Open Access Article
Abdul Hamid
*a,
Yusuf Widayantoa,
Zeni Rahmawati
*b,
Misbakhul Fataha,
Tri Esti Purbaningtiasc,
Tri Wahyunid and
Ike Dayi Febrianaa
aDepartment of Mechanical and Industrial Engineering, Politeknik Negeri Madura, Sampang, Indonesia. E-mail: ahamchimie@poltera.ac.id
bChemistry Department, Faculty of Science and Data Analytics, Institut Teknologi Sepuluh Nopember, Surabaya, Indonesia. E-mail: zeni.rahmawati@its.ac.id
cChemistry Department, Faculty of Mathematics and Natural Sciences, Universitas Islam Indonesia, Yogyakarta, Indonesia
dDharma Wanita 1 Senior High School, Pare, Kediri, Indonesia
First published on 26th November 2025
Sodalite was successfully synthesized from natural kaolin as a nanocatalyst for biodiesel production using Reutealis trisperma oil (RTO). The synthesis of sodalite was conducted at crystallization temperatures of 80, 100 and 120 °C. The pure sodalite phase was formed at a crystallization temperature of 100 °C, as confirmed by characterization using FTIR spectroscopy and XRD. The sodalite catalyst demonstrated outstanding performance in the catalytic conversion of RTO into biodiesel. The optimum biodiesel yield and conversion achieved under a molar ratio of oil to methanol of 1
:
30 using the S-100 catalyst were 94.14% and 81.79%, respectively. Unlike conventional CaO or NaOH catalysts, kaolin-derived sodalite provides a low-cost, reusable alternative with enhanced efficiency. This study demonstrates the potential of sodalite as a sustainable nanocatalyst, supporting clean energy development and contributing to the United Nations Sustainable Development Goals, particularly SDG 7 (Affordable and Clean Energy) and SDG 13 (Climate Action).
Holilah et al. reported the production of biodiesel derived from RTO using a homogeneous NaOH catalyst.7 The feasibility of utilizing non-edible Reutealis trisperma oil as a novel carbon feedstock for biodiesel production was evaluated. The kernels contained 50–52 wt% oil when extracted using the hot pressing method. Crude oil was directly converted into biodiesel without prior purification. Methanol concentration, reaction temperature, and catalyst loading were identified as critical parameters for achieving a high biodiesel yield. Under the optimized conditions, a maximum yield of 95.15% was obtained at 65 °C. Rahmawati et al. presented a study focusing on RTO biodiesel derived through transesterification using a CaO–ZnO catalyst.8 Parameters, including the methanol-to-oil ratio, reaction time, and Ca/Zn composition, were optimized using the Taguchi method. Statistical analysis indicated similar contribution percentages for the reaction time and the Ca/Zn composition parameter, each around 35%, while the methanol-to-oil ratio showed a contribution of 26.6%. The optimal conditions predicted using the S/N ratio were a Ca/Zn composition of 1, reaction time of two hours, and methanol-to-oil ratio of 30, which resulted in an optimum yield of 98%. The study also suggested that RTO could potentially be used as crude oil for biodiesel production.
The efficiency of biodiesel production largely depends on the catalyst employed in the transesterification process. Based on the previous explanation, homogeneous catalysts, such as NaOH, are widely used due to their high reactivity, but they suffer from drawbacks such as soap formation, catalyst recovery challenges, and wastewater generation.9,10 Heterogeneous catalysts, like CaO, offer better separation but are prone to leaching, which reduces their stability and reusability.11 Mixed oxide systems, such as CaO–ZnO, can improve activity but still face limitations in terms of long-term durability and synthesis complexity.12 Zeolite-based catalysts have also been applied due to their well-defined pore structure and thermal stability. However, their synthesis often relies on expensive commercial precursors, such as sodium aluminate or colloidal silica, restricting their large-scale application.13 To address these limitations, sodalite-type zeolite has emerged as a promising heterogeneous catalyst due to its strong basicity, thermal stability, and cage-like structure, which enhance the catalytic activity. Importantly, sodalite can be synthesized from natural kaolin, which is an abundant and inexpensive clay mineral that is rich in silica and alumina. Kaolin is widely distributed in Indonesia, particularly in the Bangka Belitung Islands.14 The abundant availability of kaolin in Bangka Belitung provides a strategic opportunity to develop value-added applications beyond conventional uses. The utilization of kaolin as a precursor reduces synthesis costs and promotes the use of local, sustainable resources for catalyst development.15 Furthermore, converting kaolin into advanced catalytic materials for biodiesel production exemplifies a circular-economy approach in which natural resources are upgraded into high-performance, environmentally friendly technologies. This approach represents a significant step toward more sustainable and affordable biodiesel production. Table 1 summarizes the various catalysts employed in biodiesel production from Reutealis trisperma oil (RTO), along with their respective advantages and disadvantages. This work aims to synthesize sodalite from natural kaolin at different crystallization temperatures, characterize its physicochemical properties, evaluate its catalytic activity in biodiesel production from non-edible Reutealis trisperma oil, and measure its effect on diesel engine emissions.
| Catalyst | Reaction conditions | Biodiesel yield (%) | Advantages | Disadvantages | References |
|---|---|---|---|---|---|
| Sodium hydroxide (NaOH) | 1 hour, 70 °C, 1 wt%, 1 : 6 |
96.38 | High yield, fast reaction and widely available | Not reusable, sensitive to free fatty acids (FFA), leading to soap formation, produces wastewater (environmental issue) | Supriyadi et al.16 |
| ZnO from limestone | 3 hours, 65 °C, 5 wt%, 1 : 15 |
52.34 | Heterogeneous and reusable, cheap and abundant natural source, more eco-friendly than homogeneous | Long reaction and high methanol ratio, limited activity without modification | Shalihah et al.17 |
| Potassium hydroxide (KOH) | 1.5 hours, 60 °C, 0.5 wt%, 1 : 60 |
95.29 | High yield and fast reaction | Not reusable, sensitive to free fatty acids (FFA), leading to soap formation, more expensive than NaOH, produces wastewater (environmental issue) | Riayatsyah et al.18 |
| CaO–ZnO | 1 hour, 60 °C, 3 wt%, 1 : 30 |
94.7 | High yield, synergistic effect improves activity | Complex preparation and risk of metal leaching | Rahmawati et al.19 |
| KOH impregnated CaO | 1 hour, 60 °C, 7 wt%, 1 : 12 |
97.95 | High yield, short reaction | Preparation is more complex, risk of K leaching | Kusmiyati et al.20 |
| CaO from limestone | 2 hours, 60 °C, 1 wt%, 1 : 1 |
56.13 | Cheap, sustainable (natural resource), reusable and eco-friendly | Low yield, requires high calcination temperature | Suprapto et al.21 |
| Sodalite from natural kaolin | 2 hours, 65 °C, 4 wt%, 1 : 30 |
94.14 | High yield, sustainable (kaolin abundant in Indonesia), high surface area, reusable, better stability than simple oxides | Requires synthesis (hydrothermal/alkaline), activity may drop after reuse | This work |
| Sample | Si/Al molar ratio | NaOH/kaolin molar ratio | Crystallization temperature (oC) | Crystallization time (h) |
|---|---|---|---|---|
| S-80 | 2 | 1.5 | 80 | 24 |
| S-100 | 2 | 1.5 | 100 | 24 |
| S-120 | 2 | 1.5 | 120 | 24 |
A stirring speed of 600 rpm was selected to ensure homogeneous dispersion of the precursors without causing excessive turbulence, which might disrupt crystal nucleation. Crystallization temperatures of 80, 100, and 120 °C were chosen to evaluate the influence of thermal energy on sodalite phase formation. Lower temperatures favor slow nucleation, intermediate temperatures provide balanced crystal growth, and higher temperatures accelerate crystallization but may lead to secondary phase formation. According to previous studies, most zeolite crystallizations occur within the temperature range of 80–150 °C over a 24 h period. Therefore, this study aims to investigate the effect of crystallization temperature on sodalite phase formation.
FTIR characterization was performed using a Nicolet Avatar 360 IR spectrometer employing KBr pellets and a wavenumber range of 500–1400 cm−1 to identify the functional groups present in the catalysts. In addition, the solids were characterized using a SEM–EDX instrument (Hitachi FlexSEM 100) to examine the morphology and elemental composition of the catalysts. The catalysts were coated with Pd/Au for 15 s under a pressure of 6 × 10−2 mbar using the ion-sputtering coating method before being mounted on a carbon tape base. Meanwhile, the pore volume, surface area, and pore size of all samples were determined using nitrogen adsorption–desorption measurements with a Quantachrome NovaTouch LX4 instrument. Prior to analysis, the samples were degassed at 300 °C. The surface areas and pore size distributions were analyzed using the Brunauer–Emmett–Teller (BET) and Barrett–Joyner–Halenda (BJH) methods, respectively.
:
1 molar ratio, followed by the addition of a 2% (w/w) H2SO4 catalyst at 65 °C and stirring at 900 rpm for 2 h for the esterification process. The esterified product was subsequently subjected to the transesterification process. In this process, methanol was first reacted with a 1% (w/w) S-80 catalyst under continuous stirring, followed by the addition of pre-esterified oil. The molar ratios of methanol to oil used in the transesterification process were 20
:
1 and 30
:
1. Transesterification process was carried out at 65 °C with stirring at 900 rpm for 2 h. The resulting mixture was allowed to settle into two layers. The biodiesel layer was then analyzed using GC-MS. The same procedure was repeated using the S-100 and S-120 catalysts.
The conversion and biodiesel yield were analyzed using gas chromatography-mass spectrometry (GC-MS, Shimadzu QP 2010 SE) equipped with an RTX capillary column (length 30.0 m, internal diameter 0.25 mm, and film thickness 0.25 µm) at a flow rate of 0.46 mL min−1. The injector temperature was set to 250 °C, while the oven temperature was initially held at 80 °C and then increased to 300 °C at a heating rate of 10 °C min−1. Methyl heptadecanoate was used as the internal standard in this study. The conversion and methyl ester yields were calculated using the following equations:24,25
:
0 to C24
:
1), Ais is the internal standard peak area, Cis is the internal standard concentration (g mL−1), Vis is the internal standard volume (ml) and ms is the sample mass (mg). The produced biodiesel was also analyzed for exhaust gas emissions, including NO, NOx, and CO, using a gas analyzer with various fuel blend compositions.
Table 3 summarizes the diffraction peaks (2θ values), corresponding phases, and products formed in kaolin, S-80, S-100, and S-120 samples. When the crystallization temperature increased to 100 °C and 120 °C (samples S-100 and S-120), only sodalite peaks remained, accompanied by the complete disappearance of kaolinite signals. This confirms that higher crystallization temperatures promote the total conversion of the kaolinite structure into sodalite. The absence of kaolinite reflections indicates that the layered structure of kaolin has been entirely reorganized into the sodalite framework. These findings emphasize the critical role of temperature in governing phase transformation: lower temperatures allow the coexistence of mixed phases, while higher temperatures favor the complete crystallization and phase purity of sodalite, which is desirable for applications requiring uniform zeolitic properties.
| Sample | Phase (2θ) | Product | |
|---|---|---|---|
| Kaolinite | Sodalite | ||
| Kaolin | 12.31°, 20.38°, 24.78°, 35°–40°, 35.86° and 45.69° | — | Kaolinite |
| S-80 | 12.36°, 19.91°, 24.91°, and 38.94° | 13.94°, 24.26°, 31.82°, 34.61°, and 42.68° | Kaolinite and sodalite |
| S-100 | — | 13.94°, 24.26°, 31.82°, 34.61°, and 42.68° | Pure sodalite |
| S-120 | — | 13.94°, 24.26°, 31.82°, 34.61°, and 42.68° | Pure sodalite |
The transformation of the kaolinite phase into sodalite, as observed from the FTIR spectra, is shown in Fig. 3. The absorption bands of kaolin were observed at 1116, 1029, 913, 791, 755, 694, and 540 cm−1. The Si–O stretching vibrations appeared at peaks around 1107 and 1029 cm−1,32 while the Al–OH stretching vibrations were detected at approximately 913 cm−1, indicating the deformation of hydroxyl (OH) groups within the inner and surface regions of kaolinite.33,34 The skeletal vibration of Al–O in Al[O(OH)]6 was observed at around 541 cm−1.35 The absorption bands at 755 and 795 cm−1 correspond to the symmetric stretching of Si–O–Al,34 while the band at 694 cm−1 is attributed to Al–O–H vibrations.36 In addition, the absorption band at 540 cm−1 corresponds to Al–O deformation. The S-80 sample displayed the kaolinite phase, as indicated by slightly flattened peaks at 1116, 1029, and 913 cm−1, along with a sharp peak at 540 cm−1. This observation is consistent with the XRD results, which confirmed that the kaolinite phase was formed at a crystallization temperature of 80 °C. Some unreacted kaolinite remained in the synthesized product at this temperature, hindering the complete formation of sodalite, as verified by XRD analysis. The characteristic absorption band of sodalite, shown in Fig. 3, includes a peak at 988 cm−1, corresponding to the asymmetric stretching vibration of T–O–T (where T = Si or Al).36 Additionally, peaks at 723 cm−1 and 659 cm−1 indicate symmetric stretching vibrations of T–O–T.37 The band at 697 cm−1 is associated with Al–O–H vibrations, while the band at 558 cm−1 corresponds to the deformation of Al–O.
The results summarized in Table 4 indicate that, at higher crystallization temperatures (S-100 and S-120), the disappearance of kaolinite-specific bands and the dominance of sodalite vibrations (988, 723, 659, 697, and 558 cm−1) confirm a complete structural transformation. This progression demonstrates that higher temperatures provide sufficient energy for the full reorganization of layered kaolinite into a three-dimensional sodalite framework. These findings are significant, as they corroborate the complementary XRD evidence. At lower temperatures, incomplete transformation leaves residual kaolinite, while at higher temperatures, pure sodalite with well-defined framework vibrations is obtained. This structural evolution is crucial for catalytic applications, where the purity and crystallinity of sodalite strongly influence its performance.
| Sample | Absorption bands (cm−1) | Vibration assignments |
|---|---|---|
| Kaolin | 1116, 1029 | Si–O stretching vibrations |
| 913 | Al–OH stretching (inner/surface OH deformation) | |
| 791, 755 | Symmetric stretching of Si–O–Al | |
| 694 | Al–O–H transformation | |
| 540 | Skeletal vibration of Al–O in Al[O(OH)]6 | |
| S-80 | 1116, 1029 (weak) | Si–O stretching vibrations (kaolinite residuals) |
| 988 | Asymmetric stretching vibration of T–O–T (T = Si or Al) – sodalite | |
| 913 (weak) | Al–OH stretching (kaolinite residuals) | |
| 723, 659 | Symmetric stretching vibration of T–O–T – sodalite | |
| 697 (weak) | Al–O–H vibration – sodalite | |
| 540 | Skeletal vibration of Al–O (kaolinite phase) | |
| S-100 and S-120 | 988 | Asymmetric stretching vibration of T–O–T (T = Si or Al) – sodalite |
| 723, 659 | Symmetric stretching vibration of T–O–T – sodalite | |
| 697 | Al–O–H vibration – sodalite | |
| 558 | Al–O deformation – sodalite |
| Samples | Phases | Relative crystallinity (%) | Elemental composition (% weight) | Si/Al (mole ratio) | ||
|---|---|---|---|---|---|---|
| Si | Al | Na | ||||
| S-80 | Kaolin and sodalite | 82.69 | 22.03 | 21.44 | 18.52 | 0.99 |
| S-100 | Sodalite | 63.16 | 23.56 | 22.02 | 19.20 | 1.03 |
| S-120 | Sodalite | 100 | 24.59 | 22.36 | 19.03 | 1.06 |
The SEM–EDX analysis of the S-100 and S-120 samples revealed similar surface morphologies characterized by irregular spherical aggregates, as shown in Fig. 4. However, the S-80 sample exhibited a slightly oval-shaped morphology of kaolin, marked by a red circle. The remaining plate-like kaolin structures indicated the presence of unreacted kaolinite at low synthesis temperatures. The particle size distribution analysis, obtained from SEM images using ImageJ software, showed that sodalite particles were predominantly 10–20 nm in size, as shown in Fig. 5. In contrast, S-120 exhibited a slightly larger particle size distribution (∼20 nm) compared to the other samples. At low temperatures (80 °C), kaolin does not fully dissolve, resulting in the incomplete release of Si and Al into the synthesis gel and leaving some Al trapped within the kaolinite layers, which lowers the effective Si/Al ratio in the product. At higher temperatures (100–120 °C), kaolin dissolution becomes more complete. However, since Al–O bonds are stronger than Si–O bonds, aluminum dissolves more slowly than silicon. Consequently, increasing the crystallization temperature promotes greater incorporation of Si into the sodalite framework, slightly raising the Si/Al ratio.
The EDX results confirmed that the S-80, S-100, and S-120 samples contained the key elements of sodalite (Si, Al, Na, and O), as shown in Fig. 5 and Table 1. The S-80 sample exhibited lower Si and Al distributions compared to the S-100 and S-120 samples, indicating limited silica and alumina dissolution at lower temperatures. The Si/Al molar ratio increased slightly from 0.99 (S-80) to 1.03 (S-100) and 1.06 (S-120), reflecting greater silica incorporation into the sodalite framework with rising crystallization temperatures. A balanced Si/Al ratio enhances basicity and facilitates triglyceride activation during transesterification. The optimal ratio in S-100 provided sufficient basic sites and structural stability, while S-120, despite a slightly higher ratio, showed reduced surface area and mesoporosity, limiting active site accessibility and slightly lowering biodiesel yield (93.44%). Thus, the superior catalytic performance of S-100 results from its favorable morphology and optimal Si/Al ratio.
The largest particle sizes among all sodalite samples were approximately 120–140 nm. During sodalite synthesis, silica and alumina polymerization occurred to form amorphous aluminosilicate particles, which were subsequently organized into a three-dimensional structure due to electrostatic interactions between the particles, forming a rigid gel network. At relatively low crystallization temperatures, the solubility of aluminosilicate species decreased, leading to mixed-phase formation with incomplete sodalite crystallization.38
The nitrogen adsorption–desorption isotherm of the sodalite samples is shown in Fig. 6. For the S-80 sample, nitrogen adsorption was relatively low at relative pressures (P/P0) between 0 and 0.7. Meanwhile, a higher amount of nitrogen adsorption was observed at relative pressures (P/P0) between 0.7 and 1. At a P/P0 of approximately 0.7, the surface of the catalyst became covered by nitrogen molecules, resulting in the formation of a monolayer.39 Subsequently, a significant increase in the volume of adsorbed nitrogen was observed, indicating the presence of a hysteresis loop, which is characteristic of mesoporous materials. The hysteresis loops in S-100 and S-120 appeared larger than those in S-80.
![]() | ||
| Fig. 6 N2 adsorption–desorption isotherms and pore size distribution (insets) of S-80 (a), S-100 (b) and S-120 (c). | ||
The difference in the number of adsorbed and desorbed nitrogen molecules causes a hysteresis loop to occur. Based on the isotherm pattern in Fig. 6, the sodalite samples exhibited a type IV isotherm profile, which represents the characteristics of a solid with a mesoporous structure. Type IV isotherms are characterized by several distinct stages. In the initial stage, nitrogen molecules were gradually adsorbed onto the surface of the material as the relative pressure (P/P0) increased to below 0.7. At this relative pressure, isothermal capillary condensation occurred, initiating the formation of multilayer adsorption.39
In the following stage, the pronounced increase in nitrogen adsorption at a relative pressure (P/P0) of 0.7–0.95 indicates the filling of mesopores with nitrogen molecules, corresponding to multilayer adsorption on the pore walls. The surface area obtained from the N2 adsorption–desorption analysis using the BET method is presented in Table 6. The largest surface area was observed for S-100 (Table 6). The surface area of synthesized sodalite samples (22.59 m2 g−1), followed by S-80 and S-120 (19.34 m2 g−1 and 15.85 m2 g−1, respectively). The three samples exhibited mesoporous structures, with pore diameters ranging from 2 to 14 nm, as shown in Fig. 6. The highest pore size intensity was observed for S-100 and S-120 at a diameter of around 8.29 nm. This observation is further supported by the higher mesopore surface areas of samples S-100 and S-120, which were 16.89 m2 g−1 and 12.05 m2 g−1, respectively (Table 6). This indicates a reduction in the amorphous sodalite phase with increasing crystallization temperature, as observed when the temperature was increased from 100 to 120 °C. The total pore volume and micropore surface area of the catalyst samples also decreased as the crystallization temperature increased owing to the higher degree of crystallinity in the sodalite samples.
| Samples | SBET (m2 g−1) | Smicro (m2 g−1) | Smeso (m2 g−1) | Pore size (nm) | Vol total (cm3 nm−1 g−1) |
|---|---|---|---|---|---|
| S-80 | 19.34 | 7.49 | 11.85 | 8.26 | 0.049 |
| S-100 | 22.59 | 5.7 | 16.89 | 8.29 | 0.046 |
| S-120 | 15.85 | 3.81 | 12.04 | 8.29 | 0.044 |
At low crystallization temperatures (around 80 °C), kaolinite remains largely undissolved in an alkaline solution, resulting in only partial breakdown of the Si–O–Al framework. Because the dissolution of silica and alumina species is limited, the polymerization and condensation reactions required to form the zeolitic sodalite framework cannot proceed efficiently. As a result, kaolinite plate-like morphologies are still visible, and XRD patterns show residual kaolinite peaks, indicating that the transformation into sodalite has not yet occurred. This incomplete dissolution hinders the development of mesoporosity and limits the availability of active basic sites for catalysis. When the crystallization temperature is increased to 100 °C, the dissolution of alumina and silica becomes more effective, allowing reorganization into a sodalite framework characterized by the formation of β-cages. This balance results in pure sodalite with moderate crystallinity and the highest mesoporous surface area, enhancing catalytic accessibility. At 120 °C, however, higher thermal energy drives more extensive crystallization, producing sodalite with higher crystallinity but diminished mesoporosity. The collapse of secondary pores and the growth of larger crystals reduce the BET surface area and the number of external catalytic sites, which explains the slight decline in biodiesel yield and catalytic activity.
The composition of the RTO based on the GC-MS analysis is illustrated in Fig. 7. In general, RTO contains palmitic, linoleic, stearic, linolenic, and oleic acids. The highest contents were linoleic (33.21%) and linolenic acids (20.75%). The free fatty acid (FFA) content of the feedstock is one of the important parameters that influences the transesterification reaction. The FFA content in RTO is 2.87%. A low FFA content is required to maximize biodiesel yield during the transesterification reaction, as a high FFA content can cause saponification and soap formation, leading to a decrease in conversion and yield.40
Saponification is prevented from occurring during transesterification because it could not only reduce biodiesel yield but also inhibit the separation of esters from glycerol. Consequently, feedstocks with a high FFA content need to be pretreated through an esterification reaction. This reaction is particularly useful for oils or fats with a high FFA content. The FFA content of biodiesel samples produced using various catalysts and oil-to-methanol ratios is depicted in Fig. 8. The optimum FFA content obtained using the S-120 catalyst was 0.43% at a molar ratio of 1
:
30 (oil-to-methanol). The lowest oil-to-biodiesel conversion (63.25%) was achieved using the S-80 catalyst at a molar ratio of 1
:
20 (methanol-to-oil), as shown in Fig. 8.
![]() | ||
| Fig. 8 FFA content of the biodiesel samples with variations in the catalyst and oil-to-methanol ratios. | ||
The highest oil conversion (81.79%) was obtained using the S-100 catalyst at a molar ratio of 1
:
30 (methanol-to-oil). The optimum methyl ester yield achieved using S-100 was 94.14% at a molar ratio of 1
:
30 (oil-to-methanol), as shown in Fig. 10. The high biodiesel yield is attributed to the presence of NaOH on the surface of sodalite during synthesis. However, the yield slightly decreased when the S-120 catalyst was used, reaching 93.44%, despite maintaining the same oil-to-methanol ratio. In principle, a large amount of methanol can contribute to the reaction, which benefits the final product, although it may involve some drawbacks, such as a higher cost. Nevertheless, under heterogeneous conditions, methanol excess can be valuable because glycerol dissolves in methanol, facilitating the removal of by-products from the catalyst surface and supporting catalyst reuse.41 As displayed in Fig. 9 and 10, the oil-to-methanol molar ratio can significantly influence the reaction outcome, where increasing the ratio from 20
:
1 to 30
:
1 is sufficient to enhance both conversion and biodiesel yield. Additionally, the loss of active sites on sodalite can be attributed to reduced structural stability, as the S-120 catalyst exhibits a lower surface area and mesoporosity. A high concentration of NaOH in the synthesis solution also promotes the formation of Si–O–Na groups within the zeolite structure, which act as active sites during the transesterification process and contribute to the increased biodiesel yield.
The superior catalytic performance of S-100 can be directly attributed to its higher mesopore surface area (16.89 m2 g−1), which provides more accessible active sites for the transesterification reaction. In heterogeneous catalysis, mesopores (2–50 nm) play a crucial role in facilitating the diffusion of bulky triglyceride molecules and methanol into the catalyst framework. The larger mesoporous channels in S-100 reduce mass transfer limitations, allowing the reactants to reach internal active sites more efficiently than in S-80 and S-120. As a result, the reaction kinetics are accelerated, ensuring that triglycerides are more completely converted into methyl esters. This enhanced accessibility explains why S-100 achieved the highest biodiesel yield (94.14%) and conversion (81.79%).
The reuse of the S-100 catalyst was investigated over consecutive reaction cycles under the following conditions: a catalyst loading of 4 wt%, a reaction time of 2 hours, a methanol-to-oil molar ratio of 30
:
1, and a reaction temperature of 65 °C. The results indicated that the methyl ester yields obtained were 94.14%, 90.31%, 84.23%, and 79.68% for the first–fourth cycles, respectively, as illustrated in Fig. 11. The overall reduction in methyl ester yield from the first cycle (94.14%) to the fourth cycle (79.68%) was 14.46%. The gradual decline in catalyst activity with increasing reuse cycles during biodiesel production can be attributed to the fouling of the active sites and the progressive occupation of these sites on the catalyst surface by unreacted triglycerides.46 This phenomenon resulted in a reduction in both porosity and specific surface area, thereby decreasing the methyl ester yield. Nevertheless, the yield obtained after four consecutive cycles remained relatively high, indicating that the catalyst can be effectively reused for up to four cycles before significant deactivation occurs. Similar findings have been reported by other researchers on the reuse of heterogeneous catalysts for biodiesel production, where a decline in biodiesel yield was observed after multiple cycles.47–49
The data in Table 7 show that catalytic performance in biodiesel production generally decreases with successive cycles, indicating catalyst deactivation over time. Canola oil with Mg–Zr/CaO, waste frying oil with MoO3/RHA–CoFe2O4, and Reutealis trisperma oil with sodalite (S-100) exhibit relatively high initial yields (>94%) but a gradual decline across four cycles. This reduction can be attributed to several factors, including pore blocking or fouling by glycerol, which physically blocks access to active sites and reduces the surface area and pore volume. In addition, other causes include leaching and the chemical loss of active species in heterogeneous basic catalysts (e.g., CaO and Na-bearing materials). Alkali or alkaline earth ions can dissolve into methanol or water phases, or form carbonates and soaps, leading to the loss of catalytic basic sites. For example, Mg–Zr/CaO decreased from 96.7% to 84% over four cycles, while sodalite-based catalysts decreased from 94.14% to 79.68%, suggesting that alkaline catalysts are prone to leaching in methanol-rich environments, reducing their reusability. Interestingly, palm kernel shell ash exhibited the most stable reusability, maintaining yields above 89% even after the fourth cycle. This could be due to its carbonaceous and mineral composition, which resists leaching and maintains surface basicity. In contrast, phosphate mesoporous zirconia impregnated with CaO showed the fastest deactivation, with the yield decreasing from 86.49% to just 63.33%, likely due to significant CaO leaching and pore blockage. These comparisons highlight that while high biodiesel yields can be achieved in the first cycle with various catalysts, long-term stability is highly dependent on catalyst structure, resistance to leaching, and the ability to withstand carbon deposition or poisoning during repeated use.
| Feedstock | Catalyst | Yield (%) | References | |||
|---|---|---|---|---|---|---|
| First cycle | Second cycle | Third cycle | Fourth cycle | |||
| Canola oil | 7.5% Mg–Zr/CaO | 96.7 | 91.3 | 88.1 | 84 | Talebi et al.42 |
| Used palm cooking oil | Palm kernel shell ash | 99.01 | 94.41 | 91.70 | 89.49 | Novita et al.43 |
| Waste frying oil | 30-MoO3/RHA-CoFe2O4 | 94.6 | 94.5 | 91.1 | 89.1 | Gonçalves et al.44 |
| Used palm cooking oil | Phosphate mesoporous zirconia impregnated with calcium oxide | 86.49 | 83.02 | 78.37 | 63.33 | Sambara et al.45 |
| Reutealis trisperma oil | S-100 (sodalite) | 94.14 | 90.31 | 84.23 | 79.68 | This work |
Catalyst regeneration in biodiesel production is a crucial step in restoring activity after multiple reaction cycles, as heterogeneous catalysts are prone to fouling, leaching, and surface poisoning. Two of the most common regeneration strategies are washing and calcination, each of which addresses different deactivation mechanisms. The washing-based regeneration method involves cleaning the spent catalyst using solvents (e.g., methanol, ethanol, hexane, or acetone) to remove adsorbed organic residues, such as unreacted triglycerides, glycerol, free fatty acids, and soaps. These residues typically block the pores and cover the active sites, reducing catalytic efficiency. Solvent washing dissolves these organic deposits, while acid washing (using dilute HCl or acetic acid) is sometimes employed to remove carbonate deposits or neutralize surface soaps.50 This method is relatively mild and preserves the catalyst's structure, making it suitable for catalysts with limited thermal stability, such as zeolites. However, calcination-based regeneration relies on thermal treatment in air at elevated temperatures (typically 400–600 °C, depending on the catalyst material). This process decomposes and burns off carbonaceous deposits (coke), polymerized glycerol, and residual hydrocarbons, leaving behind a cleaner surface and reopening blocked pores. Calcination is particularly effective for solid base catalysts; however, excessive heating may cause sintering, phase transformation, or collapse of porous structures, thereby reducing surface area and limiting reusability.51
The FTIR spectra of biodiesel created from RTO are depicted in Fig. 12. The absorption band at 3484 cm−1 was associated with the O–H bond stretching vibration, while the sharp peaks at 2933 cm−1 and 2853 cm−1 were linked to the asymmetric and symmetric vibrations of CH bonds in CH2 and CH3 groups, respectively. The band at 1747 cm−1 corresponded to the C
O stretching vibration of the triglyceride carbonyl group.52 Absorptions in the 1500–1200 cm−1 range were attributed to the bending vibrations of aliphatic CH2 and CH3 groups. Peaks at 1463 cm−1 and 1379 cm−1 represented the bending vibrations of HCH and CH2. The absorption at 1164 cm−1 was due to the stretching vibration of the C–O ester. The peak at 723 cm−1 indicated overlapping vibrations of (CH2)n.53 The stretching vibrations of CH, CH2, and CH3 were evident in the 2700–3500 cm−1 range, while their bending vibrations were observed in the range of 700–1500 cm−1.54
Fig. 13 illustrates the NO and NOx emission results for each tested fuel blend. The highest NO emission was observed for the B50 blend (256.34 ppm), whereas the lowest was recorded for B10 (232.34 ppm). Similarly, the NOx emission reached a maximum of 268.67 ppm for B50 and a minimum of 243.92 ppm for B10. The NO and NOx emission levels are influenced by the oxygen content in the combustion chamber and are associated with elevated combustion temperatures. As the oxygen concentration increases, NOx emissions tend to rise accordingly.55,56 The concentrations of NO and NOx emissions were found to increase with higher biodiesel blending ratios compared to pure diesel fuel.57,58
The carbon monoxide (CO) emission results for biodiesel–diesel fuel blends are presented in Fig. 14. The highest CO emission (278.67 ppm) was recorded for pure diesel (D100), whereas the lowest (170.44 ppm) was observed for B50. The maximum CO emission reduction efficiency achieved was 38.84%. An increase in the biodiesel blending ratio led to a significant reduction in CO emissions. The formation of CO during combustion is an exothermic process, commonly referred to as catalytic oxidation. Carbon monoxide is produced when there is insufficient oxygen during combustion, resulting in incomplete oxidation of carbon atoms to carbon dioxide.59 CO emissions depend on oxygen availability, carbon content, and combustion efficiency. During combustion, the carbon in the fuel is oxidized, converting CO to CO2. A lack of oxygen leads to incomplete combustion, producing higher CO emissions.55,60 Similar findings were reported by Fareed et al., who observed a consistent trend in their emission studies, where increasing biodiesel blend ratios resulted in lower CO emission levels.61
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