Hayoung Yoona,
Kwangho Parkb,
Kwang-Deog Jung*b and
Sungho Yoon
*a
aDepartment of Chemistry, Chung-Ang University, 84 Heukseok-ro, Dongjak-gu, Seoul, Republic of Korea. E-mail: sunghoyoon@cau.ac.kr
bClean Energy Research Center, Korea Institute of Science and Technology (KIST), 5 Hwarang-ro 14-gil, Seongbuk-gu, Seoul 02792, Republic of Korea. E-mail: jkdcat@kist.re.kr
First published on 3rd January 2025
The C1 chemical species, potassium formate (K(HCO2)), known as a two-electron reducing agent, finds application in the synthesis of multi-carbon compounds, including oxalate, and plays a crucial role not only in the food and pharmaceutical industries but also across various sectors. However, the direct hydrogenation of CO2 to produce K(HCO2) remains a challenge. Addressing this issue, efficient production of K(HCO2) is achieved by integrating CO2 hydrogenation in a trickle-bed reactor using a heterogeneous catalyst with a novel separation method that utilizes potassium ions from biomass ash for formic acid derivative product isolation. Through alkaline-mediated CO2 hydrogenation using N-methylpyrrolidine (NMPI), a concentrated 5 M NMPI solution of formic acid N-methylpyrrolidine complex ([NMPIH][HCO2]) was formed, facilitating the synthesis of K(HCO2) with over 99% purity via reaction with excess K ions contained within Bamboo ash. Notably, 80% of CO2 was converted to formate ions, and NMPI was expected to be effectively recycled as it was completely removed during the evaporation process for K(HCO2) separation. Additionally, this process yielded SiO2 by-product particles with sizes ranging from 10 to 20 nm. This research highlights a novel strategy contributing to sustainable environmental management and resource recycling by effectively utilizing CO2 as a valuable feedstock while concurrently producing valuable chemical compounds from waste materials.
Recently, numerous studies have reported on catalysts and processes for the conversion of CO2 to formic acid, with some technologies pilot-scales of up to 10 kg day−1.16 However, despite these advancements, there are significant limitations to the application of CO2-to-formic acid technology as a climate change mitigation strategy, particularly in terms of societal acceptability.12,17,18 Currently, formic acid is used primarily as a reducing agent in chemical reactions, in leather tanning, and as a preservative in animal feeds,19–22 with the reported global market demand in 2023 being approximately 920000 tons per year.23 This market size inherently limits the potential of CO2-to-formic acid technology to significantly reduce atmospheric CO2, given the vast amount of CO2 that needs to be mitigated globally.
To overcome this limitation, one promising approach is to develop technologies that also produce formate species, which are extensively used in current industrial processes.24–28 This strategy could potentially enhance the overall impact of CO2 conversion technologies by expanding the range of valuable products that can be derived from CO2. Recent research has focused on enhancing the diversity of CO2 conversion products by developing methods for producing formate-based compounds such as metal formates.24–28 Metal formates, depending on the type of metal ion, can be converted into various chemical species including formaldehyde, oxalate, and methyl formate, thus possessing high market potential.5,27–34 Therefore, the study of various methods for producing metal formates is expected to significantly contribute to mitigating global warming by advancing applicable CO2 conversion technologies in society.
A representative example of such research has demonstrated the production of calcium formate using CO2 hydrogenation products and various calcium ion sources.25,26 This study suggested the possibility of generating other metal formates from CO2 hydrogenation products, though research extending beyond calcium ions to other metal formates has not yet been reported. Interestingly, recent advancements have proposed a novel approach using potassium formate (K(HCO2)) to synthesize the C2 compound oxalate, further advancing the production of multi-carbon chemical species such as C3 and C4 compounds.27,28 If K(HCO2) can be efficiently produced from CO2, it holds significant potential as an intermediate for generating oxalate from CO2. However, research in this area remains scant. The currently known methods for producing K(HCO2) involve adding KOH or K2CO3 to formic acid (Fig. 1a).35 This approach, however, entails high production costs of formic acid and issues related to CO2 emissions during the production process of formic acid from CO.36,37 Therefore, to facilitate the production of various useful carbon resources from CO2, there is a critical need for the development of efficient CO2 conversion technologies for producing K(HCO2).
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Fig. 1 K(HCO2) production routes: (a) conventional process and (b) eco-friendly CO2 utilization process. |
The utilization of readily accessible resources for the production of CO2 conversion products is crucial for ensuring cost-effective resource supply and enhancing the practical application of these processes from research to commercialization in society.25,26,38 Among these approaches, the method of producing K(HCO2) from waste-derived potassium oxide contributes significantly to sustainable environmental management and resource circulation. Biomass ash, rich in potassium oxide, can be effectively used in such research. Biomass itself holds substantial potential as an energy source, and consequently, the quantity of resulting biomass ash is expected to increase.39 In this context, employing potassium oxide from biomass ash represents an effective strategy to simultaneously achieve two critical objectives: CO2 conversion and waste valorization.
Building on this background, a method was developed for synthesizing K(HCO2) from formic acid derivatives through CO2 hydrogenation in an amine-based alkaline aqueous solution (eqn (1)), followed by using potassium ions contained in biomass ash to separate the formic acid derivatives (eqn (2)). Using amine as a base, this single-step CO2 hydrogenation process achieved a 72% reduction of CO2, producing a 5 M amine high concentration of [AmineH][HCO2]. This was then reacted with K ions from bamboo ash, resulting in K(HCO2) with a purity exceeding 99% and, additionally, producing silica (SiO2) nanoparticles with particle sizes of 10–20 nm as a by-product. This method benefits from bypassing the complex processes of producing K(HCO2) via formic acid from CO2, allowing for direct production of K(HCO2) from CO2 hydrogenation products (Fig. 1b). This approach offers an innovative method for extracting K ions from various wastes, including biomass ash, contributing to resource circulation and CO2 reduction.
Hydrogenation:
Amine + CO2 + H2 → [AmineH][HCO2] | (1) |
Separation:
[AmineH][HCO2] + KOH → K(HCO2) + Amine + H2O | (2) |
The concentration of the formic acid salt was measured using a Waters Alliance 2695 system that was equipped with a refractive index detector and an Aminex HPX-87H high-performance liquid chromatography (HPLC) column. All the HPLC analysis results were obtained at a flow rate of 0.6 mL min−1 and a column temperature of 50 °C in a 5.00 mM H2SO4 mobile phase. 1H-NMR and 13C-NMR spectra were recorded on 600 MHz 1H (150 MHz 13C) spectrometer (VNS, Varian) using D2O and CDCl3 as solvents. Fourier transform infrared (FT-IR) spectroscopy analysis was conducted using the pellet method and a Nicolet iS10 instrument with a mercury cadmium telluride detector (Thermo Fisher Scientific). X-ray diffraction (XRD) analysis was performed using a New D8-Advance diffractometer (Bruker-AXS), and X-ray fluorescence (XRF) spectroscopy was performed using a ZSX Primus II system (Rigaku). Inductively coupled plasma optical emission spectroscopy (ICP-OES) was applied to the determination of the elements K, Ca, Mg, and Si using an Agilent ICP-OES 720 system (Agilent). Field-emission scanning electron microscopy (FE-SEM) and energy-dispersive X-ray spectroscopy (EDS) were performed at 20.0 kV accelerating voltage using a Sigma 300 instrument (Carl Zeiss). Thermogravimetric analysis (TGA) was performed using SDT Q600 (TA Instruments Ltd), under a N2 atmosphere (flow of 20 mL min−1) from 24 °C to 1000 °C at a heating rate (5 °C min−1).
Following the reaction, liquid product 1 was obtained and analyzed using HPLC and NMR spectroscopy analyses to confirm the concentration of formate and the acid to amine ratio (AAR). The conversion achieved was 72%, the AAR was measured at 0.72, the productivity was 356.7 gform. gcat.−1 day−1, and the turnover frequency (TOF) was 103 h−1.
2[Et3NH][HCO2] + CaO → Ca(HCO2)2 + 2Et3N + H2O | (3) |
In contrast, the solubility of K(HCO2) is considerably higher at 331 g per 100 mL,42 eliminating the need for any dilution. Utilizing higher concentrations of formate adduct for the production of K(HCO2) can thus enhance process efficiency by minimizing the quantity of water required.
Furthermore, recent research has utilized N-methylpyrrolidine (NMPI) as a base for CO2 hydrogenation, producing formic acid N-methylpyrrolidine complex aqueous solution ([xNMPIH][yHCO2], where x and y represent the molar ratios of N-methylpyroolidinium (NMPIH+) and formate (HCO2−) ions, respectively).16 This process achieved a composition of 5.05 M NMPI and 3.64 M HCO2H, representing a reduction in water usage by approximately 37% compared to when 2.77 M Et3N is used to produce 2.03 M HCO2H (Table S5†). Based on these results, it has been decided to use [1.0NMPIH][0.72HCO2] (1) for the production of K(HCO2), leveraging the higher solubility and reduced water requirement of this approach.
NMPI + CO2 + H2 → 0.72[NMPIH][HCO2] + 0.28[NMPIH][HCO3] | (4) |
0.72[NMPIH][HCO2] + 0.28[NMPIH][HCO3] → 0.72[NMPIH][HCO2] + 0.28NMPI + 0.28H2O + 0.28CO2↑ | (5) |
This degassing process was conducted to prepare [1.0NMPIH][1.07HCO2] (2) at 90 °C for 2 h, and the removal of bicarbonate was verified by 13C-NMR spectroscopy analysis. Furthermore, the composition of 2 was analyzed using 1H-NMR spectroscopy and HPLC. 13C-NMR spectra showed that the bicarbonate peak observed at 160.92 ppm in the pre-degassed sample was completely eliminated after degassing (Fig. S2(b)†). Compositional changes before and after degassing were confirmed through 1H-NMR spectroscopy and HPLC analyses. 1H-NMR spectra indicated a shift in the ratio of NMPI to HCO2H from 1:
0.72 before degassing to 1
:
1.07 afterward (Fig. S3†), resulting from partial evaporation of NMPI and H2O. The evaporated NMPI and H2O can be captured and recycled back into the CO2 hydrogenation process, preventing any loss of NMPI. Additionally, HPLC analysis calculated the composition of 2 as 4.96 M NMPI and 5.31 M HCO2H, demonstrating that the amount of HCO2H remained stable through the degassing process without decomposing or evaporating. Consequently, 2 was applied in the production of K(HCO2).
The supplied BC was calcined at 800 °C for 24 h for use in the K(HCO2) production reaction. This temperature was selected based on TGA (Fig. S4†), which indicated no further weight loss beyond 800 °C, confirming complete decomposition. This ensured that the ash was fully processed and suitable for analysis and reaction. 800dBA was then subjected to XRF qualitative analysis to identify its elemental composition (Table 1). The results showed that the main metal elements in 800dBA were K, Si, Ca, and Mg, with relatively higher proportions of K and Si compared to Ca and Mg. These findings align with the previously studied inorganic elemental composition of bamboo ash (Table S6†), where K accounted for nearly 50 wt%, significantly higher than the other metal elements. Subsequent quantitative analysis of these metal elements in 800dBA was performed using ICP-OES (Table S7†). The ICP-OES analysis revealed that K constituted the highest proportion at 63.4 mol%, followed by Si at 14.1 mol%, Ca at 12.4 mol%, and Mg at 10.4 mol%. This confirms the predominant presence of K, further demonstrating its suitability for K(HCO2) production.
Component | K | Si | Ca | P | Mg | S | Al | Fe | Mn | Ba | Zn | Cl | Ti | Na | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Result | wt% | 43.5 | 34.9 | 8.8 | 6.3 | 2.1 | 1.7 | 0.8 | 0.8 | 0.5 | 0.2 | 0.1 | 0.1 | 0.1 | 0.1 |
FE-SEM and EDS analyses were conducted to examine the morphology and corresponding elemental composition trends of BC and 800dBA (Fig. 2 and Table S8†). BC exhibited a mixture of particles with irregular morphologies of varying sizes, which could be broadly classified into two types (Fig. 2a and b). The first type of particle (a) displayed a smooth surface with pore-like structures, while the second type of particle (b) exhibited an irregular, rough texture. In particular, the rough appearance of particle (b) seemed to cover a smooth surface, which appeared similar to that of particle (a). EDS point analysis was performed on three spots per particle, revealing that both types of particles contained a high proportion of C (Fig. 2g Entry 1–6), implying that BC sample did not achieve complete pyrolysis. In addition, spots 1–4 exhibited similar elemental compositions, where K was the most abundant element after C and O, alongside detectable amounts of Si and Cl. The rough surface of the particle (b) revealed higher proportions of Mg and P (Fig. 2h Entry 1–6). This indicates that BC likely contains phases such as KCl, K2SiO3, K–Mg silicates, phosphates, and sulfates.
In the case of 800dBA, it consisted of a mixture of particles with varying sizes and morphologies (Fig. 2c–e). The first type of particle (c) appeared flat but not smooth, while the second type of particle (e) contained a combination of two distinct crystalline forms. Spots 13 and 14 revealed thin, amorphous crystals layered over each other, whereas hexagonal crystals were observed at spots 15 and 16. The third type of particle (d) displayed a surface similar to that of particle (c), with the addition of crystals akin to those observed in particle (e). EDS point analysis of these particles showed a substantial decrease in C content in 800dBA compared to BC, accompanied by a significant increase in elements such as Si and K (Fig. 2g Entry 7–16). Furthermore, when excluding C and O, Si and K were found to be the dominant elements, with the proportion of Ca and P varying depending on the crystalline form (Fig. 2h Entry 7–16). These findings suggest that 800dBA contains K–Mg/Ca silicates, phosphates, and sulfates.
To investigate the mineral phase transformation behavior of BC after calcination at 800 °C, XRD analysis was performed (Fig. S5†). Prior to calcination, KCl and SiO2 were prominently identified, along with the presence of K2SO4 and KHCO3. However, following calcination, the peaks for KCl and KHCO3 disappeared, suggesting that KCl evaporated into the gas phase, and KHCO3 decomposed thermally, converting into other K-containing compounds such as K2SO4.47 Additionally, the emergence of KCaPO4 and Ca15(PO4)2(SiO4)6 peaks after calcination indicates that under the condition of 800 °C, sintering occurred between K and Ca with Si and P. It can also be inferred that K and Mg, which are prone to sintering with Si and P, likely contributed to the formation of other compounds such as K–Mg silicates, phosphates, and sulfates.47
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Fig. 3 Schematics of the process for producing metal formate using various metal oxides from CO2 hydrogenation adduct made under N-methylpyrrolidine (NMPI)-based basic aqueous solution. |
Two key aspects were verified in synthesizing metal formates using this method. First, the complete separation of NMPI and H2O during the evaporation process of the filtrate was analyzed, followed by measuring the yield of the generated metal formates.
Since NMPI can be recycled to the CO2 hydrogenation process, completely separating it from the filtrate is crucial. The temperature at which NMPI and H2O evaporate from the filtrate was determined, and the separated liquids at each temperature were identified using 1H-NMR spectroscopy analysis. The known boiling point of NMPI is 80–81 °C,48 and for H2O, it is 100 °C. Therefore, evaporation was conducted at 90 °C to first separate NMPI. 1H-NMR spectroscopy analysis of the liquid separated at this temperature confirmed the presence of only NMPI (Fig. S6(a)†). It was found that only about 1.04% of the initially added NMPI remained in the remaining filtrate (Fig. S6(b)†). Subsequently, evaporation of H2O was performed at 90 °C, 10−3 mbar, and the remaining solid was analyzed using 1H-NMR spectroscopy, confirming that only K(HCO2) remained, with no NMPI present (Fig. S6(c)†).
To compare the reactivity of converting K, Si, Ca, and Mg oxides, each a major component of 800dBA, into their respective metal formates, equivalent amount of these oxides was added to 2 and stirred at 30 °C for 5 min. Subsequently, the yield of the produced metal formates was examined. Specifically, for K, KOH was used as a reactant instead of K2O, as potassium oxide is highly unstable under normal conditions and readily converts to KOH in the presence of moisture. The concentration of 2 was adjusted considering the solubility at 20 °C of the metal formates (Table 2). For K(HCO2), which has a solubility of 331 g/100 mL H2O, dilution was unnecessary, hence undiluted 2 was used. For Ca and Mg, considering the solubilities of 16.6 g/100 mL H2O for Ca(HCO2)2 and 14.4 g/100 mL H2O for Mg(HCO2)2,49 dilution processes were conducted. The resulting compositions for the diluted 2 used in the Ca(HCO2)2 and Mg(HCO2)2 experiments were set at 1.77 M NMPI and 1.90 M HCO2H, and 1.76 M NMPI and 1.88 M HCO2H, respectively. Si(HCO2)4 was used at the same concentration as the Ca experiment due to a lack of solubility information.
Reaction equationb | NMPI [M] | HCO2H [M] | Metal formate yield [%] | |
---|---|---|---|---|
a The reactions were conducted at 30 °C for 5 min. The yields were calculated as an average from the results of two experiments.b [NMPIH][HCO2] is 2. | ||||
K | 2[NMPIH][HCO2] + K2O → 2K(HCO2) +2NMPI + H2O | 4.96 | 5.31 | 99.0 |
Ca | 2[NMPIH][HCO2] + CaO → Ca(HCO2)2 + 2NMPI + H2O | 1.77 | 1.90 | 65.7 |
Mg | 2[NMPIH][HCO2] + MgO → Mg(HCO2)2 + 2NMPI + H2O | 1.76 | 1.88 | 20.4 |
Si | 4[NMPIH][HCO2] + SiO2 → Si(HCO2)4 + 4NMPI + 2H2O | 1.77 | 1.90 | N/A |
The yields of each metal formate were as follows (Table 2). Given the hygroscopic properties of K(HCO2), its weight was measured inside a glove box to exclude the effects of moisture from the air. As a result, K(HCO2) was produced with a high yield of 99.0%, whereas Ca(HCO2)2, Mg(HCO2)2, and Si(HCO2)4 were generated with yields of 65.8%, 20.4%, and 0.1%, respectively. While all four metals are thermodynamically capable of converting to metal formate salts, the incomplete conversion of Ca, Mg, and Si can be inferred from factors such as kinetic limitations and the differences in the solubility of the resulting formate salts. These variations in yield can be attributed primarily to the difference in reactivity of the metal oxides with the formate ion, where basic oxides are more reactive than acidic oxides. Notably, alkali metal oxides like K2O exhibit higher reactivity compared to alkaline earth metal oxides such as CaO and MgO. Within the group of alkaline earth metals, CaO, owing to its higher solubility in hydroxide form, reacts more readily than MgO, which contributes to its relatively higher yield in the formate form. These intrinsic differences in chemical behavior among the metal oxides are crucial for the selective conversion of K compounds to K(HCO2) from bamboo ash. However, depending on reaction conditions, Ca and Mg may also be converted into metal formates. In particular, when Ca, which has higher reactivity after K, coexists with K, it was observed that the proportion of Ca converted to metal formate increases as the reaction time is extended and the temperature rises (details are provided in ESI 2†). Therefore, a pretreatment process to remove Ca and Mg from bamboo ash is essential to maintain the high purity of K(HCO2).
Optimization of the K extraction process from 800dBA was conducted by stirring at 100 °C over time. 1 g of 800dBA was added to 10 mL of water, and the extraction was set from 12 h up to 7 days. ICP-OES analysis (Fig. S7 and Table S9†) showed an increasing trend in K extraction with longer stirring times at 100 °C. However, after 5 days, the rate of increase in K extraction notably decreased, suggesting this point as the optimal extraction time. Interestingly, it was found that SiO2, generally insoluble in water, was also extracted. This indicates that the solution became sufficiently alkaline to dissolve SiO2 due to the presence of KOH extracted from bamboo ash. Additionally, Ca and Mg were found to be minimally extracted (Table S9†), leading to a solution containing 64 mol% K and 36 mol% Si obtained after stirring for 5 days at 100 °C. Furthermore, EDS analysis was conducted to identify the elements present in the solid residue after Si and K extraction (Fig. 2f–h Entry 17, 18). The results revealed a significant reduction in the Si and K content, while a substantial amount of C remained despite the sample being calcined at 800 °C.
The solution from which K was extracted was then added to 2 to produce K(HCO2) using the following procedure: the mixture was stirred at 30 °C for 5 min, then the reaction mixture was evaporated at 90 °C under vacuum to remove NMPI and H2O. The solid obtained from evaporating the filtrate was redissolved in water, insoluble solids were filtered out, and the remaining filtrate was evaporated at 80 °C under vacuum to yield a white solid. Redissolving the evaporated solid in water was aimed at precipitating and separating SiO2, which does not dissolve in K(HCO2) solution, thus efficiently producing high-purity K(HCO2).
ICP-OES analysis of the precipitated solid from the redissolved solution confirmed that the material was 95.7% Si, identifying it as SiO2 (Table S10†). FE-SEM analysis confirmed that the particles ranged in size from 10–20 nm (Fig. 5a–d). Further XRD analysis verified the material as amorphous SiO2 (Fig. 5e). Finally, XRD analysis of the solid product obtained through evaporation confirmed that it had the same XRD pattern as commercial K(HCO2) (Fig. 5f). In addition, HPLC analysis showed that 99.8% of the initially added formate was contained within the solid (Table S11†), suggesting nearly complete conversion of the extracted K compound to K(HCO2). Additional ICP-OES analysis of the produced K(HCO2) confirmed a purity of 99.0% (Table S12†). These results demonstrate the successful production of K(HCO2) from a CO2 hydrogenation adduct using K-rich bamboo ash.
The process described above has successfully demonstrated the potential to produce K(HCO2) using formic acid derivative generated from CO2 hydrogenation and bamboo ash. This innovative approach validates the feasibility of synthesizing a valuable chemical from CO2 and sustainably sourced biomass ash, highlighting an effective utilization of CO2 and biomass waste.
Utilizing NMPI as a base, the research achieved the hydrogenation of CO2 to produce a high concentration of the formic acid derivative [NMPIH][HCO2]. This compound subsequently reacted with potassium extracted from bamboo ash, yielding K(HCO2) with an exceptional purity of 99%. The method optimized the extraction of potassium from bamboo ash and showed that a prolonged extraction period at 100 °C efficiently obtains soluble potassium compounds, suitable for the synthesis of high-purity K(HCO2). Importantly, this process enabled the conversion of 80% of CO2 into K(HCO2) in a single cycle.
This findings provide a viable pathway for the production of valuable chemical compounds by effectively using greenhouse gases and biomass waste, highlighting the dual benefits of resource recovery and CO2 conversion. The approach is adaptable to various types of biomass and can be extended to synthesize different metal formates, providing a versatile platform for industrial applications. Furthermore, the successful production of K(HCO2) from CO2 paves the way for developing processes to create other multi-carbon chemicals, such as oxalic acid, further expanding the scope of sustainable chemical production methods.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4ra07360f |
This journal is © The Royal Society of Chemistry 2025 |