Abstract
Upgrading biogas to biomethane is of great interest to change the energy matrix by feeding the renewable fuel produced from biomass waste into natural gas grids or directly using it to replace fossil fuels. The study aimed to assess the adsorption equilibrium of CH4, CO2, and H2O on a coconut-shell activated carbon (CAC 8X30) to provide data for further studies on its efficiency in upgrading biogas by Pressure Swing Adsorption (PSA). The adsorbent was characterized, and equilibrium parameters were estimated from monocomponent CH4, CO2, and H2O equilibrium isotherms. Binary and ternary equilibrium isotherms were simulated, and the selectivity and adsorption capacity of the CAC 8X30 were calculated in dry and wet conditions and then compared with zeolite 13X as a reference material. Regarding characterization, Nitrogen and Hydrogen Physisorption results indicated that 94 % of the pore volume is concentrated in the region of micropores. The adsorption affinity with CAC 8X30 estimated from monocomponent isotherms was in the order KH20>KCO2>KCH4. IAST-Langmuir model simulations presented good agreement with experimental binary equilibrium data. Further simulations indicated equilibrium selectivity for CO2 over CH4 (e.g., 4.7 at 1 bar and 298 K for a mixture of CH4/CO2, 60/40 vol%), which increased in the presence of moisture, indicating its suitability for upgrading humid biogas. Simulations for zeolite 13X suggested that the material is unsuitable in the presence of water vapor but presents higher selectivity than the CAC 8X30 in dry conditions. Hence, the integration of both materials might be helpful for biogas upgrading.
Keywords: Biomethane, Water vapor, Experimental binary equilibrium, Simulated ternary equilibrium, Pressure swing adsorption
1. Introduction
Biogas has been widely studied as an essential alternative for expanding the world's energy supply since it causes lower emissions of carbon dioxide, nitrogen oxides, and particulates compared to other fuels such as oil and coal [1,2]. However, the feasibility of applying biogas as a fuel depends on the removal of minor components such as water vapor (H2O) and hydrogen sulfide (H2S) (purification) and the removal of CO2 from the main mixture of raw biogas formed by CH4/CO2 (upgrading) [[3], [4], [5]]. The fuel obtained after upgrading, namely biomethane, presents a high methane purity, whose exact value depends on local legislation. In general, biomethane must present a composition of methane of over 90 mol% (CH4 ≥ 90 mol%), whereas CO2 cannot exceed 3 mol.% (CO2 ≤ 3 mol.%).
There are currently many known techniques for biogas purification and upgrading, including Membranes [6,7], Chemical Absorption and Water Scrubbing [8,9] and Adsorption [10,11]. Among these, Pressure Swing Adsorption (PSA) stands out because it provides high-purity methane and high automation capacity, and there are no chemical agents other than the adsorbent. On the other hand, the installation of PSA plants is often impaired by the high initial investment, driven by the high cost of commonly used commercial adsorbents, such as carbon molecular sieves, zeolites, and metal-organic frameworks [2,12]. In fact, the chosen material must present a low cost, in addition to technical aspects such as high equilibrium and kinetic selectivity, elevated CO2 adsorption capacity, and easy regeneration [13].
In general, activated carbons (AC) represent costs up to 100 times lower per kilogram of material than other materials [14] and their potential for upgrading biogas has already been reported [[15], [16], [17]]. Besides that, the study of Durán and coworkers [17] using plant-origin activated carbon showed that the material was selective to CO2 even in the presence of moisture, suggesting that the carbonaceous material might remove water vapor and provide the upgrading of biogas simultaneously, eliminating the need for an additional column. Vilella and coworkers [16] synthesized a coconut AC and evaluated it at low-pressure ranges regarding the separation of the mixture CH4/CO2. The material presented selectivity and working capacity values comparable to the tested commercial adsorbents.
The commercial coconut-shell activated carbon (CAC 8X30) used in this paper was successfully used to remove H2S from raw biogas [18] and for methane storage [19]. To the best of our knowledge, however, there are no reports about its efficiency in upgrading biogas nor about the influence of moisture on the selectivity for CO2. The present study aims to develop an experimental and theoretical assessment of the adsorption equilibrium of CH4, CO2, and H2O on CAC 8X30 to provide data for further studies on its efficiency in upgrading biogas to biomethane by PSA. The AC was characterized by Physisorption, Helium Pycnometry, Mercury Porosimetry, Elemental Analysis, DSC, FTIR, and Raman. Monocomponent equilibrium data were obtained for the three components from adsorption isotherms at temperatures of 298 and 323 K, and binary equilibrium data (CH4/CO2) from breakthrough curves at 298 K. The predictions were evaluated by the Ideal Adsorbed Solution Theory (IAST), through parameters obtained from the monocomponent isotherms, fitted by Langmuir and Multisite Langmuir models, and through the respective extended models. Besides, the selectivity for CO2 was simulated for binary (CH4/CO2) and ternary (CH4/CO2/H2O) mixtures to assess biogas upgrading by the CAC 8X30 in the presence of moisture.
2. Material and methods
2.1. Materials
Coconut shell activated carbon (CAC 8X30) was supplied by the company Brascarbo Agroindustrial Ltda™. The gases used for the experiments (CO2, CH4, H2O, and He) were of analytical grade, with purity ≥ 99.995 %.
2.2. Characterization of the adsorbent
Several techniques were used to characterize the CAC 8X30 and thus provide information for the mathematical models (see Table 1). The data obtained embraced physical properties such as the size of pores, density, porosity, heat capacity, and chemical properties like functional groups and elemental composition.
Table 1.
Technique | Procedure |
---|---|
Physisorption | Textural properties were assessed following the methods described by Castro-Gutiérrez [20] and Jagiello [21] for heterogeneous surfaces. N2 and H2 isotherms were obtained using a 3FLEX (Micromeritics) adsorption apparatus. The pore size distributions (PSDs) and the surface area were calculated by combining N2 and H2 sorption data, and SAIEUS software was used to apply the two-dimensional nonlocal density functional theory (2D-NLDFT). By integration of the PSDs, total pore volumes (VT), ultramicropore volume (Vult-micro), supermicropore volume (Vsup-micro), micropore volume (Vmicro), and mesopore volume (Vmes) were calculated. The PSDs were also used to calculate the average pore size (L0) and average micropore size (L0-micro). |
Mercury Porosimetry | The material's porosity was assessed by Hg porosimetry on Auto Pore IV equipment (Micromeritics). |
Helium Pycnometry | The analysis of Helium Pycnometry (AccuPyc 1330 – Micromeritics) was carried out to obtain the density of the material, using a rate of equilibration of 0.0050 psi min−1, 20 purges and 10 runs at 19.5 psi. |
Differential Scanning Calorimetry (DSC) | DSC run was conducted from 15 to 100 °C (DSC-60, Shimadzu) with a nitrogen flow rate of 20 ml min−1. The heat capacity of the CAC 8X30 was then determined following the standard DIN 51007 [22,23]. |
Elemental Analysis | Bulk contents of C, H, N, S, and O were measured in a Vario EL Cube analyzer. Previously dried samples of 2 mg were placed in the equipment. The samples were combusted, and the generated gases were separated using selective adsorption. The content of combustion gases was analyzed using a thermal conductivity detector for C, H, N, and S. On the other hand, the oxygen content was measured based on the CO peak. |
Fourier-Transform Infrared Spectroscopy (FTIR) | FTIR spectroscopy (Perkin Elmer) was used to assess the surface functional groups of pristine activated carbon (PAC) and used activated carbon (UAC). The UAC was submitted to several CH4 and CO2 adsorption/desorption cycles. The spectra were obtained by diffuse reflectance in the mid-infrared region, between 4000 and 450 cm−1, with a resolution of 4 cm−1 and 16 accumulations. |
Raman Spectroscopy | Horiba micro-Raman system, model LabRAM HR Evolution. Laser power 10 mW, 405 nm excitation wavelength, and CCD detector with additional sample preparation. Voigt functions of the Fityk program (version 1.3.1) were used for the deconvolution of the Raman spectra. |
2.3. Adsorption isotherms - monocomponent systems
The high-pressure CO2 and CH4 adsorption isotherms were carried out at 298 K and 323 K up to 32 bar in an automatic manometric high-pressure device HPVA II (Micromeritics), whereas the H2O isotherms were measured at 298K and 323K up to the saturation pressure (Belsorp max II). Before any measurement, the samples were outgassed under a secondary vacuum (7 × 10−6 mbar) and 383 K for at least 48 h. After evacuation, the pressure was increased stepwise to 32 bar (CH4 and CO2) or up the saturation pressure (H2O), and then stepwise decreased. At each step, the amount of gas adsorbed by the sample was calculated as the difference between the amount of gas dosed and determined at the equilibrium pressure. The contribution of the empty cell was systematically measured and subtracted from all data to improve accuracy.
2.4. Binary equilibrium experimental data
Binary equilibrium was experimentally calculated from binary breakthrough curves of the mixture of CH4 (60 vol%) and CO2 (40 vol%), considering the variations of flow, temperature inside the column, molar fraction of each component, and density of the gas mixture all along the curve. The adsorbed amount of each component was calculated following the mass balance presented in Eq. (1), where Ci,in and Ci,out were calculated by the ideal gas state equation (Eq. 2), mads was measured before packing the bed, using previously dried AC. Besides, bed porosity (Ɛbed) was determined following Eq. (3), while particle (ρp) and bed density (ρbed) were calculated by Eqs. (4), (5)), respectively. True density (ρtrue) was obtained by Helium Pycnometry and particle porosity (εp) by Mercury Porosimetry.
(1) |
(2) |
(3) |
(4) |
(5) |
Note: The physical meaning and the units for each component of Eq. (1) to Eq. (5) are described in the nomenclature table.
Besides, other parameters needed to calculate the adsorbed amount (Eq. (1)) were measured during the process at the inlet and at the outlet of the adsorption bed, namely temperature (Tin and Tout), pressure (Pin and Pout), volumetric flow (Qin and Qout), and molar fraction (yin and yout), as can be seen in the scheme of the experimental apparatus used for the breakthrough curves presented in Fig. 1.
3. Mathematical modeling
The mathematical modeling within the present work was performed by determining the equilibrium parameters from the monocomponent isotherms and then using them to predict the binary behavior. The software Gproms™ was used to estimate the equilibrium parameters and for the simulations [24].
3.1. Monocomponent equilibrium
The monocomponent equilibrium isotherms for CH4, CO2, and H2O were described by the well-known models of Langmuir (L) and Multisite Langmuir (ML), whose equations are presented in Table 2.
Table 2.
The adsorption equilibrium constant (Ki) depends on temperature according to the Van't Hoff's equation (Eq. (6)), while the heat of adsorption can be related to the exponential term (Eq. (7)):
(6) |
(7) |
3.2. Binary (CH4/CO2) and ternary (CH4/CO2/H2O) equilibrium
The binary equilibrium prediction was carried out using the extended models of Langmuir and Multisite Langmuir (L-L and ML-ML, respectively), simulating the binary profiles through the parameters determined from the monocomponent isotherms. The compositions tested simulated the concentrations of CH4 and CO2 in raw biogas, which vary from 50 to 70 CH4% and 30–50 CO2% [2]. Besides, the Ideal Adsorbed Solution Theory (IAST) was also employed to simulate the binary isotherms, using parameters estimated from the Langmuir model (IAST-L) and the Multisite Langmuir model (IAST-ML).
For that, a reduced spreading pressure is calculated for all constituents at equilibrium by integrating the Gibbs’ adsorption and using the monocomponent adsorption models shown in Table 2 since, according to IAST, the spreading pressures for all constituents at equilibrium are equal to the mixture spreading pressure. So, the reduced spreading pressure of a pure component in the standard state () is given by Eq. (8), where qeq,i is given by the monocomponent isotherm, while the resulting spreading pressure for two components (i and j) can be described as shown in Eq. (9) [16,27].
(8) |
(9) |
The predicted values obtained using parameters estimated from monocomponent isotherms models (see Table 2) were compared with those experimentally obtained from the breakthrough curves, aiming to analyze the predictability of simulated binary curves and the reliability of the experimental data. Besides, ternary equilibrium was simulated by IAST-L by using the parameters estimated from the monocomponent isotherms of each component of the ternary mixture (CH4/CO2/H2O). Different concentrations of water vapor, defined according to the average composition of water in raw biogas, which varies from 1 to 5 % [2], were simulated to test the effect of moisture on biogas upgrading.
Binary and ternary isotherms were also simulated for a reference adsorbent (zeolite 13X) using experimental data for adsorption equilibrium of CH4 and CO2 [28] and H2O [29] on zeolite 13X from the literature to compare its behavior with that of the CAC 8X30.
3.3. Selectivity
As an indicative of the potential of the CAC 8X30 of separating the binary (absence of water vapor) and ternary mixtures (presence of water vapor), its selectivity to CO2 over CH4 was calculated based on the uptake of each component (qi) and the partial pressure (pi), as can be observed in Eq. (10). The same procedure was taken for the reference adsorbent (zeolite 13X).
(10) |
4. Results and discussions
4.1. Characterization
Essential information on the physical properties of the CAC 8X30 was obtained to enable the calculations of experimental binary isotherms and for the mathematical modeling of the continuous process in PSA unity in forthcoming studies. The density of the CAC 8X30 obtained by Helium Pycnometry was 1700 kg m−3, while the porosity obtained by Mercury Porosimetry was 0.374.
From the Physisorption, it was possible to assess in detail the textural characteristics of the material. The Physisorption isotherms and the Pore Size Distribution (PSD) are presented in Fig. 2a and b, respectively. One may notice that there is a trimodal distribution within the micropore region (pore with ≤2 nm). In fact, the volume of micropores correspond to 94 % of the total pore volume (Vmicro/VT), whereas the remaining 6 % are ascribed to mesopores (Vmes/VT), as can be extracted from the values of pore volume presented Table 3. Within the micropore region, 59 % are composed of ultramicropores (pore with <0.7 nm) and 41 % of supermicropores (0.7 ≤ pore with ≤ 2 nm) [30]. Besides that, the calculated overall average pore size was 1.1 nm, while the average micropore size was 0.7 nm.
Table 3.
Textural Properties | |||||||
---|---|---|---|---|---|---|---|
SNLDFT [m2 g−1] | VT [cm3 g−1] | Vmes [cm3 g−1] | Vmicro [cm3 g−1] | Vult-micro [cm3 g−1] | Vsup-micro [cm3 g−1] | L0 [nm] | L0-micro [nm] |
1105 | 0.35 | 0.02 | 0.34 | 0.20 | 0.14 | 1.1 | 0.7 |
These pore characteristics might contribute to the kinetic separation of gases because materials with narrow pores may successfully separate mixtures of gases when there is a difference in the kinetic diameter of the gases to be selectively adsorbed [30], as the case of the mixture CH4/CO2. Besides that, due to the high surface area found for this CAC 8X30 (SNLDFT = 1105 m2 g−1), the material could also be used for other purposes, such as gas storage, as reported elsewhere [19]. On the other hand, chemical aspects also play an important role because they affect the affinity between adsorbent and adsorbate [31] and thus should be addressed.
The specific heat capacity of the CAC 8X30 was determined from the DSC, comparing the signals of a standard and the carbon material. In Fig. 3a, the DSC signals of the standard (sapphire) as well as the sample (AC) are plotted along with the signal of the empty crucible, which was used to blank correct the signals [22,23]. The temperature is also plotted to have a better understanding of the methodology. In Fig. 3b, the calculated heat capacities at different temperatures are plotted, highlighting the one at 25 °C (298 K), where a value of 1.86 J K−1 g−1 was found.
The chemical properties of the CAC 8X30 were assessed in this paper by Elemental Analysis and FTIR. It can be noticed from the results presented in Table 4 that the material has high carbon content, with oxygen and nitrogen in low compositions. The carbon content is much higher than that found in other studies reported in the literature for activated carbons. According to Rattanaphan and coworkers [32], carbon atoms play an essential role in the organization of the structure of activated carbon. In contrast, nitrogen and oxygen affect the reaction that may occur on the material's surface.
Table 4.
Elemental Analysis | ||||
---|---|---|---|---|
C [wt. %] | H [wt. %] | S [wt. %] | O [wt. %] | N [wt. %] |
93.8 | 0.84 | 0.0 | 4.9 | 0.46 |
The IR spectra shown in Fig. 4 were obtained for pristine activated carbon (PAC) and used activated carbon (UAC), in which UAC was submitted to several adsorption cycles (saturation and regeneration) using CH4/CO2 binary mixtures. Since most literature reports treat the separation of CH4/CO2 binary mixtures by adsorption exclusively as physical adsorption, the objective of the FTIR analysis for PAC and UAC was to investigate if there were changes in the functional groups after the contact with these adsorbates, which could indicate if there is some chemical interaction between adsorbent and adsorbates.
Activated carbons may present both acid and basic chemical characteristics. The surface acidity is related to the functional groups that contain oxygen, such as carboxyl groups, lactones, and phenols, whereas the basicity is commonly ascribed to the presence of functional groups ether, hydroxyl, and carbonyl [33]. In general, it can be said that the CAC 8X30 presents a neutral surface containing both acidic and basic groups, which is in accordance with the point of zero charge (pHpzc = 7.03) reported elsewhere [18] for the same material.
The strong absorption band 3435 cm−1 can be assigned to the O–H bond stretching vibration. The 2434 cm−1 band was attributed to alkyne [34], while the absorption bands at 2922 cm−1, 2862 cm−1, and 1434 cm−1 refer to C–H asymmetric and symmetric stretching [35]. The band at 1728 cm−1 can be ascribed to C O in ester [36], whereas the bands at 1634 cm−1, 1385 cm−1, 1284 cm−1, 1105 cm−1, and 1048 cm−1 are associated with asymmetric and symmetric stretching vibrations of C–O bond, present in carboxylic groups, aromatic ethers, esters, and phenols [35] of lignin. The band at 1568 cm−1 can be associated with C C from alkenes [36], and one minor band at 775 cm−1 is related to out-of-plane deformation of C–H from aromatic structures [35]. All identified bands are summarized in Table 5.
Table 5.
Wavenumber | Assignments | Functional groups |
---|---|---|
3435 | O–H stretching | Hydroxyl |
2922 | C–H asymmetric and symmetric stretching and axial deformations | Alkane |
2862 | ||
1434 | ||
2434 | C C stretching bond | Alkyne |
1728 | C O stretching | Ester |
1634 | C–O symmetric and asymmetric axial deformation vibrations | Carboxylic acids, aromatic ethers, esters and phenols |
1385 | ||
1284 | ||
1105 | ||
1048 | ||
1568 | C C stretching band | Alkene |
775 | C–H out-of-plane deformation | Aromatic ring |
By carefully comparing the spectra of PAC with the one of UAC, it can be noticed that there is a pronounced modification in the latter material. The band at 1568 cm−1 found in PAC, which refers to the C C bond of alkenes, is no longer present in UAC after contact with methane and carbon dioxide. Besides that, there is a pronounced increase in the band's intensity at 3435 cm−1, which refers to the OH group of hydroxyls [34]. The disappearance of this band might be related to some level of chemical interaction between carbon dioxide and the material's surface. So, the alkene group may have undergone oxidation by CO2, breaking the double bond and forming new hydroxyl groups (higher intensity at 3435 cm−1). On the other hand, the lower affinity of CH4 with PAC, observed in the equilibrium isotherms (see Fig. 6), is justified by the weak interactions between methane molecules and the carbon surface (van der Waals). Thus, they are only intermolecular interactions, which are less intense than those between CAC 8X30 and CO2.
By analyzing the Raman spectra of PAC and UAC presented in Fig. 5, one may see two well-defined peaks, near 1345 cm−1 and around 1595 cm−1. Liu and coworkers [37] identified these same peaks for an AC used for adsorption of sulfamethazine. The authors indicated that the peak near 1345 cm−1 may be caused by reasons such as low symmetry, arrangement of the carbon structure, and lattice defects. On the other hand, the peak near 1595 cm−1 may be ascribed to graphite. Comparing the spectra of PAC and UAC (Fig. 5), one cannot define any relevant difference by the Raman technique.
4.2. Monocomponent equilibrium
As expected, the equilibrium experimental data showed that the amount of CO2 adsorbed was much higher than that of CH4 within the assessed pressure range, which means that the adsorption capacity of the CAC 8X30 for the carbon dioxide is much higher (see Fig. 6). By taking points for the adsorbed amount of CO2 and CH4 from the monocomponent adsorption isotherms at 298 K at different pressures, one may achieve ratios (qCO2/qCH4) of 2.5, 1.7, and 1.6, at the beginning (1 bar), in the middle (15 bar), and at the end (30 bar) of the tested pressure range. This behavior has already been reported in other studies on activated carbons [1,15,38] and might indicate the material's potential to separate the gaseous mixture even at low pressure.
In Table 6, a comparison with the adsorption capacities at low pressure (P = 1 bar) found in other studies can be observed. Besides, the values for qmax, ΔHads,i, and Ki (which is a function of K1 and K2 - see Eq. (6) and Eq. (7)), were all higher for carbon dioxide when compared to methane (see Table 7). Although there were indications of chemical interaction between CO2 and CAC 8X30 in the FTIR analysis, there is no pronounced difference between the values of heat of adsorption for CH4 and CO2, so the uptake of both adsorbates is mainly due to Physisorption rather than Chemisorption. As could be concluded from the FTIR results reported here and from pHpzc reported elsewhere [18], the CAC 8X30 presents basic groups that may facilitate the CO2 adsorption. Overall, less acidic AC tend to have their CO2 adsorption capacity favored [39], which may explain the higher affinity observed between CAC-CO2 than between CAC-CH4.
Table 6.
Table 7.
Model | Adsorbate | (mol kg−1) | K1 (bar−1) | K2 (K) | a | (kJ mol−1) |
---|---|---|---|---|---|---|
Langmuir | CO2 | 5.48 | 3.54 | 3504.63 | – | 29.14 |
Multisite Langmuir | 7.59 | 2.76 | 3394.67 | 2.14 | 28.22 | |
Langmuir | CH4 | 3.82 | 0.88 | 2524.48 | – | 20.99 |
Multisite Langmuir | 6.24 | 0.60 | 2465.85 | 2.61 | 20.50 |
To assure thermodynamic consistency, the product . was maintained for both adsorbates (. ) = . )) in the model of Multisite Langmuir.
Regarding the mathematical models used to describe the monocomponent isotherms, one may notice by observing Fig. 6 that both Langmuir and ML models showed good agreement with the experimental data up to approximately 8 bar, whereas at higher pressures (P > 8), ML described the experimental data better. It is worth mentioning that the ML isotherm considers that one single molecule can occupy more than one adsorption site, differently from the Langmuir isotherm (one molecule occupies only one site). This assumption is taken into account by using the parameter α, which is defined as the number of sites or equivalent spaces occupied by the component. So, a larger molecule should have a larger alpha on the same surface, which is in line with the alpha values shown in Table 7.
Although the ML isotherm also considers adsorption on a homogeneous surface and that there are no interactions between the adsorbate molecules, it has been effectively employed to describe systems in which the adsorbent surface sites are heterogeneous such as activated carbons, zeolites, and carbon molecular sieves [26,30,40]. This can be attributed to the fact that the heterogeneity of the adsorbent surface sites may affect the value for α, and thus allow a good description, even if empirical, of the adsorption equilibrium [40]. In general, it can be concluded that the estimated parameters from both Langmuir and ML may be employed to design a continuous adsorption process such as PSA at low pressures, whereas, at pressures higher than 8 bar, the latter model would be preferable.
By analyzing the water vapor isotherm presented in Fig. 7a, one may see a high uptake of H2O by the CAC 8X30 at very low pressures. In fact, the saturation pressures (Psat) for the adsorption isotherms at 298 K and 323 were 3.1 × 10−2 and 1.2 × 10−1 bar, respectively. Besides that, as expected for an exothermic process, the uptake was clearly higher at the lowest temperature within the complete pressure range, as can be seen in the zoomed part of the graph, which corresponds to the isotherm region from 0 to 10 % of the saturation pressure (P/Psat = 0.1).
Considering that the water vapor concentration in raw biogas varies from 1 to 5 vol %, the adsorption equilibrium parameters of H2O on CAC 8X30 were estimated using the limited region of the isotherm (up to P/Psat = 0.1). As can be observed in Fig. 7b, where the experimental and simulated data are plotted against relative pressure up to 0.1, the Langmuir model showed a good fit to the experimental data, generating the following estimated parameters: qmax = 1.42 mol kg−1, K1 = 2.77 × 103 bar−1, and K2 = 5.77 × 103 K. Moreover, the heat of adsorption for H2O on CAC 8X30 was 47.9 kJ mol−1, which is slightly higher than the value of 43.9 kJ mol−1 found elsewhere for the system pine sawdust-based activated carbon and water vapor [17].
4.3. Binary equilibrium (CH4/CO2) and selectivity
Experimental binary isotherms were obtained from kinetic binary breakthrough curves from 1 to 5 bar at 298 K and compared with simulated binary isotherms. By observing the values of adsorption capacities (i.e., equilibrium points of the kinetic curves) shown in Table 8, one may notice that there is a preference to adsorb CO2 over CH4 in a mixture of CH4 (60 vol%) and CO2 (40 vol%), as expected. In fact, as can be seen in the zoomed part of Fig. 6, the adsorption of carbon dioxide is considerably higher than that of methane, even at low pressures.
Table 8.
Total pressure (bar) | Partial pressure (bar) |
qeq (mol kg−1) |
qtot (mol kg−1) | ||
---|---|---|---|---|---|
CH4 | CO2 | CH4 | CO2 | ||
1 | 0.6 | 0.4 | 0.4 | 1.5 | 1.9 |
2 | 1.2 | 0.8 | 0.6 | 2.1 | 2.7 |
3 | 1.8 | 1.2 | 0.8 | 2.7 | 3.5 |
4 | 2.4 | 1.6 | 1.0 | 3.1 | 4.1 |
5 | 3.0 | 2.0 | 1.2 | 3.3 | 4.5 |
In Fig. 8a, the experimental values are plotted along with the simulations of the binary mixture made from parameters obtained from pure gas isotherms, which were performed using IAST in conjunction with the Langmuir model (IAST-L) and ML (IAST-ML) and by using the single models (Langmuir and ML). One may notice that the IAST fits become less accurate as pressure increases. This was also observed by Vilella and coworkers [16] and may be explained by the fact that at higher pressures, the interactions in the adsorbed phase may become dominant at high surface coverage applicability, thus reducing the reliability of IAST.
Moreover, the simulations are, in general, more accurate in describing the CO2 behavior, presenting average standard deviations for CO2 adsorption from 3 to 5 % for IAST-L, Langmuir, IAST-ML, and ML (the last two models provided practically identical results so that they overlaid each other in the graphic). Durán and coworkers [17] observed that the uptake of CH4 from a binary mixture by a saw-dust-based activated carbon is probably more affected than that of CO2. The experimental and simulated total amount adsorbed (CH4 + CO2) can also be observed in Fig. 8b, confirming the good agreement between experimental and simulated curves.
Considering the low deviation between the simulations using parameters from monocomponent isotherms (mainly IAST-L) and the experimental uptake calculated from binary breakthrough curves, these estimated equilibrium parameters are strongly reliable, and the model can be used to predict the binary equilibrium of adsorption for different compositions, temperatures, and pressures, which allows in turn, the calculation of the selectivity.
In Fig. 9a, binary isotherms simulated from 0 to 5 bar at 298 K for three different CH4/CO2 vol% compositions can be observed. It can be noted that, as expected, the higher the composition, the higher the absolute uptake by the AC. So, the greatest CH4 uptake occurs for the 70-30 vol% composition, while the greatest uptake of CO2 happens for the composition of 50-50 vol%. At all compositions, however, the adsorption capacity of CO2 exceeded that of CH4.
The selectivity of the CAC 8X30 for CO2 with pressure increase was calculated by IAST-L and is presented in Fig. 9b, wherein it can be observed that selectivity increases with total pressure up to 5 bar for all tested compositions. This makes sense since although the slope strongly declines after 3 bar on the monocomponent isotherms for both adsorbates (see Fig. 6), there is no well-defined plateau at 5 bar yet. Villela and coworkers [16] also achieved this profile for the selectivity of CO2 over CH4 s (70-30 vol%, CH4/CO2) at 293 K using a coconut-based activated carbon. However, the selectivity calculated based on IAST-Toth prediction in the cited study at 1 bar was slightly lower than 2, while in the present study, it was 4.7 (calculated based on IAST-L predictions).
The CAC 8X30 presents thus a high equilibrium selectivity for CO2 over CH4, which may indicate a good potential to be applied in separation processes such as PSA. However, it must be kept in mind that these results were achieved using synthetic mixtures, neglecting the presence of minor contaminants such as water vapor and considering only the major compounds of raw biogas. Therefore, simulations including water vapor were conducted to assess the material's behavior in wet conditions.
4.4. Ternary equilibrium (CH4/CO2/H2O) and selectivity
The IAST-L model was further employed to simulate ternary equilibrium uptake, including the presence of water vapor, and using the parameters estimated from the monocomponent H2O isotherms (see section 3.1). As can be seen in Fig. 10, the adsorbed amount of H2O is high even at low pressures due to its very high affinity with the AC (see values of K1 und K2 in section 4.2) and decreases with increasing pressure, while the amount of adsorbed CH4 and CO2 increases with pressure like in the dry (binary) system. By applying K1 and K2 estimated from the Langmuir isotherm in Equation (6) and taking as example the temperature of 298 K, one achieves the equilibrium constants for CO2 (K = 1.21 bar-1), CH4 (K = 0.41 bar-1) and H2O (475.9 bar-1), which clearly shows that the affinity of water vapor to CAC 8X30 is significantly higher.
CO2 adsorption on ACs at low to moderate pressures is often negatively affected by the presence of H2O, due to the strong affinity of water with surface functional groups of ACs [41]. By quantitatively comparing the binary isotherms (dry conditions, Fig. 9) with the ternary isotherms (wet conditions, Fig. 10), it can be seen that the adsorbed amount of both methane and carbon dioxide reduced in the presence of water vapor (3 wt% in Fig. 10), as expected. Taking specifically the simulated uptake for a wet ternary mixture of (CH4/CO2/H2O, 58.2/38.8/3.0 vol%) in comparison with the dry binary mixture (CH4/CO2, 60-40 vol%), the decrease was 64 % for CH4 and 60 % for CO2 at 1 bar. At 5 bar, the reductions corresponded to 41 % and 38 %, respectively.
According to the model proposed by Do and Do [42], water vapor molecules get adsorbed onto functional groups by chemisorption and chemisorbed water might then form a site for further water adsorption by hydrogen bonding forming thus clusters. When the concentration of water vapor within these cluster reaches a certain threshold, the molecules are finally adsorbed into the micropores. However, at high pressures, the presence of pre-adsorbed water can promote the uptake of CO2 even through mechanisms other than adsorption, including dissolution and hydrate formation [41]. In the present study, however, the pressure range is low to moderate, which explains the negative influence on CH4 and CO2 adsorption in the presence of water vapor.
On the other hand, since the adsorption of CH4 seems to be more affected by the presence of water vapor, the selectivity of the AC 8X30 for CO2 over CH4 tends to become even higher with increasing water vapor concentration (from 1 to 5 wt%) within the simulated pressure range for all simulated biogas compositions. This can be seen in Fig. 11, where the selectivity for mixtures containing water vapor is compared with that of dry CH4/CO2 mixtures of 50/50 vol% (Figs. 11a), 60/40 vol% (Fig. 11b), and 70/30 vol% (Fig. 11c). Thus, the presence of water vapor caused a reduction in the adsorption capacity of the AC 8X30 for both major compounds of biogas, but the selectivity towards CO2 was facilitated in comparison with the dry case.
Durán and coworkers [17] also reported such behavior for the adsorption of CH4 and CO2 by a pine sawdust-based activated carbon in the presence of moisture. In their study, the authors concluded that even reducing the adsorption capacity for CO2 in the presence of moisture, the activated carbon showed great potential and could thus provide the upgrading of biogas without the need for a complete water removal prior to the adsorption unit. In fact, reference materials such as zeolite 13X may present a much greater selectivity towards CO2 in dry conditions, but the presence of small concentrations of water may impair the removal of CO2 from biogas because of the high affinity and high adsorption capacity of zeolite 13X for H2O even at low partial pressures [29].
To demonstrate this behavior and compare it with that of the CAC 8X30, adsorption equilibrium experimental on zeolite 13X were taken from the literature data for CH4, CO2, and H2O (see Table 9). For the estimation of the equilibrium parameters, the same procedure described in sections 3.1, 4.2 was followed. By analyzing the estimated parameters presented in Table 9, one may notice that both adsorption capacity (qmax,i) and affinity (Ki = f (K1,i, K2,i, Ti)) are much higher for H2O than for the other adsorbates. Although it was also observed for the CAC 8X30, the values estimated for zeolite 13X are at least one order of magnitude greater than those estimated for the activated carbon. Using the estimated parameters K1 and K2 to calculate the affinity of the materials with water at 298 K (see Eq. (6)), we achieved 7.9 × 103 and 4.7 × 102 for zeolite and activated carbon, respectively. On the other hand, the affinities for CH4 and CO2 were in the order of 10−2 (13X) and 10−1 (AC) for CH4 and of order 1 for CO2 for both materials.
Table 9.
As shown in Fig. 12a, the reference material presents a high adsorption capacity for CO2 and provides a high selectivity for CO2 over CH4 in dry conditions. However, the presence of 3 % water vapor caused a pronounced reduction of selectivity (Fig. 12b), unlike the behavior simulated for AC 8X30, when selectivity increases with the presence of water vapor (Fig. 11). Taking as a quantitative example the simulated selectivities for zeolite 13X at 298 K, it was noticed that the values reduce from 44 (dry) to 14.5 (3 % water vapor) and from 40 (dry) to 9.8 (3 % water vapor) at 1 and 5 bar, respectively.
It is to be noticed that although the simulated selectivity of zeolite 13X in wet condition seems to be even higher than that of AC 8X30 (e.g., 11.1 and 6.1 for zeolite 13X and CAC 8X30, respectively, at 3 bar, 298 K, and 3 wt%), it does not mean that the reference material presents a good behavior in the presence of water vapor. In fact, by evaluating this result along with the adsorption capacity of CO2, one may notice that almost no CO2 uptake can be performed by the zeolite 13X in wet conditions within the complete tested pressure range (CH4/CO2/H2O, 58.2/38.8/3.0 vol%). For the same system, the carbonaceous material presents a pronounced adsorption capacity for CO2 even with the presence of water vapor (e.g., 1.9 mol kg−1 at 5 bar, see Fig. 10). Even when summed, the uptake of CH4 and CO2 by the zeolite 13X are in order of 10−6 mol kg−1. In contrast, the adsorption capacity for H2O is around 14.7 mol kg−1, as shown in Fig. 12c. This represents a reduction in the CO2 adsorption capacity of more than 99 % compared with the dry (binary) scenario.
Thus, zeolite 13X would not be suitable for upgrading humid biogas, while the CAC 8X30 could be employed without requiring complete water removal before the adsorption unit. On the other hand, the simulations performed for dry (binary) conditions showed higher values for selectivity and CO2 adsorption capacity for zeolite 13X than for the CAC 8X30, as expected. Hence, further studies, including kinetic experimental data and modeling, may indicate the suitability of integrating both materials to upgrade biogas containing minor contaminants such as water vapor, either as hybrid or as separate adsorption beds.
5. Conclusions
The present paper has shown the potential of a coconut-shell activated carbon (CAC 8X30) to remove CO2 from biogas in dry (CH4/CO2) and wet (CH4/CO2/H2O) conditions. The adsorbent presents a higher adsorption capacity of CO2 compared with CH4 within the complete tested pressure range. Binary experimental data confirmed the good prediction capacity of the IAST-Langmuir model as well as the preference of the material for removing CO2 from the binary mixture. Besides, the material presents high microporosity, which might favor a kinetic separation of the CH4/CO2 mixture in a continuous process.
By simulating ternary isotherms with the presence of moisture, it was found that, despite the reduction in CO2 uptake, the CAC 8X30 shows excellent potential in CO2 removal from a biogas stream, with an increase in selectivity in the presence of water vapor. On the other hand, zeolite 13X was not able to remove CO2 from ternary mixtures but showed a higher selectivity in dry (binary) conditions. Thus, it was evidenced that CAC 8X30 could be employed for the upgrading of biogas without the need for water removal before the adsorption unit, but a higher selectivity might be achieved by integrating the use of the carbonaceous material with the zeolite 13X.
Further studies on the kinetic of CO2 removal, including experimental data and modeling, are required to better evaluate the suitability of the tested activated carbon in continuous operation mode and the viability of integrating the use of both materials for the upgrading of biogas containing water vapor in cyclic processes such as PSA.
Funding
National Council for Scientific and Technological Development (Proc. 313734/2021-6), BRF S.A., International Center of Renewable Energies – Biogas (CIBiogás), and Araucária Foundation (Proc. PBA202211000083).
Data availability statement
Data associated with this study has not been deposited into any publicly repository. All data relevant to this study have been included in the paper. Additional data might be provided upon request.
Nomenclature table | |
---|---|
Symbols | Meaning |
Feed concentration of component i [mol L−1] | |
Outlet concentration of component i [mol L−1] | |
Equilibrium constant for component i [bar−1] | |
K1,i | Pre-exponential constant for the temperature dependence of Ki [bar−1] |
K2,i | Exponential term for the temperature dependence of Ki [K] |
Mass of adsorbent [kg] | |
P | Pressure [bar] |
qeq,i | Adsorbed concentration in equilibrium of component i [mol kg−1] |
qmax,i | Maximum adsorption capacity of component i [mol kg−1] |
Volumetric flow of component i at the inlet of the column [L min−1] | |
Volumetric flow of component i at the outlet of the column [L min−1] | |
R | Ideal gas constant [kJ mol−1 K−1] |
T | Temperature [K] |
Tref | Reference temperature [K] |
Volume of the bed [L] | |
yi | Molar fraction of component i |
yin | Inlet molar fraction |
yout | Outlet molar fraction |
Greek letters | Meaning |
Number of adsorbent sites occupied by the adsorbate molecule | |
Heat of adsorption for component i [kJ mol−1] | |
Porosity of the fixed bed | |
Porosity of the particle | |
ρbed | Bed density [kg m−3] |
ρp | Particle density [kg m−3] |
ρtrue | True density [kg m−3] |
CRediT authorship contribution statement
Junior Staudt: Writing – review & editing, Writing – original draft, Validation, Software, Methodology, Investigation, Data curation, Conceptualization. Cassiano Moreira Musial: Validation, Software, Investigation. Rafael Canevesi: Investigation, Conceptualization. Vanessa Fierro: Conceptualization. Caroline Ribeiro: Investigation. Helton José Alves: Conceptualization. Carlos Eduardo Borba: Writing – review & editing, Supervision, Software, Project administration, Methodology, Funding acquisition, Formal analysis, Conceptualization.
Declaration of competing interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgments
The authors thank the Institute Jean Lamour (IJL), Épinal - France, for technical and laboratory support.
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Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Data Availability Statement
Data associated with this study has not been deposited into any publicly repository. All data relevant to this study have been included in the paper. Additional data might be provided upon request.
Nomenclature table | |
---|---|
Symbols | Meaning |
Feed concentration of component i [mol L−1] | |
Outlet concentration of component i [mol L−1] | |
Equilibrium constant for component i [bar−1] | |
K1,i | Pre-exponential constant for the temperature dependence of Ki [bar−1] |
K2,i | Exponential term for the temperature dependence of Ki [K] |
Mass of adsorbent [kg] | |
P | Pressure [bar] |
qeq,i | Adsorbed concentration in equilibrium of component i [mol kg−1] |
qmax,i | Maximum adsorption capacity of component i [mol kg−1] |
Volumetric flow of component i at the inlet of the column [L min−1] | |
Volumetric flow of component i at the outlet of the column [L min−1] | |
R | Ideal gas constant [kJ mol−1 K−1] |
T | Temperature [K] |
Tref | Reference temperature [K] |
Volume of the bed [L] | |
yi | Molar fraction of component i |
yin | Inlet molar fraction |
yout | Outlet molar fraction |
Greek letters | Meaning |
Number of adsorbent sites occupied by the adsorbate molecule | |
Heat of adsorption for component i [kJ mol−1] | |
Porosity of the fixed bed | |
Porosity of the particle | |
ρbed | Bed density [kg m−3] |
ρp | Particle density [kg m−3] |
ρtrue | True density [kg m−3] |