1. Introduction
Over the past two decades, there has been a growing emphasis on developing sustainable and energy-efficient solutions for refrigeration, air conditioning, and thermal management systems. Cooling demand is increasing rapidly due to urbanization, data-center expansion, and electrification, placing significant pressure on conventional refrigeration systems that rely on high-global-warming-potential refrigerants. Cold thermal energy storage (CTES) technologies have emerged as a viable pathway to decouple cooling demand from energy supply while improving system efficiency and reducing emissions. This transition is driven not only by the global increase in cooling demand but also by the urgent need to reduce greenhouse gas emissions, including the elimination of high-global-warming-potential (GWP) refrigerants, which are widely used in space air conditioning. In this context, gas hydrate-based CTES systems have emerged as an innovative solution by having high energy density, environmental safety, and thermal controllability. Among various gas hydrates, CO
2 hydrates are particularly gaining attention due to their high energy storage density, wide availability at low cost, and flame retardancy of CO
2, as well as its favorable hydrate formation characteristics under moderate pressure and temperature conditions [
1,
2].
Phase change material (PCM) slurries and ice slurries are both well-known and widely considered as effective thermal carriers designed to enhance the energy transport capabilities of cooling systems. These slurries depend on the latent heat of suspended phase change materials to deliver significantly higher thermal energy per unit mass or volume compared to conventional thermo-fluids like water, water mixtures with antifreeze or glycol, or brines [
3]. Typically, PCM slurries consist of microencapsulated or finely dispersed phase change materials, such as paraffin waxes or salt hydrates, suspended in a carrier fluid. The key advantage of these slurries is their ability to utilize both sensible and latent heat during the transport process. At PCM concentrations of 10–30 wt% [
4], the thermal energy carried by these slurries can be approximately two to three times higher than that of water [
5,
6].
Because the heat is absorbed or released at nearly constant temperature during the phase change process, the outlet temperature of the fluid in heat exchangers using PCM slurries remains stable, in turn, improving thermal control and overall system efficiency. The elevated energy density of PCM slurries could help reduce the required flow rate by up to 50%. This contributes to lowering the pumping power and allows for the possible usage of smaller tubing diameters without compromising the cooling capacity. Compared to conventional thermo-fluids, these slurries also exhibit predictable pressure drops, in laminar and transitional flow regimes that make them suitable for conventional pumping and heat exchanger systems [
7].
Despite many thermal benefits, PCM slurries face challenges such as phase separation, sedimentation, or the development of a yield stress at higher solid fractions. These issues complicate a long-term and continues operation. Also, refrigeration systems using PCM slurries are usually more complex with added continuous agitation or re-suspension mechanisms. In contrast, ice slurry systems address several of these shortcomings while providing comparable or even superior thermal transport benefits. With a latent heat of fusion of approximately 334 Kj·kg
−1, ice particles contribute significantly to the energy density of slurry, and this represents higher energy density than for many organic PCMs in terms of cooling capacity per unit mass. When ice is suspended in water, the ice particles contribute to the enhanced convective heat transfer. These heat transfer coefficients can be even 2–3 times higher than those observed in conventional single-phase coolants. Ice slurries can be circulated efficiently through standard piping systems without major design changes. At low to moderate ice fractions below 20%, they behave nearly as Newtonian fluids. This can lower pumping energy by up to 30%, when compared to single-phase fluids under equivalent cooling loads [
8].
Ice slurries maintain their flowability even at relatively high solid fractions (up to 25%) when particle sizes are kept fine and uniformly distributed. This provides consistent heat delivery without the need for extra agitation systems. Their compatibility with existing HVAC and refrigeration technologies, including district cooling infrastructure, makes them feasible for large-scale applications and long-distance transport by mitigating the pressure loss and thermal stratification would otherwise be major concerns. However, ice slurry systems require refrigeration equipment that is more complicated and costlier than conventional chilled-water or ice block systems. The production of ice slurry typically involves the usage of advanced techniques such as supercooling devices. These units require precise control of nucleation and crystal growth to prevent blockages and maintain a stable ice fraction, increasing both design and operational complexity. The two-phase nature of ice slurry flow leads to elevated viscosity and higher-pressure drops, and that is why it requires stronger pumps and reinforced piping networks. The presence of ice particles also accelerates wear in valves, pumps, and heat exchangers. So, all of this is further raising equipment and maintenance costs. Motivated by these developments and technology advantages, especially the improved heat transfer rates, reduced pumping energy, and system adaptability, CO
2 hydrate technologies have increasingly shifted toward slurry-based formulations. By suspending CO
2 hydrate particles in a liquid medium, it can be helpful to overcome the limitations of bulk hydrate systems, such as poor heat extraction, slow formation, and instability, by also capitalizing on the same fluidity and thermal benefits that made ice and PCM slurries successful in refrigeration and district cooling applications [
9].
Gas hydrates are crystalline compounds composed of gas molecules encapsulated within a hydrogen-bonded water framework, that are formed under relatively high-pressure and low-temperature environments. An important group of follow-on developments based on well-established ice water mixes and microencapsulated PCM slurries are CO
2 hydrate slurries, where solid hydrate particles are suspended in a host fluid (typically water). The resulting two-phase or pseudo-three-phase mixture has improved flowability, enhanced heat-transfer potential, and adaptability to pumped systems. These slurries provide simultaneous utilization of latent heat and sensible heat storage. This made them superior to both conventional PCMs and sensible-only fluids in many thermal management systems [
10,
11].
CO
2 forms a structure I hydrate, where each unit cell has up to eight gas molecules trapped in water cages. The dissociation enthalpy of CO
2 hydrate is in the range of 350 to 520 kJ·Kg
−1 [
12], which is higher than that of ice. But it occurs at temperatures above freezing that is suitable for near-zero or slightly sub-zero thermal applications [
13].
CO
2 clathrate hydrate systems have attracted significant attention as promising candidates for CTES and thermal transport applications due to their relatively high volumetric energy density and favorable phase equilibrium characteristics. However, their practical deployment remains constrained by a combination of fundamental and engineering challenges, including slow formation kinetics, limited heat transfer rates, and difficulties associated with continuous operation under realistic thermofluid conditions. These limitations have driven extensive research into the use of nucleation promoters, surfactants, and thermal conductivity-enhancing additives, as well as the development of advanced reactor configurations and heat exchange systems. From a thermofluids perspective, CO
2 hydrate slurry systems represent a complex coupling of phase-change thermodynamics, nucleation kinetics, multiphase flow behavior, and heat and mass transfer processes. Hydrate formation is initiated through a nucleation process that can occur either heterogeneously at interfaces or homogeneously within the bulk liquid phase. The nucleation step is highly sensitive to system subcooling, dissolved gas concentration, interfacial area, and hydrodynamic conditions such as mixing intensity and shear rate. Chemical promoters such as tetrahydrofuran (THF), sodium dodecyl sulfate (SDS), and tert-butyl alcohol (TBA) are widely employed to reduce induction time and enhance nucleation reliability by modifying interfacial properties and gas dissolution behavior [
14,
15].
Despite these improvements, nucleation remains inherently stochastic and difficult to reproduce under dynamic, flow-based conditions, which poses a significant barrier for scalable systems. Following nucleation, hydrate crystal growth and agglomeration govern the evolution of the slurry microstructure. The resulting particle size distribution, morphology, and spatial dispersion directly influence both rheological behavior and thermal transport characteristics. CO
2 hydrate slurries are typically characterized by non-Newtonian flow behavior, with apparent viscosity strongly dependent on hydrate volume fraction, shear rate, and particle interactions. At low hydrate concentrations (below approximately 5–10 vol%), particles remain well dispersed, and the slurry exhibits near-Newtonian behavior with only modest increases in viscosity. As the hydrate volume fraction increases to intermediate levels (approximately 10–20 vol%), hydrodynamic interactions and particle clustering become significant, leading to shear-dependent viscosity and deviations from Newtonian behavior [
16].
At higher hydrate loadings (above approximately 20–30 vol%, the system approaches a densely packed regime where particle-particle interactions dominate, resulting in yield stress behavior, increased flow resistance, and a high risk of agglomeration and plugging [
17]. This transition imposes a fundamental limitation on slurry-based systems, as increasing hydrate fractions improve energy storage density but simultaneously degrades flowability and transport efficiency. The thermal transport characteristics of CO
2 hydrate slurries are similarly governed by the interplay between the dispersed solid phase and the continuous liquid phase. While increasing hydrate content can enhance the effective thermal capacity of the system, its influence on thermal conductivity and convective heat transfer is more complex. In laminar or transitional flow regimes, higher viscosity associated with increased hydrate loading reduces turbulence and can limit convective heat transfer coefficients, offsetting gains in thermal conductivity. Moreover, hydrate formation is an exothermic process, and inadequate heat removal during crystallization can lead to localized temperature rises that reduce the thermodynamic driving force for further hydrate growth. This coupling between heat release, transport resistance, and phase equilibrium represents a key bottleneck in hydrate-based systems [
18].
To address these limitations, various strategies have been explored to enhance both kinetics and transport properties. Surfactants and thermodynamic promoters have been shown to reduce induction time and increase gas uptake under specific conditions, although their effectiveness is highly dependent on concentration, reactor configuration, and hydrodynamic regime. Similarly, the incorporation of nanoparticles such as Cu, CuO, Al
2O
3, SiO
2, and carbon nanotubes (CNTs) has been investigated as a means to improve nucleation rates and enhance effective thermal conductivity [
15].
Proposed mechanisms include increased surface area for heterogeneous nucleation, improved micro-convection due to Brownian motion, and the formation of conductive percolation networks. However, these effects are not universally beneficial. Experimental studies have shown that enhancements in nucleation kinetics or thermal conductivity do not necessarily translate into improved overall system performance, particularly when increased viscosity or particle aggregation offsets these gains. In addition, issues related to long-term stability, sedimentation, toxicity, and scalability remain largely unresolved, limiting the applicability of such hybrid hydrate–nanofluid systems in practical applications.
Beyond material-level modifications, significant challenges arise at the system level, particularly in the context of continuous hydrate slurry production and transport. Maintaining the thermodynamic conditions required for hydrate formation such as high pressure, low temperature, and controlled gas-liquid mixing under continuous operation is inherently complex. Flow systems must simultaneously ensure sufficient heat removal, uniform mixing, and stable particle suspension, while avoiding sedimentation, agglomeration, and channel blockage. These competing requirements often lead to operational instability, making it difficult to sustain steady-state production and transport of hydrate slurries.
To overcome these challenges, advanced reactor designs such as NETmix reactors have been proposed. Unlike conventional stirred tank reactors that rely on localized mixing from impellers, NETmix systems utilize a network of flow paths to create distributed mixing throughout the reactor volume. This design enhances gas-liquid contact, improves uniformity of hydrate formation, and reduces the likelihood of particle agglomeration and sedimentation. By maintaining more homogeneous flow conditions, NETmix reactors provided improved control over slurry properties and represent a promising approach for continuous hydrate production [
19]. Even with improved mixing, achieving a balance between heat removal, particle suspension, and hydrate yield remains a critical challenge.
In parallel, microchannel heat exchangers have emerged as a promising solution for addressing the thermal management limitations of hydrate systems. Due to their extremely high surface-to-volume ratio, microchannels enable rapid heat transfer and efficient removal of the exothermic heat generated during hydrate formation. This allows for better control of local temperature profiles, helping to maintain the thermodynamic driving force for crystallization and prevent the formation of thermal hotspots. Additionally, the confined geometries in microchannels promote higher shear rates and more uniform velocity distributions, which can assist in maintaining particle suspension and reducing sedimentation. These characteristics make microchannel systems particularly attractive for applications requiring compact, high-performance thermal management and continuous operation [
20,
21].
The use of microchannel systems introduces new challenges associated with slurry handling at small scales. The narrow channel dimensions make the system highly sensitive to particle aggregation and deposition, increasing the risk of clogging and flow blockage. Furthermore, the non-Newtonian rheological behavior of hydrate slurries can lead to unpredictable pressure drops and flow instabilities, particularly under high solid loading conditions. These issues necessitate precise control of slurry properties and operating conditions, as well as the integration of advanced monitoring and control systems to ensure reliable operation [
22,
23].
Despite the extensive body of literature on hydrate formation kinetics, additives, and reactor design, a critical gap remains in the integrated understanding of CO2 hydrate slurries from a thermofluid systems perspective. Existing studies evaluate performance metrics such as induction time reduction, gas uptake, or thermal conductivity enhancement in isolation, without considering the coupled interactions between nucleation behavior, rheology, heat transfer, and flow resistance. In practical systems, these factors are inherently interdependent, and improvements in one aspect may lead to unintended consequences in another. For example, increasing hydrate volume fraction enhances energy storage capacity but significantly increases viscosity and pressure drop, limiting transportability. Similarly, additives that accelerate nucleation may promote particle agglomeration or destabilize the slurry during long-term operation.
This limitation is further compounded by the way prior research has been framed. Much of the literature emphasizes application-level configurations such as microchannel heat exchangers, while fundamental parameters governing hydrate slurry behavior have not been sufficiently highlighted. Among these, hydrate volume fraction emerges as a primary governing variable that simultaneously controls flow characteristics, thermal transport, and storage capacity. Despite its central role, it is rarely treated as a unifying parameter across studies, leading to fragmented conclusions that are difficult to translate into system design.
This work addresses these limitations by presenting a comprehensive, design-oriented review of CO2 hydrate slurry systems that explicitly links fundamental phenomena with system-level performance. Unlike prior reviews that focus primarily on kinetics or material enhancements, this study integrates nucleation physics, multiphase flow behavior, and thermal transport with reactor and heat exchanger design considerations. Particular emphasis is placed on hydrate volume fraction as a governing parameter that couples energy storage capacity with flowability and heat transfer performance. In addition, the review critically evaluates the system-dependent effectiveness of additives and highlights the trade-offs associated with their use. By bridging the gap between laboratory-scale observations and engineering implementation, this work aims to provide a framework for the development of scalable, efficient, and reliable CO2 hydrate slurry systems for real-world CTES applications.
2. CO2 Hydrate: Formation and Structure
Gas hydrates are crystalline clathrates in which hydrogen-bonded water molecules assemble into polyhedral cages that can encapsulate gas molecules. The most common structural frameworks are shown in
Figure 1 which are structure I (sI), structure II (sII), and structure H (sH). Structure I consists of 46 water molecules per unit cell, forming two 5
12 small cages and six 5
126
2 large cages. This framework is typically stabilized by small guest molecules such as CH
4 or CO
2. Structure II is larger, containing 136 water molecules per unit cell, with sixteen 5
12 cages and eight 5
126
4 cages; it accommodates larger guest molecules such as for example propane or iso-butane. Structure H is rarer, requiring a combination of small and large guest molecules, and features a hexagonal lattice with three 5
12 cages, two 4
35
66
3 cages, and one large 5
126
8 cage. Under pure CO
2-H
2O conditions, CO
2 crystallizes exclusively in the sI lattice, with large cages nearly fully occupied and small cages partially filled, leading to hydration numbers between 5.8 and 6.2 depending on temperature and pressure [
24].
The thermodynamic framework for hydrate stability is conventionally described by the van der Waals-Platteeuw (vdW-P) model that links cage occupancies to guest fugacity and host lattice chemical potentials. This solid-solution model has been refined to account for multiple occupancy and guest–guest interactions. In the case of CO
2 hydrate, this model successfully predicts both cage filling and equilibrium conditions when combined with modern equations of state for CO
2 solubility. The sI framework is particularly favored by CO
2 due to its molecular size, which fits optimally into the 5
126
2 cages, producing near-unity occupancy in the large cages while allowing only partial filling in the smaller 5
12 cages [
26,
27].
Phase equilibrium measurements confirm that CO
2 hydrates are stable under conditions near 271.6 K and 1.044 MPa, where the four-phase coexistence of vapor, liquid water, ice, and hydrate occurs. These equilibrium points are consistent with laboratory data from stirred reactors. The presence of salt shifts the stability envelope to lower temperatures and higher pressures due to activity suppression of water [
28].
The dissociation enthalpy of CO
2 hydrate is of particular interest when evaluating hydrate slurries for cold thermal energy storage. The latent heat of dissociation of CO
2 hydrate is in the range of 55–62 kJ·mol
−1 of guest, corresponding to approximately 350 to 520 kJ·kg
−1 of water, depending on cage occupancy [
1,
29].
In comparison, the latent heat of fusion for ice/water is 333 kJ·kg
−1. This means that per unit mass of water, CO
2 hydrates can store equal or higher amounts of latent heat than ice, especially when near-complete cage occupancy is achieved. CO
2 hydrate slurry combines this high enthalpy with favorable transport properties by facilitating ease of pumping as a cold fluid, unlike solid ice slurries, which require mechanical agitation to suspend ice particles [
30].
Experimental calorimetric studies shows that CO
2 hydrate slurries possess an enthalpy of dissociation approximately 20–25% higher than comparable ice slurries under equivalent volumetric fractions [
31].
Differential scanning calorimetry (DSC) and T-history method measurements consistently report this advantage of hydrates as more efficient cold thermal energy carriers. The enhancement originates not only from the hydrate dissociation enthalpy but also from the higher gas solubility in water, which sustains hydrate stability at moderately elevated temperatures compared to ice. These properties make CO
2 hydrate slurries promising candidates for refrigeration, district cooling, and air-conditioning systems where compact and efficient energy storage is required [
32].
Nucleation of CO
2 hydrates remains highly stochastic, with induction times spanning orders of magnitude under seemingly identical conditions. Classical nucleation theory adapted for hydrates describes this behavior by relating the free energy barrier to supersaturation (guest fugacity) and interfacial free energy. Once nucleated, hydrate growth proceeds through transport of CO
2 across the water-hydrate interface, and this is always enhanced by interfacial stirring. Advanced techniques including Raman spectroscopy, NMR, neutron diffraction, and X-ray diffraction converge on the structural picture of sI CO
2 hydrate with full occupancy in large cages and variable filling of the smaller cages. In the sI hydrate lattice, each unit cell consists of eight cages typically two small pentagonal dodecahedra (5
12) and six larger tetrakaidekahedral cages (5
126
2). Because the linear CO
2 molecule fits more comfortably into the larger cages, these are almost always fully occupied, while the smaller cages are often only partially filled or even left vacant. This uneven distribution arises from differences in the interaction energy between CO
2 and the water framework, as well as from temperature and pressure conditions that govern molecular stabilization within the lattice. As a result, the formed hydrate departs from the ideal stoichiometric ratio, since the crystalline structure can remain stable even when not all cavities are filled. The extent of cage occupancy directly affects the macroscopic behavior of the solid changes in occupancy modify the unit-cell dimensions, density, and bulk modulus, and are reflected in measurable shifts in the lattice constant and thermal expansion. These microscopic variations in molecular arrangement thus bridge the gap between local structural ordering and the observable thermophysical properties of CO
2 hydrates [
13].
Because guest molecules do not uniformly occupy all hydrate cages under practical formation conditions, deviations from ideal stoichiometry are frequently observed. These occupancy variations yield hydration numbers typically higher than the ideal 5.75, consistent with measured lattice parameters and observed thermal expansion [
33].
A distinct feature of CO
2 hydrate is its metastable preservation behavior on warming. Under near-atmospheric conditions, only a small fraction of gas is released until the system approaches 271 K, at which point dissociation occurs sharply. This behavior is linked to the formation of a protective ice layer and mass-transfer limitations within the hydrate–ice composite shell. Such self-preservation enhances the practical viability of CO
2 hydrate slurries as cold energy carriers, since thermal losses during short-term storage or transport are minimized compared to ice slurries that undergo continuous melting at temperatures above 273 K [
34].
Pure carbon dioxide (CO
2) usually forms a type of hydrate called structure I (sI). When larger molecules like tetrahydrofuran (THF) or propane are added, they can change the crystal to structure II (sII), which is more stable for these big molecules. In gas mixtures that contain CO
2 together with methane (CH
4) or nitrogen (N
2), the hydrate still keeps the sI form. However, the different gases don’t fill the cages equally and they spread out depending on their size and pressure (fugacity). The bigger cages are usually almost completely filled, while the smaller ones can be partly filled. This uneven filling affects both the stability of the hydrate and how much energy it releases or absorbs when it breaks down. To understand these details better, a Raman spectroscopy is used to study the gas molecules inside the cages and combine the results with van der Waals-Platteeuw (vdW-P) [
35] thermodynamic modeling. Together, these tools help explain how mixed-gas hydrates store and release energy, which is important for designing effective hydrate-based thermal storage systems [
36].
The dissociation enthalpy of CO2 hydrate must be compared with ice only after the normalization basis is clearly defined. In the literature, the enthalpy of CO2 hydrate dissociation is commonly reported as 350–520 kJ·Kg−1 of guest CO2, while the hydration number of sI CO2 hydrate varies with cage occupancy and is typically taken between 5.75 for full occupancy and 7.67 when only the large cages are occupied; experimental values around 5.6–6.6 are also widely reported.
Using the relation,
this corresponds to roughly 398–599 kJ kg
−1 of water incorporated into hydrate, which is higher than the latent heat of fusion of ice (333 kJ·kg
−1) when both are expressed on a water-phase basis. However, if the same hydrate dissociation enthalpy is normalized by the total hydrate mass rather than the water mass alone, the equivalent value is only about 302–420 kJ kg
−1 hydrate, showing that the apparent advantage depends strongly on the selected basis [
13,
29].
For slurry applications, the comparison becomes more restrictive because the relevant metric is not the enthalpy of the pure hydrate phase, but the effective cold storage capacity of the entire slurry, which includes hydrate particles, free water, and dissolved gas. Therefore, a direct statement that CO
2 hydrate slurry has a universally higher dissociation enthalpy than ice slurry is too broad. A more accurate interpretation is that the hydrate phase can provide a higher phase-change enthalpy than ice on a water-converted basis, while the slurry-level advantage depends on hydrate fraction, phase composition, operating pressure, and the normalization method used in the calorimetric measurement. An overall dissociation enthalpy of approximately 507 kJ·kg
−1 of initial water has been reported for CO
2 hydrate–ice mixtures, reflecting the combined contributions of hydrate decomposition and residual ice melting rather than an intrinsic property of the hydrate phase alone. This distinction is critical when interpreting thermal storage performance. Comparisons with ice slurry systems should therefore be presented on a consistent basis, such as per kg of carrier water, per kg of total slurry, or per unit slurry volume, with the hydration number and hydrate volume fraction explicitly specified [
37].
6. Thermal Conductivity Enhancement with Nanoparticles
CO
2 hydrate slurries are attractive working media for cold thermal energy storage and gas separation, but their performance is constrained by slow formation kinetics and the difficulty of removing the heat released during crystal growth within a circulating solids-bearing fluid [
85].
While conventional chemical promoters such as tetrahydrofuran, cyclopentane, tetrabutylammonium salts, light hydrocarbons, and surfactants like SDS or Tween 80 can accelerate formation process, their industrial use is tempered by volatility, environmental and toxicity concerns, and downstream separation burdens, motivating interest in solid-phase promoters like nanoparticles that can couple kinetic promotion with improved heat transport in the slurry phase [
86,
87].
Hydrate formation is exothermic, as crystals grow, local temperature rises reduce the thermodynamic driving force and can stall conversion, so the practical rate of CO
2 hydrate slurry production is strongly tied to how fast the suspension can conduct and convect the released heat away from the formation front [
85]. Nanoparticle dispersions (nanofluids) provide a route to raise the effective thermal conductivity of the continuous phase, with numerous measurements across Al
2O
3, Cu, CuO, SiO
2, and carbonaceous particles showing conductivity gains that scale, within stability limits, with particle loading and often with temperature in the operating range relevant to hydrate systems [
88,
89].
In parallel, high-conductivity carbon frameworks show the fundamental potential of graphitic fillers to establish percolated heat paths, underscoring why carbon-based nanoparticles frequently outperform oxides at comparable volume fractions [
90,
91].
Despite the empirical gains, predicting the thermal behavior of nanoparticle-laden hydrates remains challenging because dispersion stability, pH, ionic strength, surfactant package, and shear history modulate both structure and transport at multiple scales [
89].
Competing and possibly concurrent explanations like Brownian motion-assisted micro convection, interfacial liquid layering, percolation/clustering, ballistic phonon contributions across particle-liquid interfaces, and electrostatic effects are each supported to varying degrees depending on the chemistry and flow regime, and consensus on a single dominant mechanism has not emerged for hydrate slurries [
15,
89].
This mechanistic uncertainty complicates a priority nanoparticle selection and dose optimization for a given reactor or loop geometry. Within CO
2 hydrate slurries specifically, nanoparticles can shorten induction times and increase gas uptake, yielding higher apparent formation rates and greater conversion under otherwise identical conditions [
54].
Commonly used graphene oxide is a representative case: experiments at 279 K and 3–5 MPa reported induction time reductions of 53–74% and gas consumption increases of 5–16% relative to nanoparticle-free baselines, with performance sensitive to dose and pressure. Synergy with conventional kinetic promoters is common; combining graphene-based nanoparticles with SDS has repeatedly enhanced CO
2 hydrate formation, indicating that surfactants aid both dispersion stability and interfacial mass transfer while the nanoparticles provide nucleation sites and heat-transfer pathways. The effect of nanoparticles must be evaluated together with slurry rheology because flowability determines pump work, exchanger coefficients, and the propensity for agglomeration in recirculating loops [
92].
Recent in-loop studies of CO2 hydrate slurries report divergent behaviors from shear-thinning to apparent shear-thickening depending on solids fraction, particle/host chemistry, and measurement method, which makes generalization risky without system-specific testing.
Surfactants remain the primary handle on early-stage viscosity, but nanoparticle addition interacts with surfactant type and concentration, so combinations that accelerate kinetics can also either delay or hasten viscosity rise, with consequences for pressure drop and heat-exchange fouling in continuous service [
10].
Beyond kinetics, nanoparticles have been shown to increase the effective thermal conductivity of hydrate-bearing systems themselves, complementing the enhancement of the carrier liquid and helping to evacuate formation heat from the crystal-liquid interface within the slurry microstructure [
93].
Carbonaceous particles are particularly effective in this role due to their high intrinsic conductivity and tendency to form connected micro-networks, an effect consistent with broader nanofluid literature that ranks graphitic fillers among the strongest conductivity enhancers at low volume fractions [
90,
91]. As a result, improved thermal conductivity helps maintain more uniform temperature distribution within the reactor or flow loop during rapid hydrate formation. This supports stable growth and improves overall process efficiency [
93].
Real-world implementation requires attention to dispersion stability because nanoparticles in cold, high-shear, saline environments can agglomerate and sediment, degrading both thermal properties and kinetics over time. Stabilization strategies include coupling nanoparticles with surfactants or polymeric dispersants and, in some systems, using ionic-liquid modifiers to maintain small, well-wetted aggregates under operating temperatures and shear rates typical of hydrate slurries. Effective dosages reported for hydrate promotion are modest tens of ppm to 0.1 wt% for many carbon and oxide nanoparticles with diminishing returns or outright inhibition when concentrations are pushed high enough to trigger clustering or mass-transfer blockage. Because these windows are narrow and system-specific, dose-response screening under the intended hydrodynamic and thermal conditions is an essential part of formulation. The advantages of nanoparticle-assisted CO
2 hydrate slurries can be summarized as faster formation, higher gas uptake, and improved thermal management at comparatively low solid loadings, all of which support compact equipment and shorter cycle times [
54].
The countervailing risks which need to be considered are increased viscosity and pressure drop, agglomeration and sedimentation under transients, and sensitivity to the exact pairing of particle chemistry with surfactant package and water chemistry, which together can erode the expected net gain in heat-transfer coefficients in long-duration operation. These trade-offs argue for integrated optimization by balancing kinetics, thermal transport, and rheology rather than pursuing any single metric in isolation [
92].
The most promising route to practical deployment appears to be hybrid formulations that combine a low-dose, high-conductivity nanoparticle (often carbon-based) with a surfactant system tuned for dispersion stability and controlled agglomeration, validated in pilot-scale rigs that capture the shear histories and thermal shocks of real loops. Advances in understanding structure-property links particularly the roles of interfacial layering, clustering/percolation, and electrostatic interactions in cold, saline, multiphase flow should enable mechanistic selection of particle type, size, and surface chemistry rather than empirical trial-and-errors.These are coupled with loop-scale rheology and heat-transfer measurements, CO
2 hydrate slurries formulated with nanoparticles have a credible further development and implementation path from laboratory demonstrations to robust, clean-energy thermal storage and separation processes [
93].
In addition to oxides and carbon-based nanostructures, metallic nanoparticles such as copper (Cu), silver (Ag), and gold (Au) have attracted attention due to their superior intrinsic thermal conductivities (200–400 W·m
−1·K
−1) [
94]. Dispersions of Cu nanoparticles in water have demonstrated up to 20–25% thermal conductivity enhancement at loads below 0.1 wt% [
95], and Ag-based nanofluids have shown similar gains at even lower concentrations. These improvements arise from both the formation of conductive percolation networks and enhanced phonon transport across particle-fluid interfaces that aid in dissipating the exothermic heat of hydrate formation. Despite these advantages, metallic nanoparticles present challenges including oxidation, surface instability, and agglomeration under hydrate-forming conditions. Recent work shows hybrid formulations combining trace metallic nanoparticles with stabilizing oxides or carbon-based fillers can yield synergistic improvements in both thermal conductivity and dispersion stability by producing a balanced pathway for hydrate slurry applications [
96].
Table 2 summarizes reported work on improving thermal conductivity in gas hydrate systems using nanoparticles and nanofluids. Different additives such as metal nanoparticles, carbon nanotubes, and metal oxides show clear increases in effective thermal conductivity across different operating conditions. This shows the potential of nanomaterials to improve heat transfer in hydrate systems.
Nanoparticles have been widely investigated as kinetic promoters for hydrate formation because they can simultaneously improve heterogeneous nucleation and enhance heat transfer within the hydrate-water system. However, the magnitude of these improvements varies significantly depending on nanoparticle type, concentration, and dispersion stability. Experimental studies report that the addition of nanoparticles such as graphene oxide (GO), graphite, CuO, or SiO
2 typically increases the effective thermal conductivity of the base fluid by approximately 10–35% for concentrations between 0.01 and 0.1 wt%, primarily due to the high intrinsic conductivity of the particles and micro-scale convection induced by Brownian motion. This enhancement can improve heat removal during hydrate crystallization, which is particularly important because hydrate formation releases large amounts of heat that may otherwise inhibit further nucleation [
99,
100].
Beyond thermal conductivity effects, nanoparticles also act as heterogeneous nucleation sites that reduce the induction time for hydrate formation. For example, Yan et al. reported that graphene oxide nanoparticles reduced induction time by approximately 53–74% compared with pure water under conditions of 279 K and 3–5 MPa, while increasing CO
2 gas consumption by 5–16% [
54].
Similarly, experiments using CuO nanoparticles showed induction time reductions of roughly 30–50% depending on particle loading and mixing conditions. In some cases, hybrid promoter systems combining nanoparticles with surfactants have demonstrated even stronger effects [
15].
Li et al. reported that a mixed promoter system consisting of 0.005 wt% GO and 0.2 wt% SDS shortened hydrate formation time by nearly 70% compared with pure water and increased gas uptake by approximately 11%. These results indicate that nanoparticle promotion is typically most effective within a relatively narrow concentration range. At higher concentrations, particle agglomeration or increased slurry viscosity may reduce gas-liquid mass transfer and offset the benefits of enhanced thermal conductivity [
101].
7. Thermophysical Properties of CO2 Hydrate Slurries
The thermophysical behavior of CO2 hydrate slurries has an influence on their performance in cold thermal energy storage (CTES) and refrigeration systems. Among the key parameters, density, specific heat, and thermal conductivity determine both storage capacity and transport behavior. These properties are highly dependent on slurry composition, particularly the hydrate volume fraction, particle dispersion, and presence of additives. Understanding how these factors influence thermal performance is essential for the effective design and operation of hydrate-based systems.
7.1. Density and Specific Heat
Nanoparticles rarely change the intrinsic properties of the CO
2 hydrate crystal; rather, they shift the slurry’s composition and microstructure, which are exactly what determine density and specific heat. The hydrate phase is denser and has a lower heat capacity than liquid water, so anything that increases the hydrate volume fraction, ϕ
h, nudges the slurry toward higher density and lower sensible heat capacity. For CO
2 hydrates, the phase density is 1.09–1.11 g·cm
−3 near 0–5 °C, and many experimental and modeling papers now converge on a specific heat in the 2.1–2.7 kJ·kg
−1·K
−1 range both clearly different from water (4.18 kJ·kg
−1·K
−1) [
102].
Now nanoparticles produce measurable improvement on density. At fixed temperature and pressure, the slurry density can be approximated by a volume-weighted mixture rule,
where,
is the carrier liquid (water or brine),
the nanoparticle density. Because
for common oxides and carbons (e.g., Al
2O
3, SiO
2, graphite) exceeds
any non-zero nanoparticle volume fraction
increases
slightly. In practice, however,
is tiny (10–1000 ppm by mass in CTES work), so the direct density increase from the particles is marginal. The indirect effect dominates carbon-based nanoparticles (graphite, graphene oxide) and certain metal oxides consistently accelerate CO
2-hydrate nucleation and growth, raising
by increasing gas consumption at a given residence time. For example, graphite nanoparticles cut induction times by 80% and raised maximum CO
2 uptake by 13% in Energy & Fuels experiments, while graphene-oxide promoters shortened induction by 53–74% and increased gas consumption by 5–16% in Energies both at sub 0.1 wt% loadings [
103]. A higher
pushes the mixture toward the hydrate’s 1.10 g·cm
−3 density [
104], which is why loop and rig studies report density climbing with hydrate formation.
7.2. Effective Thermal Conductivity of CO2 Hydrate Slurry
The thermal transport behavior of CO
2 hydrate varies from that of crystalline ice, even though both consist of hydrogen-bonded water frameworks. In clathrate hydrates, guest molecules trapped within the water cages create vibrational degrees of freedom that strongly interact with lattice phonons. This produces resonant scattering, and reduces phonon mean-free paths giving rise to the nearly temperature-independent glass-like conductivity that characterizes hydrate structures. The low lattice conductivity is mainly due to energy exchange between localized guest vibrations and the host lattice acoustic modes, which suppresses collective phonon propagation through the framework. Early measurements of hydrate conductivity showed values much lower than those of ice. Experiments in the 265–280 K range reported conductivities between 0.45 and 0.70 W m
−1 K
−1, whereas ice Ih at 273 K has about 2.2 W m
−1 K
−1 [
105].
Later tests on compact methane hydrate with approximately 90% occupancy and minimal porosity gave 0.68 ± 0.01 W m
−1 K
−1. It indicates that the porosity reduction only marginally increases thermal conductivity because the dominant heat-transfer limitation arises from molecular scattering rather than structural voids [
106].
The measured thermal diffusivity of (2–3) × 10
−7 m
2 s
−1 shows this correlation between conduction and stored heat capacity. Some computational studies show the origin of guest-dependent conductivity differences. Non-equilibrium molecular-dynamics simulations of structure-I hydrates found that methane hydrate has about 15–20% higher conductivity than CO
2 and xenon hydrates across the 30–260 K range [
107].
The heavier and larger CO
2 molecules enhance lattice distortion and anharmonic scattering, shortening phonon relaxation times. Comparisons between empty, partially filled, and fully occupied frameworks revealed that empty hydrates behave similarly to ice Ih but with smaller absolute thermal conductivity value [
108].
Pressure effects have been studied up to approximately 50 MPa, showing only a 10–15% increase in thermal conductivity with compression. The influence of external pressure is therefore secondary, since phonon scattering through guest-host coupling dominates. Within the typical formation range of 5–7 MPa used in laboratory and pilot systems, pressure has little measurable effect on the intrinsic heat-transfer coefficient of CO
2 hydrate. Using transient hot-wire and plane-source techniques confirms the low and weakly temperature-dependent nature of hydrate conductivity. For semiclathrate hydrates such as TBAB and TBAC, values between 0.38 and 0.44 W m
−1 K
−1 were obtained in the 223–303 K interval with ±0.7% uncertainty. These values are roughly five times lower than ice and represent a close analogue to CO
2 hydrate because both share similar cage dynamics. The nearly constant
with temperature shows that the hydrate network behaves as a strongly disordered medium for phonon transport, comparable to molecular glasses [
109].
Thermal conductivity measurements of hydrate samples can be affected by residual unfrozen water near the probe, ice contamination, and microstructural heterogeneity such as micro-pores. If unfrozen water remains near the probe during measurement, it can produce an artificial jump near 273 K due to the four-fold difference between liquid and ice conductivities. Directional solidification during measurement forming hydrate from the bottom upward prevents such anomalies and ensures stable reading. The high reproducibility achieved under these conditions demonstrates the importance of microstructural control in obtaining intrinsic hydrate property data [
110].
For system design, hydrate slurries are more relevant than static solids. CO
2-hydrate slurry has dispersed solid hydrate particles in a carrier fluid (usually water, brine, or glycol). The effective thermal conductivity
of such a two-phase mixture depends on the intrinsic conductivities of both phases, particle volume fraction (ϕ), particle morphology, and the interfacial thermal resistance between solid and liquid phases. Because both CO
2 hydrate and water have comparable
values around 0.5–0.6 W m
−1 K
−1, the contrast is small. Analytical estimates using Maxwell-Eucken theory predict that increasing the solid fraction up to 30% only raises
marginally to about 0.55–0.57 W m
−1 K
−1. Flow-cell experiments on CO
2 and mixed-gas hydrate slurries confirm that thermal resistance is concentrated at the particle-liquid interface and within the dispersed layer rather than in the solid itself. The limiting factor in heat transfer during hydrate growth and melting is thus the interfacial contact conductance. As solid loading increases, conduction paths remain discontinuous, and convective renewal dominates over lattice conduction. Even at high hydrate fractions,
stays close to the carrier fluid value unless firm mechanical compression is used to reduce interfacial voids [
111].
Molecular-scale analyses of CO
2 hydrate under partial occupancy or external electric fields reveal an even lower K (0.3 W m
−1 K
−1), since distortion of the lattice further enhances scattering and shortens energy-correlation times of vibrational modes. This result supports the interpretation that CO
2 hydrate behaves like an amorphous solid with respect to heat transport [
112].
In hydrate-bearing sediments, the same physical principles apply macroscopically. When hydrate replaces pore water, overall conductivity decreases because
hydrate <
quartz. Laboratory studies on synthetic CO
2/CH
4 hydrates in sand report effective values of 1.2–1.6 W m
−1 K
−1 at 50% saturation, which are lower than equivalent water-saturated sediments. Thus, hydrate formation in geological formations acts as a thermal barrier by restricting heat flow during gas exchange or dissociation processes [
113].
7.3. Rheological Properties and Flow Behavior
Because of high energy density, CO
2 hydrate slurries are considered for thermofluid and secondary refrigerant applications. The flow behavior of CO
2 hydrate slurries is governed by the way solid hydrate particles form, collide, and reorganize within the surrounding liquid. As hydrates grow, the slurry gradually shifts from a simple liquid to a complex suspension whose resistance to flow depends on both particle concentration and the forces acting between particles. For this reason, the rheology of hydrate slurries cannot be reduced to a single viscosity value; instead, it evolves continuously with formation progress, operating conditions, and shear history [
114].
A wide range of experimental systems has been used to characterize CO
2 hydrate slurry rheology, and these setups collectively show how strongly measurement conditions influence the interpretation of flow behavior. Early laboratory configurations relied on stainless-steel flow loops combined with capillary-based viscosity estimation. These small-volume systems with internal diameters of 7–10 mm provide good source to track hydrate formation and quantify pressure-drop responses as the solid phase grew. Their results consistently showed that even a small increase in hydrate content leads to rapid increases in resistance to flow [
115].
Later flow-loop studies expanded the range of hydrate volume fractions tested and demonstrated how quickly a suspension transitions from a freely flowing liquid to a structured and increasingly resistant slurry. These experiments generally operated between 2.3 and 3.0 MPa and temperatures near 275–278 K, revealing clear shear-dependent behavior once the hydrate fraction reached roughly 10–15 vol% [
116].
More advanced systems incorporated both dynamic flow-loops and mechanically agitated tanks. These arrangements allowed the slurry to be exposed to controlled shear while simultaneously monitoring pressure drops and flow stability. Across hydrate contents ranging from dilute to highly concentrated, the data showed that shear thinning becomes progressively stronger as the solid phase builds up, indicating the formation and subsequent breakup of particle networks under shear [
16].
Figure 6 shows the high-pressure flow loops introduced in later work extended slurry studies into multiphase liquid environments, including cases where hydrates formed simultaneously in water and hydrocarbon phases. These systems highlighted that slurry rheology is not governed solely by solid fraction but also by interfacial behavior between immiscible phases. Under pressures near 3 MPa, mixed liquid environments exhibited distinct aggregation patterns and greater sensitivity to shear history [
117].
Chemical additives form another major factor governing slurry flowability. Surfactants such as Caflon, Tween 80, OP-10, SDS, and similar compounds reduce particle-particle attraction by imposing steric or electrostatic repulsion. Flow-loop and rheometer tests at pressures of 2.3–3.5 MPa show that these additives suppress agglomeration and significantly lower apparent viscosity, even when hydrate fraction remains unchanged [
48].
The interfacial tension (IFT) between CO2 hydrate particles and the surrounding liquid phase plays a decisive role in how hydrate slurries behave during flow. Low IFT values promote particle-particle attraction, making the solids more likely to cluster and form dense agglomerates. This aggregation strongly influences viscosity, yield stress, and overall flow stability. It directly affects whether a slurry remains mobile or transitions into a more structured network. Measurements of CO2 hydrate IFT in the literature shows considerable variation. Values reported range from approximately 1–4 mN/m in some systems to above 30 mN/m in others. These discrepancies came from differences in measurement techniques, system composition, pressure-temperature conditions, and whether additives such as TBAC, APG, or SDS were present. As a result, IFT must be interpreted in the context of the experimental setup rather than as a universal material property.
To provide a clearer comparison across systems, the range of reported IFT values is summarized in
Table 3. This compiles measurements from water, brine, and additive-containing systems under different thermodynamic conditions.
7.4. Viscosity Models and Slurry Flow Behavior
Several empirical correlations have been proposed to describe the apparent viscosity of CO2 hydrate slurries flowing in pipelines under laminar conditions. These models are derived primarily from capillary viscometer measurements in closed flow loops and relate the apparent viscosity to the hydrate volume fraction and shear rate. Although the mathematical forms are different, all the models are rooted in experimental pressure-drop data and show the evolving microstructure of hydrate particles suspended in an aqueous phase.
For CO
2 hydrate slurries formed in pure water, the apparent viscosity has been expressed as a strong function of hydrate volume fraction and shear rate. The proposed correlation takes the form
:
This formulation captures the rapid increase in viscosity even at moderate hydrate loadings. The first term represents the contribution of dispersed hydrate particles at low shear rates, while the second term accounts for shear-dependent restructuring of hydrate aggregates. The strong dependence on reflects the onset of particle-particle interactions and early agglomeration observed experimentally in hydrate-water slurries
A simplified exponential expression has also been proposed for CO
2 hydrate slurries in water [
16],
This model emphasizes the exponential sensitivity of viscosity to hydrate concentration while retaining shear-rate dependence. The decreasing exponent on shear rate indicates shear-thinning behavior at higher hydrate fractions, consistent with particle alignment and breakup of loose agglomerates under increasing flow intensity
When tetra-n-butyl phosphonium bromide (TBPB) is present, the apparent viscosity follows a different trend [
45]:
In this case, the model reflects the combined influence of hydrate fraction and the stabilizing effect of TBPB on particle dispersion. The positive exponent on shear rate indicates shear-thickening behavior, attributed to the formation of more compact hydrate clusters under flow. This behavior contrasts with hydrate-water systems and highlights the strong role of additives in modifying slurry rheology.
For CO
2 hydrate slurries formed in the presence of sodium dodecyl sulfate (SDS), the apparent viscosity is given by
:
This correlation shows a reduced sensitivity of viscosity to hydrate fractions compared with additive-free systems. The negative shear-rate exponent confirms shear-thinning behavior over the investigated range. The reduced viscosity increase at high hydrate fractions is consistent with the anti-agglomeration effect of SDS, which limits the formation of large hydrate clusters and improves slurry flowability
For hydrate slurries stabilized using Span-80, the apparent viscosity is expressed as [
117]:
This polynomial-exponential structure reflects the complex balance between particle stabilization and increasing solid content. At low hydrate fractions, viscosity remains relatively moderate, while higher fractions lead to pronounced non-Newtonian behavior. The formulation highlights the nonlinear role of surfactant concentration on hydrate particle interactions and flow resistance.
To address a broad range of hydrate concentrations, a piecewise formulation has been proposed [
92]:
This formulation distinguishes two rheological regimes. Below the transition concentration, hydrate particles remain relatively dispersed, leading to weak shear dependence. Beyond this threshold, stronger particle networks develop and produce higher apparent viscosities and more pronounced non-Newtonian effects. The transition reflects a structural change in the slurry rather than a purely hydrodynamic effect. The most direct contribution to increased viscosity and yield stress in hydrate slurries is the hydrate volume fraction, typically ranging from 5 to 30 vol% in practical systems. At lower concentrations (<10 vol%), hydrate particles are dispersed sufficiently to allow free movement of the liquid phase around them, leading to modest increases in effective viscosity and Newtonian-like flow behavior. However, as the hydrate fraction increases, interparticle spacing diminishes, enhancing hydrodynamic interactions and promoting short-range ordering or clustering effects.
Sahu et al. conducted high-pressure rheological experiments and observed that increasing the hydrate volume fraction from 10% to 30% led to a nonlinear, near-exponential increase in effective viscosity, nearly quadrupling at a constant shear rate. This behavior arises due to steric hindrance, increased excluded volume effects, and the formation of percolating particle networks that resist deformation. These observations align with colloidal suspension theory, where critical packing thresholds mark the transition to yield stress and non-Newtonian shear-thinning flow. In addition to impacting viscosity, hydrate loading also determines whether the slurry exhibits plugging tendencies, wall slip, or shear banding, particularly in narrow channel geometries. Therefore, careful control of hydrate formation kinetics and fraction is essential for ensuring stable and predictable flow, particularly in continuous systems such as pipelines and looped cooling networks. The size, shape, and surface properties of hydrate particles significantly influence both the static and dynamic rheology of the slurry. Fine, and spherical particles promote lower viscosity due to better fluid accommodation and reduced drag. In comparison, irregular or large agglomerated particles increase the hydrodynamic radius and disrupt flow symmetry and this leads to higher energy dissipation under shear [
10].
The presence of surfactants such as SDS can reduce particle agglomeration by imparting electrostatic repulsion, thereby maintaining smaller effective particle diameters and improving dispersion. However, such additives may also alter interfacial tension and modify lubrication layers between particles, introducing a secondary influence on rheological characteristics [
124]. CO
2 hydrate slurry is a multiphase flow system where solid hydrate particles form directly inside an aqueous phase under elevated pressure and low temperature. The solid phase is generated in situ through gas-liquid phase transformation and remains thermodynamically active during transport. Hydrate particles that are grown dissociate and evolve as local pressure temperature and shear conditions change. This dynamic behavior produces continuous variation in particle size surface roughness and interparticle bonding. Capillary viscometer experiments on CO
2 hydrate slurry showed time-dependent viscosity even at fixed hydrate fraction confirming that hydrate particles do not behave as inert solids as where hydrate fractions between 4 vol% and 20 vol% produced apparent viscosities ranging from 3.8 mPa·s to 42.2 mPa·s under shear rates between 500 s
−1 and 1000 s
−1.
Table 4 summarizes representative experimental observations of hydrate slurry rheology obtained using capillary-based viscometry under laminar flow conditions. The data demonstrate that hydrate slurry flow behavior is strongly dependent on hydrate fraction, applied shear rate, and the presence of additives. For CO
2 hydrate slurries, increasing hydrate fraction leads to clear rheological regime transitions, progressing from dilatant behavior at low hydrate loadings to Herschel-Bulkley and Bingham plastic behavior as particle interactions and network formation intensify. The inclusion of additives stabilizes hydrate particles and suppresses non-Newtonian effects, yielding near-Newtonian flow at comparable hydrate fractions. Shear-rate-dependent transitions observed in methane hydrate systems show that hydrate slurry viscosity cannot be described by a single constitutive model, and the concentration and shear-dependent viscosity correlations for predicting slurry flow performance is needed [
92].
8. Technology Bottlenecks Which Still Need to Be Solved
Commercialization of CO2 hydrates, which can be crucial for carbon capture and thermal energy storage applications, faces significant challenges in terms of kinetic and thermodynamic limitations. In addition to the type of reactor, the CO2 hydrate formation is highly dependent on factors such as temperature, pressure, and the presence of promoters or inhibitors. Despite the substantial progress made in understanding the phase behavior and thermodynamics of CO2 hydrates, the slow kinetics of hydrate formation at lower pressures and temperatures remain a bottleneck. This results in long induction times and low overall conversion rates, which hinder the efficiency of CO2 hydrate-based systems. Researchers are investigating new gas mixes with CO2, new nucleation promoters, such as nanoparticles, amino acids, and surfactants, to enhance the rate of formation and reduce induction time. However, the scalability of these methods and their cost-effectiveness for large-scale applications remain unresolved.
The long-term stability of CO2 hydrates is another significant challenge. Hydrates tend to dissociate when subjected to changes in pressure or temperature, especially over extended periods. In practical applications like thermal energy storage and CO2 sequestration, maintaining stable hydrate formation for long durations is essential to ensure that the stored CO2 does not escape into the atmosphere. Research is focused on identifying methods to stabilize hydrates, including the use of tailored promoters, additives, and novel reactor designs. For instance, the incorporation of solid particles such as silica and carbon nanotubes into CO2 hydrate slurries has shown promise in increasing the stability of the hydrate structure. However, the trade-off between improved stability and the potential for increased costs due to these additives presents a significant barrier for widespread adoption. Scalability is one of the most pressing issues in the commercial implementation of CO2 hydrate-based technologies. Lab-scale reactors have demonstrated the potential of CO2 hydrate formation for energy storage and CO2 capture, but scaling up these systems to industrial levels remains problematic. Challenges include managing large volumes of CO2 and water under high-pressure conditions, maintaining efficient heat and mass transfer within the reactor, and ensuring uniform flow dynamics to promote efficient hydrate formation. The integration of microchannel reactors has been proposed as a solution to enhance heat transfer and reduce the size of the reactors, but there are still significant challenges in maintaining the stability of CO2 hydrates in microchannel systems. The complexity and cost of such systems can limit their commercial viability, requiring innovations in both reactor design and process control strategies.
Transporting and handling CO2 hydrate slurries introduces another set of challenges, particularly related to the slurry’s rheological behavior. Hydrate slurries exhibit non-Newtonian flow behavior, with shear-thinning or shear-thickening characteristics that depend on the hydrate concentration and shear rate. This behavior complicates the design of pumping systems and piping infrastructure for large-scale applications, as efficient and stable slurry transport is required for continuous operations. The potential for hydrate agglomeration and blockages in pipelines poses a significant risk for system performance. To address these issues, researchers are investigating the role of nanoparticles and surfactants in stabilizing hydrate particles and preventing aggregation, but the practical implementation of these solutions at a commercial scale is still uncertain.
The environmental and economic feasibility of CO2 hydrate-based technologies remains a key concern. While CO2 hydrate systems offer a promising method for carbon sequestration and thermal energy storage, their economic viability depends on the cost of implementing the necessary infrastructure, including high-pressure reactors, slurry pumps, and heat exchangers. The operational costs, particularly the energy required to maintain the high-pressure and low-temperature conditions needed for hydrate formation, are significant barriers to their widespread adoption. Environmental concerns related to the long-term storage of CO2 in hydrates, including the potential risks of leakage or dissociation, need to be carefully addressed through rigorous monitoring and regulatory frameworks. The development of cost-effective and environmentally sustainable technologies to capture, store, and utilize CO2 hydrates will require continued investment in both research and infrastructure.
9. Conclusions
This review focused on CO2 hydrate slurries from a thermofluid-based point of view, with attention to how they form, how they flow, and how they transfer heat in practical applications. CO2 hydrate slurries store cold through phase change while still behaving as a pumpable fluid. Compared with bulk hydrate beds, slurry systems allow heat to be extracted continuously. The dissociation enthalpy of CO2 hydrates that is reported in the range of about 350 to 520 kJ per kilogram of water and is higher than that of ice. This energy can be delivered near freezing temperatures, which makes these systems well suited for cooling and HVAC applications. Hydrate formation remains one of the main constraints affecting future commercial applications. Nucleation is slow and irregular in many systems, and heat released during formation can raise local temperature and slow further growth. Slurry-based configurations help reduce these limitations by keeping hydrate particles in motion and continuously renewing the gas-liquid interface. Experimental studies show that hydrate fraction, particle size, and shear rate strongly influence formation rate and stability, and these factors must be controlled together rather than treated independently.
A wide range of catalysts and additives have been studied to improve hydrate formation and maintain slurry stability. Thermodynamic promoters such as tetrahydrofuran and cyclopentane help shift hydrate formation to milder operating conditions and while surfactants like SDS improve gas-liquid contact and reduce induction time. Highly conductive nanoparticles such as metal oxides and carbon-based materials can provide additional nucleation sites and help remove heat release during formation and this supports faster growth. More recently, amino acids have also been explored as environmentally friendly promoters with promising results. Choosing the right additive depends on balancing performance improvement, environmental impact, and long-term slurry stability. Reactor design is also important for achieving stable and continuous hydrate slurry production. Effective mixing and efficient heat removal helps maintain uniform temperature and prevent particle agglomeration or blockage during operation. Continuous stirred tank reactors and flow-loop systems are commonly used because they provide better control over operating conditions and allow longer steady operation. Proper reactor geometry, impeller selection, and residence time distribution are critical for maintaining uniform hydrate particle distribution and preventing localized overheating during formation. The flow behavior of CO2 hydrate slurries changes as solid content increases. At low hydrate fractions, the slurry behaves close to a Newtonian fluid and can be circulated using conventional pumps. As the hydrate fraction rises, particle interactions increase flow resistance and lead to shear-dependent behavior. Beyond a certain solid loading, pressure drops increase rapidly and flow stability decreases. For most systems, stable operation requires hydrate fractions below roughly 20 to 25 percent volume percent.
Heat transfer in CO2 hydrate slurries is limited by the low thermal conductivity of the hydrate phase itself. Unlike ice, hydrate crystals do not conduct heat efficiently, so heat transfer depends strongly on particle motion and contact with heat transfer surfaces. Slurry flow improves this process by constantly renewing the interface, while compact heat exchangers and microchannel geometries further enhance heat removal by increasing surface area and shear. These features lead to faster thermal response compared with bulk hydrate systems. Nanoparticles have shown potential to improve hydrate slurry performance when used at low concentrations. They reduce induction time and increase gas uptake by providing additional nucleation sites, and they can increase the effective thermal conductivity of the carrier liquid. Carbon-based and metal-oxide nanoparticles show benefits at concentrations below about 0.1 wt%, while higher concentrations may increase viscosity and lead to stability issues. The balance between thermal improvement and flow resistance is therefore critical.
Several challenges remain before CO2 hydrate slurries can be deployed at large scale. Continuous production under steady operating conditions is still difficult due to the narrow thermodynamic window required for hydrate stability. Long-term slurry stability, pressure fluctuations, and mechanical wear also require further investigation. Addressing these issues will require improved reactor designs with better mixing and heat removal, more robust process monitoring and control strategies, and careful material selection to reduce equipment degradation. Existing thermodynamic and hydrodynamic models still have limited capability in predicting slurry behavior under real flow and heat transfer conditions. Future work should focus on integrating high-quality experimental data with multiphase CFD and rheological modeling to develop validated predictive frameworks that can accurately capture particle interactions, heat transfer behavior, and flow stability across different operating regimes.