Experimental study into carbon dioxide solubility and species distribution in aqueous alkanolamine solutions

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Air Pollution XX 515 Experimental study into carbon dioxide solubility and species distribution in aqueous alkanolamine solutions H. Yamada, T. Higashii, F. A. Chowdhury, K. Goto S. Kazama Research Institute of Innovative Technology for the Earth, Japan Abstract We investigated the solubility of CO 2 in aqueous solutions of alkanolamines at 40 C and 120 C over CO 2 partial pressures ranging from a few kpa to 100 kpa to evaluate the potential for CO 2 capture from flue gas. CO 2 capacities were compared between monoethanolamine, N-ethyl ethanolamine and N-isopropyl ethanolamine. Speciation analyses were conducted in the alkanolamine solutions at different CO 2 loadings by accurate quantitative 13 C nuclear magnetic resonance spectroscopy. N-isopropyl ethanolamine showed a large capacity for CO 2 because of the formation of bicarbonate. However, we also found that at a lower CO 2 loading a significant amount of carbamate was present in the aqueous N-isopropyl ethanolamine solutions. Keywords: carbon capture, amine absorbent, CO 2 solubility, vapour-liquid equilibrium, nuclear magnetic resonance. 1 Introduction Carbon capture and storage is of central importance for the reduction of anthropogenic CO 2 emissions in the atmosphere. Amine scrubbing is the most promising and currently applicable technology used in an industrial scale for the capture of CO 2 from a gas stream [1]. To maximise the capture efficiency and to reduce energy costs we previously developed CO 2 capture systems and high performance CO 2 absorbents [2 5]. Recently, we demonstrated that hindered amino alcohols for the promotion of CO 2 capture can be developed by rational molecular design and by the placement of functional groups [4, 5]. For aqueous solutions of primary and secondary amines the CO 2 absorption proceeds by the formation of a carbamate anion or a bicarbonate anion. It is well doi:10.2495/air120451

516 Air Pollution XX known that bicarbonate formation occurs at a lower rate than carbamate formation while bicarbonate formation results in a large CO 2 absorption capacity [3]. However, we found that some moderately hindered amines have combined desirable characteristics such as high rate and large capacity for CO 2 absorption [4, 5]. In this work, we investigated aqueous solutions of alkanolamines by isothermal vapour-liquid equilibrium (VLE) measurements for CO 2 and by 13 C nuclear magnetic resonance (NMR) spectroscopic analyses. The results provide insights into the absorption mechanism and the relationship between the absorption properties and molecular structures of alkanolamines. 2 Experimental 2.1 Alkanolamines Alkanolamines of ca. 99 purity were purchased from various chemical companies and used without further purification. The molecular structures of the alkanolamines investigated in this work are shown in Figure 1. H 2 N OH OH N H N H MEA EAE IPAE OH Figure 1: Molecular structures of the investigated amines. 2.2 Vapour-liquid equilibrium VLE data were measured at 40 C and 120 C over various CO 2 partial pressures ranging from a few kpa to ca. 100 kpa to compare their CO 2 capture potentials. Approximately 700 ml of the 30 wt aqueous amine solutions were fed into an autoclave, which was then purged with N 2. During the experiment, the temperature-controlled solutions were agitated by a mechanical stirrer. The CO 2 /N 2 gas mixture was concentration-controlled using mass flow controllers and the mixture was supplied to the autoclave after flowing through a watersaturator. The outlet gas was monitored by an infrared CO 2 analyser (VA-3001, Horiba) after flowing through a condenser. An equilibrium was obtained when the CO 2 analyser indicated a constant CO 2 concentration ( 0.01 ). To analyse the equilibrium data the temperature and total pressure in the gas phase were measured while the amount of CO 2 in the liquid phase sample drawn from the autoclave was measured by a total organic carbon analyser (TOC-V CSH, Shimadzu) and the maximum coefficient of variation was 1.5.

Air Pollution XX 517 2.3 Nuclear magnetic resonance CO 2 saturated solutions were prepared by flowing the CO 2 gas at a rate of 500 ml/min into 75 g of 30 wt% aqueous alkanolamine solutions at room temperature and atmospheric pressure for 15 min. The CO 2 loading was lowered by mixing the 30 wt% aqueous alkanolamine solution and the CO 2 saturated solution. The prepared sample solutions were analysed with a NMR spectrometer (DRX-500, Bruker) at 30 C. A double-walled sample tube was used with C 6 D 6 as the lock solvent and Si(CH 3 ) 4 as the internal standard to retain the sample concentration. 13 C NMR spectra were recorded at 125.8 MHz. Quantitative spectra were obtained using the inverse-gated decoupling technique with a pulse angle of 90, a delay time of 60 s and 512 scans. 13 C spin-lattice relaxation times were measured by the inversion recovery method. The CO 2 loadings of the sample solutions were also quantified by the TOC analyser. Figure 2: Equilibrium partial pressure of CO 2 in 30 wt aqueous solutions of monoethanolamine. 3 Results and discussion 3.1 CO 2 solubility Figures 2 and 3 show the equilibrium solubility data of CO 2 in 30 wt aqueous solutions of monoethanolamine (MEA), 2-(ethylamino)ethanol (EAE) and 2-(isopropylamino)ethanol (IPAE). The loading ( ) represents the molar ratio of

518 Air Pollution XX loaded CO 2 to the total amine in the liquid phase. The solubility data in 30 wt aqueous MEA solutions were measured at 120 C by Ma mun et al. [6] and at 40 C by Shen and Li. [7], and these are also shown in Figure 2 for comparison. This data agrees well with the data obtained in this work. As shown in Figures 2 and 3, at a typical temperature for CO 2 absorption such as 40 C the aqueous solutions of N-substituted ethanolamines show higher CO 2 solubilities than that for the conventional aqueous MEA solutions in the CO 2 partial pressure range of 6 kpa to 100 kpa. On the other hand, the aqueous MEA solution has higher CO 2 solubility than the aqueous EAE and IPAE solutions at a typical temperature for the CO 2 stripping process of 120 C and at a CO 2 partial pressure of 100 kpa: the CO 2 loadings were 0.4, 0.3 and 0.2 for MEA, EAE and IPAE, respectively. The solubility data from these experiments were determined by curve fitting. A power function satisfactorily fits the data in the studied CO 2 partial pressure range. The fitted curves are also shown in Figures 2 and 3. Figure 3: Equilibrium partial pressure of CO 2 in 30 wt aqueous solutions of 2-(ethylamino)ethanol and 2-(isopropylamino)ethanol. 3.2 Cyclic CO 2 capacity The VLE data enables the calculation of the cyclic CO 2 capacity ( ), i.e., the maximum loading difference between the CO 2 rich solution in the absorber and the CO 2 lean solution in the stripper. Using conditions of 40 C and a 10 kpa CO 2 partial pressure for the absorption process, and 120 C as well as a 100 kpa CO 2 partial pressure for the stripping process we define the cyclic CO 2 capacity as follows: Δα α 40 C,10 kpa α120 C,100 kpa. (1) As shown in Figures 2 and 3, the aqueous IPAE solutions have a larger cyclic CO 2 capacity than MEA and EAE because of the high absorbability of CO 2 under the absorber conditions and the high desorbability of CO 2 under the

Air Pollution XX 519 stripper conditions. The calculated cyclic capacities are 0.14, 0.30 and 0.46 for MEA, EAE and IPAE, respectively, indicating that the substituent adjacent to the amino group drastically affects the CO 2 capacity. 30 wt aqueous solutions of MEA, EAE and IPAE contain 4.9, 3.4 and 2.9 moles of amine per kilogram, respectively. This means that MEA has an advantage because of its low molar weight compared with the CO 2 capacity between the solutions containing the same mass of amines. However, IPAE still has the largest cyclic CO 2 capacity in terms of capacity per mass of absorbent: 31, 44 and 59 grams of CO 2 per kilogram of absorbent were found for MEA, EAE and IPAE, respectively. 3.3 Quantitative 13 C NMR By the inversion recovery method we confirmed that the 13 C spin-lattice relaxation time is the longest for the carbon of carbamate or the carbon of carbonate (ca.10 s) among the various carbons in the CO 2 loaded aqueous alkanolamine solutions. For quantitative 13 C NMR measurements, a delay time allowing the system to return to thermal equilibrium in the standard inversegated decoupling sequence should be at least 5 times longer than the spin-lattice relaxation time [8]. Therefore, the delay time was determined to be 60 s in this work. The quantitative 13 C NMR spectra were confirmed by the TOC results. The deviation of the CO 2 loading between the 13 C NMR and the TOC analysis results was at most 0.01 in this work. 3.4 Species distribution The CO 2 saturated solutions of MEA, EAE and IPAE prepared at room temperature and under atmospheric pressure were analysed by 13 C NMR and the CO 2 loadings were found to be 0.56, 0.72 and 0.90, respectively, as shown in Figures 4 and 5. Figure 4 also shows an interpretation of the peaks and the relative areas of the 13 C NMR spectra for the CO 2 saturated solutions of MEA and EAE. The carbamate, carbonate (CO 2 3 and HCO 3 ) and amine (neutral amine and protonated amine) species were unambiguously identified in the spectra and no other species were detected except for trace impurities. The errors in the peak areas of the spectra were estimated to be at most 3% on the basis of the standard deviations of peak areas from the different carbons of the same amine species. It should be noted that one peak was detected for the carbon of the carbonate (HCO 3 and CO 2 3 ) species in 13 C NMR because of the fast exchange of protons. It is not possible to distinguish between amines and protonated amines from 13 C NMR spectra for this same reason. 3.5 Carbamate yield As shown in Figures 4 and 5, peaks that result from absorbed CO 2 were observed at 161-165 ppm. The yield of carbamate, which is defined as the molar ratio of carbamate to absorbed CO 2 was obtained from those peak areas, e.g., 0.74 was

520 Air Pollution XX Figure 4: 13 C NMR spectra of 30 wt aqueous solutions of (a) monoethanolamine and (b) 2-(ethylamino)ethanol at CO 2 loadings of 0.56 and 0.72, respectively, with peak interpretations and the relative values for the peak areas. obtained at a CO 2 loading of 0.56 and at 30 C in the aqueous MEA solutions. This value is close to previous data by Jakobsen et al. [9]: 0.76 (0.79) at a CO 2 loading of 0.59 and at 40 C (20 C) in 30 wt% aqueous MEA solutions. Böttinger et al. [10] also carried out quantitative speciation of 30 wt% aqueous MEA solutions by online NMR spectroscopy where the carbamate yield was 0.57 at a CO 2 loading of 0.77 and at 40 C. These results show that for aqueous MEA solutions the carbamate products dominate the carbonate and carbamate products even at a relatively high CO 2 loading.

Air Pollution XX 521 Figure 5: 13 C NMR spectra of CO 2 -loaded 30 wt aqueous solutions of 2- (isopropylamino)ethanol at CO 2 loadings of (a) 0.90 and (b) 0.38 with peak interpretations for the carbamate and carbonate species. For secondary alkanolamines, the carbamate yield decreases with an increase in the steric hindrance of the substituted amino group. The carbamate yield was 0.18 at a CO 2 loading of 0.72 for EAE, as shown in Figure 4. Alkanolamines with a more sterically hindered amino group such as IPAE give lower yields of carbamate and higher loadings. The carbamate yield was 0.00 at a CO 2 loading of 0.90 in IPAE, as shown in Figure 5. For the sterically hindered primary amine, 2-amino-2-methyl-1-propanol (AMP), it has been confirmed by previous 13 C NMR studies that CO 2 absorption in aqueous AMP solutions predominantly gives the bicarbonate anion at equilibrium [3, 11]. Ciftja et al. [11] performed speciation on 30 wt% aqueous solutions of AMP with different amounts of CO 2 at 25ºC where the carbamate yield was at most 0.03 in the loading range from 0.12 to 0.62. Even though the carbamate anion is a very minor product, carbamate formation is considered to play an important role in CO 2 absorption by AMP solutions [12]. At a loading of 0.38 in IPAE the carbamate yield was as high as 0.31, as shown Figure 5. This finding indicates that significant carbamate formation occurs for IPAE at a lower CO 2 loading despite its sterically hindered amino group and high capacity. 3.6 Reaction mechanism In aqueous solutions of primary and secondary amines, CO 2 is absorbed by the formation of carbamate or bicarbonate anions 2BH + CO 2 BCOO + BH 2 +, (2)

522 Air Pollution XX BH + CO 2 + H 2 O HCO 3 + BH 2 +. (3) For sterically hindered amines the carbamate is not stable and may be converted into bicarbonate through hydrolysis BCOO + H 2 O HCO 3 + BH. (4) Generally, the reaction shown in eqn. (2) occurs faster than the reaction in eqn. (3). Bicarbonate formation stoichiometrically requires 1 mol of amine per mole of CO 2 and allows for a large CO 2 capacity whereas carbamate formation requires 2 mol of amine per mole of CO 2. Recently, we performed a quantum chemical analysis for CO 2 absorption into aqueous solutions of IPAE and showed that carbamate forms easily via a zwitterion intermediate BH + CO 2 BH + COO. (5) However, the carbamate decomposes by the reverse reaction of eqn. (2) rather than by the reaction shown in eqn. (4). As a final product, bicarbonate forms by the reaction shown in eqn. (3) in a single-step [4]. The experimental results in this work show a large cyclic CO 2 capacity for IPAE because of bicarbonate formation. However, it has also been found that a significant amount of IPAE carbamate is formed in a low CO 2 loading regime. These results support the above-mentioned absorption mechanisms. 4 Summary The equilibrium solubility data of CO 2 into 30 wt% aqueous solutions of monoethanolamine (MEA), 2-(ethylamino)ethanol (EAE) and 2- (isopropylamino)ethanol (IPAE) were determined at 40 C and 120 C over CO 2 partial pressures ranging from a few kpa to 100 kpa. Differences in a CO 2 loading under 10 kpa CO 2 partial pressure at 40 C and in a CO 2 loading under 100 kpa CO 2 partial pressure at 120 C were found to be 0.14, 0.30 and 0.46 mol CO 2 /mol amine for MEA, EAE and IPAE, respectively. By quantitative 13 C nuclear magnetic resonance spectroscopy we showed that carbamate predominantly forms in the CO 2 saturated aqueous MEA solutions whereas it is an undetectable minor product in the CO 2 saturated aqueous IPAE solutions. However, a significant amount of carbamate was found in the aqueous IPAE solutions at a lower CO 2 loading. These findings agree with the reaction mechanism proposed by a quantum chemical analysis and explain the properties of the absorbents. References [1] Rochelle, G.T., Amine scrubbing for CO 2 capture. Science, 325(5948), pp. 1652 1654, 2009.

Air Pollution XX 523 [2] Goto, K., Okabe, H., Shimizu, S., Onoda, M. Fujioka, Y., Evaluation method of novel absorbents for CO 2 capture. Energy Procedia, 1, pp. 1083 1089, 2009. [3] Yamada, H., Shimizu, S., Okabe, H., Matsuzaki, Y., Chowdhury, F.A. Fujioka, Y., Prediction of the basicity of aqueous amine solutions and the species distribution in the amine H 2 O CO 2 system using the COSMO-RS method. Industrial & Engineering Chemistry Research, 49(5), pp. 2449 2455, 2010. [4] Yamada, H., Matsuzaki, Y., Okabe, H., Shimizu, S. Fujioka, Y., Quantum chemical analysis of carbon dioxide absorption into aqueous solutions of moderately hindered amines. Energy Procedia, 4, pp. 133 139, 2011. [5] Chowdhury, F.A., Okabe, H., Yamada, H., Onoda, M. Fujioka, Y., Synthesis and selection of hindered new amine absorbents for CO 2 capture. Energy Procedia, 4, pp. 201 208, 2011. [6] Ma mun, S., Nilsen, R. Svendsen, H.F., Solubility of carbon dioxide in 30 mass monoethanolamine and 50 mass methyldiethanolamine solutions. Journal of Chemical Engineering Data, 50(2), pp. 630 634, 2005. [7] Shen K.P. Li, M.H., Solubility of carbon dioxide in aqueous mixtures of monoethanolamine with methyldiethanolamine. Journal of Chemical Engineering Data, 37(1), pp. 96 100, 1992. [8] Giraudeau, P., Wang, J.L. Baguet, É., Improvement of the inverse-gateddecoupling sequence for a faster quantitative analysis by 13 C NMR. Comptes Rendus Chimie, 9(3), pp. 525 529, 2006. [9] Jakobsen, J.P., Krane, J. Svendsen, H.F., Liquid-phase composition determination in CO 2 H 2 O alkanolamine systems: an NMR study. Industrial & Engineering Chemistry Research, 44(26), pp. 9894 9903, 2005. [10] Böttinger, W., Maiwald, M. Hasse, H., Online NMR spectroscopic study of species distribution in MEA H 2 O CO 2 and DEA H 2 O CO 2. Fluid Phase Equilibria, 263(2), pp. 131 143, 2008. [11] Ciftja, A.F., Hartono, A., da Silva, E.F., Svendsen, H.F., Study on carbamate stability in the AMP/CO 2 /H 2 O system from 13 C-NMR spectroscopy. Energy Procedia, 4, pp. 614 620, 2011. [12] Yamada, H., Matsuzaki, Y., Higashii, T. Kazama, S., Density functional theory study on carbon dioxide absorption into aqueous solutions of 2- amino-2-methyl-1-propanol using a continuum solvation model. Journal of Physical Chemistry A, 115(14), pp. 3079 3086, 2011.