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Materials (Basel). 2012 September; 5(9): 1593–1601.
Published online 2012 September 5. doi:  10.3390/ma5091593
PMCID: PMC5449016

Permeation of Light Gases through Hexagonal Ice

Abstract

Gas separation using porous solids have attracted great attention due to their energetic applications. There is an enormous economic and environmental interest in the development of improved technologies for relevant processes, such as H2 production, CO2 separation or O2 and N2 purification from air. New materials are needed for achieving major improvements. Crystalline materials, displaying unidirectional and single-sized pores, preferentially with low pore tortuosity and high pore density, are promising candidates for membrane synthesis. Herein, we study hexagonal ice crystals as an example of this class of materials. By slowly growing ice crystals inside capillary tubes we were able to measure the permeation of several gas species through ice crystals and investigate its relation with both the size of the guest molecules and temperature of the crystal.

Keywords: ice, light gases, diffusion

1. Introduction

Separation or purification of light gases is crucial in many industrial activities. In fact, there is an enormous economic and environmental interest in the development of better technologies for relevant processes such as H2 production, CO2 separation or O2 and N2 purification from air. Membrane separation is growing as a low-cost and energy-efficient alternative to traditional methods, such as adsorption or cryo-separation. Most membranes in use in industry are polymeric [1], and despite the ongoing development of better polymeric materials, there is a trade-off between flow rates and selectivities [2]. Crystalline materials, displaying unidirectional and single-sized pores are promising candidates for membrane synthesis. Metal-organic frameworks (MOFs) [3,4] and peptide supramolecular systems [5,6,7,8] are among the most promising crystal structures, due to the variety of pore sizes and high pore density. Nevertheless, the key challenge in the context of using crystalline materials is to scale up the fabrication techniques of either dense polycrystalline layers [3] or mixed matrix membranes, which embed the selective particles inside the polymeric matrix [4].

It is well known that ordinary water and several organic compounds [9] solidify in a regular geometric lattice (crystal) containing unidirectional nanochannels. Here, using water ice as a model, we demonstrate that under controlled phase transition conditions it is possible to induce the orientation of the crystal lattice inside capillary tubes: a process that may find very interesting applications. We show that, inside capillary tubes, hexagonal ice crystals form by slowly growing in the direction of the c-axis and that they can be used as single crystal membranes able to distinguish between different gas molecules. We observed that the gas molecules cannot escape through the ice-glass capillary wall interface, which enables an easy scale-up by simply using perforated solid plates to promote multiple crystal growth. Moreover, we found that the flow rate of the gas species is severely regulated by ice temperature, expanding the number of potential species that may be separated.

2. Experimental

2.1. Crystallization

The crystallization of ultrapure water was achieved inside capillaries of variable diameters (from 2.0 mm to 0.1 mm) and applying different temperature decreasing rates. The ice crystal structures and the alignment of the c-axis relative to the capillary were determined by X-ray diffraction (see Supplementary Information). We obtained the well-known ice Ih hexagonal crystal structure [10] with an oxygen atom on each vertex (Figure 1). The crystal disorder decreased (better-diffracting crystals) when using thinner capillaries and lower cooling rates (10 K/hr down to 260 K followed by 360 K/hr until reaching the required temperature). It is worth pointing out that although the freezing process often resulted in disordered ice, the crystallographic c-axis was always coincident with the capillary axis in the well-diffracting crystals.

Figure 1
Crystal structure of ice Ih at 150 K viewed along the c-axis. Hydrogen atoms are not shown.

2.2. Single-Crystal Permeation Experiments

Single-crystal permeation experiments were performed against the atmosphere using a pressurized feed gas chamber (see the scheme in the Supplementary Information). A small volume (around 7 × 10−3 µL) of ultrapure water (milli-Q water) was introduced inside a glass capillary. The ice crystal was obtained by cooling at temperature rate of 10 K/hr until 260 K followed by 360 K/hr towards the predetermined temperature. A standard cryostream cooler for X-ray diffraction was used. Pressure of the feed gas chamber was monitored and permeabilities were determined through a mass balance on the chamber volume.

3. Results and Discussion

We measured ice permeability towards helium (Figure 2), the molecule with the smallest kinetic diameter (2.6 Å), and found that it is permeable in the c-axis direction. Disordered ice crystals were non-permeable. The hexagonal ice void nanochannels are smaller than all the gas molecular dimensions, including helium (see Supplementary Information). However, the unexpected penetration of small molecules through other hydrogen-bonded supramolecular crystals was already observed and was attributed to the flexibility of the crystal framework [7,11].

Figure 2
Feed pressure drop normalized by the pressure gradient across the ice crystal.

The increase in the pressure gradient across the ice crystals predictably enhances the helium flow rate (Figure 2). However, the helium flow rate diminishes significantly with increasing temperature, which is not expected in diffusion processes, such as diffusion of trace gases in hexagonal ice [12,13]. This behavior may be associated with a temperature effect in the stability of the ice crystal phase (Figure 3).

Figure 3
Temperature effect of the ice Ih permeability towards helium. Pressure drop in the feed gas chamber.

We then studied the permeation of other gas compounds through ice (Figure 4). Interestingly the flow rate diminishes with increasing temperature until a critical value is reached, above which the compound does not permeate.

Figure 4
Ice Ih selectivity of argon, methane, nitrogen, oxygen and hydrogen, relative to helium.

Almost all binary combinations of gas species investigated can be potentially separated at a certain temperature. Oxygen and nitrogen, however, present an overlapping exclusion temperature, whereas the helium/hydrogen pair involves critical temperatures above the studied range. The critical temperatures do not correlate completely with the kinetic diameters of the gas species (Table 1).

Table 1
Kinetic diameters and excluding temperatures of the gas compounds.

Anisotropic molecules seem to behave as being slightly “smaller” than expected from the kinetic diameters, probably because they become partially aligned inside the nanochannels. We have already observed this behavior in the permeation through dipeptide microporous crystals [7].

In addition, we also investigated the temperature effect on ice structure by single-crystal X-ray diffraction. It has already been observed that above 100 K there is a residual thermal expansion, virtually isotropic, of powdered ice Ih. [14] Hexagonal ice confined to 0.1 mm capillary tubes exhibits, in the 150–240 K temperature range, a slight decrease in the a crystal lattice (4.5167(15) Å @150 K to 4.492(4) Å @240 K, uncertainties in parenthesis) and an increase in the c crystal lattice (7.290(3) Å @150 K to 7.335(7) Å @240 K). Overall, there is a negative thermal expansion of the cell volume (128.79(8) Å3 @150 K to 128.16(19) Å3 @240 K) as it was formerly obtained by Dantl (1962) by single crystal experiments [15]. Accordingly, there is a small contraction of the hexagonal ice rings which can hardly explain the magnitude of the temperature effect in the gas flow rates (Figure 5).

Figure 5
Ice Ih hexagonal ring dimensions at (a) 150 K; (b) 195 K; and (c) 240 K.

The increase in thermal motion of the oxygen atoms is probably more decisive. Figure 6 shows the thermal ellipsoids of the oxygen atoms at 150 K, 195 K and 240 K of ice formed inside 0.1 mm capillaries. High-resolution neutron diffraction studies of ice Ih had already shown an increase in the average thermal displacement of O atoms from 0.118 Å @66 K to 0.208 Å @223 K rmsd [16]. The increase with temperature of O thermal motion is also correlated with a decrease of the ice crystal structure stability. It is possible that when reaching a given temperature, the gas molecules interact with the ice structure, blocking the flow through. However, we checked that the flux is re-established after replacing a non-permeating gas by helium.

Figure 6
Thermal ellipsoids of the oxygen atoms of ice Ih crystal structures formed inside 0.1 mm capillaries at 150 K, 195 K and 240 K (from light to dark grey respectively). The three ellipsoids are shown at the same probability level.

The mass transport through the ice structure is considerably fast. The helium flow rate through the hexagonal ice columns is approximately as fast as the flux through the permanent nanochannels of the L-valyl-L-isoleucine (VI) crystals [7]. The estimated VI nanochannels diameter stands between 3.0 and 3.7 Å depending on the determination method [11]. The high flow rates through the channels reflect the negligible tortuosity of the hexagonal columns and the high flexibility of the ice framework. In addition to this, the almost unbeatable pore density of the Ih crystalline form results in very high permeabilities.

Ice phase transitions and ice–gas interactions (gas hydrate stability and gas diffusion mechanisms) are deeply investigated but poorly understood. Neverthless, our results are intriguing in light of the global perspective in the field.

The ice Ic–ice Ih transition temperature is located between 160 K and 205 K [17] and the reasons behind such variability are not yet clear. However we are confident, based on the X-ray diffraction data, that by slowly decreasing the temperature of water inside capillary tubes at atmospheric pressure, the hexagonal form is maintained down to 150 K.

Gas molecules with molecular dimension lower than 0.9 nm can be incorporated in water crystalline inclusions—known as clathrate hydrates. Most hydrates belong to three structural families, two cubic forms and one hexagonal form [18,19,20,21]. All the gas species used in this work are described as being among the ones known to form clathrate-like structures [17,22,23]. The mechanism of dissociation of clathrate hydrates is still not well understood. Some clathrate hydrates show a self-preservation behavior, even outside the zone of thermodynamic stability of the hydrate, that is dependent on the type of the guest molecule [22,23,24,25]. Guest molecules can impose variations in the lattice constants of the hydrate structure and induce a significant weakening of the host structure [26]. Temperature transition to a non-permeable behavior towards gases is very drastic (Figure 4). As mentioned above, this may be related to the formation of a new ice phase where the guest molecules become trapped. A similar mechanism was already proposed to the dissociation behavior of clathrate hydrates in the 180–220 K range [20]. Unfortunately, diffusion measurements of trace gases in ice are scarce and sometimes contraditory. Molecular dynamics simulation studies are more frequent but the understanding of the diffusion mechanisms remains poorly understood. Ikeda-Fukazawa et al. [27,28,29] argued that small apolar guest molecule, such as He, Ne, Ar or H2, diffuse without distorting the ice lattice while large molecules, such as O2, N2, CO2 and CH4, diffuse by a bond-breaking mechanism. However, Demurov and colleagues [30] reported molecular dynamic simulations of CO2 through defect-free hexagonal ice at 200 K and observed no evidence of diffusion. Alavi and Ripmeester [22] on the other hand showed that H2 can diffuse out of the hydrates through the hexagonal rings, or even through the smaller pentagonal rings. Mitlin et al. [31] argued that Xe can easily penetrate the ice hexagonal structure by a mechanism of adsorption and induced crystal disorder. Peters et al. [32] observed that methane does not fit through the six membered ring without distortion, so one hydrogen bond in the water ring must break at a transition state. Ballenegger and colleagues [33] showed that formaldehyde diffuses predominantly through a bond-braking mechanism of the ice structure.

Here we show that H2, O2, N2, CH4 and Ar can diffuse through the hexagonal ice structure. Diffusion of these compounds was already predicted theoretically by other authors [34]. However, we cannot ascertain whether defects in the crystal matrix or local disorder induced by guest species are relevant or not for the diffusion mechanism. We tried to obtain gas sorption equilibrium data to corroborate our findings but without success. The hexagonal ice sample size (around 7 × 10−3µL) is too small to measure gas sorption uptake. Neverthless, adsorption isotherms of light gases, such as H2, N2 and CO2 in hexagonal ice, were already reported in the literature [35,36].

4. Conclusions

Ice was already used as a chromatographic stationary phase to separate enantiomers [37]. Here, we have shown that hexagonal ice may be used as a molecular sieve to separate light gases with commercial value. Despite the high selectivities and permeabilities, the practical use of ice for gas separations is certainly limited by low stability of the ice structure and low operating temperatures. Nevertheless, our results have a long-term interest as they will motivate the search for other compounds that solidify at higher temperatures into similar but more stable crystalline structures. The possibility of easy scale-up into polycrystalline membranes with exceptional performance certainly looks very promising.

Acknowledgments

This work was supported by Fundação para a Ciência e Tecnologia (project PTDC/CTM/64191/2006) and by a PhD scholarship to Joana Durão (SFRH/BD/69960/2010).

Supplementary Files

Supplementary File 1

References

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