E. saligna charcoal fines showed the following average values: basic density = 0.57 g.cm- 3; extractives = 5.79%; lignin = 25.8%; ash = 0.15%, and porosity = 68.22%. These properties relate directly to pyrolysis products. Basic density and lignin content are relevant for charcoal production, increasing coal volumetric and gravimetric yields and favoring greater biocomposite manufacture8,9. Yield also depends on pyrolysis variables, such as reaction atmosphere, heating rate, and, especially, final temperature (Fig. B – supplementary).
The results show that 400°C pyrolysis obtained the highest yield, 37.15%, whereas 800°C, the lowest, 27.42%; results inversely proportional to pyroligneous liquid yield. Fig. B shows non-condensable gas yields failed to significantly vary with increasing temperatures (supplementary material): 25.7, 23.27, and 22.04% in 400, 600 and 800°C, respectively.
To optimize production, greater charcoal yields favor biocomposite filling due to larger volumes of the material of interest, though its chemical and physical properties will effectively contribute to the synergy of the materials involved in producing carbon biocomposites10. A higher final pyrolysis temperature (600 to 800ºC) increased in 7% the apparent density of charcoal (Fig. 1A).
This behavior is due to intense hydrogen output, an element capable of strong molecular bonds absorbing significant energy in pyrolysis above 500°C11. This relates to the rearrangement of the chemical structure of biomass under heat, producing a graphitic structure that benefits the mechanical resistance of the material12,13. By proposing charcoal as a reinforcing agent in polymeric matrices, we expect increased mechanical strength and developed density in the new material. We hope biocomposites filled with high-temperature charcoal will show higher strength, facilitating their use in structural applications.
Porosity is another relevant parameter for producing biocomposites. Charcoal is highly porous (up to 85% of its volume) and its pore sizes range from sub-nanometers to tens of micrometers, depending on raw materials and pyrolysis temperatures14,15. Fig. 1B shows that higher temperatures result in a more porous charcoal — 800ºC pyrolysis favored their formation. Studies state that the progressive removal of volatile materials from charcoal pores, increased connection of existing pores, and condensation of the remaining skeletal structure cause this behavior14–17. Their immediate chemical composition (Fig. 2) shows that higher pyrolysis temperatures increase the percentage of fixed carbon and, proportionally, the reduction of volatile materials.
Evaluating the immediate chemical composition of charcoal fines as a function of pyrolysis temperature is important for predicting biocomposite performance18. Studies discuss that materials with a higher carbon content provide greater mechanical strength, which can positively increase the resistance of the biocomposites produced19,20. We observe a decrease in the ash content of coal produced at 800°C which may enable a greater interaction between polymeric matrices and charcoal fines due to its high fixed carbon and lower ash contents. We expect these characteristics to provide biocomposites with greater interaction and mechanical resistance. Confocal microscopy images show the increased porosity of charcoal at higher temperatures (Fig. 3).
We identify more pores, usually of a nonpolar nature, in the material produced at 800°C21,22. These characteristics are relevant for using the material as reinforcing agents in biocomposites since they can promote greater adhesion to polymeric matrices, better wetting, and greater mechanical resistance by high impregnation and better spreadability. The literature indicates that a more porous structure allows polymeric resins to fuse and entangle with charcoal, creating a strong interfacial support between fillings and matrices, resulting in improved properties, especially mechanical resistance16,23,24. However, polymer penetration into charcoal pores will depend on the viscosity of the polymer resin and pore size23. We highlight that such aspects depend on particle dimensions of charcoal fines used as filler. Fig. 4 shows the SEM images of charcoal fines produced at different final temperatures.
Charcoal fines have a rough surface, due to pores collapsing and ash filling the porous system. Different temperatures did not produce significant morphological differences, which would require higher heating rates. Despite homogenization, we observe charcoal fines of varied sizes. Pyrolysis conditions influence surface morphology and the physical properties of charcoal fines. This evidences the need for a more rigorous preparation of the material prior to filling biocomposites, and further studies should investigate the nanometric scale in preparing this carbon raw material25. Fig. 5 shows the FTIR spectra of charcoal fines produced at three pyrolysis temperatures and changes to their chemical structure.
The stretching vibration of the asymmetric OH group — referring to phenol, alcohol, carboxylic acid groups, and water — formed a 3663 cm-1 broad peak. The 1671 and 1728 cm-1 peaks refer to the vibration and elongation of the CO double bond, whereas the 1500 cm-1 peaks, to the vibration in the double bond between aromatic carbons with olefins and aromatic structures. On the other hand, 1180 to 1297 cm-1 peaks relate to elongating vibrations of the C-O connection. Fig. 5 shows that higher temperatures affected functional groups, changing coal structures. The formation of hydroxyl groups at 800ºC favors the elevated polarity of the material, profoundly influencing charcoal and polymer matrix interaction in composites26, essential for good mechanical properties27,28. Moreover, the free hydroxyl groups in coal produced at 800ºC allow greater interaction between materials, contributing to the generation of highly compatible composites2,3.
We performed a XPS analysis to understand how the chemical changes to charcoal can contribute to resin interaction. Fig. 6 shows the deconvolution of the XPS spectra of coal fine samples.
Note the spectral region comprising the binding energies characteristic of C1s in the materials synthesized at 400 (Fig. 6A), 600 (Fig. 6B), and 800°C (Fig. 6C). Analysis of C1s spectra showed five peaks related to the different carbon species in charcoal fines. The most intense peak (EB= ~284.0 eV) corresponds to functional states of species with C=C or C-sp2 bonds in aromatic/allophatic carbons29. Due to the nature of the atoms surrounding these species, the binding energy in this peak may undergo small variations due to changes in pyrolysis temperature, since heating affected the chemical composition of the surface30.
Higher pyrolysis temperatures changed the structure and chemical nature of charcoal; attested by the increased intensity of peaks of aromatic/allophatic groups in XPS spectra. As expected, heating develops more compact aromatic carbon structures and more intense spectral peaks. On the other hand, higher temperatures decrease the proportion of functional groups formed by carbon atoms and heteroatoms, especially oxygen, in the composition of charcoal fines31. Table 1 shows this aspect by comparing the mean relative percentages related to the contribution of each carbon species to the total composition of the material.
Table 1
Average percentage of functional states in C1s XPS spectra.
Sample
|
C=C, C-C, C-H
(aromatic, aliphatic carbon)
|
C-O, C-O-C, C-OH
(hydroxyl, ether, phenol)
|
C-O
(ketone)
|
C=O
(carbonyl)
|
O-C=O
(carboxylic acid, ester)
|
CV 400
|
62.1 ± 1.9
|
19.3 ± 0.9
|
10.8 ± 0.7
|
3.9 ± 0.3
|
3.95 ± 0.08
|
CV 600
|
72.1 ± 1.7
|
12.7 ± 2.5
|
7.5 ± 0.5
|
3.4 ± 0.2
|
4.3 ± 0.1
|
CV 800
|
70.4 ± 1.8
|
12.5 ± 1.5
|
7.7 ± 0.8
|
3.8 ± 0.2
|
5.7 ± 0.2
|
Analyzing XPS spectra shows the majority presence of aromatic or aliphatic carbon species, and C-O/C-O-C/C-OH groups (ether, phenol, etc.), C-O (ketone), C=O (carbonyl) and O-C=O (carboxylic acid, ester), located at 284.70 eV, 286.15 eV, 287.75 eV, and 288.80 eV binding energies, respectively30,31. These functional carbon and oxygen groups comprise a smaller proportion of the composition, tending to decrease as temperatures rose from 400 to 600°C. However, they remained stable from 600°C upward since we observed no significant variations in percentage contributions as temperatures neared 800°C.
Note in the XPS spectra (Fig. 6) that the energy of the C-C/C-H group dominates the charcoal composition, intensifying as temperatures increased, whereas oxygen functional groups showed an inversely proportional trend. We can classify the functional groups on the surface of charcoal fines with carbon chains, such as the C-C/C-H group, as hydrophobic; and those containing oxygen, such as C-O/C-O-C/C-OH, C-O, C=O and O-C=O, as hydrophilic31. The hydrophobic surface of charcoal fines improved with higher temperatures, attested by the increased contribution of C-C/C-H species dominating the material composition.
Studies point out that greater hydrophobicity ensures greater polymer compatibility28,32,33. More hydrophobic materials result in better polymer filling and compatibility, evenly incorporating charcoal particles into polymer matrices and improving the tensile strength and flexion of biocomposites22. Thus, charcoal fines could reinforce polymer matrices due to their hydrophobicity which can provide resistance to biocomposites.