E.
Duffy
a,
X.
He
b,
E. P.
Nesterenko
b,
D.
Brabazon
b,
A.
Dey
c,
S.
Krishnamurthy
c,
P. N.
Nesterenko
a and
B.
Paull
*ad
aAustralian Centre for Research on Separation Science, School of Physical Sciences, University of Tasmania, Hobart, Tasmania, Australia. E-mail: brett.paull@utas.edu.au
bIrish Separation Science Cluster, National Centre for Sensor Research, Dublin City University, Dublin 9, Ireland
cDepartment of Engineering and Innovation, The Open University, Milton Keynes MK7 6AA, UK
dARC Centre of Excellence for Electromaterials Science, School of Physical Sciences, University of Tasmania, Hobart, Tasmania, Australia
First published on 23rd February 2015
Unique porous carbon monoliths containing thermally annealed carbon onions, were prepared from a resorcinol formaldehyde precursor rod, containing silica gel acting as a hard template, detonation nanodiamond, and Fe3+ as a graphitisation catalyst. Detonation nanodiamond was converted to carbon onions during controlled pyrolysis under N2, where the temperature cycle reached a maximum of 1250 °C. Thermal characterisation and high resolution electron microscopy have confirmed the graphitisation of nanodiamond, and revealed the resulting quasi-spherical carbon onions with an average particle size of 5.24 nm. The bimodal porous composite contains both macropores (5 μm) and mesopores (10 nm), with a BET surface area of 214 m2 g−1 for a nanodiamond prepared monolith (0.012 wt% nanodiamond in the precursor mixture), approximately twice that of blank monoliths, formed without the addition of nanodiamond, thus providing a new approach to increase surface area of such porous carbon rods. Raman spectroscopy and X-ray photoelectron spectroscopy also confirmed an enhanced graphitisation of the monolithic carbon skeleton resulting from the elevated thermal conductivity of the added nanodiamond. TEM imaging has confirmed the nanodiamond remains intact following pyrolysis at temperatures up to 900 °C.
Several excellent reviews on the subject of porous carbon production and applications have recently emerged.7–9 One novel route to the production of porous carbon materials is the formation of so-called carbon monoliths. These typically exhibit a hierarchical porous structure, and are often produced through various templating methods, for example the use of hard and soft removable templates. Silica particles (including mesoporous silica or silica nanoparticles) are commonly used in the hard-templating synthesis of porous carbon monoliths, to facilitate creation of a controlled macroporous structure in the final material. The inorganic template is embedded in the carbon precursor, or the carbon precursor is introduced into the pores of the template. After undergoing carbonisation via pyrolysis, the template is removed, thus generating a porous material with isolated pores or an interconnected pore network. Mesopores may also be created by catalytic graphitisation and this is commonly achieved using a metal ion catalyst, or by the carbonisation of a polymer blend containing a carbon precursor polymer and a decomposable polymer that is removed to produce the pores. Reports on the production of such hierarchical porous carbons with bimodal pore structures have been published,7–10 several of which are based on the polymerisation and carbonisation of silica particle embedded resorcinol formaldehyde (RF) resin, using Fe3+ as a catalyst to enhance graphitisation.10,11
Porous carbon monoliths offer inter-connected channels within their pore network, with a high flow-through permeability, good thermal and electrical conductivity hence their potential application in adsorption or separation processes,10–12 and electrochemical energy storage applications.13 Recently, the use of nanocarbons to form porous carbon monoliths or carbon–carbon composite materials has produced some exciting results, showing considerably enhanced electrochemical properties for potential applications in the above areas.14,15 Indeed, changes to the physical, chemical and electrochemical properties of the nano-composite monoliths have been reported, when compared to simple carbon monoliths without embedded or surface exposed nanocarbons. Physical enhancements include higher specific surface area, greater mesopore volume and a narrower pore size distribution.16 However, to-date such studies are limited in number, and controlled approaches to achieve substantially enhanced properties, e.g. surface area, for such monolithic substrates are rather limited.
It can be expected that with the inclusion of nanocarbons within porous carbon monoliths, there will be a transfer of unique physical–chemical properties to the final composite, provided the nanocarbon is preserved through any carbonisation process. These unique nanocarbon properties have seen them applied in a wide variety of ways in recent times, e.g. in environmental applications as sensors, filters, and sorbents,17 with fullerenes, carbon nanotubes and carbon onions having demonstrated high sorption capacities for organic pollutants and heavy metal contaminants.18 Recently, nanodiamond (ND) has received renewed attention, primarily due to its biocompatibility and potential applications in drug delivery.19,20 Nanoscale diamond (sp3 carbon) may be produced by detonation synthesis, where the detonation soot is purified under oxidative acidic conditions to yield detonation nanodiamond (DND), which is known to have a high thermal conductivity, mechanical stability and surface chemistry readily amenable to functionalisation. Carbon onions may be produced by the thermal annealing of ND21 in an inert atmosphere or under vacuum. They too have a variety of interesting properties (such as high surface area and electrical conductivity), making them of interest for use in supercapacitors,22 lubrication, and in environmental remediation.18
Therefore, herein is described a novel route for the preparation and characterisation of a new porous carbon monolith with significantly enhanced surface area and graphitic character, via embedded carbon onions produced through the controlled thermal annealing of DND during the carbonisation process. The new carbon on carbon composite material was formed by pyrolysis of a precursor rod containing a mixture of RF resin, silica particles and DND, with a Fe3+ catalyst used to increase localised graphitisation. The thermal conductivity of the DND was also expected to enhance the graphitisation process, and the precise thermal conversion of diamond particles to carbon onions during the pyrolysis (to a maximum temperature of 1250 °C) was explored.
Fig. 2(a) shows a low magnification SEM image of a cross section of the precursor rod containing DND prior to undergoing carbonisation. The surface area of the uncarbonised material determined using nitrogen adsorption measurements was a low 55 m2 g−1, with a pore volume of 0.21 cm3 g−1, and an average pore diameter of 15 nm. The isotherm displayed a limiting step after the hysteresis loop suggesting that pores were completely filled during the analysis.
In prior reports on the formation of similar carbon monoliths, thermogravimetric analysis (TGA) has been used to observe the various phases of carbonisation and graphitisation.11,14 Here the impact of DND inclusion on these processes was also observed using TGA, under conditions similar to those used in the normal carbonisation process, although here under argon flow. The TGA curve for DND itself (Fig. 2(b)) shows an initial weight loss of ∼7% between 30–160 °C, which is due to water losses. DND is known to be particularly hygroscopic and can contain multiple layers of water molecules on its surface, including those bound directly to the carbon surface or to the negatively charged surface functional groups. Further layers may also be bound through hydrogen bonds or other non-covalent interactions.26 Following this initial weight loss, the TGA curve shows an unusual slight drift upwards between 200 and 350 °C, followed by a steady decline in weight between 400–900 °C, which is likely due to the removal of surface organic groups27 and the loss of some elemental impurities, which can make up a significant amount of the DND mass (13.8 mg g−1 with large contributions from B, Na, Si, Ca, and Fe).28,29 It is known that the loss of oxygen-containing groups occurs below 900 °C in an inert atmosphere, and of CHx groups between 900–1150 °C.30,31 Above ∼700 °C the graphitisation of the DND normally begins. A total weight loss of 33.7% occurred between 30–1100 °C. It has been shown that DND evolves large quantities of CO2 and CO during thermal annealing.32
During thermal annealing, the DND will become graphitised, as the sp3 hybrid is less energetically stable than the sp2, and graphite is a more stable phase. Graphitisation occurs in a layer-by-layer fashion, from the more reactive surface regions inwards. Xu et al. have studied the thermal annealing of DND in an inert atmosphere, showing that the DND undergoes graphitisation between 670–1100 °C.33,34 As seen in Fig. 2(b), the precursor rod containing DND undergoes 8% weight loss below 200 °C. At lower temperatures these losses can be accounted for as the evolution of water, excess phenol or other low molecular weight compounds, as well as the release of CO, CO2, H2 and other gases.35 During the pyrolysis process, the RF resin undergoes further weight losses, physical shrinkage and pore formation as the condensation of the polymer structure takes place, and the resin is gradually converted to amorphous carbon.36 The total weight loss for the composite material between 30–1100 °C was 26.2%, which is very similar to the total weight loss (25%) observed for carbonisation of a composite monolith prepared with an RF precursor rod containing an Fe3+ catalyst, and a C60-modified silica template.16 However, these losses are both lower than those reported for a similar RF resin, prepared without the addition of any nano-carbons.
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Fig. 3 SEM images showing the porous graphitic carbon monolith with carbon onions. (a) Macroporous network mag X 1 K, (b) mag X 10 K. |
Closer examination of the wall structure of the macropores revealed smooth pore walls with a low instance of raised surface features visible by low magnification SEM imaging. These regions showing irregular raised porous surfaces may be linked to some infiltration of the precursor polymerisation solution in to the 55 nm pores of the silica template. This effect is highly dependent on wetting of the silica particles, as well as the viscosity of the precursor solution. An SEM image showing such areas with irregular surface morphology is shown in ESI Fig. S1.† Furthermore, SEM imaging was performed on cross sections of the uncarbonised monolith precursor and has revealed some instances of accumulation of polymerised resin on the surface of silica beads (highlighted in ESI Fig. S2†). Abundant mesopores were also visible by SEM imaging, and this structure was similar for materials annealed at both 900 and 1250 °C. Examination of monoliths graphitised at the lower temperatures also revealed the presence of surviving DND embedded within the mesoporous walls and attached upon the surface, both as single digit DND (<10 nm) and clusters of up to 100 nm size (see Fig. 4(a)). Surface EDX analysis was performed on the macroporore walls of each of the composite materials, confirming the carbon purity of the composite throughout (Fig. 4(b)). Platinum was detected due to the thin layer of platinum coating the samples to facilitate imaging by SEM. Negligible amounts of Si were also detected in some regions of the macropore walls, although there was no evidence of the Fe3+ catalyst remaining.
Comparison of the carbon monoliths annealed at 900 and 1250 °C using TEM revealed the graphitic nature of the monolith, with localised graphitic structures visible. The RF resin does not undergo full graphitisation, as evidenced by the regions of amorphous carbon also visible within the TEM images. However, the thermal conversion of the DND to carbon onions within the 1250 °C monolith was confirmed. Within this sample no obvious evidence of untransformed DND particles could be seen. These TEM images are shown within Fig. 5. It has previously been shown that carbon onions begin to form in the range of 900–1100 °C under a low vacuum,37 and in the range of 1100–1200 °C in an inert atmosphere.38 In this case the one hour hold period at 1250 °C during pyrolysis was sufficient to quantitatively transform the DND. The carbon onions resulting from the thermal annealing of DND within the monolithic composite are shown in Fig. 5(b). The onions were quasi-spherical in shape, and they had an average diameter of 5.24 nm (±0.85 nm). The average interlayer spacing between the graphitic shells is 3.32 Å, which is between values previously reported for onions with five (3.35 Å) to ten (3.24 Å) shells.38
TEM analysis confirmed that by reducing the maximum temperature of pyrolysis to 900 °C, the DND structures could actually be preserved within the composite material. Fig. 5(c) shows a cluster of intact DND structures present within the final composite material. The DNDs shown were not graphitised at 900 °C and do not show evidence of the graphitisation of their outer layers. It is likely their structure was preserved at this temperature as a result of their being embedded within the carbon monolithic rod. The lattice fringes corresponding to the (111) planes of diamond are clearly visible, and the average interlayer spacing measured on the DND within the composite was 2.06 ± 0.28 Å. The average particle size as observed by TEM was 11.4 ± 0.9 nm, as expected based upon the specification of the commercial sample (5–15 nm particle diameter). However, some DND particles did show partial graphitisation at 900 °C, which agrees with work by Cebik et al., which demonstrated that annealing DND in an inert atmosphere at 900–1000 °C can lead to the conversion of some of the surfaces of ND to layered sp2 carbon.39 DND present at the surface level of the composite material would not experience the same environment as those particles which were embedded in the rod during pyrolysis at 900 °C, and so partial layer-by-layer conversion to sp2 carbon has occurred, as visible in Fig. 5(d). Thus, careful control of temperature of pyrolysis allows control of the nature of the nano-carbons present in the final monolithic composite materials.
Raman spectroscopy was applied to shed further light on the structure of the monolithic composite materials. The disorder in graphite can give rise to several characteristic Raman peaks.40 The 800–2000 cm−1 region in the Raman spectrum shows common features for all carbons. The G and D peaks are typically around 1560 and 1360 cm−1 respectively, for visible excitation.41 The spectrum for the blank porous carbon monolith is also shown in Fig. 6(a). Three peaks were observed in the Raman spectrum for the monolithic composites containing carbon onions (Fig. 6(b)). These three peaks are usually seen for carbonaceous materials with both sp2 and sp3 bonds present. The G band appears at ∼1580 cm−1 and corresponds to the E2g optical mode in a two-dimensional network structure, always seen for sp2 carbon materials. The D band is visible at ∼1335 cm−1 and it is associated with disordered carbon,42 denoting a loss of hexagonal symmetry in the material (for highly ordered pyrolytic graphite, this peak is very small or even negligible, see Fig. 6(c) for comparison). The intensity of the D band to the G band (R = ID/IG) can be used to illustrate the degree of graphitisation in a material. Here, the blank carbon monolithic material showed an R-value of 0.64, and the 1250 °C formed composite monolith gave a value of 0.37 (the R-value for commercial graphite was 0.14), thus confirming the greater graphitic nature of the carbon on carbon composite material. This supports the proposal that inclusion of the DND promotes localised graphitisation, both due to its inherent high thermal conductivity, and self-graphitisation during pyrolysis.
Temperature of pyrolysis is an important factor to consider here, as the composite resin remains a predominantly disordered material following its carbonisation up to 1250 °C. The G′ band is seen to appear at ∼2680 cm−1 and typically appears for sp2 carbon materials resulting from a second order two phonon process.43 These results confirm the presence of both graphitic and amorphous carbon in the carbon framework of the monolithic composites. Analysis by XPS further demonstrated the effect of pyrolysis temperature on partial graphitisation of the composites (Fig. 7). A downshift in the binding energy was observed for the carbon core level (C 1s) spectral comparison of monoliths carbonised at 900 °C (285.5 ± 0.05 eV) and 1250 °C (284.5 ± 0.05 eV) under a nitrogen atmosphere. This observation was similar to that reported by Xie et al. for the annealing of DND at 900 and 1500 °C,44 and within studies by Krishnamurthy and co-workers.23,45 This shift in binding energy relates to the material moving towards graphitisation as a function of the pyrolysis temperature. The binding energy of 284.5 eV for the composite that underwent pyrolysis at 1250 °C is slightly higher than one for graphite (284.4 eV).30 Also evident in the 1250 °C annealed sample, but not featured within the 900 °C sample, was the shake-up feature related to the π to π* transition at around 290.8 ± 0.05 eV, commonly seen in more graphitised materials.
It is widely known that DND typically has a high concentration of structural defects on its surface, which increases the surface reactivity. Pyrolysis of the composites at 900 °C produced some hybrid nanocarbons combining the core properties of ND, with the surface reactivity of sp2-based nanocarbons, as discussed above in relation to Fig. 5(d).46 The production of hybrid nanocarbons is similar in effect to previous work reported by Ostrovidova et al. where ND particles were bonded by a graphite-like matrix in order to produce a high surface area porous nanodiamond composite press-moulded tablet for immobilisation of biomolecules.47
Monolith | S BET a (m2 g−1) | V p a (cm3 g−1) | Pore diameterb (nm) |
---|---|---|---|
a The Brunauer–Emmett–Teller (BET) method was used to calculate specific surface areas. b The Barrett–Joyner–Halenda (BJH) method was used to calculate mesopore diameters from the adsorption branch of the isotherm. | |||
Bare carbon monolith | 115 ± 8 | 0.33 ± 0.05 | 11.7 ± 0.8 |
Carbon monolith with carbon onions | 214 ± 17 | 0.35 ± 0.04 | 10.5 ± 3.9 |
To the best of the authors' knowledge, this is the first report of the controlled production of carbon onions from DND within such a carbon monolithic composite. It demonstrates that the type of nano-carbons present in the final monolithic composite can be tuned, simply by controlling the temperature of pyrolysis.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c5ra00258c |
This journal is © The Royal Society of Chemistry 2015 |