Eka Putra Ramdhaniab,
Eko Santosoa,
Holilah Holilahc,
Reva Edra Nugrahad,
Hasliza Bahrujie,
Suprapto Supraptoa,
Aishah Abdul Jalilfg,
Nurul Asikin-Mijanh,
Syafsir Akhlusa and
Didik Prasetyoko*a
aDepartment of Chemistry, Faculty of Science and Data Analytics, Institut Teknologi Sepuluh Nopember, Keputih, Sukolilo, Surabaya 60111, Indonesia. E-mail: didikp@chem.its.ac.id
bDepartment of Chemistry Education, Faculty of Teacher Training and Education, Raja Ali Haji Maritime University, Dompak, Tanjungpinang, Indonesia
cResearch Center for Biomass and Bioproducts, National Research and Innovation Agency of Indonesia (BRIN), Cibinong, 16911, Indonesia
dDepartment of Chemical Engineering, Faculty of Engineering, Universitas Pembangunan Nasional “Veteran” Jawa Timur, Surabaya, East Java 60294, Indonesia
eCentre of Advanced Material and Energy Sciences, Universiti Brunei Darussalam, Jalan Tungku Link, BE 1410, Brunei
fCentre of Hydrogen Energy, Institute of Future Energy, Universiti Teknologi Malaysia, 81310, Skudai, Johor Bahru, Johor, Malaysia
gDepartment of Chemical Engineering, Faculty of Chemical and Energy Engineering, Universiti Teknologi Malaysia, 81310, Skudai, Johor Bahru, Johor, Malaysia
hDepartment of Chemical Sciences, Faculty of Science and Technology, Universiti Kebangsaan Malaysia, 43600 UKM Bangi, Selangor, Malaysia
First published on 31st October 2023
Conversion of red mud (RM) that contains a high level of silica, alumina and iron minerals into heterogenous catalysts, offers a route for the utilization of abundant toxic by-products of bauxite refining. In this study, the conversion of red mud into mesoporous Fe-aluminosilicate produced selective catalysts for the deoxygenation of waste cooking oil to green diesel hydrocarbons. Direct conversion of red mud in the presence cetyltrimethylammonium bromide into Fe-aluminosilicate (RM-CTA) produced a highly mesoporous structure with oligomeric Fe2O3 clusters within the pores. When red mud was treated with citric acid (RM-CA-CTA), a wide distribution of Fe2O3 particles was obtained on the aluminosilicate external surface. TEM analysis showed a well-defined hexagonal mesoporosity of Fe-aluminosilicate obtained from untreated red mud, while the treated red mud produced lower regularity mesopores. RM-CTA exhibits 60% WCO conversion and 83.72% selectivity towards liquid products with 80.44% diesel hydrocarbon (C11–C18) yield. The high selectivity was due to the high acidity of Fe-aluminosilicate to dissociate the C–O bond and the regularity of mesostructure for efficient hydrocarbon diffusion, preventing a cracking reaction.
Various studies have been carried out to seek routes for producing fuel from biomass waste, for instance, via esterification,22 hydrocracking,23 and deoxygenation.24 Esterification of fatty acid biomass requires methanol to produce fatty acid methyl ether (FAME), in which the methanol is currently generated from fossil fuel-derived syn-gas (CO + H2). The use of methanol can be avoided via hydrocracking or deoxygenation of fatty acid to form hydrocarbon biofuels. Hydrocracking removes oxygen from fatty acids via reduction under hydrogen gas at high pressure, enhancing the biofuel properties.25 On the other hand, the deoxygenation reaction removes the carbonyl group from fatty acids to generate hydrocarbon and CO/CO2 gases.26 Global consumption of biomass-derived fuel is expected to increase every year to compensate for the depletion of oil reserves.27 Green diesel is an environmentally friendly renewable fuel, generated from sustainable and renewable resources. The quality of green diesel depends on the efficiency of catalytic process, while the use of biomass waste reduced production costs and minimized waste production. Waste cooking oil (WCO) contains oleic acid and linoleic acid, suitable for conversion to green diesel.28 Vegetable oil production and consumption continue to increase, generating large amounts of WCO. Cooking at high temperatures and long hours generates a variety of toxic chemicals, raising trans-fat proportion in the oil, generating free radicals, and causing other potentially detrimental effects.29 Repeated frying causes dissolved oxygen in the oil to react with unsaturated acylglycerols, resulting in the development of various products such as dimeric and polymeric acids, dimeric and acylglycerols polyglycerol which increases the viscosity of cooking fat.30 Food processing industries and restaurants are the largest WCO producers, contributing to 47% of WCO production in the world.31 Thus, WCO conversion to green diesel while utilizing catalysts from red mud serves as an efficient waste management system to improve the value-added properties of the two industrial wastes.
Noble metals such as Pd,32 Pt,33 and Ru34 are generally employed as catalysts in deoxygenation reactions. Transition metal catalysts such as Fe and Ni have shown promising activity as heterogeneous catalysts for deoxygenation reactions.35,36 Fe complex has been employed in homogeneous decarbonylation of aliphatic carboxylic acid that showed high selectivity to α-olefins, although toxic phosphine ligand is required for the synthesis of Fe-complex catalyst. Heterogeneous Fe catalyst prevented the breakdown of C–C bonds in biomass and encouraged the hydrogenation of the C–O bonds.37,38 Ni metal catalyst reduced the polymerization of unsaturated hydrocarbons that resulted in the formation of coke.39 This study utilized hematite minerals in the red mud to generate mesoporous Fe-aluminosilicate. Red mud was used directly without chemical treatment and after citric acid treatment to synthesize Fe-aluminosilicate. Characterization analysis revealed the effect of citric acid treatment on the mesoporosity of Fe-aluminosilicate and the formation of Fe2O3 species. The synthesized Fe-aluminosilicates were employed as catalysts in the deoxygenation of waste cooking oil to produce green diesel hydrocarbon. The high selectivity of Fe-aluminosilicate exhibits the advantage of utilizing iron minerals in the red mud to transform WCO into green diesel hydrocarbons.
Catalyst | SBETa (m2 g−1) | Smesob (m2 g−1) | Vb (c g−1) | Db (nm) | Element compositionc (%) | Acid sitesd (μmol g−1) | ||||
---|---|---|---|---|---|---|---|---|---|---|
Al Si Fe | O | Brønsted | Lewis | |||||||
a SBET (specific surface area) by the BET method.b Smeso (mesopore surface areas), V (volume) and pore diameter by DFT method.c Elemental composition estimated by SEM-EDS.d Lewis Brønsted acid sites by pyridine adsorption. | ||||||||||
RM | 56.95 | 57.13 | 0.284 | 13.68 | 26.77 | 19.13 | 10.72 | 41.51 | 5 | 13 |
RM-CTA | 786.99 | 733.84 | 0.548 | 3.77 | 3.74 | 48.93 | 3.72 | 42.60 | 69 | 84 |
RM-CA-CTA | 383.17 | 162.43 | 0.302 | 5.65 | 3.11 | 36.07 | 0.95 | 58.18 | 10 | 9 |
The synthesis method was repeated on treated red mud with citric acid. Red mud was treated by adding 1 M citric acid solution (red mud/acid ratio 1:5 g ml−1) to dried red mud and stirring at 90 °C for 2 h. The mixture was centrifuged to separate the powder from the supernatant. The solid was dried at 110 °C for 12. The synthesis followed similar procedures to produce RM-CA-CTA.
(1) |
(2) |
(3) |
(4) |
The aluminosilicate catalysts are observed by a broad amorphous peak as the typical pattern of amorphous aluminosilicate.42 Characteristic peaks of Fe2O3 and other Fe species were not found for RM-CTA and RM-CA-CTA samples, which suggested that iron species might be in the framework or highly dispersed on the surface of the catalyst.43 The low-angle XRD patterns of RM-CTA and RM-CA-CTA are shown in Fig. 1b. A peak at 2θ = 2.2° was observed in RM-CTA and RM-CA-CTA catalysts, indicating the presence of mesoporous hexagonal pore arrangement.44 The difference in peak intensity suggests that the RM-CTA catalyst has a higher mesoporous regularity than RM-CA-CTA.
FTIR analysis of RM, RM-CTA, and RM-CA-CTA catalysts was determined to see vibrational changes in the red mud and the synthesized catalysts (Fig. 2). In general, there are no significant changes in the FTIR bands apart from the changes in intensity. Red mud and the synthesized Fe-aluminosilicate catalysts exhibit the absorption bands at 1629, 1230, 1082, 960, 796, 570 and 457 cm−1, which can be assigned to different tetrahedral framework atoms vibrations in the silicate structure. The broad absorption band near 3400 cm−1 and the peak at 1629 cm−1 are attributed to the hydroxyl vibration mode of the surface Si–OH groups.45 The intensity enhanced on the synthesized catalysts, suggesting the incorporation of a high-density water or OH group in the structure. The peaks at 1082 and 796 cm−1 were attributed to external linkage vibrations in the silicate structure. The broad peak at 1082 cm−1 is assigned to asymmetric Si–O–Si vibrations, while the peak centered at 796 cm−1 is due to the symmetric Si–O–Si vibrations. The absorption peak at 960 cm−1 is assigned to the Si–OH.46 The peak at 570 cm−1 assigned to Fe–O bending vibration was reduced on the Fe-aluminosilicate, which implies the reduction of Fe concentration.47,48 The characteristic band of Si–O–Si (SiO4 tetrahedron) bending vibrations appeared at 457 cm−1.49
Fig. 3 shows the infrared spectra of the RM, RM-CTA, and RM-CA-CTA catalysts in 1400–1650 cm−1 following adsorption with pyridine. The pyridine ring vibration is analyzed to determine the concentration of Brønsted and Lewis acid sites.50 The Brønsted acid site is evaluated using the pyridinium ion band at 1545 cm−1. Lewis acid site is determined from the pyridines that are coordinated to Al3+ at 1450 cm−1. Pyridine-FTIR spectra on all catalysts show three peaks at 1545, 1450 and 1490 cm−1. These peaks appeared at a lower intensity on RM and RM-CA-CTA compared to RM-CTA catalysts. The band at 1490 cm−1 is attributed to the vibration of the pyridine ring on both Brønsted and Lewis acid sites in the RM, RM-CTA, and RM-CA-CTA catalysts.51
Quantitative analysis of the peak area provides the amount of Brønsted and Lewis acid sites in RM, RM-CTA, and RM-CA-CTA as summarized in Table 1. The highest number of Brønsted acid sites of 69 μmol g−1 and Lewis acid sites of 84 μmol g−1 were measured in the RM-CTA catalyst. Aluminosilicate produced from treated red mud, RM-CA-CTA has lower Brønsted and Lewis acid sites than Fe-aluminosilicate, RM-CTA. Analysis was also conducted on the red mud that indicates a small number of acid sites, presumably arising from the amphoteric properties of alumina and hematite. The acidity of aluminosilicate is generated from the Al atoms, in which at a high ratio of silica/aluminium (Si/Al), the high proportion of Al compared to Si enhanced the amount of Brønsted acid sites.52 There is a possibility that Fe presence in the aluminosilicate further contributed to the Lewis acidity of Fe-aluminosilicate. High oxidation states of Fe, either as Fe(II) or Fe(III) possess Lewis acid properties.53 During bond dissociation, the Fe species can coordinate with oxygen or nitrogen atoms of the CO and CN double bonds.54 A large surface area of RM-CTA generates a higher extra framework aluminium and might also expose more Fe species on the surface, enhancing the overall number of acid sites.
The textural properties of the RM measured using the N2 adsorption–desorption analysis showed a mixture of type II and type IV isotherms (Fig. 4a). This indicates that RM consists of a large mesopore with a broad pore size distribution up to a macropore size.55 The hysteresis loop is narrow, with the adsorption and desorption branches almost vertical at P/P0 above 0.8. The N2 adsorption–desorption analysis indicates the red mud has a 56.95 m2 g−1 of external surface area.56 The RM-CTA isotherm shows a steep step at P/P0 = 0.2–0.4 due to nitrogen condensation in the primary mesoporous, as a characteristic of type IV isotherm (Fig. 4b).57 Type IV isotherm has three regions of mild N2 uptake at low relative pressure, indicating monolayer N2 adsorption. The sharp inflection between 0.4 < P/P0 < 0.95 implies the capillary condensation in the mesopore.58 The RM-CA-CTA catalysts have type IV isotherm with type H4 hysteresis, indicating the presence of slit-shaped and non-uniform size mesopores.59
Fig. 4 N2 adsorption–desorption isotherm and pore size distribution of RM (a), RM-CTA (b), RM-CA-CTA (c). |
Fig. 4a–c shows the pore size distribution obtained from the nitrogen adsorption isotherm. RM-CTA shows a narrow mesopores distribution with an average diameter of ∼3.77 nm. RM-CA-CTA catalyst shows multiple adsorptions between 2–6 nm with an average pore size of 5.65 nm. The resulting aluminosilicate catalysts contained mesoporosity, indicating upgraded textural properties compared to the red mud. Table 1 shows the calculated pore size, pore volume, and mesoporous volume of the RM, RM-CTA, and RM-CA-CTA catalysts. The RM-CTA catalyst has the highest SBET of 786.99 m2 g−1, followed by RM-CA-CTA at SBET of 383.17 m2 g−1. RM-CTA has a large pore volume of 0.548 cm3 g−1 followed by RM-CA-CTA at 0.302 cm3 g−1, and RM at 0.284 cm3 g−1.
The surface morphology and elemental mapping of the RM, RM-CTA, and RM-CA-CTA catalysts can be seen in Fig. 5a–f. SEM analysis of red mud (RM) shows non-uniform aggregates with a homogenous distribution of Fe in the minerals (Fig. 5a–c). Slightly different morphology was observed on RM-CTA and RM-CA-CTA catalysts, with approximately rounder and larger crystallites. No significant differences can be observed in the morphology of the two catalysts. The EDS analysis showed a homogeneous distribution of Fe particles. The elemental analysis in Table 1 showed that 3.75% of Fe was detected on RM-CTA, and 0.95% of Fe was analyzed on RM-CA-CTA. Fe concentration was significantly lower than the red mud (10.72%), suggesting the dissolution of hematite has occurred that reduced the incorporation of Fe into the aluminosilicate framework. Further reduction of Fe concentrations on RM-CA-CTA implied the removal of Fe has occurred during citric acid treatment of red mud. The concentration of Si is also higher in RM-CA-CTA than RM-CTA, indicating the aluminosilicates have different efficiencies in incorporating the additional colloidal SiO2 in the framework during hydrothermal synthesis. EDS data show a slightly similar amount of aluminium in the RM-CTA and RM-CA-CTA catalysts, at 3.74%, and 3.11%, respectively (Table 1).
Fig. 5 SEM analysis of RM (a), RM-CTA (b), RM-CA-CTA (c), EDX mapping of RM (d), RM-CTA (e), RM-CA-CTA (f). |
Fig. 6 displayed the TEM analysis of the mesoporous RM-CTA and RM-CA-CTA catalysts. RM-CTA shows a well-defined, two-dimensional mesopore channel estimated at 3.15 nm diameter. The average mesopore diameter is approximately similar to the pore diameter obtained from N2 analysis. The RM-CA-CTA exhibited less-defined mesoporous structures compared to RM-CTA. The results are in agreement with the low-angle XRD analysis in Fig. 1b. The results derived from TEM analysis confirmed the formation of mesoporous long-range order of Fe-aluminosilicate obtained from direct synthesis using untreated red mud. The TEM analysis of RM-CA-CTA also showed the formation of spherical Fe2O3 particles, with high density contrast due to the difference in electronic density between Fe and aluminosilicate.60 The diameter of Fe2O3 was estimated between 5-15 nm, indicating the deposition of Fe2O3 on the external surface of aluminosilicate. However, no visible dark shade particles were observed on RM-CTA, presumably due to no large Fe2O3 crystallites were formed that can be detected using TEM.
H2-TPR analysis was conducted to support further the results obtained in UV-visible analysis. Fig. 7b showed two main peaks at 254 °C and 366 °C on the RM-CTA catalyst. The reduction of isolated Fe2O3 within the aluminosilicate domain occurred at ∼250 °C.65 The reduction of oligomeric Fe2O3 to FeO occurred at the temperature range of 350–450 °C,66 with no reduction profiles detected at higher temperatures up to 800 °C. The spatial constraints of the uniform porous channel of the aluminosilicate restricted further reduction of FeO into Fe0. The slight increase at temperatures above 800 °C is due to the disintegration of the aluminosilicate framework, allowing further reduction of FeO to Fe.67,68 On RM-CA-CTA catalyst, the isolated extra-framework Fe2O3 species were observed at a slightly low temperature of 250 °C. The reduction of Fe3+ to Fe2+ occurred at 360 °C, slightly lower than RM-CTA. The shift to lower temperatures implies that the ferric species in RM-CA-CTA are present at the external surface or outside the pore of aluminosilicate, therefore more susceptible to reduction.63 RM-CA-CTA also showed continuous H2 uptakes at high temperatures, suggesting the continuous release of framework Fe(III) for further reduction that might occur via the successive reduction of Fe2O3 → Fe3O4 → FeO → Fe.66
Fig. 8 Selectivity and conversion product (a) selectivity of liquid products (b), hydrocarbon selectivity from catalytic deoxygenation (c) of RM-CTA and RM-CA-CTA. |
Fig. 8c divides the hydrocarbon yields into gasoline (C8–10), diesel (C11–18), and heavy oil (C18) composition. The catalysts mainly produced diesel (C11–18) with more than 80% selectivity. However, RM-CTA also produced heavy oil with C18 hydrocarbon products, while no C18 hydrocarbon was analyzed from RM-CA-CTA catalysts. Both catalysts produced short-chain hydrocarbons (C8–C14) at approximately similar selectivity of ∼9%, which confirmed the hydrocracking occurred during the deoxygenation reaction. Deoxygenation and hydrocracking required solid acid catalysts to dissociate the C–C bonds and increase oil conversion to hydrocarbons. However, it was suggested that hydrocracking mainly occurs on Brønsted acid sites, while the deoxygenation reaction requires a high concentration of Lewis acid.69
The deoxygenation temperature, LHSV (Liquid Hourly Space Velocity), and the temperature used during catalyst preparation can have an impact on the composition of by-products in the deoxygenation process as well.79 The catalytic deoxygenation of WCO using Fe-aluminosilicate catalyst produces green diesel hydrocarbon via two primary processes, namely decarbonylation (DCO) and decarboxylation (DCO2). The WCO comprises C12:0 to C20:3 fatty acid molecules, with 40.02% oleic acid (C18:1) and 34.72% palmitic acid (C16:0).72 Straight-chain hydrocarbons formed through DCO/DCO2 reactions, removing carboxylate and/or carbonyl fragments from fatty acids.73 The proposed mechanism of WCO conversion to green diesel hydrocarbon was depicted in Scheme 1. The first reaction step is the β-elimination of hydrogen to break triglyceride C–C bonds, forming one unit of carboxylic acid/fatty acid.74 The carboxylic acid subsequently undergoes decarboxylation/decarbonylation (deCOx) reaction, removing the carbonyl group as CO2 and CO gases, producing hydrocarbon with one less carbon chain from the parent fatty acid. H2 is generated in situ during the decarbonylation process via the water gas shift reaction.75 The ketone compound was also observed in this study via ketonic decarboxylation of carboxylic acid.76 The formation of mono-aromatic compounds involves the dehydrogenation reaction of cycloalkane compounds with six carbon atoms and alkenes, while polyaromatics are formed through polymerization and dehydrogenation reactions of mono-aromatic compounds or intramolecular radical cyclization mechanisms.77,78
The Fe2O3 position in the aluminosilicate strongly influenced the reaction mechanism. Non-treated red mud produces aluminosilicate with small Fe2O3 clusters predominantly confined in the well-defined hexagonal mesopores. The highly dispersed Fe2O3 increased the Lewis acidity of the RM-CTA catalysts, which is crucial to catalyze C–O bond dissociation. Studies on Fe-based catalysts for the hydrodeoxygenation of aromatic compounds suggested the importance of maintaining the stability of Fe species.70 Fe tends to interact with the oxygen atom on the carbonyl group as the main step towards deoxygenation reaction.71 The synergy between high acidity and uniform mesoporosity produces selectivity towards long-chain hydrocarbon. Direct conversion of raw red mud into Fe-aluminosilicate was suggested to provide close crystal growth within the Fe3+ ion, allowing self-assembly of Fe2O3 nanoparticles within the mesopores. This study has revealed the advantage of well-dispersed Fe2O3 in enhancing Lewis acidity, surface area and mesoporosity of aluminosilicate, consequently enhanced deoxygenation of WCO into green diesel hydrocarbons.
However, modification of hematite in the red mud by treating with citric acid significantly altered the mesoporosity of aluminosilicate and the dispersion of Fe2O3. Citric acid reduced the alkalinity of red mud by reaction with the OH− and CO32− anions, forming the citrate compounds.21 Furthermore, organic acid is used to remove iron contamination in minerals such as kaolin and quartz.80 Citric acid acts as a complexing agent to increase the dissolution of iron species.81 Pre-treatment of red mud in citric acid transformed hematite into Fe(III) complex. The dissolution of hematite can be achieved when accompanied by reducing agents such as EDTA or sodium thiosulfate to form Fe(II) complex.82 However, citric acid alone is unable to reduce Fe3+ to Fe2+.83 The adsorption and saturation of citric acid on the hematite surface, forming Fe(III) complex, presumably responsible for forming large Fe2O3 species on aluminosilicate. Furthermore, the changes in alkalinity inadvertently reduce CTAB inclusion during the amorphous gel rearrangement due to poor CTAB and AlO−/SiO− interaction.
This journal is © The Royal Society of Chemistry 2023 |