Production of silica gel from Tunisian sands and its adsorptive properties
Introduction
Current global silica sand world production for industrial purposes is around 140 Mt/year (Mansour, 2015), with the USA accounting for 24%, the Netherlands for 20% and France for 5%. The price of quartz sand varies as a function of its characteristics, such as particle size and purity. In the case of Tunisia, this raw material is essential to the economy, and various Tunisian manufacturers and industries (glass, foundry sand …) are obliged to import huge quantities from countries like Belgium, France, Germany, Italy, Spain, the USA and Mexico, despite the obvious natural resources that Tunisia possesses of this material. This operation is costly (1.8 Million USD in 2000 to 5.2 Million USD in 2015, INS 2016) for the state and the economy, while there exist abundant unstudied and unexploited silica sand deposits from the Early Cretaceous to Quaternary periods in the country (Jamoussi, 1991, Essid, 1997, Aloui, 1999, Harrabi, 1999, Sdiri et al., 2010, Hajjaji et al., 2009, Hajjaji, 2011). In addition, it has been shown that Tunisian sand is a high purity material that can be used in many different industrial areas, such as glass making (Hajjaji et al., 2009), cements (Aloui, 2010, Mechti et al., 2012), electro-metallurgy (Khalifa et al., 2014), chemicals (Mansour, 2015), and especially as air and water waste purifiers (Farrukh et al., 2014).
In this context, silica gel is an interesting amorphous material (annual world production 25,000 t/year; Meljac, 2004) with a high adsorption capacity (Gómez et al., 2014), and is used as an adsorbent of moisture, or for the purification of effluents with its hydrophilicity (the high moisture content trapped within the silica structure creating the ideal environment to attract polar impurities) (Armarego and Chai, 2013). This material has several advantages: for example, it is easy to regenerate, as when it has become saturated with water the silica gel can be regenerated by heating at 100–120 °C until it returns to its original state (indicated by a change in colour), the heating literally drives off the adsorbed moisture. Silica gel is also chemically inert and non-toxic, with a very high melting point, it is very much like quartz sand and thus can safely be sent by any means of transport, has a long life, and has low abrasion (the wear rates decreasing with increasing of the porosity) (Trabelsi et al., 2009). In recent years, new studies are underway into the use of this versatile amorphous material as fillers (Lin et al., 2014), coatings (Liu et al., 2013), and hygroscopic packaging for optical (Château, 2013), electronics (Xu et al., 2010) and pharmaceutical (Brown et al., 2014) products. Silica gel exhibits superior adsorption and high surface area properties which paves its way for use in water filtration, as growing environmental concerns, coupled with the need to comply with stringent government regulations concerning waste-water treatment, are driving the industry. The global water filtration market was valued over 17 million USD in 2012, and the transition towards the physical treatment of water from conventional water-treatment methods is expected to have an impact on the need for more silica gel (Grand View Research Report). The Global Silica Gel market is forecast to grow at a rate of 4% annually over the period 2014–2019 (Tech Navio Report, 2015).
Dyes are widely used by textile industries to colour their products, and one of the major problems concerning textile wastewaters is the highly coloured effluent (Moursli and Bengueddach, 2010), which can be difficult to decolourise. Over 15% of the textile dyes are lost in the wastewater stream during dyeing operations, and so dye pollutants from the textile industry are a significant source of environmental contamination. About half of the global production of synthetic textile dyes (700,000 tons per year) is classified as azo compounds that have the NN chromophore unit in their molecular structure, such as methylene blue (C16H18ClN3S). These azo dyes are known to be largely non-biodegradable in aerobic conditions, and they reduced to form more hazardous intermediates in anaerobic conditions. These releases pose a real danger to humans and the environment because of their stability and poor biodegradability (Sakr et al., 2015). Several treatments have been used to reduce the harmful effect of discharged effluents. Traditional methods such as biological processes give unsatisfactory results, due to the composition of these discharges toxic materials and dyes that are difficult biodegradable (Sakr et al., 2015). Adsorption remains among the most used techniques for dye removal, and is easy to implement. Removal of dyes in aqueous solutions by adsorption on various solid materials, especially on silica gel, has been the subject of many studies (Kushwaha et al., 2010, Samiey and Toosi, 2010).
Methylene blue (MB) (3,7-bis(dimethylamino)-phenothiazin-5-ium chloride trihydrate)is a cationic dye that is used in the dyeing of cotton, wool, coating for paper stock and silk. The classification provided by ECHA European Chemical Agency (2016) in CLP notifications (EC/List no.: 615-731-6) showed that this substance is harmful if swallowed, causes serious eye irritation, may cause damage to organs through prolonged or repeated exposure, causes skin irritation and may cause respiratory irritation (Karim et al., 2010). It can cause chest pain, shortness of breath; an anxiety, tremors, hypertension, and even skin coloration if the dose is high (Kushwaha et al., 2014). Despite this, the toxicological data on the use of MB in humans for many years have not yet indicated a specific hazard in the use of this product, (Yi and Zhang, 2008), and although MB is not classed as highly dangerous, it clearly has a harmful effect on living organisms (Gobi et al., 2011) and waters (Rafatullaha et al., 2010). Many synthetic dyes and pigments generate harmful by-products, particularly when dumped directly into the environment without any specific treatment of toxic constituents (Saidi, 2013).
This work is aimed to promote local georesources (silica sands) for the preparation of silica gel, and to investigate its decontamination capacity for the treatment of synthetic dyes in solution.
Section snippets
Geological setting
In this study, three representative samples were collected from different sites:
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Jebel Menchar (M): Fortuna formation (Burdigalian), Tunisian Dorsal structural domain,
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Jebel SidiAïch (S) and Jebel Attaf (A): Sidi Aich formation (Barremian), meridional Atlas.
The deposits of the Fortuna formation are located about 2 km north east of the village of El Hammem Jedidi and 15 km south of the city of Hammamet. It is an ENE/WSW anticlinal structure with an Eocene level extending over 3.5 km long and
Characterisation of studied sands
The XRD powder patterns are shown in Fig. 1. The studied sands are mainly composed of quartz (71–98%) and feldspars (1–27%). Minor proportions of kaolinite and calcite were also detected. The dominance of quartz suggests that the depositional basins were associated with a passive margin (Gallala et al., 2009). Where as the presence of feldspar suggests that quartz sands could probably be of magmatic origin, or even metamorphic, from the Hoggar Massif (Hajjaji, 2011). Table 2 also gives the
Conclusions
This work was undertaken to exploit the potential of local Tunisian quartz sands for the preparation of silica gels, and to study their potential retention of a cationic dye (methylene blue, MB). It was concluded that the quartz sands consisted mostly of silica and feldspars more than 88% silica, and the specific surface areas of the silica gels reached values as high as194 m2/g. For MB adsorption, it was clear that silica gel GM3 shows the highest adsorption capacity (81%) due to the larger
Acknowledgements
We would like to thank the reviewer for their detailed comments and suggestions for the manuscript. We believe that the comments have identified important areas which required improvement. This work was supported by FCT-Grant SFRH/BPD/72398/2010 and by UID/GEO/04035/2013 project. This study was supported by funding from MEDYNA: “FP7-Marie Curie Action funded under Grant Agreement PIRSES-GA- 2013-612572”, and the Tunisian Belgium Wallonie-Bruxelles International WBI Research Project
References (75)
- et al.
Potential of using green adsorbent of heavy metal removal from aqueous solutions: adsorption kinetics, isotherm, thermodynamic, mechanism and economic analysis
Ecol. Eng.
(2016) - et al.
Tectonic evolution of the northern African margin in Tunisia from paleostress data and sedimentary record
Tect. Phys.
(2002) - et al.
Preparation of amorphous silica gel from Algerian siliceous by-product of kaolin and its physico chemical properties
Ceram. Int.
(2014) - et al.
Efficient anionic dye adsorption on natural untreated clay: kinetic study and thermodynamic parameters
Desalination
(2011) - et al.
Detrital mode, mineralogy and geochemistry of the Sidi Aïch Formation (Early Cretaceous) in central and south western Tunisia: implications for provenance, tectonic setting and paleoenvironment
J. Afr. Earth Sci.
(2009) - et al.
Dye adsorption onto mesoporous materials: pH influence, kinetics and equilibrium in buffered and saline media
J. Environ. Manage
(2014) - et al.
Natural Portuguese clayey materials and derived TiO2-containing composites used for decolouring methylene blue (MB) and orange II (OII) solutions
Appl. Clay Sci.
(2013) - et al.
Composition and properties of glass obtained from early Cretaceous Sidi Aich sands (central Tunisia)
Ceram. Int.
(2009) - et al.
Removal of cationic methylene blue and malachite green dyes from aqueous solution by waste materials of Daucuscarota
J. Saudi Chem. Soc.
(2014) - et al.
Synthesis and grafting of silica aerogels
Colloids Surf. A
(2004)