD revealed distinct support-dependent behaviors. Fe/SiO2 exhibited deactivation due to severe sintering and encapsulation. Nevertheless, Fe3C species were identified as a stable phase under reaction conditions. Fe/MgO showed high stability against sintering but severe FeNPs encapsulation. Surprisingly, FeNPs on Si3N4 retained their nanometric size, probably due to strong anchoring in the support. Nevertheless, the support partially reacts with CH4 leading to C3N3 species. In contrast, Fe/MgAl2O4 demonstrated the highest activity towards carbon nanostructures formation, producing abundant CNTs via the tip growth and base growth mechanisms. Beam-enhanced in situ TEM confirmed a base growth process, with FeNPs remaining attached to the spinel support. The results evidenced the oxophylic nature of the support as an important descriptor of the stability of preformed FeNPs. This study provides a systematic comparison of colloidal FeNPs on various supports for CH4 decomposition to form CNTs and CO2-free H2, offering insights into active phase formation, CNTs growth mechanisms, and optimal support selection for efficient CNTs production.
State-of-the-art methods for the preparation of heterogeneous catalysts typically involve techniques such as impregnation of metal precursors onto preformed supports or co-precipitation from precursor solutions. While these approaches enable large-scale production, they offer limited control over key metal site properties, such as particle size distribution. As a result, it becomes challenging to attribute the intrinsic catalytic properties to a single type of metal site, unlike in model systems based on well-defined supported metal nanoparticles.3
Furthermore, conventional thermal treatments needed during the preparation, such as calcination and reduction, often promote the incorporation of metal species into the support structure. In this context, commonly used supports such as SiO2, TiO2, MgO, and Al2O3 can lead to the formation of stable metal-support phases, including silicates, titanates, magnesium spinels, and aluminates.4–8 These metal-containing phases are typically difficult to reduce, often requiring harsh reduction conditions to generate the active catalytic phase. Consequently, this can lead to the coexistence of metal species with distinct chemical nature and reactivity. In this regards, the colloidal synthesis of metal nanoparticles allows the pre-formation of metal (and metal oxides) particles with controlled properties. Afterwards, their incorporation into the support by simple impregnation or physical mixture avoid or minimize the formation of undesired phases, since the interaction between the metal sites and the support are only based on physical adsorption.9
Carbon nanotubes (CNTs) represent a class of functional materials characterized by exceptional properties at the nanoscale. Their high mechanical strength, lightweight structure, superior electrical conductivity, and high thermal stability make them highly versatile for applications including electronics, energy storage, structural materials, and healthcare.10 Aligning with the global energy transition, CNTs are increasingly being explored in energy storage and conversion technologies such as batteries, capacitors, and fuel cells.11–13
The production of CNTs is predominantly achieved through chemical vapor deposition (CVD), a method favored for its simplicity, scalability, and cost-effectiveness. CVD typically involves the thermal decomposition of carbon sources, such as ethylene (C2H4) or acetylene (C2H2), at elevated temperatures in the presence of catalysts, commonly based on iron (Fe), cobalt (Co), or nickel (Ni). Fe is particularly interesting among other transition metals due to its high catalytic activity and stability at high temperatures, where thermodynamic conversions are favored,14 and due to its crustal abundance.15
Within this context, methane (CH4) decomposition has garnered significant attention due to its dual production of high-purity CO2-free H2 and carbon as sole products. The process holds industrial relevance, as it utilizes an inexpensive carbon source and relies on well-established operational units and distribution technologies.16 CH4 decomposition is an endothermic reaction conducted at atmospheric pressure and temperatures ranging from 500 to 900 °C. Nevertheless, formation of undesired carbonaceous structures contribute to catalyst deactivation, either through sintering and/or the blockage of active sites caused by carbon encapsulation.
In this work, we explore the catalytic activity of preformed colloidal iron nanoparticles (FeNPs) impregnated on selected supports (SiO2, MgO, Si3N4 and MgAl2O4). Thus, allowing a fair comparison between pre-formed active sites, the nature of the support and the final morphology of carbon products. By combining both ex situ techniques like TEM, STEM-EDS, SEM, XPS, Raman spectroscopy, in situ XRD and in situ TEM, it was found that the nature of the support greatly affects the catalytic activity in terms of carbon yield and the properties of the final carbonaceous products.
Surprisingly, studies on colloidal iron nanoparticles for CH4 decomposition are scarce, with reports limited to SiO2 films and MgO powders.17–20 Therefore, this study provides a systematic investigation of different support materials. Among them, MgAl2O4 was the only support that facilitated the formation of micrometer large CNTs. This system was further examined using beam-enhanced in situ TEM, revealing that the Fe-based catalyst undergoes reduction and promotes CH4 cracking, ultimately leading to the formation of base-growth CNTs.
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Fig. 1 Schematic representation of the overall process regarding synthesis, preparation and testing of the supported colloidal nanoparticles. |
The catalytic experiments were carried out at atmospheric pressure and the catalysts were activated under 50% H2: he from room temperature up to 750 °C (see further details in experimental section). After 5 minutes, H2 was switched off and CH4 was fed. The reaction was kept for 90 minutes.
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Fig. 3 (a) SEM, (b) STEM-EDS, (c) in situ XRD, (d) C1s and Fe 2p XPS and (e) schematic representation of Fe/SiO2 after reaction. |
Han et al. studied the non-oxidative conversion of CH4 over different silica based Fe catalysts prepared by different approaches. Those ones prepared by fusing methods increased the formation of Fe–O–Si species, leading to increased selectivity towards C2+ and aromatics products.23Conversely, those ones based on FeOX particles of weaker interaction were selective towards carbon deposition. Similar results were found by Zhou et al., where the authors claim that CH4 decomposition proceeded first on Fe0 sites.24 After Fe3C species are formed, supersaturation leads to carbon precipitation and formation of encapsulating graphite layers. Nevertheless, these claims are based on ex situ XRD studies.
Wirth et al. investigated the phase evolution of Fe nanoparticles during CNT growth via C2H2 decomposition on 5 nm Fe films. Their study revealed that the formation of Fe3C as a stable intermediate depends on the initial Fe phase. Specifically, for γ-Fe-rich particles, metallic Fe serves as the intermediate for CNT formation, whereas α-Fe-rich particles promote the formation of carbide species as stable intermediates.25
Fig. 3c shows the diffractograms collected in situ during CH4 decomposition. At room temperature (RT), Fe species are not observed, indicating that the crystallite size of initial FeNPs is below the detection limit of the diffractometer. After 15 minutes of reaction, FeNPs are observable as Fe0, evidenced by the characteristic reflection at 44.5° from the (110) plane of α-Fe (JCPDS 65-4899). After 30 minutes, a transition toward Fe3C species is observed, remaining stable after 90 minutes (JCPDS 23-1113). These findings align with experimental observations employing both XRD and Mössbauer spectroscopy during CH4 pyrolysis using ore as iron source.25,26
The slight shift in 2 theta values observed between measurements at 750 °C and at room temperature after cooling can be attributed to lattice expansion due to thermal effects, as well as a minor displacement of the catalytic bed within the reaction chamber during the carbon nanostructures formation.
Thus, it is inferred that after Fe3C formation, metal particles saturation is followed by carbon precipitation. Due to the relatively large particle size promoted by migration and coalescence of preformed FeNPs, encapsulation is promoted and the reaction stops. After cooling down, the reflections characteristics of Fe3C species are less intense, in agreement with carbon precipitation and the phase-diagram of Fe–C system. The evidence corroborates that FeNPs are first present in a reduced state, prior to Fe3C formation, highlighting the relevance of in situ techniques for unraveling the true state of the active sites under dynamic conditions.
Fig. 3d presents the XPS analysis of the C1s and Fe2p core levels before and after the reaction. The C1s spectrum of the fresh sample reveals three primary peaks at 284.8 eV, 286.3 eV, and 288.2 eV, which correspond to adventitious carbon, C–O, and CO carboxylic groups, respectively.27 The presence of surface C–O and C
O species prior to the reaction is attributed to chemisorbed species formed during the decomposition of the metal precursor and the use of capping agents for colloid stabilization.28,29 After reaction, C1s peak at 284.8 eV becomes more pronounced, corresponding to the encapsulating graphitic carbon covering the catalyst, as observed by SEM and STEM-EDS.
Fe 2p core level of the fresh sample shows peaks between 709.6 and 710.8 eV, corresponding to surfaced oxidized Fe2+ and Fe3+ species. After reaction, Fe is practically not detected due to the dense encapsulation with graphitic carbon. These findings indicate that the SiO2 support facilitates significant sintering of FeNPs during the reaction, resulting in the formation of Fe3C as a stable intermediate during CH4 decomposition. The carbon nanostructures fully encapsulate the sintered particles, leading to catalyst deactivation and the formation of nano-onion structures, as schematically depicted in Fig. 3e.
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Fig. 4 (a) STEM-EDS, (b) in situ XRD, (c) C1s and Fe 2p XPS and (d) schematic representation of Fe/MgO after reaction. |
Fig. 4b shows the diffractograms collected during CH4 decomposition. The main reflections at 42.7° and 36.7° correspond to the (111) and (200) planes of MgO (JCPDS 4-829). The absence of C (002) graphite reflections suggests the absence of long-range carbon nanotubes formation, or the presence of small amounts of crystalline carbon. The slight shift towards lower 2 theta values between 750 °C and room temperature corresponds to the lattice expansion of MgO due to thermal effects.30 In addition, Fe phases are not detected due to the formation of well-dispersed amorphous particles and/or with crystallite sizes below the detection limit of the diffractometer.6
Ago et al. investigated CH4 decomposition on colloidal Fe nanoparticles (FeNPs) supported on MgO.19,20 Their study revealed that 10 nm FeNPs were unable to grow CNTs, whereas 4 nm FeNPs facilitated the formation of double- and single-walled CNTs, albeit in very low yields, as identified by TEM. The limited catalytic activity of the 10 nm FeNPs was attributed to their size, suggesting either insufficient CH4 diffusion under their experimental conditions or inadequate particle reactivity for initiating C–H bond cleavage.
Another possible factor inhibiting CNT formation is the strong metal–support interaction between Fe and MgO. It is well known that Fe particles on MgO are prone to interdiffusion,31,32 which, particularly at high temperatures, can lead to particle size reduction and the formation of unreduced Fe phases. However, under our experimental conditions, this effect is unlikely, as FeNPs exhibited growth from an initial size of 6.02 ± 0.49 nm to 14.4 ± 3.4 nm.
Topsøe et al. investigated the effect of metal–support interactions in the Fe–Mg–O system, demonstrating that iron diffusion into the MgO structure is strongly promoted at high temperatures, regardless of metal loading.33 Subsequent studies further confirmed that Fe diffusion leads to the formation of formal Fe–O–Mg bonds between Fe nanoparticles (FeNPs) and the support, enhancing both dispersion and thermal stability.34–36
A key distinction from traditional catalyst preparation methods is that preformed FeNPs exhibit only weak interactions with the catalyst surface. Therefore, the final particle size in this study is determined by a balance between partial sintering and stabilization via subsurface Fe diffusion into the MgO support. This final size does not favor the growth of extended CNT structures. Instead, partial CH4 decomposition results in surface encapsulation of the metal sites. Similar behavior has been observed when using other carbon precursors, such as C2H2 and C2H4.37
To gain further insights into the chemical state of the catalyst before and after reaction, Fig. 4c presents the XPS spectra of the C1s and Fe 2p core levels. The C1s signal remains nearly constant, attributed to adventitious carbon from the environment. The Fe 2p spectrum exhibits a distinct peak at 710.6 eV, corresponding to oxidized Fe2+/3+ species. However, after the reaction, this peak disappears, indicating FeNP encapsulation.
High-resolution TEM further supports these findings (Fig. S4†). The images reveal the formation of FeNPs smaller than 15 nm. Notably, these nanoparticles are uniformly encapsulated by well-defined carbon layers, as confirmed by the presence of lattice fringes at 3.4 Å, corresponding to the (002) plane of graphitic carbon. Both detached and anchored FeNPs are observed, where carbon structures are predominantly encapsulating FeNPs with short-range ordering.
The combined results from HR-TEM, STEM-EDS, in situ XRD, and XPS indicate that FeNPs are thermally stabilized under reaction conditions, exhibiting significantly less sintering compared to Fe/SiO2 and becoming encapsulated by graphitic carbon.
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Fig. 5 (a) STEM-EDS, (b) in situ XRD, (c) C1s and Fe 2p XPS and (d) schematic representation of Fe/Si3N4 after reaction. |
STEM-EDS mapping indicates a strong correlation between oxygen and silicon, suggesting the presence of a silicon oxide phase. Notably, Fe/Si3N4 seems to be covered by a shell-like structure. Elemental mapping further reveals that this shell is composed of nitrogen and carbon, in agreement with the lower contrast in HAADF mode consistent with the lower atomic numbers of these elements.
Fig. S7a† shows a low-magnification TEM of the spent catalyst. Unlike Fe/MgO, which exhibits clear carbon encapsulation and the formation of nanometric carbon structures, Fe/Si3N4 does not show evidence of carbon deposition. Fig. S7b† displays a HR-TEM micrograph of an individual supported nanoparticle. No carbonaceous structures are observed, and the measured lattice fringe spacing of 3.0 Å corresponds to the (220) plane of partially oxidized Fe2+Fe3+O4 magnetite.38 Similar to Fe/MgO, in situ XRD does not reveal any detectable C (002) graphite reflections or iron-containing phases (Fig. 5b). Thus, suggesting that the iron particles are rather stable and below the detection limit of the diffractometer, and the absence of carbon formation.
The diffraction peaks observed in the fresh Fe/Si3N4 catalyst at 2 = 23°, 32.5°, and 46.5° can be attributed to the (110), (002), and (122) planes of –Si3N4, respectively. However, the most intense reflections of this phase, located at 20.6° and 31° 2 and corresponding to the (111) and (221) planes (ICSD 6004), are not clearly observed. A similar analysis excludes the presence of –Si3N4, as its most intense reflection at 27.1° 2 (220) (ICSD 8263) is also absent. Interestingly, these additional diffraction peaks are present only in the fresh catalyst after FeNPs deposition and disappear after reaction and subsequent cooling to room temperature. At the industrial scale, SiN is typically produced via nitridation of silicon or carburization of silicon oxide under nitrogen atmosphere. Therefore, although the exact origin of these reflections cannot be fully determined, we infer that they may arise from residual precursor species remaining from the SiN synthesis process.
The XPS spectra of the sample before and after reaction are shown in Fig. 5c. Prior to reaction, the C1s core-level spectrum exhibits two distinct peaks at 284.8 eV and 287.4 eV, corresponding to adventitious carbon and adsorbed CO species. After reaction (i.e., reduction under H2 followed by exposure to CH4 at 750 °C for 90 minutes), two carbon species appear at 284.3 eV and 288.5 eV. The first is again attributed to adventitious carbon, while the second, at a relatively higher binding energy, is assigned to surface-bound C–N
C species, as discussed below.
To gain further insights into nitrogen-containing species, Fig. 6a presents the XPS spectra of the N1s core level before and after reaction. The contribution at 400.7–401.8 eV is associated with silicon oxynitride (Si–N–O2 and Si2–N–O) species, commonly found in industrially synthesized silicon nitride supports.39 A second peak, appearing at 397.5–397.8 eV, is attributed to both N–Si bonds from the silicon nitride structure and C–NC species. The total nitrogen concentration at the surface remained practically the same (17.9% at. before reaction and 17.5% after reaction). Nevertheless, the contribution at 397.5–397.8 eV increases from 5.3% to 7.2% after reaction. Given that the reaction conditions were nitrogen-free, the increase of N–Si bonds from the silicon nitride structure and C–N
C species would suggest a slight segregation of nitrogen from the silicon nitride support to the surface or the formation of carbon nitrides species after methane cracking.
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Fig. 6 (a) STEM-EDS, (b) in situ XRD, (c) C1s and Fe 2p XPS and (d) schematic representation of Fe/SiN after reaction. |
Fig. 6b shows additional HR-TEM images of the Fe/Si3N4 catalyst, illustrating the amorphous nature of the support, in agreement with the XRD results. Some isolated crystalline regions are observed (Fig. 6c), with lattice fringes measuring 3.9 Å, corresponding to the (110) plane of Si3N4. Fig. 6d reveals a distinct phase with a lattice fringe spacing of 3.5 Å, attributed to the (002) plane of triazine (C3N3), a structure composed of stacked sheets of sp2-hybridized carbon and nitrogen atoms.40
Previous studies have reported the formation of carbon nitride films through chemical vapor deposition (CVD) using CH4, H2, and NH3 on flat Si wafers. Regardless of decomposition conditions, the most probable structure is α-C3N4, which exhibits the same lattice plane distances as those observed in HR-TEM. However, in the present case, the proposed phase is a solid solution of SiXNYCZ, in which carbon occupies interchangeable nitrogen sites.41 AlShibane et al. previously reported the catalytic activity of amorphous silicon nitride composites for CH4 cracking.42 While these materials exhibit low catalytic activity, the nature of the carbon deposits was not characterized to verify the formation of CXNY species.
In this context, it has been shown that the basic properties of Si3N4 can enhance alkane dehydrogenation reactions.43,44 More recently, Si3N4 has been demonstrated as an effective support for zinc-based complexes that promote propane dehydrogenation to propylene, contrasting with the inertness of SiO2. The active sites are attributed to the Lewis basicity of nitrogen species, which facilitates heterolytic C–H bond activation. Therefore, Si3N4 could play a role in promoting C–H cleavage of methane and stabilizing intermediates formed during the cracking process.45 However, further studies are needed to fully elucidate the underlying mechanism.
Therefore, the present results suggest that CH4 can be partially decomposed on the support, leading to the formation of a surface layer of carbon nitride. Iron silicide species were not detected. The preformed FeNPs remain stable on the Si3N4 support without undergoing carbon encapsulation, as indicated by STEM-EDS, HR-TEM, and XPS (Fig. 5d).
Fig. 7a presents SEM micrographs of Fe/MgAl2O4 catalysts after reaction, revealing abundant CNT formation with a broad diameter distribution. Backscattered electron imaging verifies the presence of large metal particles, resulting from the sintering of the initial FeNPs. This observation is further supported by STEM-EDS microscopy (Fig. S8†), which reveals micrometer-long CNTs containing elongated Fe nanoparticles encapsulated within their tubular structures. Additionally, particles of varying sizes, including larger aggregates up to 100 nm and smaller supported particles below 10 nm, are observed. As shown in Fig. 7b and the corresponding spectra in Fig. S9,† it is also verified the formation of base-growth CNTs, with FeNPs remaining anchored to the spinel support. This anchoring prevents detachment and mitigates significant sintering.
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Fig. 7 (a) SEM, (b) in situ XRD, (c) C1s and Fe 2p XPS and (d) schematic representation of Fe/MgAlOx after reaction. |
X-ray diffractograms collected in situ indicate that the MgAl2O4 spinel structure remains intact (Fig. 7c). The characteristic reflections at 30.9°, 36.6°, 42.7°, and 44.5° correspond to the (221), (311), (200), and (400) planes, respectively (JCPDS 21-1152).55 Similar to Fe/MgO, a slight shift toward lower 2θ values is observed, attributed to lattice expansion due to thermal effects. However, after 30 minutes of reaction, a slight positive shift emerges, likely resulting from vertical sample expansion caused by CNT growth. This interpretation is consistent with the appearance of the characteristic reflection at 25.9°, corresponding to the (002) plane of graphitic carbon. Fig. S10a and b† illustrate the temporal evolution of the C(002) plane and a photograph of the sample post-reaction, highlighting the expansion of the catalytic bed inside the holder. The potential formation of FeCX species cannot be ruled out due to the strong reflections of the support and the overlap of diffraction peaks associated with MgAl2O4 and Fe-containing species.
The chemical states of the catalyst before activation and after reaction were analyzed by XPS (Fig. 7d). The C1s core level spectrum reveals a significant increase in carbon content following the reaction. Before exposure to CH4, the Fe 2p core level displays peaks at 709.6 eV and 710.8 eV, corresponding to surface Fe2+ and Fe3+ species, respectively. After the reaction, Fe 2p signals are no longer detectable. This could be related to a dilution effect of the FeNPs contained between the large amount of formed CNTs, but also agrees with STEM-EDS observations indicating complete encapsulation of FeNPs by carbonaceous structures after CH4 cracking.
Therefore, the balance between metal–support interaction and reactivity led to the formation of active Fe nanoparticles, promoting the formation of long-range CNTs structures following both a tip- and a base growth mechanism (Fig. 7e).
The intensity ratio ID1/IG provides a quantitative measure of structural disorder in carbon materials, where higher values indicate increased structural defects. Additionally, second-order bands above 2250 cm−1, such as the G′ (or 2D) band at 2700 cm−1, are often enhanced in carbon nanotubes and serve as markers of long-range order.
Fig. 8a and b present a representative Raman spectrum and the mean ID1/IG values obtained from six independent spectra collected at different locations, respectively. As observed, Fe/MgAl2O4 exhibits the highest degree of crystallinity, consistent with previous characterizations indicating the formation of long-range, well-ordered carbon nanotubes. Among all samples, Fe/MgO displays the highest degree of disorder. However, unlike Fe/SiO2 and Fe/Si3N4, the Fe/MgO spectrum features a prominent G′ band and lacks significant contributions from the D3 and D4 bands. Based on previous characterizations, this suggests that the observed disorder primarily arises from strain effects due to the curvature of relatively small, encapsulated Fe nanoparticles rather than significant structural defects.
Fe/SiO2 exhibits a lower ID1/IG ratio compared to Fe/Si3N4. Nevertheless, both spectra display similar contributions from the D3 and D4 bands, indicating the presence of impurities such as ionic species from the support, metal nanoparticles, interstitial defects, or structural disorder induced by oxygen-containing functional groups (e.g., carbonyls).58,59
These results agree with the previous characterizations and illustrate how the morphology and structural characteristics of carbon materials can be rapidly inferred from a Raman spectrum, assessing the quality and nature of carbon-based nanostructures.
The specimen was heated under 1 mbar H2 from room temperature up to 700 °C. Despite 3 hours of treatment, selected area electron diffraction (SAED) patterns showed no evidence of metallic Fe formation and predominantly the diffractions of the MgAl2O4 support (Fig. S11†). Subsequently, CH4 was introduced increasing the total pressure to 2 mbar. However, even after 2 hours of exposure, no CNTs formation was observed.
Yoshida et al. were the first to report CNTs growth on Fe particles supported on SiO2 at 600 °C and 0.1 mbar of C2H2.60 Their study demonstrated that CNTs growth was driven by fluctuating Fe3C nanoparticles, where carbon atoms diffused through the bulk of the carbide phase. A key distinction in their work was the use of C2H2, a carbon source with significantly lower activation energy due to the high reactivity of its triple C–C bond compared to CH4. Similar findings were reported by Wirth et al., who also used C2H2 at 0.01 mbar.25 Their results indicated that the formation of iron carbide is not necessarily a prerequisite for CNTs growth, as the process strongly depends on the specific iron phase present during the reaction.
Using CO as the carbon source, He et al. demonstrated the base-growth of single-walled CNTs on a Fe–Cu/MgO catalyst at 690 °C and 6.9 mbar.61 However, it was not confirmed whether the active catalyst phase was metallic Fe or an FeCX phase under dynamic conditions. Later, Liu et al. verified the complete reduction of 20 nm Fe2O3 nanoparticles after pretreatment at 700 °C in 4 mbar of H2 for 2 hours. Their study also indicated that Fe5C2 was the most stable phase when using a syngas mixture (CO/H2) at 6 mbar.62
Although several studies have explored by in situ TEM the growth mechanisms of CNTs on Fe-based catalysts using CO or acetylene at both low and atmospheric pressures, CNTs growth with CH4 as the carbon source has not been reported.63,64 As expected, CNTs growth and kinetics are highly dependent on parameters like temperature, partial pressure and nature of the carbon source.65 Therefore, it is inferred that at low CH4 partial pressures, Fe nanoparticles are unable to effectively activate C–H bonds. In contrast, under atmospheric pressure conditions, iron oxides have been shown to directly activate CH4, leading to the formation of carbon structures with a carbide phase as a stable intermediate.66
To facilitate CH4 decomposition, the electron beam was condensed on the microscope screen (see experimental section for details). The enhancement of chemical reactions under electron beam irradiation in in situ TEM has been previously documented. This can be related to several factors like heating effect, defects formation, charging of the particle, or excitation of surrounding gases.67 For example, the electron beam has been shown to accelerate the oxidation of model copper nanoparticles due to promoted diffusion of Cu+1 species towards the outer shell of the particles.68 Similarly, the electron beam can greatly promote the oxidation of iron nanoparticles due to enhanced mass transport of oxygen species across the outer shell.69 Similarly, the enhanced formation of SiO2−X layers on perovskites electrodes as also been reported.70,71
Upon focusing the electron beam on the studied region, CNTs growth was observed. As shown in Fig. 9, no metal nanoparticles were detected at the tips of the CNTs, indicating a base-growth mechanism. This suggests that FeNPs remained anchored to the MgAl2O4 support, facilitating CNTs growth. The internal structure of the nanotubes revealed graphene layers forming within the tubes. These features, previously observed in Ni catalysts, have been attributed to the dynamic elongation of metallic sites during growth, followed by contraction due to cohesive forces.72 It is inferred that the catalytic decomposition of CH4 is promoted by C–H bond cleavage under electron beam irradiation. However, quantifying electron beam-induced local temperature changes or promoted excitation of surrounding reactive gases remains a challenge and a field of current development.73
For comparison, FeNPs were also deposited on Au grids coated with Lacey carbon. Using a custom-made holder, the grid was placed in the in situ XRD chamber and heated from room temperature to 700 °C at a rate of 10 °C min−1 under a 50 ml min−1 He flow. Once the reaction temperature was reached, a 35% CH4 mixture was introduced, and the reaction proceeded for 1 hour. Fig. S12† presents TEM images before and after the reaction, where CNTs formation were observed following exclusively a tip-growth mechanism. The CNTs diameters correlated with the sizes of FeNPs located at their tips. The elongated shape of the metallic tips suggests that under these reaction conditions, the FeNPs were in a molten state, enabling tip-growth CNTs formation.
These findings highlight the importance of selecting an appropriate catalyst support that enables FeNPs anchoring without deactivation due to sintering or encapsulation, thereby promoting the growth of large CNTs. This is further discussed in the section “metal–support interaction and role of the support”, where we demonstrate that the oxyphilic character of the support and the anchoring of metal sites significantly influence both the stabilization of the nanoparticles and the resulting CNT growth mode.74 The results suggest that CH4 decomposition is significantly influenced by reaction conditions, including CH4 partial pressure, catalyst phase, and electron beam-induced effects. While Fe/MgAl2O4 enables CNTs growth under beam-enhanced conditions, further investigations are required to elucidate the exact role of electron irradiation. Nevertheless, these observations are in agreement with the observed activity of Fe/MgAl2O4 at atmospheric pressure, where a combination of encapsulating carbon, base- and tip-growth CNTs were observed.
This process differs from Ostwald ripening, where growth occurs indirectly through the movement of atomic or molecular species (adatoms) rather than whole nanoparticles. In Ostwald ripening, smaller particles dissolve and release atoms, which then redeposit onto larger particles, driven by differences in surface energy. This results in the gradual growth of larger particles at the expense of smaller ones without particle migration.77 While both processes lead to larger particle formation, migration and coalescence involve entire nanoparticles moving and merging, whereas Ostwald ripening relies on atom-by-atom transfer.
The formation of large metallic particles due to migration and coalescence of preformed metal nanoparticles is influenced by factors like temperature, particle size, and metal–support interaction. Higher temperatures increase the mobility of nanoparticles, promoting their migration and potential coalescence when particles come into close proximity. Smaller particles tend to be more mobile due to their high surface energy, leading them to migrate more readily than larger particles. Additionally, the interaction between the metal and the support material plays a crucial role; weak metal–support interactions can facilitate particle mobility, while stronger interactions can stabilize particles and reduce the likelihood of migration and coalescence.
Specific surface area is an important factor that can influence the sintering behavior of metal nanoparticles. However, the catalyst that exhibited the most pronounced sintering, Fe/SiO2, was supported on the material with the highest specific surface area (according to the supplier, SiO2: 200 m2 g−1, MgO: 7 m2 g−1, Si3N4: 113 m2 g−1. For the MgAl2O4 spinel, the SSA measured by N2 sorption is 148 m2 g−1. Therefore, under the harsh reaction conditions applied in this study (750 °C, reducing atmosphere, 2 hours), the influence of surface area on preventing the sintering of the preformed colloids can be reasonably excluded.
In view of the previous results, it is clear that the nature of the support greatly influences the final type of carbon nanostructures, where other factors like temperatures, reaction conditions and characteristics of preformed FeNPs remained constant. Meanwhile SiO2 led to large migration, coalescence and sintering; other supports like MgO and Si3N4 preserved the nanometric size of FeNPs, even under harsh conditions. Interestingly, MgAl2O4 showed an intermediate behavior, limiting the degree of sintering but promoting the formation of long-range carbon nanotubes.
The oxyphilic character of catalytic supports plays a crucial role in determining the stability of supported metal nanoparticles, particularly under harsh thermochemical conditions. A key factor is the enhancement of metal–support interactions through the formation of formal metal–oxygen bonds, which reduces nanoparticle mobility and sintering. A relevant descriptor in this context is the adhesion energy, as proposed by Campbell et al., which depends on the surface oxygen density, the chemical nature of the support, and the size and composition of the metal nanoparticles. In addition to metal–oxygen bonding, certain oxyphilic supports such as CeO2 or TiO2 can stabilize nanoparticles via oxygen vacancies. These defective sites are generally considered nucleophilic and can act as anchoring or stabilizing centers for metal particles.78
In contrast, nitrogen-containing supports such as Si3N4, BN, and C3N3 lack surface oxygen and are therefore less effective at stabilizing metal nanoparticles through conventional metal–oxygen bonding. However, these materials can be engineered to contain nitrogen vacancies, which serve as effective anchoring sites for metal species. Additionally, they offer the potential for the formal incorporation of metal single atoms into their lattice structure, providing alternative stabilization pathways beyond conventional metal–support interactions.79–81
Campbell et al. correlated experimental observations with thermodynamical calculations to predict the strength of metal–support interactions.82–84 In this model, the chemical potential of hemispherical metal nanoparticles supported on model planar surfaces are described by two predictors: the surface energy (γmetal) of the metal particle (which is highly dependent on the particle size) and the adhesion energy (Eadh), dependent on the oxophylic nature of the support (Fig. 10).
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Fig. 10 Schematic representation of a metal nanoparticle on a generic oxidic support, and the estimation of its adhesion force. Adapted with permission from ref. 83. Copyright 2017 American Chemical Society. |
The predicted Eadh agrees with expected trends, where adhesion energy per surface oxygen atom increases with decreasing tendency of certain chemical compounds to form oxides, i.e., the weaker the oxidic support holds its oxygen atom, the larger is the adhesion energy per mole of surface oxygen atoms.
The adhesion energies were calculated considering the same initial FeNPs size, and chemical nature of the metal nanoparticle. Values of enthalpies of reduction were taken from literature and normalized per oxygen atom.82–85 As expected, SiO2 holds the lowest adhesion energy (−27 kJ mol−1 O) leading to a poor FeNP–SiO2 interaction and thus, large migration and coalescence. On the other hand, MgO and MgAl2O4 give rise to values of 79 kJ mol−1 O and 102 kJ mol−1, respectively. Thus, predicting a higher interaction within the preformed Fe colloids and the support, in agreement with the experimental observations. Therefore, it is expected that highly oxophylic supports (e.g., spinel MgAl2O4, perovskites and CeO2) can preserve the nanometric size of preformed colloids and show promising activity towards CH4 cracking at high temperatures. Nevertheless, it should be mention that this is a simplified model that does not predict simultaneous chemical transformations due to, e.g., preferential diffusion of Fe into the MgO, Fe carbides formation under CH4 decomposition or large particle size changes due to thermal effects.
This study explores pre-formed FeNPs deposited on various supports as model catalytic sites for methane decomposition. The results enable the selection of an optimal support for the growth of micrometer-scale carbon nanotubes (CNTs), providing insights into the active phase and growth mechanisms under controlled conditions.
Fe/SiO2 formed FeC3 during methane decomposition, but severe sintering and carbon encapsulation led to complete deactivation. Fe/MgO was rapidly deactivated by encapsulation, yet the support stabilized FeNPs, preventing extensive sintering even under high temperatures and reducing conditions. Surprisingly, FeNPs were also stabilized on Si3N4, though carburization led to the formation of a protective carbon nitride surface layer.
The most active catalyst for CNTs formation was Fe/MgAl2O4. However, the harsh reaction conditions yielded a mixture of carbon structures, including nanofibers, multiwalled CNTs, and encapsulated FeNPs. Beam-enhanced in situ TEM confirmed a base-growth mechanism, with FeNPs remaining anchored to the support.
Despite using identical FeNPs, the oxophylic nature of the support s a key descriptor influencing catalytic activity in terms of carbon yield and the nature of the formed nanostructures. MgAl2O4 demonstrated an optimal balance between Fe–O–Mg–Al interactions and nanoparticle reactivity, making it an excellent support for CO2-free H2 and CNTs formation via CH4 decomposition.
The MgAl2O4 support was synthesized via the co-precipitation method with a Mg2+/Al3+ molar ratio of 2:
1. To obtain 5 g of the calcined catalyst, an aqueous solution (114 ml) with a total molarity of 1 M was prepared, containing 19.9 g of Mg(NO3)2·6H2O (99%) and 14.5 g of Al(NO3)3·9H2O (≥98%). This solution was added dropwise into 228 ml of a 1 M Na2CO3·10H2O (99%) solution (65.2 g) at 60 °C under constant stirring. The pH was maintained at 10.5 by the controlled addition of 3 M NaOH (approximately 200 ml). All reagents were purchased from Sigma-Aldrich. The resulting precipitate was aged for 1 h under the same synthesis conditions, subsequently filtered, washed until reaching a neutral pH, and dried overnight at 60 °C. The dried material was then subjected to calcination in static air at 800 °C for 12 h, employing a heating rate of 10°C min−1.
Octadecene (99%), oleic acid (70%, technical grade) was purchased from Sigma-Aldrich, Germany. Iron oxide hydroxide (FeO(OH), 99%) was obtained from Carl Roth, Germany. Acetone was obtained from Honeywell Riedel-de-Haën, Germany.
The reaction time was settled in 60 min, followed by cooling down naturally at room temperature. In a final step, the colloidal nanoparticles were recovered from the organic suspension by adding 25 ml of a hexane/ethanol mixture 30:
70% v/v. and the product could be easily recovered by centrifugation at 9000 rpm for 10 min. The procedure was repeated 3 times. The final product was easily dispersed and stored in hexane, forming a stable suspension of 15 mg Fe ml−1.
The catalytic experiments were carried out at atmospheric pressure and 750 °C. 50 mg of the powder sample was loaded and heated to 300 °C with a heating rate of 5 K min−1 under vacuum for 2 h. Afterwards, the catalysts were activated under 100 ml min−1 flow of 50% H2/He. After 5 minutes, hydrogen was switched off and 50 ml min−1 CH4 was fed, leading to 50% CH4 in He. The reaction was kept for 90 minutes. XRD diffractograms were collected from 20° to 55° and a scan rate of 1.3° min−1 at different temperature steps and at room temperature before and after each experiment.
In situ TEM experiments were performed in a FEI Titan ETEM operating a 300 kV. A differential pumping system is employed for the dosing of reacting gases into the microscope column. For the sample preparation, a few milligrams of the MgAl2O4 support are dispersed in 2 ml of absolute ethanol and homogenized to have a stable suspension. One microliter of the suspension is drop-casted on the center of the wildfire® microchip (Denssolutions, previously cleaned with plasma) and left to room temperature for drying. Afterwards, one microliter of 1:
1000 dilution of FeNP was drop-cast and left drying at room temperature. Employing this strategy, it is possible to image not only supported FeNPs but also free-standing nanoparticles in the edges of the silicon windows of the chip.
For the experiment, the sample was heated to 700 °C under 1 mbar H2 employing a heating rate of 11 °C min−1 and kept for 3 h. Afterwards, CH4 was fed reaching a total pressure in the column of approximately 2 mbar. For the beam-enhanced experiment, the electron beam was focused over the specimen leading to an electron dose of 3·103 e− Å−2 s−1. The micrographs were acquired with an acquisition of 2 frames per second.
Scanning electron microscopy studies (SEM) were performed on a Helios 5 Hydra Dual Beam (ThermoFisher Scientific) operating a 5 kV and 0.2 nA. Samples were prepared by direct contact with the powder catalysts on Lacey carbon 400-mesh gold grids (Agar scientific).
Raman spectra were recorded using the 647 nm emission of a Krypton ion laser (Innova 300c, Coherent) for excitation and a confocal Raman spectrometer (Lab Ram HR-800 Jobin Yvon) equipped with a liquid-nitrogen cooled charge-coupled device (CCD) camera for data acquisition. The typical laser power at the sample was 1 mW. Spectra were acquired for 5 × 10 s.
XPS data were collected using the Theta Probe X-ray Photoelectron Spectrometer from Thermo Scientific™ with a monochromatic Al Kα X-ray source (1486.68 eV). The XPS spot size was set to 400 μm, the pass energy to 50 eV, and the step size to 0.1 eV. For each core level, 50 scans were averaged. The data analysis and peak fitting was performed using Avantage software.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d5ta03667d |
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