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Sunflower oil bleaching by adsorption onto acid-activated bentonite

Abstract

Two bentonite clays with different mineralogical compositions from Mendoza, Argentine, were activated with H2SO4 solutions of 4 and 8 N at 90ºC for 3.5 hours. This treatment affected clay structural properties, as was shown by thermogravimetry, infrared spectrometry and chemical analysis. Bleaching efficiency for sunflower oil was strongly dependent on the acid concentration used for clay activation. The samples have bleaching capacity comparable to that observed with a commercial adsorbent standard. The mineralogical composition of natural clays influenced the properties of the activated clays.

Acid-treated clays; Bentonite; Oil bleaching; Sunflower oil


SEPARATION PROCESSES

Sunflower oil bleaching by adsorption onto acid-activated bentonite

E. L. FolettoI,* * To whom correspondence should be addressed ; G. C. ColazzoI, C. VolzoneII; L. M. PortoIII

IDepartment of Chemical Engineering, Federal University of Santa Maria (UFSM), 88040-900, Santa Maria - RS, Brazil. E-mail: efoletto@gmail.com

IICenter of Technology of Mineral Resources and Ceramic, CETMIC (CIC-CONICET), C.C. 49, (1897) M. B. Gonnet, Prov. Buenos Aires, Argentina

IIIDepartment of Chemical and Food Engineering, Federal University of Santa Catarina (UFSC), P.O. Box 476, 88040-900, Florianópolis - SC, Brazil

ABSTRACT

Two bentonite clays with different mineralogical compositions from Mendoza, Argentine, were activated with H2SO4 solutions of 4 and 8 N at 90ºC for 3.5 hours. This treatment affected clay structural properties, as was shown by thermogravimetry, infrared spectrometry and chemical analysis. Bleaching efficiency for sunflower oil was strongly dependent on the acid concentration used for clay activation. The samples have bleaching capacity comparable to that observed with a commercial adsorbent standard. The mineralogical composition of natural clays influenced the properties of the activated clays.

Keywords: Acid-treated clays; Bentonite; Oil bleaching; Sunflower oil.

INTRODUCTION

Acid activated bentonites have been used as solid acid catalysts and catalyst supports for a number of organic applications that require an extreme degree of reaction control of considerable industrial interest (Mokaya and Jones, 1995, Breen et al., 1997, Volzone et al., 2001, Foletto et al., 2002, Didi et al., 2009). They have also been used in the foodstuffs industry, for sulphur production, forest and water conservation, in the chemical industry, for environmental protection, and in the paper industry (Clarke, 1985, O'Driscoll, 1988), as well as for bleaching of vegetable oils (Srasra et al., 1989, Christidis et al., 1997, Foletto et al., 2003, Kirali and Laçin, 2006). The bleaching of edible vegetable oils involves the removal of a variety of impurities, which include phosphatides, fatty acids, gums, trace metals, etc., followed by decolorization. The bleaching capacity of bentonites is greatly increased by activation treatment. While some of these clays are naturally bleaching, some have to be treated with mineral acids (Grim, 1962; Patterson, 1992; Norris, 1982; Rossi et al., 2003; Rožić et al., 2010). Bentonite consists predominately of smectite, a 2:1 clay mineral containing an octahedral sheet between two tetrahedral sheets. Smectite crystals are negatively charged due to the substitution of the trivalent aluminium ions by divalent ions like Mg2+ and Fe+ and substitution of tetrahedral Si4+ by Al3+ (Kirali and Laçin, 2006). Activation proceeds with partial dissolution of smectite and includes an initial replacement of the interlayer cations by H+, followed by dissolution of the octahedral and tetrahedral sheets, with subsequent release of structural cations. This attack alters the structure, chemical composition and physical properties of the clay while increasing the adsorption capacity (Mokaya et al., 1993). Christidis et al. (1997) examined the bleaching capacity and acid activation of bentonites from Aegean, Greece, observing a five-fold increase of the surface area of raw materials. The activated samples were rendered suitable for bleaching of rapeseed oil. It was determined that the optimum bleaching capacity in not associated with maximum surface area and the optimum conditions for activation are obtained by using a variety of combinations of acid strength and residence time. Despite numerous studies, no definite relationship exists between the performance of the acid-activated clay and the composition or properties of the original clay. Hence, each clay has to be specifically activated and tested for its performance (Hymore, 1996). The preparation of acid-activated bentonite must be controlled in order to obtain maximum bleaching capacity (Kirali and Laçin, 2006, Rožić et al., 2010).

The present study deals with the acid activation of Argentine bentonites and testing of their bleaching capacity for sunflower oil, in comparison with the bleaching capacity of a standard commercial bleaching clay.

EXPERIMENTAL

Two natural bentonites (named K and W) from two different deposits of the Mendoza province, Argentine, were used as the starting materials. Tonsil, a commercial acid-activated bentonite extensively used in the vegetable oil industry, was used as reference for the evaluation of the bleaching capacity in the experiments. Alkali-refined sunflower oil was gently donated by Bunge Alimentos S.A (Gaspar-SC, Brazil).

The bentonite sample (40 g) was treated with 400 mL of 4 N or 8 N sulphuric acid (analytical grade) at 90ºC for 3.5 h (Foletto et al., 2003) in a stirred glass reaction vessel with reflux. After the acid treatment, the sample was filtered and washed with distilled water until free of SO42-. The samples were dried at 60ºC for 12 h and ground to pass through a 0.074 mm sieve. Activated samples were designated as K4, K8, W4 and W8, where the numerical value indicates the concentration of acid solution used for the treatment. Bleaching experiments were conducted by a procedure analogous to that of the American oil Chemical Society (AOCS) Official Method Cc 8a-52. The bleaching process was carried

out under a vacuum of 450 mmHg at the constant temperature of 100ºC with a contact time of 30 min. Stirring and heating were carried out by means of a mechanical stirrer and an electric heating band. The ratio of the mass of clay to the volume of acid solution was 1:10 (w/v). During the bleaching, a stream of N2 was maintained above the oil surface. The hot oil and clay mixture was filtered under vacuum and the color of the bleached oil was measured spectrophotometrically (WFJ525-W UV-visible spectrophotometer). The bleaching capacity percentage of the clays was determined from the equation (Falaras et al., 1999):

BC (%) = [(A0 - A)/A0] x 100

where "A0" and "A" are the absorbance of neutral oil and bleached oil, respectively, at the maximum absorbance wavelength of the neutral oil (420 nm). The structural changes of the Argentinean acid bentonites were examined by means of thermogravimetric (TGA) and infrared spectrometric (IR) analyses and chemical analysis (XRF). TGA was performed with a Netzsch STA 409 thermal analyzer at a heating rate of 10ºC.min-1 under a flow of atmospheric air of 35 mL min-1, in the temperature range 25-1000ºC. IR spectra were recorded in the region 4000-350 cm-1 with a Perkin-Elmer 16 PC spectrophotometer, using the KBr pellet technique. Chemical compositions of the samples were determined by X-ray fluorescence with a Philips PW 2400 spectrometer.

RESULTS AND DISCUSSION

The mineralogical compositions of two clay samples were determined by Foletto et al. (2000). Smectite is the main clay mineral in both samples (35 % in K and 47 % in W). The K bentonite contains quartz and feldspar as impurities, whereas W bentonite contains also gypsum and kaolinite. Table 1 shows the chemical analysis of the bentonites after treatment with sulfuric acid. The interlayer cations of the bentonites were removed.

The residual Ca2+, Na+ and K+ are due to the presence of impurities such as micas and feldspars, which are insoluble in acid medium (Barrios et al., 1995). Part of the Mg2+, Fe2+/3+ and Al3+ was removed from the octahedral sheet. Ti4+ cations were insoluble. The increase of Si4+ and the reduction of the octahedral cations, with the increase of the acid concentration resulted in an increase of the Si/(Al+ Mg +Fe) ratio. The loss of weight due to dehydroxylation (%) of the samples, obtained from TGA curves, occurred in the range 450-750º C (Figure 1); the TGA curves were used for the evaluation of the extent of the attack of the acid treatment on the octahedral sheets (Table 2). The octahedral sheet destruction was calculated as a relative percentage reduction of the weight loss, with respect to the original sample (Foletto et al., 2003). The activated K samples showed 14 to 19% destruction of the octahedral sheet, while the activated W samples showed 12 to 15% destruction. These results showed that, even at high acid concentration (i.e., a concentration of 8 N), the structure of smectites was not totally destroyed.


Figure 2 shows the infrared spectra of the original and the acid-treated bentonites. No important changes were observed, although the Si-O-Al (525 cm-1) and Si-O-Si (465cm-1) bands were modified. The intensity ratios of both bands are shown in Table 3. Table 3 presents the results of the characterizations of the natural and activated samples and for bleaching of sunflower oil. Figures 3, 4 and 5 show the relation between the structural changes and bleaching capacity of the bentonites. The results of the analyses indicate that an increase of the acid concentration causes a greater attack on the bentonite structure and, consequently, improves the bleaching capacity. The level of clay attack was higher for the K that the W sample.





The acid activated K bentonites showed a slightly superior bleaching capacity than the acid W bentonites and this behavior could be attributed to the greater effect of the acid attack on the K smectite structure when compared to the W smectite. Comparing the mineralogical compositions, the sample K presents a higher MgO content than sample W. It has been observed that smectites with greater MgO contents in their structure are more activated by mineral acids than those smectites with minor MgO content (Volzone and Ortiga, 2000). An optimization of the experimental conditions of acid treatment of the W bentonite would probably cause a higher attack on its structure and, consequently, would lead to a better adsorptive capacity, because this sample has a higher clay content than K bentonite (Foletto et al., 2000).

The best bleaching capacity (BC) results of the activated bentonites obtained in this work were compared with a commercial sample, as shown in Table 4. The retention of colored impurities of sunflower oil by Tonsil (commercial sample) was similar to those of the bentonites treated with 8N sulphuric acid.

CONCLUSION

Attack on the bentonite structure as a result of sulfuric acid treatment is strongly dependent on the acid concentration. The effects of these treatments on clay structural properties were determined by thermogravimetric, infrared spectrometric analysis and chemical analysis. The activated samples were tested in order to verify their bleaching capacity for sunflower oil and were compared to a standard commercial bleaching clay. Bleaching efficiency was strongly dependent on the acid concentration used for clay activation. The treated samples showed a bleaching capacity comparable to the standard. The mineralogical composition of natural clays influenced the properties of the treated clays and these properties increased its bleaching power.

ACKNOWLEDGMENTS

Financial support of CAPES and CNPq, Brazilian governmental agencies for education and research, and PIP02100-CONICET, Argentina are thankfully acknowledged.

(Submitted: March 26, 2010 ; Revised: May 4, 2010 ; Accepted: August 31, 2010)

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  • *
    To whom correspondence should be addressed
  • Publication Dates

    • Publication in this collection
      15 Mar 2011
    • Date of issue
      Mar 2011

    History

    • Received
      26 Mar 2010
    • Accepted
      31 Aug 2010
    • Reviewed
      04 May 2010
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