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Varila, T., Bergna, D., Lahti, R., Romar, H., Hu, T., and Lassi, U. (2017). "Activated carbon production from peat using ZnCl2: Characterization and applications," BioRes. 12(4), 8078-8092.

Abstract

The process for producing activated carbon from peat was optimized. The peat was impregnated with different ratios of ZnCl2, and the impregnated biomass was activated at different temperatures. The specific surface area, pore size distribution, total carbon content, and yield of the activated carbon were investigated. The best results for the specific surface area and mesoporosity of the activated peat were obtained by using a high impregnation ratio (2) and high activation temperature (1073 K). Highly porous activated carbon was produced that had a specific surface area of approximately 1000 m2/g and total pore volume that was higher than 0.5 cm3/g for most samples. The activated carbon had a high degree of mesoporosity. The adsorptive properties of the activated carbon were determined with methylene blue and orange II dyes.


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Activated Carbon Production from Peat Using ZnCl2: Characterization and Applications

Toni Varila,b Davide Bergna,a,b Riikka Lahti,a,b Henrik Romar,a,b,* Tao Hu,and Ulla Lassi a,b

The process for producing activated carbon from peat was optimized. The peat was impregnated with different ratios of ZnCl2, and the impregnated biomass was activated at different temperatures. The specific surface area, pore size distribution, total carbon content, and yield of the activated carbon were investigated. The best results for the specific surface area and mesoporosity of the activated peat were obtained by using a high impregnation ratio (2) and high activation temperature (1073 K). Highly porous activated carbon was produced that had a specific surface area of approximately 1000 m2/g and total pore volume that was higher than 0.5 cm3/g for most samples. The activated carbon had a high degree of mesoporosity. The adsorptive properties of the activated carbon were determined with methylene blue and orange II dyes.

Keywords: Peat; Zinc chloride; Activation; Activated carbon; Mesoporous carbon; Optimization

Contact information: a: University of Oulu, Research Unit of Sustainable Chemistry, P.O. Box 3000, FI-90014 University of Oulu, Finland; b: University of Jyvaskyla, Kokkola University Consortium Chydenius, Applied Chemistry, P.O. Box 567, FI-67101 Kokkola; *Corresponding author: henrik.romar@chydenius.fi

INTRODUCTION

Over the last few decades, the preparation of activated carbon with the desired chemical and physical properties has gained a lot of interest (Marsh and Rodríguez-Reinoso 2006). A highly porous structure and high specific surface area are features of activated carbon that are widely desired in many purification applications in industrial and municipal processes. Wastewater treatment, gas cleaning processes, metal removal from waste streams, and usage as a catalyst are the main applications for activated carbon (Patrick 1995; Ahmadpour and Do 1996; Cox et al. 2005; Mohammad-Khah and Ansari 2009; Caglayan and Aksoylu 2013; Fu and Li 2015). Recently developed applications of activated carbon include electrical charge storage (i.e., super capacitors) and gas storage (i.e., hydrogen) (Li et al. 2016). However, the high cost of activated carbon limits its applications in many cases (Özdemir et al. 2011). For this reason, low-cost and renewable starting materials are widely used to produce activated carbon. Biomass-based activated carbon can be prepared from a number of carbon rich biomasses, such as coconut shell, coal, saw dust, and peat (Ahmedna et al. 2000; Antal and Grønli 2003; Mohammad-Khah and Ansari 2009; Khadiran et al. 2015). Peat is commonly used as a raw material for energy and heat production, especially in Finland. This is mainly because the peat, as a raw material, is relatively cheap and has been considered as a renewable energy resource. By a decision of the European Union in 2008, peat is no longer regarded as a renewable energy resource. Recently in Finland, the usage of peat to produce activated carbon has gained some interest among researchers and companies in order to find new applications for the peat.

There are two well-known methods for producing activated carbon, which are physical activation and chemical activation. Physical activation is performed in a two-step process. First, the biomass is placed in a reactor flushed continuously with a nitrogen atmosphere in order to avoid total oxidation. Heat is then fed into the system, which results in the carbonization of the biomass at temperatures near 673 K. The carbonization temperature is one of the most important parameters that affects the physical properties of the activated carbon. Generally, peat contains cellulose, hemicellulose, lignin, ash, and other organic compounds. The carbonization process is needed in order to decompose these organic compounds into activated carbon. The properties of the activated carbon vary according to the temperature used. The carbonized biomass is activated by a partial oxidant agent, such as steam or carbon dioxide, at high temperatures (873 to 1073K) (Hanna et al. 2015). Activating agents are responsible for the creation of the pore structure.

The advantages of physical activation are the relative simplicity and low cost, while the disadvantage is low yields (Lillo-Ródenas et al. 2003; Yorgun et al. 2009). For example, more volatile compounds are formed at higher carbonization temperatures, while decomposed organic compounds exit the carbonization process, which leads to lower yield of activated carbon. Furthermore, the holding time effects the yield of activated carbon in the same way as the carbonization temperature. The longer the holding period is, the more time organic compounds have to decompose (Baçaoui et al. 2001; Lua and Yang 2004; Yang et al. 2010).

In addition to physical activation, chemical agents, e.g., zinc chloride (ZnCl2), KOH, NaOH, and H3PO4, can be used for activating carbon (Lillo-Ródenas et al. 2003; Yorgun et al. 2009). In the chemical activation process, the biomass is first impregnated with a solution containing the chemical activating agent, dried in an oven, and then heated in a furnace, with rather lower temperatures (673 to 873 K) compared to physical activation, under an inert atmosphere (nitrogen atmosphere). In the case of chemical activation, important factors include the correct mass to carbon ratio to avoid excessive consumption of reagents and proper activation temperature, which can vary according to the type of chemical agent used. From the mechanical point of view, chemical reactions that occur during the carbonization process are not well known. Only few studies have reported about how the chemical activation occurs. In the case of hydroxides (NaOH and KOH), the reactions between carbon and alkaline metals produces metal, hydrogen and metal carbonates. The following reaction can be described with equations 1 and 2 (Lillo-Ródenas et al. 2004).

6NaOH + 2C ↔ 2Na + 3H2 + 2Na2CO3 (1)

6KOH + 2C ↔ 2K + 3H2 + 2Na2CO3 (2)

However, there is a lack of information about how the reaction between carbon and ZnCl2 or H3PO4 occur during the carbonization process. Only assumptions can be made at this point. Further investigation is needed in this field.

The typical advantages of using chemical activation include the possibility of achieving higher final carbon yields, the fact that it can be a one step process, the generally lower activation temperatures that are required, and an easier adjustment of porosity compared with physical activation (Hayashi et al. 1995; Ahmadpour and Do 1996; Benaddi et al. 1998; Yorgun et al. 2009; Yorgun and Yıldız 2015). The main disadvantages of using chemical compounds are that they are not environmentally friendly substances and are corrosive towards the equipment used during research. An acid washing step is also needed in order to remove the chemical activating agent (Teng and Lin 1998; Yorgun et al. 2009; Yorgun and Yıldız 2015).

A large specific surface area, well-developed highly porous structure, stability, and surface chemical functional groups are key factors of activated carbon. The adsorption of dyes with large diameters can be used to determine the possible pore structure and interaction mechanisms of activated carbon. Methylene blue and orange II are commonly used dyes. Methylene blue is a basic (cationic) dye, while orange II is an acidic (anionic) dye. The adsorption of dyes is favored by mesoporous (2 to 50 nm) carbon because the molecular size of the dyes is larger than the micropores. In addition to the diffusion into pores, the dye molecules can interact with the surface charge of the activated carbon (Rodríguez et al. 2009; Peng et al. 2014; Kumar and Jena 2016a). In this work the above-mentioned dyes were used to measure the adsorption ability of peat based activated carbons.

The aim of this study was to optimize the chemical activation process using ZnCl2 in order to produce highly mesoporous activated carbon with a pore size distribution suitable for use as a catalyst support and adsorption of larger organic molecules. The effect of the activation temperature and different impregnation ratios of peat and ZnCl2 on the specific surface area, pore size distribution, yield, total carbon (TC), and adsorption abilities of the peat-based activated carbon were investigated. The term “impregnation ratio” describes the ratio of mass of ZnCl2 to the dry mass of peat.

MATERIALS AND METHODS

Biomass and Materials

The peat used in this experiment was obtained from peatlands in the Oulu region of northern Finland. The peat was initially washed with distilled water to remove any impurities, such as metals, and then oven dried at 393 K for 24 h. The peat was then sieved so that a fraction 0.5 to 1 mm in size was collected. The resulting fraction was used for further experiments. All reagents used in this research were ordered from VWR International (Helsinki, Finland).

Moisture, Ash Content, and Elemental Analyses of the Peat

The moisture content and ash content of the peat was measured by using the standard test methods for peat (ASTM D 2974-87). A known amount of peat was weighed in a tared crucible. The crucible was dried overnight in an oven at 378 K. The dried sample was placed in a desiccator and allowed to cool down to room temperature. The crucible was weighed, and the moisture content was calculated by dividing the weight loss by the initial weight of the sample. The crucibles with dried peat was used for determination of the ash content. Organic matter was totally carbonized and removed in a furnace at 713 K for 3 h. The sample was allowed to cool down in a desiccator to room temperature before weighing it. Ash content was calculated as the mass ash as percent of the initial mass. Elemental analysis of the peat was performed with a Flash 2000 analyzer (ThermoScientific, Waltham, MA, USA). Ground elements were converted into simple gases (CO2, H2O, N2, and SO2) in an oxygen atmosphere and detected with a TDC detector.

Preparation, Chemical Activation, and Carbonization of the Peat-Based Activated Carbons

Four series, each containing different impregnation ratios of ZnCl2 to peat, were prepared according to the method described in Liu (2010). The impregnated peat was dried and carbonized at different temperatures, which are given in Table 1. Each peat sample (P) was named according to the carbonization temperature and ZnCl2 to peat ratio used. The samples were prepared by adding a known amount of peat and zinc chloride solution to an 800-mL beaker. Under mechanical stirring, the prepared solution was heated to 358 K for 3 h in order to complete the chemical impregnation. Deionized water was added into the solution at various time intervals to prevent it from completely drying out. The impregnated biomass was then dried at 378 K for 24 h in an oven with natural convection.

The impregnated peat samples were crushed in a mortar and activated in a stainless-steel fixed-bed reactor. The reactor was placed in a tubular heating oven for carbonization. During the heating process, the reactor was flushed with an inert gas (nitrogen) in order to avoid oxidation. The oven temperature was increased from room temperature to the final temperatures, which are shown in Table 1, using a heating ramp of 10 K/min and hold time of 2 h at the final carbonization and activation temperature. To obtain the final activated carbon, the chemical activating agent remaining in the sample after carbonization was removed by refluxing the sample with 3 M HCl for 1 h. The carbon was filtered and washed with distilled water until a neutral filtrate was obtained. The activated carbon was finally oven-dried overnight at 378 K (Yorgun et al. 2009).

Table 1. Preparation Method of the Activated Carbons

Calculation of the Yield and Total Carbon (TC)

The yield of activated carbon for each sample was calculated from the weight of the resultant peat-based activated carbon divided by the weight of the initial sample used for carbonization and activation (Yorgun et al. 2009). The content of carbon present in each sample, given as the TC percent, was measured using a solid phase carbon analyzer (Skalar Primacs MCS, Breda, The Netherlands). The dried and crushed samples were weighed in quartz crucibles, combusted at 1373 K in an atmosphere of pure oxygen, and the resulting CO2was analyzed by an IR analyzer (Skalar Formacs, Skalar, Breda, The Netherlands). The carbon content values were obtained by comparing the signal from the IR analyzer with a calibration curve derived from known masses of a standard substance (citric acid). The total mass of carbon in each sample was calculated as a percent of the mass initially weighed, and was only determined in the final product, which was carbonized, chemically activated, and acid washed.

Specific Surface Area and Pore Size Distribution

Prior to measurement, portions of each sample (approximately 200 mg) were pretreated at low pressures and high temperatures in order to clean the surfaces. Isothermal conditions were obtained by immersing the sample tubes in liquid nitrogen (76 K). Nitrogen was then added to the samples in small steps, and the adsorption isotherms were obtained. The specific surface areas were calculated from the adsorption isotherms according to the Brunauer–Emmett–Teller (BET) method (Brunauer et al. 1938). The pore size distributions were calculated using the Barrett-Joyner-Halenda (BJH) algorithm (Barrett et al. 1951). With a Micromeritics ASAP 2020 (Norcross, USA), pores down to 1.5 nm in diameter could be measured.

Field Emission Scanning Electron Microscope (FESEM) and Transmission Electron Microscope (TEM) Imaging

A field emission scanning electron microscope (FESEM) (Zeiss Sigma, Jena, Germany) equipped with an energy-dispersive X-ray spectrometer (EDS) and Electro Backscatter Diffraction (EBSD) camera, located in the Center of Microscopy and Nanotechnology, University of Oulu, was used to study the microstructure of the peat samples. Scanning electron microscope (SEM) images were taken with an acceleration voltage of 5 kV and working distance of approximately 5 mm without any coating. High-resolution transmission electron microscope (TEM) images were taken with a JEOL JEM-2200FS TEM (Tokyo, Japan) at an acceleration voltage of 200 kV.

Adsorptive Properties

The adsorptive properties of the peat-based activated carbon were tested using the adsorption of dyes, methylene blue (MB) and orange II (OII), into the pores, as previously described (Hirata et al. 2002; Raposo et al. 2009). A solution containing 300 mg of MB or OII per liter of H2O was prepared, and 100 mL of this solution was then transferred into 250-mL Erlenmeyer flasks. Fifty milligrams of activated carbon were added next, and the solutions were continuously agitated for 24 h to achieve equilibrium between adsorption and desorption of the test dye. Portions of each solution were filtered and diluted if needed. The absorbance of the solution was measured at 664 nm for MB and at 485 nm for OII on a Shimadzu UV-1700 double-beam spectrophotometer (Kyoto, Japan). The concentrations of the solution was calculated from calibration lines obtained with known concentrations of MB and OII respectively. The absorbed mass (qabs) was calculated for each compound using Eq. 6, and the percent MB and OII removed was calculated using Eq. 7,

qabs = ((C0 – Ct) x V) / m (6)

% removed = (C0 – Ct) / C0 (7)

where C0 is the initial concentration of the dye (300 mg/L), Ct is the measured concentration (mg/L) after 24 h, V is the volume of dye solution used (L), and m is the mass of the activated carbon used (mg). In this work, the kinetics of MB and OII adsorption were not considered.

RESULTS AND DISCUSSION

Peat Analysis

As mentioned earlier in material and methods part, the physical properties of peat obtained from northern part of Finland were investigated. Data obtained from the moisture, ash content, and elemental analysis tests are presented in Fig. 1.

According to the results peat is mostly consisting of carbon-containing materials, especially lignin, cellulose, and hemicellulose, 54% on a wet basis. Water content (34%) is also very high compared to carbon content. Elemental analysis of peat showed that nitrogen (1%), sulfur (2%), and hydrogen (6%) content were relatively small compared to carbon and water content. The remaining 3%, ash content, consist mostly of metals or their oxides.

Fig. 1. Results from the moisture, ash content, and elemental analyses of the raw peat sample

Effect of the Carbonization Temperature on the Activated Carbon Yield and Total Carbon of the Activated carbon

The effect of the carbonization temperature, which ranged from 723 to 1073 K, on the total yield and TC was investigated. The results are shown in Table 2. According to the results, the yield decreased from 45.7% to 14.2% when the carbonizing temperature increased from 723 to 1073 K. This finding was in line with earlier studies (Baçaoui et al. 2001; Lua and Yang 2004; Ozdemir et al. 2014).

Higher TC values were obtained when using high carbonization temperatures. More volatile compounds were formed, which increased the TC content (measured as % TC) but decreased the total mass of the activated carbons. Stimely and Blankenhorn (1985) obtained the same results while investigating the behavior of different wood species treated at different temperatures.

Table 2. Effect of the Carbonization Temperature and Impregnation Ratio on the Yield and Total Carbon Content of the Activated Peat Samples

Effect of the Impregnation Ratio on the Yield and Total Carbon content of the Activated Carbons

The effect of the impregnation ratio on the TC and yield of peat-based activated carbon was also investigated. According to the results, which are shown in Table 2, there was a slight correlation between the impregnation ratio and yield. Increasing the impregnation ratio from ¼ to 2 at any temperature lowered the overall yield by a few percentage points. At low concentrations, ZnCl2 reacts with H and O on the surface of the peat and forms H2O and H2, rather than burning away the carbon (CO and CO2), which leads to higher yields, as shown by Liu et al. (2016) and Qian et al. (2007).

Effect of the Carbonization Temperature and Impregnation Ratio on the Specific Surface Area and Pore Size Distribution of the Peat-Based Activated Carbons

The isotherms of the activated peat samples are presented in Fig. 2. The specific surface area and pore size distribution were determined at different activation temperatures (723 to 1073 K) and ZnCl2 impregnation ratios (¼ to 2).

According to the data obtained and presented in Table 3, increasing the temperature from 723 to 1073 K resulted in higher specific surface areas, which was independent of the impregnation ratio. Increasing the carbonization temperature accelerates the volatilization and decomposition of the sample, which leads to an increase in the specific surface area and enhanced pore development (Yorgun and Yıldız 2015).

High impregnation ratios and a high temperature (1073 K) led to a lower surface area and pore volume. The specific surface area and pore volume of the samples that had an impregnation ratio of 2 decreased from 923 to 790 m2/g and from 0.78 to 0.50 cm3/g, respectively, when the carbonization temperature was increased from 873 to 1073 K. The boiling point of ZnCl2 is 732 K, and at 1073 K, melted ZnCl2 expands existing micropores into mesopores. This process leads to a lower overall specific surface area and pore volume (Demiral et al. 2008; Bouchemal et al. 2009). The pore size distribution in all of the peat samples were mainly in the mesoporous region. Increasing the impregnation ratio from ¼ to 1 rapidly increased the specific surface area and pore volume of the activated peat samples. The specific surface area and pore volume for P¼_873 were 341 m2/g and 0.16 cm3/g, respectively, and for P1_873 were 1361 m2/g and 0.69 cm3/g, respectively.

Fig. 2. Adsorption isotherms for peat activated at different temperatures using different impregnation ratios: a) 1:1 impregnation ratio; b) 1:2 impregnation ratio; c) 1:4 impregnation ratio; d) 2:1 impregnation ratio

Table 3. Effect of the Impregnation Ratio and Temperature on the Specific Surface Area (SSA) and Pore Size Distribution of the Activated Peat Samples

The impregnation ratio also had an effect on the pore size distribution. The microporosity decreased when the impregnation ratio increased. In contrast, the mesoporosity increased when the impregnation ratio increased. Other research groups have also come to the same conclusions concerning the effects of the carbonization temperature and chemical activating agent ratio on the specific surface area and pore size distribution (Yang and Qiu 2011; Kumar and Jena 2015; Kumar and Jena 2016b).

Adsorption Tests

The adsorptive properties of the activated carbon were tested using MB and OII adsorption tests. The results of the tests are presented in Table 4 and Fig. 3.

Table 4. Adsorption Ability of the Activated Peat Samples

MB: Methylene blue; OII: Orange II

Fig. 3. Effect of the pore volume on the adsorption ability. The samples are in order of increasing pore volume.

The percentage of dye adsorbed increased with an increasing pore volume. A pore volume of at least 0.3 cm3/g was necessary for any adsorption to occur. The removal of the acidic OII dye was more efficient than the removal of the basic MB dye. The maximum removal of OII was 95% (300 mg/g) for sample P½_723, and the maximum removal of MB was 77% (244 mg/g) for sample P½_873. In addition to the pore volume, the surface groups on the activated carbon might affect the adsorption. Because the removal of the anionic dye (OII) was more efficient than the removal of the cationic dye (MB), there might have been more positively charged functional groups on the activated carbon surface than negatively charged groups. Earlier Ma et al. (2015) reported contradictory findings while investigating the adsorption abilities, with methylene blue and orange II, of the activated carbon produced from banana peels.

Scanning Electron Microscope (SEM) and Transmission Electron Microscope (TEM) Images

The surface structure of the activated peat samples was studied by scanning electron microscopy. Four activated peat samples with different impregnation ratios activated at the same temperature are presented in Fig. 4. According to the SEM images, large pores can clearly be seen on the surface of all of the samples, regardless of the impregnation ratio. These pores can be regarded as transportation pores into the porous systems created by the activation processes even if the meso- and microporous structures are impossible to be visualized at the magnification levels used. Furthermore, a fine porous structure could be observed at the edge or cross-section of the particles using a high magnification (data not shown).

Fig. 4. SEM images of the activated peat samples. The magnification in the images is 5000 X; a) P2_873; b) P1_873; c) P½_873; d) P¼_873

The TEM images of these four peat samples (Fig. 5) showed they had similar structures. All four peat samples had an amorphous structure that is typical of carbon black. According to Fig 5 no remaining metal can be found indicating that the process for metal removal is complete.

Fig. 5. TEM images of the activated peat samples. The magnification for a, b, and c is 100 kX, and for d is 200 kX; a) P1_873; b) P½_873; c) P¼_873; d) P2_873

CONCLUSIONS

  1. The yield of activated carbon varied according to the impregnation ratio and activation temperature used.
  2. The carbon content increased with an increasing activation temperature.
  3. The specific surface area and pore volume increased with increasing temperature and an impregnation ratio of up to 1. However, higher impregnation ratios caused a decrease for both parameters.
  4. The pore size distribution was remarkably changed from micro- to mesoporous when the impregnation ratio was increased from ¼ to 2.
  5. In order to achieve proper adsorption of MB and OII, pore volumes higher than 0.3 cm3/g were needed.
  6. Finally, a slightly higher removal of OII compared with MB was observed.

ACKNOWLEDGEMENTS

Toni Varila acknowledges the Bioraff Botnia foundation (21000030171 Intterreg Botnia-Atlantica), Henrik Romar acknowledges the RenePro foundation (20200224 Intterreg Nord), and Davide Bergna acknowledges the Central Ostrobothnia Cultural Foundation for personal grants. Facilities in the Nanocentre at the University of Oulu were used.

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Article submitted: June 9, 2017; Peer review completed: September 3, 2017; Revised version received and accepted: September 11, 2017; Published: September 15, 2017.

DOI: 10.15376/biores.12.4.8078-8092