1. Introduction
The escalating global demand for clean and sustainable energy has catalyzed extensive research into alternative energy sources and sophisticated energy-conversion technologies. The efficient utilization of carbon-neutral fuels and carbon capture have both become important trends in the field of energy. Biomass, recognized as a renewable and carbon-neutral resource, has come to the fore as a promising alternative fuel [
1,
2].
Various methods exist for biomass utilization, among which gasification stands out as a compelling thermochemical conversion technique. This technology holds significant potential for the production of syngas, heat, renewable power, hydrogen, and chemicals [
3,
4,
5], as it offers the potential to overcome the fluctuations in quality and calorific value of feedstocks. However, traditional biomass gasification faces challenges such as low hydrogen yield, tar formation, and carbon dioxide emissions [
6]. Additionally, the syngas is always diluted by nitrogen. To address these issues, the integration of biomass steam gasification with calcium looping processes (CaLP) has attracted attention due to its potential to enhance hydrogen production and enable efficient carbon dioxide capture, forming sorption-enhanced gasification (SEG) [
7,
8,
9,
10]. The hydrogen concentration in syngas from SEG is usually higher than 70% [
7]. In SEG, the CO
2 capture capacity as well as the stability of the bed material have a huge influence on the performance of the SEG process. Previously, different CO
2 sorbents were employed to investigate the gasification performance, such as the CaO, MgO, and Li
4SiO
4. It was found that SEG with a CaO sorbent can produce syngas with the highest hydrogen concentration [
11]. Consequently, CaO-based sorbents have been predominantly utilized as the bed material in the SEG process, primarily due to their superior CO
2 capture capacity and economic viability. This process is shown in
Figure 1a. Both the feedstock and steam are fed into the gasifier while the CO
2 sorbent (typically CaO) circulates into it simultaneously. During the biomass steam gasification process, CaO reacts with CO
2 to shift the equilibrium of the reactions to improve the hydrogen yield. The carbonation product, CaCO
3, is then calcined in a calciner for CaO regeneration.
Different sorbents of limestones are employed in a lab-scale dual interconnected fluidized bed (DIFB) reactor for biomass SEG (BSEG) [
12]. In an experimental demonstration using a 30 kW
th bubbling fluidized bed reactor, the SEG was tested with municipal solid waste as feedstock. The results reveal that the SEG exhibited a commendable performance in preventing tar formation, maintaining a content of as low as 7 g/Nm
3 [
13]. In the same pilot plant, the SEG of sewage sludge was compared with steam–oxygen gasification, showing a high H
2 content of 70–73% [
14]. Adjusting the steam-to-carbon ratio and the utilization of a high-sorption-capacity CO
2 sorbent are proven to be effective strategies for modifying the H/C ratio in syngas [
15]. Mbeugang et al. conducted an experimental investigation into the SEG performance of cellulose within a fixed-bed reactor. Their findings suggest that the role of CaO as either a CO
2 absorbent or a catalyst is intrinsically linked to the gasification temperature [
16]. In a bubbling fluidized reactor, the BSEG of sawdust was experimentally studied by Han et al. [
17]. The highest concentration of hydrogen reached 62% and the optimal conditions were found at CaO/C = 1, H
2O/C = 2.18, and T = 740 °C.
In addition to experimental investigation, simulation provides a useful tool for system evaluation and optimization [
18,
19]. Pitkäoja et al. proposed a strategy for H
2O staging to tailor the gas composition of syngas derived from BSEG. Their research indicated that employing H
2O staging and cooling in a fluidized bed gasifier significantly boosted the carbonation of limestone and water–gas shift reactions [
20]. A process simulation model for the SEG of corn stalk was established, in which the steam gasification and CO
2 sorption were separated in two stages to enhance the H
2 yield [
21]. Although this increased the hydrogen yield, the reaction system was more complex. A modified thermodynamic equilibrium model was established for BSEG, which had high accuracy compared with the experimental results. Any increase in temperature, CaO/C, and steam/biomass helped to increase the H
2 concentration in the syngas [
22]. Santos et al. evaluated the techno-economic feasibility of the SEG, demonstrating a higher H
2 production efficiency when using SEG compared to traditional steam gasification [
23]. In a techno-economic assessment by Cormos, green hydrogen generation from BSEG obtained good results, with high efficiency, a low energy cost, few economic penalties, and negative CO
2 emissions [
24]. As the SEG showed a favorable performance for hydrogen generation and carbon capture, it was integrated with other systems, such as thermal energy storage [
25].
Furthermore, the conversion of CH
4, another greenhouse gas, has attracted much attention. The dry reforming of methane (DRM) utilizes the CO
2, converting it into CO and H
2, and thereby reducing the greenhouse gases into fuels [
26,
27]. While CO
2 capture using CaO can form CaCO
3, a method of calcium looping coupled with DRM has already been proposed and widely studied in the field of post-combustion CO
2 capture [
26,
28,
29,
30,
31]. Zhang et al. developed an integrated process of CaLP and in situ DRM using Fischer–Tropsch, which reduces the heat energy demand, with a drop of 28.08% [
32]. This demonstrates the advances of integrating process CaLP with DRM.
It was shown that the BSEG is beneficial in generating high-quality syngas with adjustable gas compositions while CaCO
3 is formed. For the regeneration of CaO, this work proposes coupling it with DRM, instead of the traditional calcination. The principle of the proposed CaLP, integrating BSEG and CaCO
3-based methane reforming (CaMR), is shown in
Figure 1b. In contrast to conventional CaLP, which relies on energy-intensive high-temperature calcination for CaO regeneration, this study proposes an innovative integration of BSEG with CaMR. The novelty lies in utilizing CaCO
3 (generated during BSEG) as a feedstock for methane reforming, thereby eliminating the need for calcination while enabling in situ CO
2 utilization. This dual-function approach simultaneously regenerates CaO for CO
2 capture and converts methane into syngas, enhancing process efficiency and reducing the carbon footprint. Prior studies primarily focused on standalone BSEG or methane reforming; this work bridges the two processes, establishing a synergistic pathway for sustainable energy production. The integration of BSEG and CaMR introduces a closed-loop carbon-utilization strategy.
The global demand for rice is projected to increase by over 1.2% annually, in response to the escalating food requirements caused by worldwide population growth and economic development [
33]. Typically, the processing of one ton of rice results in the generation of approximately 240 kg of husks [
34]. Consequently, the production of rice husks is a significant global phenomenon. Its valorization aligns with the principles of circular economy principles. Thus, rice husk was chosen as the feedstock in this work. To evaluate the performance of the proposed process, a thermodynamic process model was established based on the Gibbs free energy minimization to analyze the effects of different operating parameters on product distribution in both the gasifier and the reformer. The results demonstrate the feasibility of this CaLP and offer a practical concept for the conversion of methane.
2. Model of the Calcium Looping Process
Rice husk is a globally abundant agricultural residue, particularly in rice-producing regions. Utilizing it aligns with the circular economy principles as it valorizes waste. Due to its abundance, low cost, and carbon neutrality, it has been used as an alternative fuel in many fields. Therefore, rice husk was used as the feedstock for the BSEG. The proximate and ultimate analyses of the rice husk were derived from the literature and are presented in
Table 1 [
35].
In this work, a thermodynamic analysis model is established to investigate the coupling cycle of BSEG and CaMR. As has been mentioned, CaO can play multiple roles in the biomass gasification process, namely as a catalyst for tar-cracking and as a CO
2 sorbent. It was used as the bed material for BSEG. The CaLP process integrating BSEG and CaMR is principally shown in
Figure 2, and consists of a gasifier, reformer, and other components.
When the rice husk (RH) is fed into the gasifier, it goes through a fast pyrolysis step and the products are then gasified with the addition of the gasification agent. During the pyrolysis period, the volatiles are evaporated from the solid phase and some of them form tar. The reaction can be described as follows:
Usually, the tar undergoes a second thermal decomposition period with the catalyst. As the CaO serves as the catalyst for tar-cracking, while the tar can be converted to syngas in the steam gasification period, the tar is regarded as having been totally converted into light hydrocarbons in this work.
The pyrolysis products then react with the gasification agent steam. The gasification period relates to many reactions and is quite complex. The gasification period should consist of the following reactions:
Additionally, the light hydrocarbons (e.g., C
2H
4 and C
2H
6) can also react with steam:
When the CaO is introduced into the gasifier, it can react with CO
2 and weaken the CO
2 partial pressure to shift the equilibria. The CaO carbonation is given as follows:
By shifting the equilibria, this reaction in gasifier is beneficial to enhance the purity of the H2 in syngas and lowers the operating temperatures for RH gasification.
After BSEG, the solid phase is separated from the gaseous products in two separators. The CaCO3 and unconverted CaO then flow into the reformer. Meanwhile, a stream of CH4 is introduced into the reformer for the reforming reactions. In the reformer, the CaCO3 can be decomposed into CaO and CO2. The CO2 can react with CH4 for the dry reforming process. In addition, CaCO3 may react with CH4 directly for the in situ reforming. During this process, CaO is regenerated. After separation, the gaseous CaMR products are separated from the CaO. Then, the regenerated CaO is circulated into the gasifier for a whole CaLP integrating BSEG and CaMR.
4. Performance of CaLP Integrating BSEG with CaMR
4.1. Effects of the Gasification Temperature
When the gasification temperature increased from 600 °C to 700 °C, the other parameters remained constant with those under the fundamental conditions. The products at the outlet of the gasifier are shown in
Figure 3.
It is shown that when the gasification temperature increased from 600 °C to 700 °C, the flowrates of CO and CO
2 exhibited an increasing trend. Specifically, the CO at the outlet of the gasifier increased from 0.653 kmol/h at 600 °C to 11.699 kmol/h at 700 °C, while the CO
2 increased from 0.220 kmol/h to 3.440 kmol/h over the same temperature range. This indicates enhanced carbon monoxide and carbon dioxide production at higher temperatures. The increase in CO and CO
2 can be attributed to the endothermic nature of gasification reactions, such as the Boudouard reaction and char steam gasification, which are enhanced at elevated temperatures [
36,
37]. Additionally, the calcium oxide serves as a CO
2 sorbent. When the temperature increases, the carbonation reaction of CaO is weakened, which leads to an increased generation of CO
2. A higher CO
2 content can promote the char CO
2 gasification and CH
4 reforming reactions in the reaction system. Meanwhile, the H
2 in syngas showed a gradual increase, from 43.999 kmol/h at 600 °C to 48.536 kmol/h at 700 °C, suggesting a relatively stable but slightly improved hydrogen yield. This increase is likely due to the enhanced steam gasification and water–gas shift reactions that occur at higher temperatures, which are facilitated by the presence of CaO. The molar ratio of H
2/CO in syngas decreased from 67.38 to 4.15. The sorption of CO
2 by CaO shifts the equilibrium of these reactions toward H
2 production, contributing to the increase in hydrogen generation. However, from the perspective of the volume concentration, the H
2 concentration in the dry-basis syngas decreased from 86.15% to 73.56% as the temperature increased. However, the CH
4 flowrate declined from 6.108 kmol/h to 2.212 kmol/h when the temperature increased from 600 °C to 700 °C. This decrease can be explained by the endothermic methane reforming reactions, which become more dominant at higher temperatures, leading to the decomposition of methane into CO and H
2. This is in close alignment with the reforming property of CH
4 [
38]. Additionally, the CaO may react with the CO
2 during the BSEG process, suppressing CH
4 formation. These trends highlight the temperature-dependent behavior of the BSEG process, with higher temperatures favoring the production of CO and H
2. The role of CaO as a CO
2 sorbent can enhance the gasification process and dramatically improve the overall hydrogen yield by shifting the reaction equilibria.
As for the solid-phase products, the CaO at the gasifier outlet increased steadily, from 7.027 kmol/h at 600 °C to 17.397 kmol/h at 700 °C, while the CaCO3 decreased from 26.673 kmol/h to 16.303 kmol/h during the BSEG process. The carbonation reaction between CaO and CO2 is exothermic and increasing the temperature shifts the equilibrium toward the reactants, reducing the formation of CaCO3. During this process, the CaO conversion correspondingly decreased from 79.15% to 48.38%. This decrease in CaO conversion at higher temperatures aligns with the increase in CO2 flowrates in the gasification products. As CaO captures less CO2, more CO2 is released into the gas stream and shifts the equilibrium of the gasification reactions toward CO formation. Though high temperatures are beneficial to gasification, they weaken the sorption reaction between CaO and CO2, which negatively impacts the CO2 capture and the generation of hydrogen-rich syngas.
The effects of the gasification temperature on the CaMR products are shown in
Figure 4.
When the gasification temperatures changed, the CaCO
3 flowing into the downstream reformer varied from 26.673 kmol/h to 16.303 kmol/h and showed the ability to react with methane for reforming. When the gasification temperature increased from 600 °C to 700 °C, the flowrate of CO decreased from 51.103 kmol/h to 32.361 kmol/h, while H
2 decreased from 49.724 kmol/h to 32.222 kmol/h. This indicates that a higher CaCO
3 flowrate can increase CO and H
2 production in the reforming process. During this process, the CO
2 flowrate decreased from 0.777 kmol/h to 0.084 kmol/h as the gasification temperature increased. Similarly, the H
2O flow rate decreased from 0.690 kmol/h to 0.076 kmol/h. This suggests that a higher CaCO
3 flowrate results in more CO
2 and H
2O being produced from the CaCO
3 decomposition and/or the CH
4 reforming. Under the simulated conditions, the model predicts negligible carbon formation due to the suppression of methane cracking and the Boudouard reaction. Additionally, as seen in the calculation results, due to some side reactions, H
2O is produced. The absence of steam in the methane reforming system is beneficial to avoid the decomposition of the coke. However, the CH
4 flowrate at the reformer outlet increased from 4.792 kmol/h to 13.842 kmol/h, corresponding to a decrease in CH4 conversion in CaMR from 84.03% to 53.86%, as illustrated in
Figure 4b.
During the CaMR process, the CaCO3 may decompose at high temperatures to form CaO and CO2. The produced CO2 can then participate in the dry reforming of methane, which increases the production of CO and H2. Thus, the CO and H2 flowrate are positively related to the CaCO3 flowing into the reformer. As the H2O is generated, there must be some side reactions taking place in the reformer. It is clear that low flowrates of C2H4 and C2H6 are also produced in the reformer due to the side reactions, varying in from 0.390 mol/h to 5.691 mol/h and from 0.153 mol/h to 1.967 mol/h, respectively.
4.2. Effects of the Steam Flowrate into Gasifier
In the gasifier, the steam is an important gasification agent for the conversion of the rice husk. As has been mentioned in the previous section, the steam is involved in several relevant reactions in the BSEG process. When the equivalence steam-to-carbon ratio in the gasifier
αG(H2O/C) varies from 0.8 to 1.5, the products of BSEG are shown in
Figure 5.
As the equivalence ratio αG(H2O/C) increased from 0.8 to 1.5, the flowrates of CO and CH4 decreased at the outlet of the gasifier. In these cases, the CO flowrate dropped from 3.736 kmol/h to 2.197 kmol/h while that of CH4 declined from 7.011 kmol/h to 1.752 kmol/h. In contrast, the flowrate of H2 dramatically increased from 37.305 kmol/h to 59.879 kmol/h, which correspond to the increase in H2 concentration from 76.29% to 92.02% (in dry basis). Meanwhile, the CO2 flowrate slightly increased from 0.753 kmol/h to 1.151 kmol/h. These trends indicate that an increase in steam availability suppresses CO and CH4 formation while significantly promoting H2 production. Additionally, the gradual increase in CO2 and the sharp rise in H2 suggest a shift in the dominant reaction pathways as the αG(H2O/C) increases. These phenomena can be explained by the interplay of several key gasification reactions, which are influenced by the equivalence ratio αG(H2O/C) and the presence of CaO. At a lower αG(H2O/C), the primary reactions include the water–gas reaction and methane reforming reactions (dry reforming and/or steam reforming), which produce a large amount of H2. These reactions are further enhanced by the presence of CaO, which captures CO2 through the carbonation reaction, shifting the equilibrium of the water–gas shift and steam reforming reactions toward H2 production. The decrease in CH4 flowrate is a direct result of this enhanced reforming process. On the other hand, excess steam drives the water–gas shift reaction, converting CO into CO2 and further increasing H2 production. This explains the decline in CO and the rise in CO2 and H2 at a higher αG(H2O/C). The steam in the gasifier has the dual roles of promoting both H2 production and CO2 generation, as well as showing the limitations of CaO in fully mitigating CO2 release under high-steam conditions. These insights highlight the need to optimize this ratio to maximize H2 production and minimize undesirable byproducts in the BSEG process.
When the αG(H2O/C) increased from 0.8 to 1.5, the flowrate of CaO at the gasifier outlet gradually decreased from 11.547 kmol/h to 5.146 kmol/h, while that of CaCO3 increased from 22.153 kmol/h to 28.554 kmol/h. This indicates that CaO is continuously consumed and converted into CaCO3 during the BSEG process when more steam is introduced into the gasifier. Correspondingly, the CaO conversion rate increased from 65.74% to 84.73%. The presence of more steam in the gasifier can significantly affect CaO conversion via enhancing the reactions through CO2 generation.
The effects of the equivalence ratio
αG(H2O/C) on the CaMR products are shown in
Figure 6.
When the equivalence ratio αG(H2O/C) varied from 0.8 to 1.5, different CaCO3 flowrates were introduced into the reformer. The flowrates of CO, CO2, H2, and H2O at the reformer outlet showed a consistent upward trend. Specifically, the CO flowrate increased from 43.435 kmol/h to 53.802 kmol/h and the H2 flowrate increased from 42.898 kmol/h to 51.785 kmol/h. The flowrates of CO2 and H2O have approximately the same variation trends. Specifically, when the αG(H2O/C) increased from 0.8 to 1.5, the CO2 flowrate rises from 0.300 kmol/h to 1.149 kmol/h, and H2O increased from 0.271 kmol/h to 1.009 kmol/h. However, the CH4 flowrate decreased significantly from 8.414 kmol/h to 3.603 kmol/h, indicating higher CH4 consumption at a higher αG(H2O/C). In the CaMR, CaCO3 may decompose at high temperatures to produce CaO and CO2. The CO2 participates released during the dry reforming of methane drive the production of CO and H2. As the increase in αG(H2O/C) results in an increase in the CaCO3 flowrate into the reformer, more CO2 is available for the dry reforming reaction, leading to higher CO and H2 production and greater CH4 consumption. Under these conditions, no steam is introduced into the reformer; however, steam is generated at the outlet. The reverse water–gas shift reaction may also contribute to the observed trends, as it further converts CO2 and H2 into CO and H2O, particularly at higher CaCO3 flowrates, due to the higher partial pressure of CO2 in the reaction system. This can be demonstrated by the phenomenon that the increasing rate of CO is higher than that of H2 at a higher αG(H2O/C). As a comprehensive result, the CH4 conversion in the reformer also increased in line with the αG(H2O/C). When the αG(H2O/C) increased from 0.8 to 1.5, the CH4 conversion increased from 71.95% to 87.99%.
4.3. Effects of the Reforming Temperature
Under fundamental conditions, the CaO and CaCO
3 flowrates at the gasifier outlet were approximately 9.204 kmol/h and 24.496 kmol/h, respectively. They separated from syngas and flowed into the gasifier downstream. When the temperature of the reformer changed from 700 °C to 900 °C, the CaMR products obtained were as shown in
Figure 7.
The results illustrate the effects of reforming temperature variations on the product distribution in the CaMR process. As the temperature increased from 700 °C to 900 °C, the flowrate of CO increased from 40.68 kmol/h at 700 °C to 48.82 kmol/h at 900 °C. This increase is consistent with the endothermic nature of the reforming reactions, which favor higher temperatures. As another product of the reforming reaction, the flowrate of H2 increased from 37.05 kmol/h at 700 °C to 48.70 kmol/h at 900 °C. This increase is consistent with the enhanced reforming reactions at higher temperatures, as mentioned previously. The flowrate of CO2 decreased from 3.25 kmol/h at 700 °C to 0.052 kmol/h at 900 °C. Additionally, the decomposition of CaCO3 releases CO2, but this is rapidly consumed in the reforming process. The flowrate of CH4 decreased from 10.57 kmol/h at 700 °C to 5.61 kmol/h at 900 °C, indicating an increase in CH4 conversion at higher temperatures. This reduction is due to the consumption of CO2 and CH4 in the reforming reactions, particularly the dry reforming of CH4, which becomes more favorable at higher temperatures. The generation of H2O should be caused by side reactions such as the reverse water–gas shift reaction. Its flowrate decreased from 1.81 kmol/h at 700 °C to 0.066 kmol/h at 900 °C. This reduction is due to the consumption of H2O in the steam reforming reaction and the water–gas shift reaction. The increase in CO and H2 production, along with the decrease in CH4, CO2, and H2O, indicates that the reforming reactions favor higher temperatures, leading to more CH4 being converted into syngas in CaMR. Interestingly, the side reactions can produce C2H4 and C2H6, as mentioned in the previous section. However, they show different variation trends. The flowrate of C2H4 increased from 0.244 mol/h to 4.312 mol/h with the increase in reforming temperature. The flowrate of C2H6 first decreased from 0.427 mol/h at 700 °C to 0.293 mol/h at 780 °C, then increased to 0.435 mol/h at 900 °C. Overall, the CH4 conversion in CaMR increased from 64.78% to 81.29% as the temperature increased from 700 °C to 900 °C.
4.4. Effects of the Steam Flowrate into Reformer
It has been demonstrated that some side reactions in the reformer can produce H
2O. In reality, the addition of H
2O in the CH
4 reforming system is beneficial to avoid carbon deposition, changing it to a bio-reforming process. Therefore, a stream of steam was added to the reformer to investigate the effects of the steam flowrate on the CaMR process. The CaMR products obtained whenthe equivalence ratio
αR(H2O/C) increased from 0 to 0.5 are shown in
Figure 8.
As illustrated in
Figure 8, the flowrate of CO initially increased from 47.57 kmol/h at
αR(H2O/C) = 0 to a maximum of 50.23 kmol/h at
αR(H2O/C) = 0.2, after which it gradually decreased to 48.38 kmol/h when the
αR(H2O/C) reached 0.5. This trend is caused by the competing effects of steam reforming and the water–gas shift reaction. At low steam flowrates, steam reforming dominates, leading to an increase in CO production. However, as steam flow increases further, the water–gas shift reaction becomes more significant, consuming CO and producing CO
2. The steam reforming reaction produces H
2 as a primary product while the water–gas shift reaction also contributes to H
2 production. As they are enhanced, hydrogen generation is improved. It is shown that the flowrate of H
2 increased substantially from 46.69 kmol/h to 68.38 kmol/h when the
αR(H2O/C) rises from 0 to 0.5. The flowrate of CO
2 increased steadily from 0.49 kmol/h at
αR(H2O/C) = 0 to 5.31 kmol/h at
αR(H2O/C) = 0.5. This increase is due to the water–gas shift reaction, which converts CO and H
2O into CO
2 and H
2. It may also be affected by the competing reactions of steam reforming and CO
2 reforming. When the steam flowrate increases, CO
2 reforming should be weakened due to the increase in the partial pressure of steam. When the
αR(H2O/C) increased from 0 to 0.5, the flowrate of H
2O at the outlet increases from 0.44 kmol/h to 6.85 kmol/h. However, the rate of the H
2O increase in the outlet is lower than the rate of the increase in inlet steam, indicating that more H
2O is consumed during the reactions. This is consistent with the increased activity observed in both steam reforming and the water–gas shift reaction at higher steam flowrates. Correspondingly, the flowrate of CH
4 decreased from 6.43 kmol/h to 0.81 kmol/h as
αR(H2O/C) increased from 0 to 0.5, indicating improved CH
4 conversion with higher steam flowrates. This is expected because steam reforming is enhanced with an increase in steam availability, leading to the greater consumption of CH
4. In these cases, the generation of C
2H
4 and C
2H
6 is very low compared with that observed previously. As the methane reforming is enhanced, the CH
4 conversion increases from 78.56% to 97.30% in line with the increase in
αR(H2O/C).
The proposed integrated calcium looping process directly contributes to green hydrogen production by coupling biomass gasification with methane reforming. The integration of BSEG and CaMR eliminates energy-intensive calcination, enabling in situ CO2 utilization and closed-loop carbon management. The SEG has a comparable economic feasibility with that of conventional steam gasification. If the cost of carbon capture is considered, SEG has significant advantages. While the CaMR is coupled, it reduces the CO2 cost of methane reforming. For a detailed analysis of the techno-economic feasibility, further systemic work should be conducted.