Rajamani Krishna1, Jasper M van Baten1. 1. Van't Hoff Institute for Molecular Sciences, University of Amsterdam, Science Park 904, 1098 XH Amsterdam, The Netherlands.
Abstract
Using configurational-bias Monte Carlo simulations of adsorption equilibrium and molecular dynamics simulations of guest diffusivities of CO2, CH4, N2, and O2 in FAU zeolites with varying amounts of extra-framework cations (Na+ or Li+), we demonstrate that adsorption and diffusion do not, in general, proceed hand-in-hand. Stronger adsorption often implies reduced mobility. The anti-synergy between adsorption and diffusion has consequences for the design and development of pressure-swing adsorption and membrane separation technologies for CO2 capture and N2/O2 separations.
Using configurational-bias Monte Carlo simulations of adsorption equilibrium and molecular dynamics simulations of guest diffusivities of CO2, CH4, N2, and O2 in FAU zeolites with varying amounts of extra-framework cations (Na+ or Li+), we demonstrate that adsorption and diffusion do not, in general, proceed hand-in-hand. Stronger adsorption often implies reduced mobility. The anti-synergy between adsorption and diffusion has consequences for the design and development of pressure-swing adsorption and membrane separation technologies for CO2 capture and N2/O2 separations.
Despite
the burgeoning research and development activities on novel
metal–organic frameworks (MOFs) in separation applications,
cation-exchanged zeolites remain viable contenders for use as adsorbents
in the industrial practice. For post-combustion CO2 capture,
Na+ cation-exchanged FAU (faujasite) zeolite, NaX, also
commonly known by its trade name 13X (with Si/Al ≈ 1.2), is
considered to be the benchmark adsorbent, with the ability to meet
government targets for CO2 purity and recovery.[1] NaX zeolites are also of potential use in natural
gas purification,[2,3] alkane/alkene separations,[4−8] and hydrogen purification processes.[3,9−23] Coulombic interactions of CO2 and unsaturated alkenes
with the extra-framework cations (e.g., Na+, Ca++, Li+, and Ba++) result in strong binding;
the binding strength and selectivity can be tuned by the appropriate
choice of the extra-framework cations and the adjustment of the Si/Al
ratios.[9,11,20,24−26]Li+ cation-exchanged
FAU (faujasite) zeolite is commercially
used for separation of N2/O2 mixtures.[23,27,28] For supplying medical grade oxygen
to prevent hypoxemia-related complications related to COVID-19, portable
medical oxygen concentrators commonly use LiLSX (LS = low silica;
Si/Al ≈ 1) to achieve high N2/O2 adsorption
selectivities, ensuring enhanced rejection of purified O2, the desired product.[29,30]For separation
applications using pressure-swing adsorption (PSA)
technology, consisting of adsorption/desorption cycles, there is often
a mismatch between the requirements of strong adsorption and ease
of desorption.[31] For example, NaX has a
very strong affinity for CO2, but the regeneration requires
application of deep vacuum. For CO2 capture from flue gases,
Prats et al.[25,26] have used molecular simulations
of mixture adsorption in FAU to determine the optimum Si/Al ratio
for PSA operations.In the design and development of PSA technologies
employing cation-exchanged
zeolite adsorbents, we also require data on the intracrystalline diffusivities
of guest molecules. Most commonly, diffusion limitations cause distended
breakthrough characteristics and reduction in the purities of the
desired products.[31−36] Diffusivity data are also of vital importance in the development
of zeolite membrane constructs for mixture separations in which cation-exchanged
zeolites are used as thin layers or as fillers in mixed-matrix configurations.[37−43]The primary objective of this communication is to gain some
fundamental
thermodynamic insights into the adsorption and diffusion characteristics
of a variety of guest molecules such as CO2, CH4, N2, and O2 in FAU zeolites with varying amounts
of extra-framework cations: Na+ and Li+. The
desired insights are obtained by performing configurational-bias Monte
Carlo (CBMC) simulations of adsorption and molecular dynamics (MD)
simulations of diffusion in Na- and Li-exchanged FAU zeolites with
varying Si/Al ratios. The CBMC and MD simulation methodologies, along
with details of the force field implementations, are detailed in the Supporting Information accompanying this publication.
We aim to demonstrate the anti-synergy between adsorption and diffusion;
the stronger the binding of a guest molecule, the lower is its mobility.
Such insights are of vital importance in determining the optimum Si/Al
ratio of zeolite for use in PSA technologies or in membrane constructs.
The Gibbsian Concept of Spreading Pressure
The spreading
pressure, π, is related to
the molar chemical potential, μ, by the Gibbs adsorption equation[44]where A represents
the surface area per kg of framework, and q is the component molar loading in the adsorbed phase mixture. At
thermodynamic equilibrium, the μ are related to the partial fugacities in the bulk fluid mixtureIn developing the ideal adsorbed solution theory (IAST), Myers
and Prausnitz[45] write the following expression
relating the partial fugacities in the bulk gas mixtureto the mole fractions, x, in the adsorbed phase mixtureIn eq , P0 is the pressure for sorption of
every component i, which yields the same spreading
pressure, π, for each of the pure components
as that for the n-component mixture:In eq , q0(f) is the pure component adsorption isotherm.
Since the surface area A is not directly accessible
from experimental data, the surface potential πA/RT ≡ Φ, with the units mol kg–1, serves as a convenient and practical proxy for the
spreading pressure π.[46−49] As derived in detail in the Supporting Information, the fractional pore occupancy, θ, is related to the surface potential bywhere qsat, mix is the saturation
capacity for mixture adsorption. Equation implies that Φ
may also be interpreted as a proxy for the pore occupancy; it is the
fundamentally correct yardstick to compare the adsorption and diffusion
characteristics of different host materials.[41,48−50]In view of eq , we
may express the adsorption selectivity for the i–j pair as followsApplying the restriction specified by eq , it follows that Sads is uniquely determined by the surface potential Φ, irrespective
of the mixture composition and total fugacity, ft.
Results and Discussion
CO2 Capture Using Na-Exchanged
FAU
Figure a plots the CBMC data on isosteric heats of adsorption, Qst, a measure of the binding energies, of CO2 and CH4 in FAU (0 Al, all-silica), NaY (54 Al uc–1), and NaX (86 Al uc–1) zeolites,
plotted as a function of the surface potential Φ. For CO2, the hierarchy of Qst is NaX
> NaY > FAU; this hierarchy reflects the strong electrostatic
interactions
with the extra-framework cations, engendered by the large quadrupole
moment of CO2. For CH4, the differences in the Qst in the three different hosts are considerably
smaller because the adsorption of CH4 is due to van der
Waals interactions that also increase with increasing number of cations.
Figure 1
(a) CBMC
simulations of the isosteric heats of adsorption, Qst, of CO2 and CH4 in
FAU (0 Al, all-silica), NaY (54 Al uc–1), and NaX
(86 Al uc–1) zeolites, determined at 300 K, plotted
as a function of the surface potential Φ. (b) MD simulations
of the self-diffusivities, D, of CO2 and CH4 in FAU, NaY,
and NaX zeolites, determined at 300 K, plotted as a function of the
surface potential Φ. All simulation details and input data are
provided in the Supporting Information accompanying
this publication.
(a) CBMC
simulations of the isosteric heats of adsorption, Qst, of CO2 and CH4 in
FAU (0 Al, all-silica), NaY (54 Al uc–1), and NaX
(86 Al uc–1) zeolites, determined at 300 K, plotted
as a function of the surface potential Φ. (b) MD simulations
of the self-diffusivities, D, of CO2 and CH4 in FAU, NaY,
and NaX zeolites, determined at 300 K, plotted as a function of the
surface potential Φ. All simulation details and input data are
provided in the Supporting Information accompanying
this publication.Strong binding of guest
molecules also implies a higher degree
of “stickiness” and, consequently, lower mobility.[51,52] To demonstrate this, Figure b presents the MD simulations of the unary self-diffusivities, D, of CO2 and CH4 in FAU (0 Al), NaY, and NaX zeolites. Compared
at the same surface potential Φ, the hierarchy of self-diffusivities
is precisely reverse of the hierarchy of Qst. Noteworthily, CH4, the guest with the larger kinetic
diameter of 3.8 Å, has a higher mobility than CO2,
which has a smaller kinetic diameter of 3.3 Å. The fallacy of
using kinetic diameters to anticipate hierarchies in the diffusivity
values has been underscored in published works.[15,51]CBMC simulations were carried out for equimolar (f1 = f2) CO2(1)/CH4(2) mixtures in FAU (0 Al), NaY, and NaX zeolites. The values
of the adsorption selectivities, Sads,
are plotted in Figure a as a function of Φ. The hierarchy of Sads values is NaX > NaY > FAU (0 Al), reflecting the
stronger
binding of CO2. The corresponding hierarchy of diffusion
selectivities, Sdiff = D1, self/D2, self, is precisely the reverse of Sads; evidently,
mixture adsorption and diffusion do not proceed hand-in-hand. This
anti-synergy has important consequences of use of cation-exchanged
zeolites in membrane constructs. If the partial fugacities of the
components at the downstream face are negligibly small in comparison
with those at the upstream face, the component permeabilities may
be estimated from the following expression[41]
Figure 2
Comparison
of CBMC/MD simulations of (a) adsorption selectivities, Sads, and (b) diffusion selectivities, Sdiff, of CO2/CH4 mixtures
in FAU (0 Al), NaY, and NaX zeolites at 300 K. The selectivities are
plotted as a function of the surface potential Φ. All simulation
details and input data are provided in the Supporting Information accompanying this publication.
Comparison
of CBMC/MD simulations of (a) adsorption selectivities, Sads, and (b) diffusion selectivities, Sdiff, of CO2/CH4 mixtures
in FAU (0 Al), NaY, and NaX zeolites at 300 K. The selectivities are
plotted as a function of the surface potential Φ. All simulation
details and input data are provided in the Supporting Information accompanying this publication.For FAU (0 Al), NaY, and NaX zeolites, Figure a,b compares the values of the CO2 permeabilities, Π1, and the permeation selectivity
Figure 3
Comparison
of (a) CO2 permeability, Π1, and (b) permeation
selectivity, Sperm, for CO2(1)/CH4(2) mixtures in FAU (0 Al),
NaY, and NaX zeolites at 300 K; the x-axis represents
the surface potential Φ. (c) Robeson plot of Sperm vs Π1 data at ft = f1 + f2 = 106 Pa and 300 K. All simulation details
and input data are provided in the Supporting Information accompanying this publication.
Comparison
of (a) CO2 permeability, Π1, and (b) permeation
selectivity, Sperm, for CO2(1)/CH4(2) mixtures in FAU (0 Al),
NaY, and NaX zeolites at 300 K; the x-axis represents
the surface potential Φ. (c) Robeson plot of Sperm vs Π1 data at ft = f1 + f2 = 106 Pa and 300 K. All simulation details
and input data are provided in the Supporting Information accompanying this publication.The CO2 permeabilities, Π1, decrease
with increasing values of Φ. The Sperm is a product of the adsorption selectivity and diffusion selectivity
(cf. Figure a,b).
While the Sdiff increases with Φ
for all three hosts, the Sads increases
with Φ until a maximum is reached for NaX and NaY and decreases
on a further increase in Φ. Consequently, the Sperm also shows a maximum value for NaX and NaY. For the
specific choice of upstream operating conditions, ft = f1 + f2 = 106 Pa, Figure c shows the Robeson[53] plot of Sperm vs Π1 for the three host structures. We note that the performances of
both NaY and NaX lie above the line representing the Robeson upper
bound.[53] Since both Sperm and Π1 are important metrics governing
the choice of the appropriate membrane material, there is room for
optimization of the Si/Al ratio depending on the relative weightage
to be assigned to permeation selectivity and permeability. CBMC/MD
data that are analogous to those presented in Figures and 3 are obtained
for CO2/N2, CO2/H2, CH4/H2, CH4/C2H6,
and CH4/C3H8 mixtures in FAU (0 Al),
NaY, and NaX (see Figures S60–S64 of the Supporting Information).
N2/O2 Separations Using
Li-FAU and Na-FAU
Figure a presents MD simulations of the unary self-diffusivities, D, for N2, at 300 K in Li-exchanged FAU zeolites, with different Al contents
per unit cell: 0, 48, 54, 86, and 96, plotted as functions of the
surface potential Φ; the contents of Li+ are equal
to that of Al. The magnitudes of D decrease with increasing values of Φ, which
also serves as a proxy for the pore occupancy. At any specified value
of Φ, the values of the self-diffusivity, D, show the following trend:
FAU (0 Al) ≫ FAU (48 Al) ≈ FAU (54 Al) > FAU (86
Al)
≈ FAU (96 Al). This hierarchy of D values correlates, inversely, with the
corresponding values of the isosteric heats of adsorption of N2 (cf. Figure b). N2 has a significant quadrupole moment, and the electrostatic
interaction potentials increase with increasing Al content, leading
to increasing binding energies. The data in Figure a,b confirm that the diffusional mobility
of N2 is reduced with increased binding energy.
Figure 4
(a) MD simulations
of the unary self-diffusivities for N2 at 300 K in Li-exchanged
FAU zeolites, with different Al contents
per unit cell: 0, 48, 54, 86, and 96, plotted as a function of the
surface potential Φ. (b) Isosteric heats of adsorption, Qst, plotted as a function of the number of Al
atoms per unit cell. (c) MD simulations of the unary self-diffusivities
for O2 at 300 K in Li-exchanged FAU zeolites, with different
Al contents per unit cell: 0, 48, 54, 86, and 96, plotted as a function
of the surface potential Φ. All simulation details and input
data are provided in the Supporting Information accompanying this publication.
(a) MD simulations
of the unary self-diffusivities for N2 at 300 K in Li-exchanged
FAU zeolites, with different Al contents
per unit cell: 0, 48, 54, 86, and 96, plotted as a function of the
surface potential Φ. (b) Isosteric heats of adsorption, Qst, plotted as a function of the number of Al
atoms per unit cell. (c) MD simulations of the unary self-diffusivities
for O2 at 300 K in Li-exchanged FAU zeolites, with different
Al contents per unit cell: 0, 48, 54, 86, and 96, plotted as a function
of the surface potential Φ. All simulation details and input
data are provided in the Supporting Information accompanying this publication.On the other hand, we note from Figure b that the isosteric heats of adsorption
of O2 are practically uninfluenced by the addition of extra-framework
cations due to the significantly lower quadrupole moment of O2. Therefore, we should anticipate that the mobility of O2 should be practically independent of the degree of Li exchange;
this expectation is fulfilled by the MD simulations of the self-diffusivities
of O2 in Li-FAU (see Figure c).For 80/20 N2/O2 mixture
adsorption, Figure a plots the adsorption
selectivities, Sads, of Li-exchanged FAU
zeolites, with different Al contents. We note that the Sads increases with increasing Al content. MD simulations
of the N2/O2 diffusion selectivities, Sdiff, plotted in Figure b, demonstrate the anti-synergy between adsorption
and diffusion; the higher the adsorption selectivity, the lower is
the corresponding diffusion selectivity. Analogous CBMC and MD simulations
with Na-exchanged FAU zeolites were also carried out; the results
are provided in Figures S73–S81 of the Supporting Information.
Figure 5
(a) CBMC simulations of the adsorption
selectivity, Sads, for binary 80/20 N2/O2 mixture
adsorption in Li-FAU, with different Al contents per unit cell: 0,
48, 54, 86, and 96. (b) MD simulations of the N2/O2 diffusion selectivity, Sdiff,
at 300 K in Li-FAU zeolites. All simulation details and input data
are provided in the Supporting Information accompanying this publication.
(a) CBMC simulations of the adsorption
selectivity, Sads, for binary 80/20 N2/O2 mixture
adsorption in Li-FAU, with different Al contents per unit cell: 0,
48, 54, 86, and 96. (b) MD simulations of the N2/O2 diffusion selectivity, Sdiff,
at 300 K in Li-FAU zeolites. All simulation details and input data
are provided in the Supporting Information accompanying this publication.For 80/20 N2/O2 mixture separations at a
total fugacity of 100 kPa, Figure a compares the adsorption selectivities of Li-FAU and
Na-FAU. For the same Al content, we note that the Sads values with Li-FAU are significantly higher than for
Na-FAU. The interaction potential, engendered by the quadrupole moment,
is inversely proportional to the cube of the center-to-center distance
between nitrogen molecules and the extra-framework cation (see the
detailed explanation provided in Chapter 2 of the Supporting Information). Due to the smaller ionic radius of
Li+, compared to Na+, the N2–Li+ distances are smaller than the N2–Na+ distances; this is confirmed by radial distribution functions
for N2–Li+ and N2–Na+ pairs for 80/20 N2/O2 mixture adsorption
in Li-FAU(96Al) and Na-FAU(96Al) (see Figure ).
Figure 6
Comparison of the (a) adsorption selectivity
and (b) diffusion
selectivity for 80/20 N2/O2 separations using
either Li-exchanged or Na-exchanged FAU zeolites, with different Al
contents per unit cell: 0, 48, 54, 86, and 96. All simulation details
and input data are provided in the Supporting Information accompanying this publication.
Figure 7
Radial
distribution functions for N2–Li+ and
N2–Na+ pairs for 80/20 N2/O2 mixture adsorption in Li-FAU (96Al) and Na-FAU (96Al)
at 100 kPa and 300 K.
Comparison of the (a) adsorption selectivity
and (b) diffusion
selectivity for 80/20 N2/O2 separations using
either Li-exchanged or Na-exchanged FAU zeolites, with different Al
contents per unit cell: 0, 48, 54, 86, and 96. All simulation details
and input data are provided in the Supporting Information accompanying this publication.Radial
distribution functions for N2–Li+ and
N2–Na+ pairs for 80/20 N2/O2 mixture adsorption in Li-FAU (96Al) and Na-FAU (96Al)
at 100 kPa and 300 K.The N2/O2 diffusion selectivities for Na-FAU
are only slightly higher than those of Li-FAU (see Figure b). The CBMC/MD data rationalize
the use of LiX, with Al ≈ 96 uc–1, in the
industrial practice.[29,30]Figure shows a
Robeson plot of Sperm vs N2 permeabilities of N2 for binary 80/20 N2/O2 mixture permeation across the Li-FAU zeolite membrane at
an upstream total pressure of 100 kPa. We note that the separation
performance increases monotonously with increasing degrees of Li+ exchange; the permeabilities are significantly higher than
the values reported in the literature[54] for polymeric and mixed-matrix membranes.
Figure 8
Robeson plot of Sperm vs N2 permeabilities for binary
80/20 N2/O2 mixture
permeation across the Li-exchanged FAU zeolite membrane, with different
Al contents per unit cell: 0, 48, 54, 86, and 96. All simulation details
and input data are provided in the Supporting Information accompanying this publication.
Robeson plot of Sperm vs N2 permeabilities for binary
80/20 N2/O2 mixture
permeation across the Li-exchanged FAU zeolite membrane, with different
Al contents per unit cell: 0, 48, 54, 86, and 96. All simulation details
and input data are provided in the Supporting Information accompanying this publication.
Conclusions
A combination of CBMC and MD
simulations for adsorption and diffusion
of guest molecules CO2, CH4, N2,
and O2 in FAU zeolites with varying amounts of extra-framework
cations (Na+ or Li+) was carried out to investigate
the influence of varying Si/Al ratios on mixture separations. Stronger
adsorption, with increasing amounts of extra-framework cations, results
in lowered diffusivities. For CO2/CH4 and N2/O2 mixture separations, the adsorption selectivity, Sads, and diffusion selectivity, Sdiff, do not proceed hand-in-hand. The anti-synergy between
adsorption and diffusion has important consequences for the choice
of the extra-framework cation, Na+ or Li+, and
the Si/Al ratio for use in PSA and membrane separation technologies.