Abstract

A carbonate mineral, dolomite, was used as a heterogeneous catalyst to produce methyl-esters from soybean oil. The samples were analyzed by XRF, TGA, XRD, TPD-CO2, and SEM. The calcination of dolomite at 800°C/1 h resulted in a highly active mixed metal oxides. In addition, the influence of the reaction variables such as the temperature, catalyst amount, and methanol/soybean oil molar ratio in methyl-ester production was optimized by the application of a central composite design in conjunction with the response surface methodology (RSM). The XRF analysis is carried out after the reuses procedure which shows that the deactivation process is mainly due to the selective calcium leaching. Overall, the calcined dolomite exhibited high catalytic activity at moderate operating conditions for biodiesel production.

1. Introduction

The increase in the number of publications addressing the topic biodiesel in recent years is noticeable [1]. This is due to the environmental benefits that the biodiesel fuel provides [2]. Conventional biodiesel production is performed through a transesterification reaction of triglycerides with mono-alkyl alcohols (i.e., methanol and ethanol) [3]. Homogeneous alkaline catalysts have been widely used since the process produces high amount of methyl-esters in a short reaction time [4, 5]. In order to solve the problem related to the purification step, solid base catalysts have been considered as an alternative to homogeneous base catalysts [6, 7].

Occasionally, the synthesis processes of heterogeneous catalysts can contribute to an additional cost of the final product. However, the use of a simple, safe, and low cost heterogeneous catalyst for the biodiesel production reaction can be effective to an industrial application [8, 9].

Dolomite is a natural carbonate mineral typically represented by a stoichiometric chemical composition of CaMg(CO3)2 [10]. During the calcinations, the carbonate groups are decomposed generating their respective basic oxides (MgO and CaO) [11, 12]. The alkaline oxides CaO and MgO are frequently used as heterogeneous catalysts for biodiesel production [1315]. Therefore, the solid dolomite catalyst, which is an environmentally acceptable material with high basicity and low cost, is possibly an efficient and promising alternative catalyst for biodiesel production.

Several studies [11, 1620] have reported the use of calcined and/or modified dolomite as a solid catalyst for biodiesel production; however the operating conditions involved a longer reaction time with high methanol/oil ratio and catalyst weight, none of which are commercially attractive features for a catalyst. In order to study the optimum reaction conditions for the catalytic activity of dolomite in transesterification reaction of triglyceride to methyl-esters, a central composite design and a response surface methodology (RSM) were employed. The experimental design and RSM is a useful statistical technique that involves multiple regression analysis and fewer experimental runs for designing experiments, constructing models, evaluating the effects of factors, and analysing the optimum conditions of factors for optimization processing [21, 22].

It is known that the catalytic performance is highly dependent of the operating conditions (reaction temperature, catalyst amount, and methanol/oil molar ratio) as well as the temperature heat treatment used in natural dolomitic rock [20]. Thus, a preliminary study of the catalytic activity of dolomite as a function of calcination temperature was also investigated. Furthermore, the structural, textural, surface, and morphological properties of dolomite catalyst were determined to justify their overall catalytic performance, additionally to the chemical analysis in order to detect a composition change due to the reuse process.

2. Materials and Methods

2.1. Dolomite Heat Treatment and Characterization

The dolomite used in the present study was obtained from ITAMIL (Itaóca Mineration, located in Fortaleza city, Brazil). Before being used as a catalyst, the dolomite was calcined in a tubular furnace under flowing air for 1 h.

The optimum calcinations temperature was determined by thermogravimetric analysis simultaneously to the differential thermal analysis (TG/DTA), which was performed at a heating rate of 10°C/min under flowing air (40 mL/min). Elemental composition analysis was performed on an energy-dispersive X-ray fluorescence (XRF) spectrometer operating with Pd X-ray tube at 40 kV and 1.2 mA, for semiquantitative analysis of elements with atomic mass greater than or equal to that of fluorine. The crystal structure of the dolomite was characterised by X-ray diffraction (XRD) analysis using Kα-Co source ( Å) at 40 kV and 40 mA, over a 2θ range of 10 to 90°.

The temperature-programmed desorption of CO2 (TPD-CO2) was performed under flowing He (30 mL/min) at a heating rate of 10°C/min. The catalysts (200 mg) were preheated under flowing N2 (30 mL/min) at 800°C for 1 h, after which the temperature was decreased to room temperature under flowing N2. A flow of pure CO2 (30 mL/min) was subsequently introduced into the reactor for 0.5 h. The flowing CO2 was switched to flowing He, and the temperature program was started after the baseline of an online thermal conductivity detector (TCD) had stabilised. The desorbed CO2 was detected by the same system (TCD) after passing through a trap (−20°C).

In order to evaluate the textural properties, the samples were analysed by scanning electron microscopy and nitrogen adsorption/desorption isotherms. Prior to the adsorption experiments the calcined sample (180–200 mg) was evacuated at 100°C for 2 h.

2.2. Preliminary Study of Dolomite Catalytic Activity in the Transesterification of Soybean Oil

In order to fix the reaction time to be used in the experiments, were carried out catalytic tests were carried out using methanol/oil molar ratio of 6 : 1, reaction temperature of 55°C, and catalyst loading of 0.6 (wt% of oil), in different reaction time. A refined deodorised soybean oil with acidity of 0.05 wt% (as oleic acid), moisture oil of 0.11% wt, a density at 20°C of 0.9237 kg/L, and a kinematic viscosity of 30.1 mm2/s (40°C) was used as reactant.

The contents were charged into a 250 mL three-neck round-bottom flask equipped with a reflux condenser, and the reaction mixtures were magnetically stirred. The reaction temperature was controlled by a hotplate, utilizing an oil bath. Following, the desired catalyst amount was activated in a tubular furnace under N2 flow and immediately added into the reaction mixture.

At the end of each test, the catalyst was separated by centrifugation, and the mixture was transferred to a decanting funnel for phase separation. Following, the glycerine phase was separated, and the less-dense phase, which contains the methyl-ester mixture, was then loaded into a rotary evaporator to remove the excess of methanol. The methyl-ester content was analysed by gas chromatography using an instrument equipped with a FID detector and a nonpolar capillary column. The content of the FAME that is expressed in terms of weight percentage was calculated based on the standard method EN 14103 in the presence of methyl laurate as an internal standard [23].

2.3. Design of Experiments and Optimization Method

The response surface methodology (RSM) has already proven to be a reliable statistical tool in the investigation of chemical treatment processes to optimize parameters with a minimal number of experiments [24]. Accordingly, in this study a central composite design (CCD) and RSM was used to investigate the effect of the parameters on the dolomite catalyst activity for biodiesel production and to obtain a good model equation to predict the optimum FAME yield conditions. The factors selected for the optimization of the dolomite activity in transesterification reaction of soybean oil to esters were reaction temperature, catalyst amount, and methanol/oil molar ratio. Then, a set of 17 experiments, which included the 23 factorial experiments and three central points, together with the six additional star points, were performed. The experiments were performed in randomized order (to minimize the effects of the uncontrolled factors) with three replications at the design center to obtain an accurate estimation of the experimental error. The complete design matrix of the applied experiments is showed later.

An empirical model correlating FAME yield to the three parameters was developed. Analysis of variance (ANOVA) was applied to evaluate the fitness of the model and identify the interactions between the variables and the responses thought statistical significance test by value and value. The goodness of fit of the polynomial model was expressed by the coefficients of determination, , which indicated the quality of the fit of polynomial.

3. Results and Discussion

The elemental chemical composition (Table 1), determined with X-ray fluorescence spectroscopy, indicated that the natural dolomite is composed mainly of calcium and magnesium with a small amount of impurity, in which silicon was the most significant component.

On the other hand, the presence of silicon oxide will not promote a change in the catalytic behaviour because SiO2 is known to be a neutral support for catalytic process [25]. Therefore, due to the basic properties of CaO and the high Ca percentage observed, it suggests that the material may present a good catalytic performance.

The thermal behaviour of natural dolomite was studied by TGA/DTA and experimental curves for the same are presented in Figure 1. Only one endothermic weight loss at 756°C was observed in TGA/DTA curve of the dolomite before the calcination. The weight loss, which corresponds to a total of 42.9%, starts from 570°C and is complete at 785°C.

This endothermic event is related to the thermal decomposition process of dolomite (CaMg(CO3)2), leading to the formation of MgO and CaO. Therefore, the TG profile suggests that the calcination temperature required for complete decomposition of the carbonates groups should be higher than 700°C. To support the results as seen by TGA/DTA curve, XRD studies were taken on dolomite, before the calcinations, and for the powder obtained by its calcination at 700°C and 800°C, to confirm the CaO and MgO phase formation.

The XRD profile of natural dolomite and dolomite calcined at 700 and 800°C are shown in Figure 2. It can be seen clearly that in the natural dolomite a mixture of CaMg(CO3)2, CaCO3 and SiO2 phases are present; however, dolomite is the main phase (Figure 2(a)). This result was confirmed by Rietveld method [26] applied for the refinement of the diffraction profiles. Moreover, by the Rietveld method, it was possible to quantify the different phase in the sample (Table 2). These results agree with those of the XRF elemental composition analysis, which showed Ca and Mg with small amount of silicon as main chemical element.

Figure 2(a) shows a more complex diffraction profile with primary 2θ-diffraction peaks (28.0, 36.1, 39.1, 41.1, 44.0, 48.6, 52.7, 59.7, and 60.1) that correspond to dolomite phase (CaMg(CO3)2), with rhombohedral structure and R-3 space group (JCPDS file 01-079-1342). In addition, diffraction peak of SiO2 phase (2θ at 31.1), with hexagonal structure and P3121 space group (JCPDS file 01-086-1628), and CaCO3 phase (2θ at 34.4 and 56.1), with rhombohedral structure and R-3c space group (JCPDS file 01-072-1650), were detected in the raw dolomite material. The results in Figure 2(a) lead to the conclusion that the solid is a natural dolomite that contains Ca and Mg with a small amount of calcite and silicon oxide.

The reflections intensity arising from dolomite (Figure 2) is reduced significantly for the samples calcined at 700°C and 800°C, which is coincident with the appearance of new crystalline phases (Figures 2(b) and 2(c)). Therefore, it is not possible to confirm the presence of dolomite phase after the calcinations process, differently from what was observed by Niu et al. [20], which detected the presence of dolomite after calcination at 700°C.

The sample calcined at 700°C showed intense diffraction peaks (2θ of 50.3 and 73.7) related to a cubic structure of MgO phase, with Fm-3m space group (JCPDS file 01-075-0447). In addition, characteristics and intense 2θ-diffraction peaks (26.8, 34.3, 46.2, 55.8, and 56.9) related to CaCO3 (calcite, JCPDS file 01-072-1650) and a hexagonal structure of Ca(OH)2 phase (2θ of 21.0, 39.9, 55.2, 59.9, and 64.2), with P-3m1 space group (JCPDS file 01-084-1263), were also observed. The presence of Ca(OH)2 may be explained by the air exposure of the formed sample, which resulted from water adsorption; likewise, the adsorption of carbon dioxide on CaO may form CaCO3 [17]. Therefore, the presence of Ca(OH)2 phase suggests that a certain percentage of CaO also is formed at 700°C, which, due to air humidity exposure can result in the formation of Ca(OH)2. It happened because the sample was not subjected to XRD procedure immediately after the calcinations process, consequently the sample was exposed to the atmospheric air.

After thermal decomposition at 800°C (Figure 2(c)), it is observed diffraction peaks at 2θ of 37.7, 43.7 and 63.7, which are related to CaO phase (cubic structure with Fm-3m space group, JCPDS file 01-078-0649). CaO simultaneously with MgO (2θ of 50.3 and 73.7) and Ca(OH)2 (2θ of 21.0, 33.4, 39.9, 55.6, and 59.9) are the main phases formed, and no diffraction peak of CaCO3 phase was detected. Therefore, the calcination process at 800°C is sufficient to give a higher amount of MgO and CaO phases, which are basic metal oxides active in the transesterification reaction.

These results agree well with the TG results (Figure 1) and indicate that, at 800°C, the thermal decomposition reaction of dolomite is completed. Therefore, based on this finding, the dolomite was activated at 800°C for the reaction process and further characterizations.

Applying the Scherrer equation (1) for all diffraction peaks, after Rietveld refinement, for each phase, it was possible to estimate the mean crystallite diameter for the phases confirmed (Table 2). As can be seen in Table 2 the CaMg(CO3)2 phase has the average crystallite size of 96 nm, corresponding to 92.05 wt% of the crystalline phase. In addition to the dolomite phase decomposition, the effect of the heat treatment at 700°C is also observed over the CaCO3 phase, which point to a noticeable increasing on the wt% of the phase (6.72 to 27.56 wt%): where is the crystallite diameter; is a crystallographic constant; is the irradiation wavelength applied in the XRD; is the half width; is the diffraction angle.

Increasing the calcinations temperature to 800°C has no effect over the wt% and the crystallite diameter of the MgO and Ca(OH)2 phases, while the CaCO3 is lost. The lower average crystallite size observed for the CaO and MgO phases pointed to a low effect in the sintering process at 800°C (Table 2). The SiO2 phase, however, shows an enlargement of the average crystallite size due to the increase of the calcination temperature.

To gather information about the basicity of the dolomite sample after calcination at 800°C, the TPD-CO2 analysis was performed. TPD-CO2 profiles (Figure 3) clearly revealed the presence of two basic sites with different strengths. The low-temperature peak, with a maximum desorption near 400°C, may be attributed to the interaction of CO2 with sites of medium basic strength. According to [7, 17], these sites are mainly associated with the oxygen in the Mg2+–O2− pairs. The high-temperature peak, with a maximum at approximately 650°C, is associated with CO2 desorption from sites with strong basicity, which correspond to CaO. Similar value was reported by Shajaratun Nur et al. [18].

The maximum of 656°C is lower than those observed by Yoosuk et al. [17]. However, such difference may be due to the experimental procedure. In this work the sample was preheated at 800°C. This ensures that the existing CaCO3 is decomposed before the TPD run.

Therefore, although the TG analysis (Figure 1) shows the inflexion point at 725°C for the CaCO3 decomposition, one should keep in mind that for the TPD-CO2 analysis what is observed is the CO2 adsorbed on the outer surface of the oxide, and not in the bulk of the sample. In other words, a lower amount of CO2 is eliminated from the sample. Consequently it seems to present a shift to lower temperature [17].

Assuming that CO2 from MgO should desorb at lower temperatures compared to the CO2 from CaO [27], the profile in Figure 3 shows that CO2 is mainly adsorbed on CaO. Based on the information collected by the TPD technique, the coexistence of two different basic oxide components in a solid can be advantageous for transesterification. Apparently, the presence of Mg in the sample does not promote any prejudicial influence on the basic properties of CaO; the maximum in the CO2 desorption peak at 656°C points to a strongly basic site and corroborate with the TPD-CO2 results previously reported for CaO by Constantinou et al. [27].

The specific surface area was obtaining by the N2 adsorption/desorption isotherm. The sample exhibited a type-II isotherm (not shown), with almost no hysteresis loop. These features are typical of nonporous or macroporous materials. The values of the surface area and pore volume are 14 m2/g and 0.015 cc/g, respectively. This result suggests that the complete decarbonation of CO2, along with the sintering effect, results in a material with low value for the textural properties. Therefore, these values suggest that the active site access will not present a diffusion problem because the active site is present at the external surface, which may result in a faster interaction between the material and the alcohol present in the reaction mixture.

The surface morphology of natural and calcined dolomite was also examined by SEM (Figures 4(a) and 4(b)). The natural dolomite shows comprised large particles, exposing smooth planes with surface relatively homogeneous. The calcination process generates fractures on these particles, as expected from the decomposition of the carbonate groups, liberating CO2 with the formation of CaO and MgO phases, which have small surface area.

Considering the results presented so far, 800°C was the temperature fixed for the calcination process. Therefore the independent variables chosen for the catalytic test were reaction temperature (), methanol/oil ratio (), and amount of catalyst (); the reaction time was fixed in 4 h. This time was chosen after reviewing the results present in Figure 5, which shows that after 4 h of reaction time, the methyl-ester production is 85%, and the maximum (93%) were reached after 8 h.

The increase of the methyl-ester production from 85 wt% to 93 wt% is not so expressive in order to keep the reaction system plus 4 h (total of 8 h). In addition, the reaction condition for the results presented in Figure 5 is the less favourable between those chosen and presented in Table 3. That is to say, the temperature of 55°C, methanol/oil ratio of 6, and catalyst amount of 0.6 wt% are the lower values for the variables and will probably present the lower methyl-ester production.

Therefore, by fixing the calcination temperature at 800°C and the reaction time in 4 h, 17 catalytic tests were carried out, whose conditions and methyl-ester (FAME) production are presented in Table 3. It is important to point out the triplicate for the centred point.

The experimental results shown in Table 3 were submitted to a multiple regression analysis and were fitted to the polynomial equation. The regression equation as a function of the selected variables for FAME yield (%) is given by where is the reaction temperature, is the methanol/oil ratio, and is the catalyst weight.

Statistical analysis of variance (ANOVA) was used to evaluate the adequacy of the fitted model studying the significance of the individual terms and their interactions on the FAME yield (Table 4). In ANOVA analysis, information from all the experiments is used in the analysis of the results, making ANOVA a more powerful tool than varying only one factor at a time. The coefficient of determination () and the parameters value ( test) and value were used to judge the adequacy of the model [27].

According to the ANOVA results (Table 4), for the term to be considered statistically significant the calculated value should be greater than the tabulated value ( test with 95% confidence level) and the values should be less than 0.05 (probability of error value). The calculated value is defined as the ratio between the mean of the square regression and the mean of the square residual error.

From Table 4 it is clear that the linear terms for methanol/oil ratio () and catalyst amount () have large effects on FAME yield due to high values and low values. In addition, the linear term for temperature () is also significant but with a smaller effect on the FAME yield due to its smaller value than the other linear terms. However, the quadratic term for methanol/oil ratio () has a large value and a lesser value. Thus, the effect of methanol/oil ratio on the FAME yield is most strongly modelled with the quadratic term. The quadratic term for the temperature () and catalyst amount () were insignificant comparing their corresponding linear terms. The coupling terms between temperature-catalyst amount (TC) and the molar ratio-catalyst amount (RC) were significant indicating a higher interaction between those two variables. The accuracy and variability of the above model could be evaluated by the coefficient of determination. The coefficient of determination () of the model obtained is 0.9130, which indicates that 91.30% of the variability in the dependent variable could be explained.

A comparison of the experimental results with the model values of FAME yield predicted from the above equation is depicted in Figure 6. As can be seen, the experimental values were distributed relatively near to a straight line and a satisfactory correlation between these values is observed. This plot, therefore, provides visual confirmation that the regression model equation provided a good description of the experimental data with the model.

The response surface plot (Figure 7) can illustrate very well the effect of the three studied operating conditions and their interactions on FAME yield. Figure 7(a) shows that the maximum FAME yield was achieved when the ratio of methanol to oil and catalyst amount are increased to approximately their mid-range because these factors have positive effects on the response (2). However, an increase in the values of the variables beyond a certain amount of mid-range leads to a slight reduction in FAME yield. This decrease is observed in (1), since the quadratic term has negative sign. Therefore, as observed by Constantinou et al. [27], the reaction rate increase for triglyceride conversion to FAME was obtained because of the increment in the number of active sites; the excess of catalyst, however, can disturb the oil-methanol-catalyst mixture and cause a phase separation that, for diffusion reasons, inhibits the reaction.

Since the transesterification reaction is reversible in nature, an increase in the amount of methanol in the reaction mixture shifts the equilibrium to the right-hand side, with more methyl-ester formation. On the other hand, performing the reaction at high ratios of methanol/oil promotes difficulties in the separation of the methyl-ester and glycerol layers [16]. Thus, monoglycerides and diglycerides can homogenise the phases of methanol, glycerol, and methyl-ester, which favours the reverse reaction and decreases the FAME yield. However, as may be a high FAME content in the glycerine rich phase, the FAME rich phase may have a high content of glycerine. Therefore, this phenomenon provides the determination of FAME content lower than expected [16].

Figures 7(b) and 7(c) show the influence of the interactive factor of methanol/oil ratio and catalyst amount as a function of temperature. It can be seen that an increase in the values of each parameter—temperature, molar ratio, and catalyst amount—to approximately the middle of the corresponding investigated range, achieves the maximal amount of FAME yield (see Figures 7(b) and 7(c)). This shows that the transesterification reaction can be favoured when adequate temperatures are used [12, 28].

According to Figures 7(b) and 7(c), the FAME yield was highest at a temperature of 60°C and when the molar ratio and catalyst amount were increased to values at approximately their mid-range. The transesterification reaction rate increases as the temperature increases; this result is expected because of the temperature dependence of the reaction kinetics. However, the operation temperature cannot reach the boiling point of the mixture due to methanol evaporation. The evaporation of methanol results in the formation of bubbles, which inhibit the interaction between the reactants and the catalyst interface.

The coupling terms between temperature and molar ratio (Figure 7(b)) show a low effect due to the temperature increase; this behaviour is perceived in (1).

Applying the response surface design for the results presented here, it was observed that the optimum values for the variables of the process to reach a maximum in methyl-ester production were obtained when central point conditions were used, that is, a reaction temperature of 60°C, a methanol/oil ratio of 10.5, and 1.3 wt% of catalyst. Under such conditions, a FAME yield of 97.0% was reached. This conversion percentage is within the limits established by the European Union Standard EN 14214, which stipulate that the ester content should be greater than or equal to 96.5 wt%.

Although it is possible to carry out an additional transesterification reaction, in order to improve the FAME content in the biodiesel produced, at this point it is interesting to make a comparison of the results presented in the literature. Table 5 summarizes such comparison considering the temperature, methanol/oil ratio, reaction time, and catalyst amount. Because the number of papers related to the CaO performance in the transesterification of vegetable oil to produce biodiesel is considerable [29], the data from Table 5 are for the natural dolomite application only.

In general the results presented in Table 5 show a high FAME yield for the first transesterification process. Jaiyen et al. [19] showed the higher FAME yield (98.6 wt%) at 60°C and 180 min of reaction time. However, this result is achieved with a methanol/oil ratio of 30, in addition to the high catalyst content (6 wt%). Similar FAME yield (98 wt%) was achieved by Shajaratun Nur et al. [18] with a catalyst content of 1 wt%. However this conversion is reached after 360 min of reaction time and a methanol/oil ratio of 20 at 65°C. Niu et al. [20] showed a FAME yield of 97.9 wt% with 1890 min of reaction time, but using 4 wt% of catalyst content.

An interesting result for the FAME yield is presented by Ilgen [11], 91.8 wt% (FAME) with 180 min of reaction time and a methanol/oil ratio of 6. However, the temperature and the catalyst amount also are high.

Although the FAME yields from the present work were achieved with 240 min of reaction time, it is important to point out the similar result presented by Yoosuk et al. [17] (Table 5). Despite (2) being valid in the catalyst amount range of 0.6 to 2.0 wt%, applying in (2) the reaction condition from Yoosuk et al. [17] (Table 5), the FAME yield calculated is 93.56 wt%, which is similar to the result presented by Yoosuk et al. (94.3 wt%).

Therefore, the results presented here show the importance of statistical approach to determine the best reaction conditions.

From the economical point of view the catalyst recycling is very important. Therefore, reusability tests were also carried out in the same reaction conditions cited above (, , and ). Before each reuse process the catalyst was regenerated by calcinations at 800°C.

Figure 8(a) shows the FAME yield after two-reuse process. The FAME yield for the first reuse is practically the same of the fresh catalyst; however, in the second reuse the FAME yield falls to 95%. This is a high methyl-ester content; but a third or fourth reuse process will present lowest content of FAME.

As previously mentioned, the catalyst was always reactivated before each reuse. So, it would not be expected catalytic deactivation due to residual organic substances deposited on the sample surface.

Therefore, it is necessary and interesting to analyze the catalyst composition after each test. The elemental analysis results are shown in Figure 8(b). Practically there is no catalytic composition change after the first using; however, after the first and the second reuse process the catalyst composition change significantly. These results point to a leaching of the main active specie from the catalyst solid sample. Thus, as the calcium oxide is the main active site, the decrease in calcium content results in the methyl-ester production decrease.

As showed in previous papers [3032], both MgO and CaO are active in the transesterification reaction. However, it is known that CaO is more active than MgO [33, 34]. Therefore, despite the significant decrease in calcium content (Figure 8(b)), the decrease in the FAME wt% production is not considerable (from 97 to 95 wt%) because of the MgO content.

The leaching is prejudicial to the catalytic process; thus, these results may suggest that dolomite is not applicable for transesterification process. On the other hand, if it is considered the low cost of obtaining the dolomite, three cycles of use can be significant. In addition, the calcium content in the biodiesel, due to the leaching process, can be removed efficiently by using a sulfonic resin [35].

4. Conclusions

The calcined dolomite was found to be an effective basic catalyst in the transesterification of triglycerides for biodiesel production. Using the response surface methodology, a suitable method to study the effect of three operating variables, it is shown that within the experimental range considered, the most important factors were the molar ratio and the amount of catalyst. In spite of the calcium to be the main leached component, which limits the reuse process to a few times, the dolomite application in the FAME production is favourable from an economic and environmental point of view.

Conflict of Interests

The authors declare that there is no conflict of interests regarding the publication of this paper.

Acknowledgments

The authors acknowledge Dr. J. M. Sasaki (Lab. de Raios X-UFC) for the DRX and FRX analysis, Dr. E. R. Leite, and A. N. Pinheiro (LIEC-UFSCar) for the SEM analysis and ITAMIL (Itaóca Mineration) for the donation of the dolomite, and the Brazilian research-funding support agency, CNPq.