3.1. XRD Analysis
XRD patterns of C1-TS sample prepared by pyrolysis at temperatures between 500 and 1000 °C are presented in
Figure 1. The patterns are characterized by broad peaks in the 15–30° and 40–50° regions, indicative of absence of long-range crystallinity. Peaks become larger with the increase in pyrolysis temperature. The pattern of sample C1-TS pyrolyzed at 500 °C contains a shoulder at ~13°, which disappears at higher pyrolysis temperatures. Such a feature could be attributed to the presence of oxygenated species in an analogous manner to graphene or graphite oxide.
The lateral size (L
a) and stacking height (L
c) of graphite nanocrystallites was calculated from XRD patterns via the following Equations (1) and (2).
where λ is the wavelength of the employed X-ray, B
a and B
c are the widths at half maximum of (100) and (002) graphite peaks, and φ
a and φ
c are the corresponding diffraction angles. The corresponding regions in the XRD patterns were deconvoluted with XPSPEAK, Version 4.1 software (Informer Technologies, Inc. Developer: Raymund Kwok).
The d(002) spacing of nanocrystalline graphite has been calculated by Bragg’s equation.
Table 1 presents the parameter values calculated from Equations (1)–(3) for sample C1-TS, which has been prepared from the corresponding resin by pyrolysis at 700–1000 °C. Parameter values could not be obtained from the corresponding XRD pattern of the sample pyrolyzed at 500 °C due to its essentially amorphous nature. The d(002) interlayer spacing is in the range of 0.351–0.363 nm for all samples, which is greater than the value of 0.335 nm corresponding to crystalline graphite. The stacking height, L
c, which indicates the crystallite size along the c axis, does not vary considerably and is in the range of 1.64–1.84 nm. This corresponds to an average number of layers stacking in coherent regions equal to five. The lateral size, L
a, is in the range of 4.18–5.54 nm and appears to increase slightly at the highest pyrolysis temperature employed. The obtained L
a and L
c values are quite low and correspond to highly disordered carbon material. The increase in pyrolysis temperature does not seem to affect significantly the dimensions of these domains, but rather their number density.
The corresponding XRD patterns of C2-Fe samples pyrolyzed at 500–1000 °C are shown in
Figure 2. The crystalline phase of magnetite (Fe
3O
4) is present after pyrolysis at 500 °C. At higher pyrolysis temperatures, magnetite is reduced to metallic iron (2θ = 45°), which catalyzes the graphitization of carbon, as evidenced by the growth of the (002) (2θ = 26°) graphite peak. In addition, the cohenite (Fe
3C) crystalline phase is formed after pyrolysis at 700 °C, whereas small peaks of iron carbide are also present at higher pyrolysis temperatures. The intensity of the graphite (002) peak increases with the increase in pyrolysis temperature from 700 to 1000 °C. The use of FeCl
3 as a catalyst during resin synthesis leads, therefore, to the formation of metallic iron during pyrolysis and, as a result, to the creation of graphitic structures, probably in the vicinity of iron crystallites.
Table 2 presents the parameter values calculated from Equations (1)–(3) for sample C2-Fe, which has been prepared from the FeCl
3-containing resin by pyrolysis at 700–1000 °C. Parameter values could not be obtained from the corresponding XRD pattern of sample pyrolyzed at 500 °C due to its essentially amorphous nature. The d(002) interlayer spacing is in the range of 0.341–0.344 nm for all samples, which is slightly greater than the value of 0.335 nm corresponding to crystalline graphite, but smaller than the values for the C1-TS sample. The stacking height, L
c, which indicates the crystallite size along the c axis, does not vary considerably and is in the range of 4.66–5.52 nm. This corresponds to an average number of layers stacking in coherent regions higher than 13. The lateral size, L
a, is in the range of 14.60–19.63 nm and does not show a specific trend with pyrolysis temperature. The obtained L
a and L
c values are higher than the ones observed over the C1-TS sample, which is indicative of a more ordered carbon material. The increase in pyrolysis temperature does not seem to affect significantly the dimensions of these domains, but rather their number density.
3.2. Nitrogen Physisorption
The N
2 physisorption isotherms for sample C1-TS pyrolyzed at 800 °C and 900 °C are shown in
Figure 3. The isotherms are characterized by wide, open-loop adsorption–desorption branches (Ι and ΙΙ type) and of type H4 hysteresis loop [
14]. The presence of the open hysteresis loop is evidence of the microporous structure of narrow slit-like pores [
15].
The N
2 physisorption isotherms for sample C2-Fe pyrolyzed at 500 °C and 800 °C are shown in
Figure 4. The observed isotherms are of type ΙΙ (500 °C) και IV (800 °C) and, similarly to sample C1-TS, are characterized by open-loop adsorption–desorption branches, which, however, are less wide than those of the C1-TS sample, indicating the existence of micropores and mesopores. The observed hysteresis is of type H2 and at p/p
o = 0.42 the opening of the hysteresis loop becomes smaller as the desorption curve falls rapidly and tends to approach the adsorption branch. It is worth noting that, for both samples, the hysteresis extends to low p/p
o values, which is indicative of non-reversible adsorption of nitrogen in ultra-small pores, with size comparable to the size of the N
2 molecule [
9].
Table 3 presents the specific surface area (SSA), the total pore volume and the micropore volume as calculated using the adsorption/desorption isotherms for both samples. It is noted that the micropore volume was calculated using the t-plot method and de-Boer equation.
As shown in
Table 3, sample C1-TS does not have a porous structure after pyrolysis at 500 °C, the calculated specific area is only 2 m
2 g
−1 and pore volume is 0.0002 cm
3 g
−1. On the other hand, sample C2-Fe after pyrolysis at the same temperature has developed a porous structure with a SSA of 226 m
2 g
−1 and a pore volume of 0.15 cm
3 g
−1. The SSA of sample C1-TS is maximized (135–138 m
2 g
−1) after pyrolysis at 700 or 800 °C, while the maximum SSA (395 m
2 g
−1) of the C2-Fe sample is obtained after pyrolysis at 700 °C. Fitzer et al. [
9] have reported that, during synthesis of glassy carbon from a polyfurfuryl alcohol precursor, the maximum specific surface area appears after pyrolysis at 700 °C. Comparing the micropore volume with the total pore volume, it is concluded that the micropore volume amounts to 70–88% of the total for sample C1-TS and to 83–91% of the total for sample C2-Fe.
As stated above, the presence of open-loop hysteresis for both samples suggests that the pore size is similar to that of the N2 molecule. In sample C2-Fe, the pores are grown up after pyrolysis at 500 °C, whereas for sample C1-TS after 700 °C. Moreover, the presence of Fe favors the creation of mesopores. The maximum specific surface area for sample C1-TS was ~ three times smaller than that for sample C2-Fe, confirming the fact that the presence of Fe promotes the development of a porous structure.
3.4. Raman Spectroscopy
Raman spectroscopy has been proven a versatile technique in studies of carbon-based materials, providing information on crystallinity, defects and disorder; hence, being able to distinguish various graphitic forms. The
sp2 carbon networks of graphite-type materials are characterized by a prominent doubly degenerate (
E2g symmetry) G-band at ~1582 cm
−1 originating from the in-plane bond-stretching motion. [
16,
17]. The Raman spectrum changes appreciably when the crystal size decreases down to the nanometer scale as the D-band appears at ~1350 cm
−1 for visible excitation. The D-band is not Raman active in a perfect, defect-free
sp2 lattice and corresponds to the breathing mode of the
sp2 rings.
Tuinstra and Koenig [
18] were the first to show that the D-band intensity depends upon the crystallite size. They combined Raman and XRD data of several graphitic samples with different crystallite sizes L
a, (in-plane correlation length) and found that the intensity (peak height) ratio of the
D and
G bands is given by
where
C(
λ) is an excitation wavelength-dependent factor; e.g.,
C(514.5 nm) ≈ 44 Å. This model assumes a uniform breakdown of graphite to nanocrystals and has been verified for a minimum of L
a ≈ 2 Å. Later, it was shown [
19] that the D/G band intensity ratio strongly depends on the excitation wavelength according to the relation
where
A denotes the integrated Raman peak area.
Representative Raman spectra of the pyrolyzed materials are shown in
Figure 7. The spectra are composed of broad and overlapping G and D bands. To estimate the influence of the pyrolysis temperature on the crystallite size L
a, using the above relation, the Raman bands have been deconvoluted into Gaussian lines, as shown in
Figure 7. Apart from the G and D bands, as denoted by hatched areas, two additional bands are needed for a reliable fitting of the experimental Raman spectra. These bands, denoted by dashed lines, are located at ~1200 cm
−1 and 1550 cm
−1. Their frequencies are used as free fitting parameters and are scattered by less than ±10 cm
−1 from the above values for the various Raman spectra. These two bands originate possibly from residuals of the pyrolysis process. The band at ~1200 cm
−1 has been assigned to a combination of vinylene and C-H in-plane deformations while the band at ~1550 cm
−1 arises from the stretch of furan rings [
20]. The situation is a bit more complicated for the C2-Fe Raman spectra shown in
Figure 7b, where a reliable band fitting necessitates the use of an additional weak peak, superimposed on the wide D-band. This is more evident for the spectra that correspond to 700, 900, and 1000 °C pyrolysis temperatures. The energy and narrow width of this band testify towards its graphitic origin. The formation of a graphitic phase dispersed in the nanocrystalline/amorphous carbon phase is in agreement with the XRD results that revealed a graphitic phase surrounding Fe nanoparticles.
Ferrari and Robertson proposed a detailed a three-stage mechanism about how the increase in disorder leading from graphite to amorphous carbon affects the spectral features of the Raman bands [
16]. They considered that the Raman spectrum depends upon the following factors: (i) clustering of the
sp2 phase, (ii) bond disorder, (iii) presence of
sp2 rings or chains, and (iv) the
sp2/
sp3 ratio. In the first stage (I), where graphite turns to nanocrystalline graphite, no
sp3 sites are still created and the
G-band shifts from ~1582 cm
−1 to ~1600 cm
−1. In this regime, the intensity ratio
I(
D)/
I(
G) follows the Tuinstra–Koenig prediction [
18]. In the second stage (II), the further increase in defects will turn nanocrystalline graphite to mainly amorphous
sp2 bonded carbon. In Raman spectra, one observes a shift of the G-band to lower wavenumbers, the Tuinstra–Koenig relation fails and the intensity ratio
I(
D)/
I(
G) decreases.
Figure 8a,b illustrate the dependence of various spectral parameters of the G and D bands as a function of the treatment temperature for C1-TS and C2-Fe, respectively. The following observations emerge from these results. (i) The G-band frequency is located at ~1600 ± 2 cm
−1 for both systems and for all temperatures of pyrolysis, apart from the highest one for the C2-Fe, where it shows a slight red-shift to 1590 cm
−1. In the frame of the Ferrari–Robertson model, the G-band energy at ~1600 cm
−1 shows that pyrolysis produces nanocrystalline graphite (stage I of the model), while the small red-shift to 1589 cm
−1 at 1000 °C heralds the incipient transformation of nanocrystalline graphite to mainly amorphous
sp2 bonded carbon (stage II of the model). (ii) The D-band frequency increases systematically with increasing pyrolysis temperature for both C1-TS and C2-Fe. (iii) The full width of the D and G bands follows a common trend, namely, it increases from 700 to 800 °C and then remains practically constant for the C1-TS. On the contrary, the band widths are constant up to 900 °C for C2-Fe while they decrease for the highest temperature. In the present case, the band width is mainly affected by the nanocrystal size and the size distribution. (iv) The
A(
D)/
A(
G) intensity ratio (or the crystallite size L
a) drastically increases (decreases) from 700 to 800 °C and remains constant for higher temperatures.
3.5. Gas Permeation Measurements
The performance of the two carbon membranes (C1-TS and C2-Fe) was evaluated by single gas permeation measurements of H
2, CH
4 and CO
2 using the Wicke–Kallenbach method. Gas permeation measurements of H
2, CO
2 and CH
4 were performed after each cycle of dip-coating/pyrolysis for both samples. The pyrolysis temperature for the initial cycles was 500 °C and was increased stepwise to 700, 800, 900 or 1000 °C in successive cycles. This carbonization scheme was selected based on results of preliminary experiments, which showed that initial carbonization of membranes with few layers at temperatures higher than 500 °C (600–900 °C) leads to membranes with inferior characteristics (lower selectivity) than the ones prepared with initial carbonization at 500 °C. When a switch to higher pyrolysis temperature was made, the membrane was subjected to treatment at the higher pyrolysis temperature without prior additional dip-coating. The results are presented in
Figure 9 and
Figure 10 for the permeance of H
2, CH
4 and CO
2 and the ideal H
2/CH
4 and H
2/CO
2 selectivity of the C1-TS membrane. The results are also provided in tabulated form in
Table S1. The permeance of the blank support tube was of the order of 10
−5 mol m
−2 s
−1 Pa
−1. Deposition of the initial eight membrane layers, which were pyrolyzed at 500 °C, leads to a decrease in the permeance by more than two orders of magnitude, which is not accompanied by an appreciable increase in selectivity. Deposition of four additional layers prepared via pyrolysis at 700 °C leads to H
2/CH
4 selectivity higher than 70 and H
2/CO
2 selectivity around 15. Subsequent deposition of additional layers accompanied by an increase in pyrolysis temperature to 800 and 900 °C leads to a further decrease in permeance without a concomitant increase in selectivity, at least for the H
2/CH
4 pair, while the H
2/CO
2 selectivity attains values around 40. The increase in pyrolysis temperature to 1000 °C causes additional reduction of selectivity to values < 10.
Figure 11 and
Figure 12 present the results for the permeance of H
2, CH
4 and CO
2 and ideal H
2/CH
4 and H
2/CO
2 selectivity, respectively, of the C2-Fe membrane. The results are also provided in tabulated form in
Table S2. Deposition of the initial eight membrane layers that were pyrolyzed at 500 °C leads, similarly to the C1-TS membrane, to a decrease in the permeance by more than two orders of magnitude, which is accompanied by an increase in H
2/CH
4 selectivity to 34, while the H
2/CO
2 selectivity is only 2. After pyrolysis at 700 °C without additional coating, the CH
4 permeance increased approximately two orders of magnitude. Deposition of four additional layers with pyrolysis at 700 °C leads to H
2/CH
4 selectivity of 38 and H
2/CO
2 selectivity less than 10. Subsequent deposition of additional layers with pyrolysis at 800 and 900 °C leads to further decreases in permeance without concomitant increases in selectivity, with the exception of the membrane #18, for which permselectivities increased to H
2/CH
4 = 35 and H
2/CO
2 = 58. The increase in pyrolysis temperature to 1000 °C leads to the loss of membrane selectivity.
The effect of permeation temperature on permeation characteristics of C1-TS#16 and C2-FE#18 membranes is depicted in
Figure 13 and
Figure 14 for H
2, CO
2 and CH
4 permeance, and H
2/CH
4 and H
2/CO
2 selectivity, respectively. The specific membranes were among the ones that showed favorable selectivity results. The gas permeation order for sample C1-TS#16 is H
2 > CO
2 > CH
4 whereas for sample C2-FE#18 is H
2 > CH
4 > CO
2. H
2 permeance increases slightly with temperature for both membranes, indicating an activated diffusion mechanism. The permeance of CO
2 and CH
4 seems to remain unaffected by the permeation temperature for the C1-TS#16 membrane, while it appears to increase slightly with temperature in the case of the C2-FE#18 membrane. The ideal H
2/CH
4 selectivities increase with temperature for both samples, and the same applies for H
2/CO
2 in sample C1-TS#16.