Veluturla, Singh, and Fatima: A comprehensive review of carbon dioxide sequestration: Exploring diverse methods for effective post combustion CO2 capture, transport, and storage
Review
Environmental Engineering Research 2025; 30(1): 230452.
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Abstract
Carbon dioxide (CO2) is a prominent anthropogenic greenhouse gas known for its detrimental impact on climate change and contribution to global warming. The significant rise in CO2 emissions has prompted extensive research into Carbon Capture and Storage (CCS) technology. The primary objective of CCS technology is to mitigate CO2 levels in the atmosphere through the recovery of CO2 from industrial flue gases, achieved through three key stages: CO2 capture from flue gases, CO2 transport, and subsequent storage. This review provides a comprehensive overview of various techniques employed to remove CO2 from flue gases, focusing on physical, chemical and biological methods. The article included comprehensive information about the chemical process, including its benefits and limitations. An extensive overview of the biological and physical approaches was also provided. A brief discussion is given of the engineering aspects of CO2 transfer via pipelines and ships, as well as its storage alternatives (oceanic, geological, and mineralization). Through an analysis of these various approaches, this review directs scientists and researchers toward improving their comprehension and use of effective CO2 collection techniques, consequently tackling the problems associated with global warming.
The alarming rise in global temperatures and its catastrophic consequences have heightened the urgency to combat climate change. One of the key contributors to this phenomenon is the excessive emission of greenhouse gases (GHGs), primarily carbon dioxide (CO2) [1]. Fig. 1 shows the CO2 trend in the atmosphere over the past few decades [2]. One of the main sources of CO2 emissions is the combustion of fossil fuels. Fossil fuel combustion has been the backbone of global energy production for decades, due to its abundance and high energy density. However, the release of CO2 during the combustion process significantly contributes to the accumulation of GHGs in the atmosphere, intensifying the greenhouse effect and accelerating global warming [3]. Consequently, increased CO2 levels in the atmosphere contribute to climate change, ocean acidification, melting ice and rising sea levels, health concerns and ecosystem disruption. Therefore, transitioning to cleaner and more sustainable energy sources, such as renewables, has become imperative.
Renewable energy technologies, including solar, wind, hydro, and geothermal, offer environmentally friendly alternatives for power generation by producing energy without the associated release of CO2 and other harmful emissions, making them crucial in mitigating climate change. However, despite their growing adoption and advancements, the intermittent nature and limited scalability of renewable energy systems pose challenges to their widespread implementation as the sole solution [4].
To bridge this energy transition gap, Carbon Capture and Storage (CCS) technology has gained considerable attention as a complementary approach to reduce CO2 emissions from fossil fuel-based power plants [5,6]. CCS involves the capture, transportation, and secure geological storage of CO2 emissions, preventing their release into the atmosphere [7].
This review paper aims to provide an overview of CCS technology, mainly focusing on the basic principles involved in post combustion capture techniques (such as adsorption and absorption), transportation methods and storage options. The use of dry alkali metal – based sorbents, aqueous amine solutions and hot potassium carbonate solutions has been highlighted along with their advantages, drawbacks and process modification suggestions. By critically examining the strengths and limitations of CCS technology, this review aims to contribute to a comprehensive understanding of its potential as a viable strategy for achieving climate change mitigation targets. Ultimately, this review can help inform policymakers, researchers, and industry stakeholders about the importance of CCS in the transition towards a more sustainable and low-carbon energy future.
2. Carbon Capture
The Carbon Capture and Storage technology involves recovery of carbon dioxide from flue gas streams followed by transportation to a safe storage space where it is sequestered and can be reused as a raw material in several processes such as production of methanol, manufacture of pharmaceutical products, etc. Fig. 2 shows an overview of the CCS technology. There are three types of CO2 capture [8]:
• Pre-combustion capture
• Oxy – fuel combustion capture
• Post combustion capture
Among these, post combustion CO2 capture is the most widely used method as it can be retrofitted into the existing power plants and industries without significant modifications to their existing infrastructures [9]. The main objective of this technology is to control CO2 concentration in the atmosphere by removing it from flue gases via various physical, chemical, and biological separation techniques. Post-combustion capture system can reduce up to 90% of the CO2 emissions [10]. However, its installation and operations are expensive [11,12]. Fig. 3 shows the classification of different methods of CO2 capture that have been discussed in the following sections.
2.1. Chemical Methods
CO2 sequestration through chemical methods involves absorption of CO2 using solid sorbents or liquid solutions, followed by regeneration of the sorbent or solution. Dry alkali metal-based sorbents, aqueous amine solutions, and aqueous potassium carbonate solutions are the most common techniques used for the recovery of CO2 from flue gases.
2.1.1. K2CO3 based sorbent
Absorption of CO2 present in moist flue gases by solid K2CO3 sorbents is carried out at low temperatures of around 40–80°C resulting in the formation of potassium bicarbonate (KHCO3) according to the carbonation reaction Eq. (1):
(1)
K2CO3 must first be pre-treated with some quantity of moisture in order to activate the sorbent. The quantity of moisture used in the pre-treatment process significantly affects the CO2 uptake capacity of the sorbent [13–16].
The chemical sorption of CO2 on K2CO3 was considered to be a series mechanism consisting of two steps. In step 1, as shown by Eq. (2). K2CO3 is converted to its hydrated form K2CO3· 1.5 H2O which is considered as the activated species. In step 2, the active K2CO3·1.5H2O reacts with CO2 via the carbonation reaction Eq. (3). and forms KHCO3. However, Jayakumar et al. showed that hydration of K2CO3 to K2CO3· 1.5H2O, and carbonation of K2CO3 to KHCO3 are reversible reactions that occur in parallel rather than series Eq. (4). and Eq. (5) [17].
(2)
(3)
Other reactions taking place are:
(4)
(5)
Once the solid sorbent is saturated with CO2, it is regenerated by heating so that it can be reused for another absorption cycle. K4H2(CO3)3·1.5H2O(s) plays an important role in affecting the carbonation process [18,19]. Formation of potassium bicarbonate is faster from K4H2(CO3)3·1.5 H2O than from K2CO3·1.5H2O [20].
While selecting the support material, it is important to take into consideration not only the absorption capacity but also the ease of regeneration of the sorbent. In an experiment conducted by Lee et al. although MgO supported sorbent showed the highest absorption capacity [21], its regeneration temperature was 350°C, whereas, in another experiment it was shown that TiO2 could be regenerated at 150°C with a reasonably high capture capacity (83mg CO2/g sorbent) [22]. Table 1 gives an overview of the use of different supports for K2CO3.
Concerning the physical properties of the support material, since K2CO3 is highly deliquescent, it requires a porous support material with a large surface area and pore volume [23,24]. As K2CO3 loading on the support increases, CO2 capture capacity increases and becomes maximum at a certain limit, decreasing with further loading. This happens because the active material being less porous than the support, when loaded onto the support material beyond a certain limit, will tend to block the pores, thereby lowering the amount of CO2 absorbed [25].
A two-stage integrated fluidized bed system was studied for continuous CO2 capture using K2CO3/Al2O3 sorbent [26,27]. The integrated system required a lower bed height and showed higher CO2 uptake efficiency than conventional reactors. Similar studies were also conducted on CO2 removal using K2CO3/Al2O3 in a single stage circulating fluidized bed reactor [28,29]. Microfluidized bed reactors have been used to study the process optimization of carbon capture using K2CO3/Al2O3 sorbent [30].
2.1.2. Aqueous amine solutions
One of the most common methods of CO2 recovery from flue gases, natural gas etc. is the use of aqueous solutions of primary (MEA), secondary (DEA), tertiary (MDEA) and sterically hindered (AMP) alkanolamines [34]. The process involves the counter current flow of CO2 rich flue gas upwards and aqueous amine solution downwards in an absorber resulting in chemical absorption of CO2 from the gas phase into the liquid phase. After the amine solution is saturated with CO2, it is heated and regenerated in a stripper to release the captured CO2. Since the gas to liquid absorption process depends largely on the solubility of the gas in the liquid, extensive research has been done on the CO2 + water + amine system [35–38]. Additionally, the literature contains detailed insights of CO2 absorption using different solvents in the CCS technology [39,40].
Several researchers have studied the reaction mechanism and kinetics in order to analyse the effect of different types of amines on CO2 capture capacity [41–46]. The kinetic data for the carbonation reaction of alkanolamines is overviewed in Table 2. The carbonation reaction of primary, secondary and sterically hindered amines with CO2 follows the zwitterion mechanism, whereas tertiary amines follow the base catalysed hydration mechanism [48–50].
(6)
(7)
Two molecules of primary amines react rapidly with carbon dioxide to form one carbamate ion, as shown in Eq. (6). In Eq. (7). the carbamate ion is hydrolysed to regenerate one molecule of amine. However, owing to the stability of the carbamate ion, this regeneration does not occur readily [52]. Also, formation of the carbamate ion is associated with high heat of absorption which makes the regeneration of alkanolamines an expensive process in terms of cost and energy [53].
Tertiary amines are blended with primary or secondary amines, thereby combining the fast reaction kinetics associated with primary or secondary amines and the low heat of absorption associated with tertiary amines [54,55]. Gray et al. demonstrated that secondary amines have a stronger affinity towards CO2 capture from flue gases than primary amines [56]. A novel computational screening method was developed by Orlov et al. which was able to detect tertiary amines that had faster CO2 absorption kinetics than regular commercial solvents [57].
Amine based solid sorbents can be used to capture CO2 from flue gases. Gray et al. showed that tertiary amine based solid sorbent was stable at temperatures of 298K – 360K and that the system required 30–50% lesser energy than aqueous amines [59].
Piperazine (PZ) can be used as a rate promoter to enhance CO2 absorption by aqueous amines [62–65]. PZ is a diamine with a cyclic, symmetric structure. Theoretically, one mole of PZ can absorb two moles of CO2, and it may favour rapid formation of carbamate ions [66]. Studies have been conducted on the PZ + water + CO2 system to develop equations which predict the solubility of PZ in water and to determine the kinetics of the reaction of PZ with CO2 [67–69]. PZ promoted amines have experimentally been proven to show higher CO2 uptake capacity than neat aqueous amine solutions [70–73]. Impregnation of polyethylenimine (PEI) into a nanosilica support or activated carbon support is also an effective way to enhance the efficiency of neat aqueous amine solutions [74–78].
2.1.3. K2CO3 solution
Hot potassium carbonate solution facilitates the absorption and subsequent removal of CO2 from the flue gas stream, as shown in Fig. S1. This carbon capture process is commonly referred to as “wet scrubbing” or “chemical absorption”. Advantages of process [79, 80]
• its resistance to high temperatures and pressures,
• ease of regeneration,
• low toxicity, and
• low cost of the solvent
The basic principle of CO2 removal using aqueous K2CO3 solution involves passing the flue gases through a liquid scrubbing solution containing K2CO3. The CO2 present in the flue gases reacts chemically with the K2CO3 in the liquid, forming a soluble compound known as potassium bicarbonate (KHCO3) as shown in Eq. (8). and Eq. (9). The following reactions take place in the absorption process [81,82]:
(8)
(9)
(10)
(11)
Neat K2CO3 solution shows slow mass transfer (via absorption) of CO2 into the liquid phase making it an undesirable choice for treatment of flue gases from coal fired power plants. The carbonation reaction rate depends on the hydroxyl ion concentration Eq. (10). The CO2 hydrolysis reaction Eq. (11). being the slowest step, results in low hydroxyl ion concentration causing the overall carbonation reaction rate to slow down, consequently affecting the rate of mass transfer [82]. In order to overcome this problem, it is preferred to blend the K2CO3 solution with rate promoters which enhance the reaction rate, making the process faster and more efficient [83–88].
When amines are used as rate promoters with potassium carbonate solution, the rate of absorption increases due to the presence of amines, and CO2 uptake capacity and ease of regeneration increase due to the carbonate-bicarbonate buffer effect [89]. Thee et al. added 5%wt and 10%wt MEA to 30%wt potassium carbonate solution and obtained a higher absorption rate by a factor of 16 and 45 respectively [90]. Between primary and secondary amines, secondary amines such as pipecolic acid and sarcosine are the best rate promoters [58, 91]. Two mechanisms – shuttle mechanism and homogeneous catalysis are used to explain the rate promotion effect of amines in potassium carbonate solutions [90, 92].
2.1.4. Chilled ammonia process
The chilled ammonia process (CAP) represents a viable approach for CO2 sequestration, utilizing a regenerable solvent-based method that employs an aqueous ammonium solution to capture CO2 by forming ammonium bicarbonate. Subsequently, the bicarbonate undergoes a heating process (100°–150°C) in the desorber to liberate CO2, with the resulting carbonate being recycled back to the CO2 absorption system for reuse [93]. CO2 absorption takes place in the temperature range of 0°–20°C, or optimally 0°–10°C, effectively reducing the concentrations of moisture, acidic compounds, and volatile components [94]. Chehrazi et al. presented a review on the use of chilled ammonia process to recover CO2 from ammonia plant flue gases and its utilization in a urea plant [95]. Fig. 4 illustrates the advantages of CAP over other aqueous amine processes [96–98].
2.2. Physical Methods
CO2 can be sequestrated by physical methods such as adsorption or membrane technology. Some of the techniques for adsorption of CO2 include the use of carbon nanotubes, electric swing adsorption, and zeolites.
2.2.1. Carbon nanotubes
Carbon nanotubes (CNTs) are nanoscale cylindrical structures made of carbon atoms. Physical adsorption of CO2 on the surface of CNT is highly effective owing to its porous structures with large surface area and high thermal stability [99–102]. After the CNT is saturated with CO2, it is regenerated by heating to release the CO2 so that the nanotube can be reused. CNTs exhibit exceptional CO2 adsorption capacity attributed to their favourable kinetics, reversibility, and low regeneration energy requirements [103]. Fig. 5 shows the structural, physical properties and advantages of CNT. Researchers have explored the modifications of multi-walled CNTs such as addition of 3-aminopropyl-triethoxysilane(APTS), N-(3-trimethoxysilylpropyl), diethylenetriamine,1,3–diaminopropane etc., to enhance the physicochemical characteristics and adsorption capacity of the nanotubes and promote CO2 adsorption [104–106]. Recently, Heidari et al. introduced a novel method in which CNTs are used as additives to sol–gel based CaZrO3 – CaO adsorbents to enhance their CO2 capture capacity [107]. Additionally, a combined thermochemical method has been explored to improve the efficacy of CNTs in CO2 capture. This involves subjecting the CNTs to a heating process at 300°C for 60 minutes, followed by immersion in a chemical solution, resulting in an increased CO2 absorption capacity [108]. Although CNTs offer high adsorption capacity and selectivity for CO2, the challenge lies in achieving cost – effective mass production of CNTs and maintaining their stability and recyclability over multiple cycles.
2.2.2. Electric swing adsorption
Electric Swing Adsorption (ESA), is an adsorption technique in which CO2 is passed through a bed of adsorbent material such as activated carbon fibre, followed by application of an electric field to enhance the adsorption of CO2 on the adsorbent [109]. Regeneration of the adsorbent material is done by reversing the electric field to desorb the CO2. Application of electrical current results in an increase in temperature leading to generation of Joule’s heat in the adsorbent. This process is termed as electrothermal desorption [110]. ESA has been assessed for the removal of CO2 from flue gases, particularly those emitted by natural gas combined cycle (NGCC) power plants [111,112]. ESA has four basic steps, including feed, electrification, purge and cooling [113] Fig. S2 illustrates the ESA process. Faradaic electro-swing reactive adsorption offers a novel approach for carbon capture by utilizing PAQ-CNT material deposited on the electrodes of an electrochemical cell [114]. In this process, CO2 is adsorbed onto the cathodes during the capture phase, forming a stable CO2 adduct. The captured CO2 can be subsequently released by applying a different potential to the cell, causing desorption from the electrodes and release back into the chamber. ESA is a second-generation technique that provides an efficient means for CO2 capture, demonstrating its potential in addressing carbon emissions and climate change mitigation [115].
2.2.3. Membrane technology
Membranes can be used to separate CO2 from flue gases or CO2 rich sources [116, 117]. Membrane technology plays a significant role in efficient CO2 separation, particularly when the CO2 concentration exceeds 20%, with energy-efficient absorption for lower CO2 inputs [118]. The underlying principle behind this technology is that the difference in partial pressures of the components of the flue gas is used to separate CO2, enabling its capture and storage [119]. Combining moderate vacuum technology with membrane modules reduces energy requirements and enhance absorption capabilities [120]. The field of membrane-based CO2 separation primarily focuses on two configurations: flat sheet and hollow fibres [120–122]. Liquid membranes offer advantages such as high diffusivity and the ability to be tailored for specific separation processes [123].
Ceramic porous membranes have demonstrated the capability to capture up to 90% of CO2 from flue gas, while polymeric membranes exhibit excellent permeability and selectivity [124]. In recent developments, mixed matrix membranes (MMMs) and metallic-organic frameworks (MOFs) have emerged as promising materials for membrane-based CO2 separation. These materials combine the transport and separation properties of polymeric matrices with the stabilization provided by nanoparticle/metallic fillers [121]. Moreover, the integration of membrane modules with moderate vacuum technology has proven effective in reducing energy requirements and enhancing the absorption capabilities of the system [125]. However, membrane units necessitate higher permeability and more intensive operations for efficient CO2 transport [126,127]. Overall, membranes offer significant potential for efficient CO2 separation, and require further research that focuses on improving their performance, stability, and scalability for practical application in CO2 capture and mitigation strategies.
2.3. Biological Methods
Biological methods for post-combustion CO2 capture involve utilizing living organisms, typically microorganisms or plants, to absorb and convert carbon dioxide from industrial emissions into biomass or other products. Some of the key biological methods commonly considered for CO2 capture are discussed below.
2.3.1. Microalgae
Microalgae are microscopic, photosynthetic organisms that can uptake carbon dioxide directly from the atmosphere or flue gases and produce biomass through photosynthesis[128]. Microalgae have gained sufficient attention in recent years due to the following advantages:
• Potential for CO2 capture and production of biofuel and other value-added products such as polysaccharides, proteins etc. [129–131] termed as biosequestration [132].
• Microalgae strains such as Botryococcus braunii, Chlorella s, Chlorella vulgaris, Scenedesmus obliquus, and Scenedesmus s have demonstrated great potential in both CO2 assimilation and lipid production for biodiesel generation.
• Using microalgae through photosynthesis allows fossil fuels to be used in an environmentally friendly manner by capturing carbon as biomass, creating a symbiotic relationship between power plants and microalgae farms to enhance CO2 utilization and reduce greenhouse gas emissions [133,134].
A comparison of the performance of these microalgae is given in Table 3. Fig. S3 represents the Carbon dioxide sequestration using Microalgae representing the process in the simplest of manner.
2.3.2. Microbes
Microbial CO2 sequestration uses microorganisms to convert CO2 into biomass or minerals, reducing CO2 in the atmosphere. However, improving efficiency remains a challenge due to CO2 emissions from microbes [139]. This has led to the development of strategies like engineering of CO2-fixing pathways, energy-harvesting systems, and metabolic rewiring to boost CO2 fixation efficiency in microorganisms [140]. Microbial CO2-fixing organisms are classified as:
• Autotrophs: Autotrophic microorganisms, which use CO2 as their sole carbon source, primarily include bacterial and archaeal taxa such as Cyanobacteria, Crenarchaeota, and Betaproteobacteria [141]. Among these, cyanobacteria, such as Synechocystis sp. PCC 6803 and Anabaena sp. PCC 7120, are the best-developed autotrophic cell factories [142]. Eukaryotic microalgae, like Chlamydomonas reinhardtii and Phaeodactylum tricornutum, and acetogens, such as Clostridium ljungdahlii are utilized in metabolic engineering to enhance CO2 fixation and produce biofuels and chemicals.
• Heterotrophs: Heterotrophic microorganisms such as Propionibacterium pentosaceum, E. coli, and S. cerevisiae, fix CO2 through carboxylation reactions in metabolic pathways, relying on organic substrates for both carbon and energy [143]. Despite the commercial potential, the application of microbial CO2 fixation is still limited, with microalgae being the primary CO2-fixing organisms used industrially [144].
Microbial electrolysis cells (MECs) enhance CO2 sequestration by generating acid and alkali solutions that facilitate CO2 absorption and carbonate precipitation, improving methane production in biogas by 16.9%. Biomimetic sequestration leveraging enzymes like carbonic anhydrase from bacteria such as Pseudomonas fragi can significantly boost CO2 sequestration, with enzyme consortia achieving efficiencies up to 61%, compared to 17.8% with bovine carbonic anhydrase [145].
Microbial carbon capture cells (MCCs) combine algae with microbial systems, effectively sequestering CO2 and generating power and biodiesel. For example, Chlorella vulgaris in MCCs can convert CO2 into algal biomass, effectively eliminating CO2 generated from the anode [146]. Furthermore, certain Bacillus species are capable of growing in supercritical CO2 environments, suggesting their potential role in deep subsurface CO2 sequestration. Studies have demonstrated that bacteria isolated from geologic carbon sequestration sites can thrive in scCO2 conditions, indicating their influence on CO2 fate and transport in such environments [147].
2.3.3. Bacteria
CO2 sequestration using bacteria can be achieved through various biochemical pathways. The use of certain bacteria in CO2 sequestration has been highlighted as follows:
• Cyanobacteria, such as Synechococcus sp. NIT18, has demonstrated high efficiency in sequestering CO2, with a reported maximum sequestration rate of 71.02% under optimal conditions, producing valuable biomolecules such as proteins, carbohydrates, and lipids in the process [148].
• Marine bacteria, like Bacillus safensis, employ the enzyme carbonic anhydrase to catalyze the hydration of CO2, significantly reducing CO2 levels in soil microcosm studies [149]. Advances in genetic engineering have further optimized CO2 fixation pathways in microorganisms, enhancing their metabolic efficiency for improved CO2 sequestration and the concurrent production of biofuels and chemicals [150].
• Bacillus sp. strain ISTS2 has been shown to produce biosurfactants while sequestering CO2, utilizing both carbonic anhydrase and RuBisCO enzymes, presenting a sustainable bioprocess for industrial CO2 utilization [151]. Recent innovations also include a light-driven system in Escherichia coli, integrating CO2 fixation and mitigation modules to significantly boost CO2 sequestration efficiency and yield value-added chemicals [152].
2.3.4. Miscellaneous methods
Stable and efficient CO2 absorption has been demonstrated by amino acid salts derived from inorganic bases, such as potassium hydroxide (KOH), whereas temperature sensitivity affects the CO2 absorption capabilities of these salts [153]. Innovative approaches involve immobilizing different amines on zeolites such as zeolite 13X and HZSM-5 zeolites to create functionalized adsorbents for CO2 capture [154–157]. Carbonation/calcination looping, employing two fluidized bed reactors, demonstrates potential for effective CO2 collection [158, 159]. The calcium technology, widely employed in industries like cement production, offers a low-cost and highly efficient post-combustion CO2 capturing method [159]. Hydrogen membrane reactors have emerged as a compelling solution for CO2 capture in gas-fired power plants, enabling efficient conversion of natural gas into hydrogen (H2) for power generation while simultaneously capturing the remaining CO2 [160,161].
3. Transportation
On a commercial scale, CO2 is mainly transported in the gaseous or liquid phase through pipelines or ships [162]. Once CO2 is recovered from the source, it is subjected to conditioning, a process in which the impurities such as moisture content, H2S, O2, CH4 and other hydrocarbons are removed in order to obtain the desired composition [163]. The dried gas is then compressed to the required pressure level (so as to meet the transportation criteria) before it is transported. Fig. S4 illustrates the steps involved in the transport and storage of CO2. The distance to the storage location, volume of CO2 to be transported, and the cost of the technology, all play a vital role in selecting the mode of CO2 transportation. CO2 transport of large capacities over short distances is suited to pipeline transport, whereas ship transport is preferred for small capacities and long distances [164].
3.1. Pipelines
Pipelines is the primary mode of CO2 transport as it is the most economical method to transport large volumes of CO2 [165]. Pipelines offer the advantage of a constant, steady CO2 supply without the requirement for temporary storage along the transmission line [166].
The key factors of a pipeline transport system are [167–168]:
• Design and material of pipelines: The design and material considerations are based on the temperature and pressure of CO2, which necessitates thicker walls or special coatings to prevent corrosion. Carbon steel is the most common material of construction.
• Planning of infrastructure: Infrastructure planning depends on whether the CO2 transport pipelines are onshore or offshore depending on the location of the storage facility.
• Pressure and temperature of CO2: Depending on the temperature and pressure, in the pipelines, CO2 may be in the gaseous state, subcooled liquid state, or in the form of a supercritical fluid. The most efficient phase of CO2 for pipeline transport is the supercritical fluid. When CO2 is transported in this phase, it is denser, has a lower tendency to change phase, and undergoes lower pressure drop along the pipeline [169].
3.2. Ships
For international or offshore transport, CO2 is mainly transported through ships in the liquid phase and is commonly used in the food and brewery industries [170]. Decarre et al. has given a detailed description of the complete CO2 transport process through ships [173]. The main factors in the transport of CO2 through ships are:
• Liquefaction of CO2: CO2 is cooled and pressurized to convert it into a liquid state, typically at temperatures around −50°C and pressures of about 7 MPa.
• Tanker design: Specialized tankers are designed to maintain low temperatures and high pressures.
• Loading and unloading: The ease of loading and unloading CO2 depends on how far the source is located from navigable waterways. If this distance is significantly long, a pipeline network connecting the CO2 source to the port terminals must be laid down [171,172].
3.2.1. Economics of transportation
Cost analysis and economic optimization are essential for evaluating the financial viability of CO2 transport in the CCS technology. Several researchers have explored various cost-effective options to determine the economic feasibility of the CO2 transport system [174–177]. Kazmierczak et al. developed an algorithm under the EU – funded GeoCapacity project to create low – cost pipeline networks connecting CO2 sources and storage sites [178]. Similarly, one of the outcomes of the COATE European Project was the development of an economic model for the CO2 transport network which minimized the overall transport cost [179]. In order to ensure safe and effective implementation of CO2 transport, certain risks and challenges associated with the pipeline transport have to be addressed [180–182]. Guidelines for CO2 capture, transport and storage are crucial for ensuring the safe, effective and environmentally responsible deployment of the CCS technology, contributing to climate change mitigation efforts and sustainable development [183,184].
4. Storage
To guarantee that CO2 can be kept contained, a suitable location must be selected and evaluated for safety and feasibility before injection. A CO2 storage site must be evaluated for the following characteristics:
• Safety and permanence – CO2 must be stored safely and permanently away from the atmosphere.
• Capacity – the storage reservoir should have the capacity to store large volumes of CO2.
• Leakage – it should be equipped with reliable monitoring systems that are easy to access and control to ensure safe, leak-proof storage of CO2.
There are three types of CO2 storage–ocean storage, geological storage and carbon mineralization, as shown in Fig. S5 [185].
4.1. Ocean storage
Oceans readily absorb atmospheric CO2 [186] and are viewed as one of the largest carbon sinks [187]. Ocean storage of CO2 is classified into the following two types based on the depth of CO2 injection:
• Deep ocean injection: This process requires the deliberate injection of large amounts of CO2 into the ocean at a certain depth. The deeper the injection, the larger is the fraction of CO2 retained [185, 188]. The percentage of CO2 that will remain sequestered for over 500 years is 74, 83, and 90 at depths of 1500m, 2500m, and 3000m respectively [189].
• Lake formation: For longer retention, CO2 can be stored in the form of solid hydrates or by creating CO2 lakes on the ocean floor. The storage process involves the transportation of compressed CO2 via ships or offshore pipelines to the storage site, followed by direct injection of CO2 into the seawater or deposition of CO2 into CO2 lakes on the ocean floor [185, 190].
Fig. S6 illustrates storage of CO2 in oceans. Khoo et al. have given a brief outlook on the different techniques used to inject and store CO2 in the ocean, including vertical injection, pipe carried by ship, inclined pipe, dry ice (blocks of solid CO2), hydrates of CO2 and gas lift advanced dissolution for low purity carbon dioxide gas [188].
Although the ocean has a great potential for CO2 sequestration, it is also important to highlight the following risks and adverse effects associated with the large-scale implementation of such a technology [191–193]:
• Injection of CO2 results in ocean acidification in which pH falls below 7.
• Increased CO2 levels can harm marine organisms, especially those with calcium carbonate shells or skeletons, such as corals, shellfish etc.
• Ocean acidification leads to ecosystem disruption, oxygen level depletion and other uncertain, unintended consequences which are hard to predict owing to the complex marine food webs and vast biodiversity of the ocean.
4.2. Geological Storage
Deep saline aquifers, depleted oil and gas reserves (including Enhanced Oil Recovery), deep coal beds (including enhanced coal bed methane recovery), and mined caverns are suitable geological carbon sinks [194, 195]. Saline aquifers have the largest storage capacity followed by coal beds and oil and gas reserves [196].
4.2.1. Deep saline aquifers
These are large underground reservoirs of saltwater with high enough pressure and temperature to keep the CO2 in a supercritical state [197]. Additionally, several researchers have presented detailed insights on storage of CO2 in saline aquifers [198–200]. The factors affecting the storage efficiency of an aquifer are [201]:
• Temperature and pressure: The aquifer must handle high temperatures and pressures.
• Configuration of the aquifer: A horizontal aquifer has a better residual CO2 trapping system.
• Caprock: Properties such as porosity, permeability, and heterogeneity determine the capacity and efficiency of the aquifer. Porous, water-wet rocks are highly efficient for CO2 storage.
Zhang et al. studied the effects of a supercritical CO2–water system on the geological, micromechanical, and mechanochemical properties of sandstone and reported that the introduction of such a system would lower the compressive strength of the rock [202].
4.2.2. Enhanced oil recovery
Another reliable method of CO2 storage is through enhanced oil recovery (EOR) [203–206]. In this process, the overall cost of CO2 storage is reduced by integrating oil and gas recovery from reservoirs with CO2 storage [207–209]. The advantages of this method include [210]:
• Large storage capacity,
• Compensation of CO2 sequestration cost by revenues obtained from producing oil,
• Since the oil or gas reservoir has already been geologically surveyed and analysed, expenditure on the geological characterization of the site is saved.
However, storage through EOR is thermodynamically sustainable only if the energy produced from the recovered oil is greater than the energy consumed in the CCS process [211]. Dai et al. developed an economic model to estimate the profitability of the CO2 - EOR system [212]. Raza et al. developed a new analytical method to estimate the amount of residual CO2 trapped in depleted oil and gas reservoirs [213]. CO2 storage through enhanced oil recovery is summarized in Fig. S7.
4.2.3. Coal seams
Coal seams are underground coal beds that are suited to the geological storage of large volumes of CO2. They have a large surface area due to the presence of a highly porous, heterogeneous matrix onto which methane molecules are stored in the adsorbed state. When CO2 is injected into the coal seams, having a greater affinity towards coal than methane, the injected CO2 readily gets adsorbed onto coal by displacing methane (desorption) [214]. Such a process in which methane is recovered by injection of CO2 into coal beds is called Enhanced Coal Bed Methane (ECBM) recovery [215–218]. The following characteristics of coal seams have been studied:
• Porosity: Li et al. studied the effects of a deionized H2O-CO2 mixture on the porosity of different types of coal, and reported that the interaction of the mixture enhances the development of macropores, thus improving the capacity of the coal seam [219].
• Geochemical interaction of CO2 with coal: The fast reaction of carbonate minerals, the continuous dissolution of sodium and potassium, and the change in pore structure due to CO2 acid fluid are the important geochemical reactions to be considered [220].
• Adsorption behaviour: With the adsorption of CO2, the permeability of the coal seam first reduces due to adsorption swelling, and then increases due to reduced stress [221].
Other aspects of CO2 sequestration such as coal wettability have been studied in order to gain a better understanding of this technology [222].
4.2.4. Leakage
One of the most important aspects of geological sequestration of CO2 that is to be considered is underground leakage [223]. Although the sedimentary basins contain impermeable cap – rocks that are capable of trapping CO2, there is always a risk of slow leakage of the stored CO2 into the surroundings [224]. Leakage can be due to natural causes such as open faults, or man – made causes such as abandoned wells. CO2 leakage can increase the pH of the surroundings and cause acidification of potable water present in nearby aquifers [225]. The financial risks associated with the underground leakage of CO2 must also be given due attention [226]. The Leakage Risk Monetization Model (LRiMM) was developed by Bielicki et al. to quantify the loss incurred in case of CO2 leakage [227]. In addition to proper design and monitoring systems, in order to minimize the potential risks of underground CO2 leakage, effective gas leakage detection techniques must also be implemented [228]. Alcalde et al. presented a numerical program which estimates CO2 storage security and the amount of CO2 leakage into the atmosphere over a period of 10,000 years [229].
4.2.5. Carbon mineralization
In this method, CO2 is injected into the ground and made to react with alkaline minerals such as oxides of calcium and magnesium or alumino – silicates and magnesium silicates so as to form thermodynamically stable carbonates[230,231]. CO2 storage through carbon mineralization does not require any monitoring system as there are no chances of leakage of the stored CO2 [209, 232]. However, this method of storage has low efficiency (32.9% – 49.7%) and is expensive in terms of overall cost and energy of the CCS process [233]. These barriers can be overcome by (i) use of recyclable residues such as solid waste residue, alkaline industrial residues (such as fly ash), steel residues etc. to mineralize CO2 [209, 234] and (ii) optimization of the heat energy produced by the exothermic carbonation reaction [233, 235].
Recently, carbon mineralization using Basalt, a common type of volcanic rock containing calcium, magnesium and iron, has been recognized as an effective method of CO2 sequestration. However, it is still an emerging field, and there are ongoing research and development efforts to optimize the process and determine its scalability and long – term effectiveness [236–239]. Sim et al. introduced a novel concept in which CO2 is stored through carbonation reaction with NaOH and oxalic acid along with simultaneous recovery of rare earth elements [240].
5. Future Scope
Countries worldwide are making ambitious commitments to reduce CO2 emissions and combat climate change. However, there are challenges associated with CCS technology, particularly in terms of energy consumption during the capture and compression of CO2. Improving the efficiency and cost-effectiveness of CCS operations is crucial for its widespread deployment. Research and development efforts should focus on advancing CCS technologies to enhance carbon capture efficiency and reduce operational costs. As the world strives to meet climate targets and transition to a low-carbon future, exploring and developing more efficient and economically viable CCS technologies is a promising avenue for further research. Continued innovation in CCS holds the potential to significantly contribute to global emissions reduction and facilitate the transition to a sustainable and decarbonized energy system.
6. Conclusions
In conclusion, this review paper comprehensively examined the various aspects of CO2 capturing, transportation, storage, and modern technologies in the context of carbon capture and storage (CCS). The focus was placed on post-combustion capturing methods, including sorption techniques such as K2CO3 dry alkali metal sorbents, aqueous amine, and PEI. Transportation of captured CO2 was explored, encompassing different methods such as ships, trucks, and pipelines. The storage of CO2 was also extensively discussed, covering ocean storage, geological storage, carbon mineralization, and storage in coal seams. Each storage approach was evaluated in terms of its feasibility and potential environmental impact.
Furthermore, this paper highlighted modern technologies that show promise in CO2 capture, including CAP (chilled ammonia process), CNTs (carbon nanotubes), microalgae, membranes, and ESA (electric swing adsorption). These methods offer innovative approaches to enhance efficiency and address the challenges associated with CCS technology. Looking towards the future, it is evident that there is a pressing need to reduce the cost of CCS technology and increase its overall efficiency.
Continued research and development efforts should be directed towards optimizing existing methods and exploring new techniques to meet the growing demand for carbon capture and storage. By improving the cost-effectiveness and performance of CCS systems, we can contribute significantly to global efforts in mitigating climate change and achieving sustainable energy systems.
Authors are thankful to M S Ramaiah Institute of Technology for providing the necessary support.
Notes
Conflict-of-Interest Statement
The authors declare that they have no conflict of interest.
Authors Contributions
S.F. (B.Tech student) have done extensive literature review on the present work and compiled the information. S.S. (B.Tech student) contributed for the preparation of the manuscript. S.V. (Assistant Professor) have critically supervised and improved the manuscript in various aspects.
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K2CO3-AR* (Sigma Aldrich, ACS reagent, ≥99.0%), and K2CO3-RC** Recrystallized K2CO3 was made by dissolving 1 g of the K2CO3 reagent in 10 ml of deionized water in a stainless-steel crucible and drying it for 24 hours at 70°C.
Table 2
Reaction kinetics of various alkanolamines with CO2