ARTICLE
Received 3 May 2014 | Accepted 1 Jul 2014 | Published 31 Jul 2014
Loading with guest molecules is a crucial step for most applications of porous materials. For metal-organic frameworks, which are one of the most intensely investigated classes of porous materials, the experimentally determined rate of mass transfer into the material may vary by several orders of magnitude for different samples of the same material. This phenomenon is commonly attributed to the presence of so-called surface barriers, which appear to be omnipresent but poorly understood. Here we quantitatively study this phenomenon with a quartz crystal microbalance, using well-dened, highly crystalline, epitaxially grown thin lms of metal-organic frameworks as a model system. Our results clearly demonstrate that surface barriers are not an intrinsic feature of metal-organic frameworks, as pristine lms do not exhibit these limitations. However, by destroying the structure at the outer surface, for instance by exposure to air or water vapour, surface barriers are created and the molecular uptake rate is reduced.
DOI: 10.1038/ncomms5562
The surface barrier phenomenon at the loading of metal-organic frameworks
Lars Heinke1, Zhigang Gu1 & Christof Wll1
1 Karlsruher Institut fr Technologie (KIT), Institut fr Funktionelle Grenzachen (IFG), Hermann-von-Helmholtz-Platz 1, Eggenstein-Leopoldshafen 76344, Germany. Correspondence and requests for materials should be addressed to L.H. (email: mailto:[email protected]
Web End [email protected] ).
NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications 1
& 2014 Macmillan Publishers Limited. All rights reserved.
ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5562
Metal-organic frameworks (MOFs)1 are an important class of nanoporous crystalline materials with several exclusive properties: large surface areas2, high
diversity3,4 and the ability to alter these properties over wide ranges in a rational manner5,6. MOFs already have many interesting applications, such as storing hydrogen7 or greenhouse8 gases and for gas separation9. In other areas, including catalysis10 and sensor techniques11, the rst applications of MOFs are emerging. A crucial factor in all of these applications is guest molecule loading. Mass transfer of the guest molecules is a critical parameter governing performance; for example, in gas separation, poor transfer rates result in low separation efciencies. Despite its importance, the loading of MOF materials with guest molecules is poorly understood on a quantitative level, and the values of diffusion coefcients measured for different samples of the same material may differ by several orders of magnitude. A prominent example is the diffusion of hydrogen in MOF-5. Experimental values reported for the corresponding diffusion coefcient vary by four orders of magnitude, between 10 5 m2 s 1 (ref. 12) and 10 9 m2 s 1 (ref. 13). Even when restricting the comparison to results reported by the same group using the same synthesis procedure for the MOF material used in the studies, variations of three orders of magnitude are found for CO2 in MOF-5 (diffusion coefcients of 10 9 m2 s 1 and 10 12 m2 s 1 (refs 14,15)). Another example is shown in Fig. 1a,b, where dramatic differences were found in the uptake of cyclohexane by thin MOF lms and powder MOFs of the same structure. Analysing the experimental data, the (effective) diffusion coefcient of cyclohexane is roughly 1,000 times (or three orders of magnitude) larger for the thin lm than for the powder material. In the case of ferrocene inltration from a hexane solution, these differences are smaller, but the diffusion coefcient between the thin lm and the powder material still differs by a factor of 5.
First hints regarding the microscopic origin of these strong sample-to-sample variations have been provided by studies using interference microscopy16 and infrared microimaging17. Analysis of intracrystalline concentration proles found that so-called surface barriers may inuence the uptake of molecules into these porous materials. These surface barriers, which act as additional mass transfer resistance at the outer crystal surfaces (Fig. 1c), hinder the molecules from entering and leaving the pores18,19. Although these barriers often dominate the entire mass transfer, particularly in the case of small powder particles, the underlying mechanism is, at best, qualitatively understood. In addition, whether all MOFs exhibit surface barriers and whether these barriers are an intrinsic feature of the material is unknown. Qualitatively, these surface barriers can be described as a thin layer with (reduced) permeability covering the external crystal surface20,21.
To a good approximation, the uptake by a thin lm, m(t), can be described by an exponential decay function:
m t
meq 1 exp
t t
1 with a time constant of
t
l23D
la 2 where l denotes the lm thickness, D is the (transport) diffusivity, a is surface permeability, meq the equilibrium loading and t the time. On the basis of equation (2), the uptake time increases quadratically with lm thickness in the case of (bulk) diffusion-limited uptake processes. However, for surface barrier-limited uptake processes, the uptake time increases linearly with lm thickness. Furthermore, the relative inuence of the surface barrier on overall uptake increases with decreasing lm thickness. Thus, the uptake of thin MOF lms should be studied as a
Crystal surface: Slow mass transfer
Defect free crystal: Intracrystalline diffusion
a
Cyclohexane
b
Uptake m(g cm2 )
0.15
0.10
0.05
0.00
2.0
1.5
1.0
Uptake m(g cm2 )
0.5
0.0
Ar
Cyclohexane nC6
Ferrocene in nC6
0 50 100 200
150 250
Ferrocene in n-hexane
0 50 100 200
150 250
Time, t (s)
Time, t (s)
c d
Figure 1 | Uptake by MOFs. The uptake of (a) cyclohexane (vapour) and (b) ferrocene from liquid n-hexane was signicantly faster in thin HKUST-1 lms (red, 150-nm thick) than in the corresponding powder material (black, B200 nm crystal diameter, see Supplementary Fig. 1). Uptake was determined using a quartz crystal microbalance24. (c and d) Model of the mass transfer in MOFs. (c) Unhindered mass transfer in the nanoporous crystal. (d) Surface barriers hinder the guest molecules from entering the pore space and signicantly slow down the mass transfer.
2 NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications
& 2014 Macmillan Publishers Limited. All rights reserved.
NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5562 ARTICLE
0.40.350.3
0.25
0.2
0.15
0.1
0.05
800
EtOH
406
Cu(Ac)
EtOH
BTC
700
x480
SURMOF thickness l(nm)
600
404
300 301
500
x340
400
Cyclohexane uptake time t(s)
300
x240
x180
x125
200
100
x70
x30
0
0 100 200 300 400 500
Number of synthesis cycles
0
Figure 2 | Layer-by-layer growth of the HKUST-1 SURMOF on the QCM sensor. The synthesis was interrupted after 30, 70, 125, 180, 240, 340 and 480 cycles to perform uptake experiments with the probe molecule cyclohexane. The inset is a magnication of the layer-by-layer growth of the SURMOF. The left scale shows the quadratic increase in the uptake time of the probe molecule with increasing lm thickness.
Rel. cyclohexane uptake
m C 6 H 12/m SURMOF
0.3
0.2
0.1
0.0
Normalized uptake m/m eq
Normalized uptake m/m eq
1.00.80.60.40.20.0
1.00.80.60.40.20.0
52 nm 110 nm 190 nm 260 nm 340 nm 490 nm 690 nm
0 200 400 600 800
0.0
0.3
0.6
0.9
1.2
SURMOF thickness l (nm)
Time, t (s)
Uptake time constants [afii9848] (s)
0.300.250.200.150.100.050.00
260 nm 340 nm 490 nm 690 nm
1 1 2 3 4
0
0 200 400 800
600
SURMOF thickness l (nm) Normalized time t /l 2 (s m2)
Figure 3 | Cyclohexane uptake. (a) Cyclohexane loading relative to the mass of the HKUST-1 SURMOF. The relative cyclohexane loading was unaffected by the SURMOF thickness. The dotted line represents the average value of 0.26 g g 1. (b) Normalized cyclohexane uptake for varying lm thicknesses. The uptake rate slowed down with increasing lm thickness. The inset shows the SURMOF thicknesses. (c) Time constants for cyclohexane uptake. The time constant for cyclohexane uptake increased quadratically with increasing SURMOF thickness. The black line is t l2/D with D 6 10 13 m2 s 1.
(d) Normalized uptake as a function of normalized time (that is, time divided by the square of the lm thickness). The error bars in a,c represent the s.d.s of the experimental results.
function of their thickness. A quantitative analysis of these results would allow more detailed insights into the microscopic origins of these surface barriers.
Here we use surface-mounted MOFs (SURMOFs) of different thicknesses to quantitatively analyse the importance of surface barriers. SURMOFs are highly crystalline, oriented, thin MOF lms grown by liquid-phase epitaxy on solid substrates in a well-dened layer-by-layer manner22. Suitable functionalization of the substrate is required for nucleating SURMOF growth
on the substrate surface and controlling crystal orientation. Under adequate conditions, SURMOFs grow uniformly and lm roughness as low as the size of a MOF unit cell can be achieved23. Apart from many potential applications, including chemical sensors and membranes, SURMOFs are well suited for a quantitative analysis of dynamic phenomena within MOFs2426. In the present study we used HKUST-1, which is also known as Cu3(BTC)2, MOF-199 or Basolite C300 (ref. 27). HKUST-1 is one of the most popular MOFs28,29 and is among the few that are
NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications 3
& 2014 Macmillan Publishers Limited. All rights reserved.
ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5562
a
Exposed toMOF synthesis solution
Exposed to air
Exposed to water vapour
20
After MOF solution
Cyclohexane uptake m(g cm2 )
Cyclohexane uptake m(g cm2 )
Pristine
15
10
5
0
Ar Cyclohexane
2 0 2 4 6 8
Time, t (s)
b
15
10
5
0
Pristine
30 s
30 Min
1 Day
Ar
Ar
Cyclohexane
Cyclohexane
0
5
10
15 25
20
Time, t (s)
c
Pristine
Cyclohexane uptake m(g cm2 )
15
10
5
0
10 s
0
10
5 Time, t (s)
15 25
20
Figure 4 | Cyclohexane uptake after treatment of the thin MOF lm. (a) The SURMOF was exposed to MOF synthesis solution and MOF crystallites grew on the SURMOF. Uptake by the SURMOF with MOF crystallites on top (red) was larger and marginally slower than the uptake by the pristine SURMOF (black). (b) Uptake by the SURMOF was signicantly decreased and retarded by exposing the SURMOF to air for 30 min and 1 day. (c) Exposing the SURMOF to water vapour with a partial pressure of 23 mbar for 10 and 30 s at 30 C caused a decrease in and signicant deceleration of uptake. All three pristine SURMOF samples had a thickness of B700 nm.
commercially available30. HKUST-1 has a three-dimensional, isotropic pore space of big cages that are connected by0.9-nm-diameter windows27,31. In addition to the large pores, the material has small side pockets with 0.46-nm-diameter windows. Cyclohexane is used as a prototype guest molecule. It has a kinetic diameter of B0.6 nm32 and the small side pockets are not accessible.
ResultsUptake by pristine HKUST-1 SURMOFs of varying thicknesses. A quartz crystal microbalance (QCM) was employed to synthesize the HKUST-1 SURMOF in a clean and well-controlled
manner and to perform the uptake experiments. The QCM sensor was placed in a ow cell (Q-Sense E4). Inltration with guest molecules was achieved via a ow of gas or a stream of liquid through the cell25. The SURMOF to be investigated was grown directly on the gold-coated QCM sensor after functionalization with a 16-mercaptohexadecanoic acid self-assembled monolayer (MHDA SAM). SURMOF growth was carried out in situ in the QCM ow cell by alternating between the metal source solution (1 mM copper(II) acetate), a solution of0.2 mM 1,3,5-benzenetricarboxylic acid (BTC) in ethanol and pure ethanol as described previously33. Not only does this synthesis procedure allow study of the growth process in situ, it also guarantees that the sample is never exposed to any environmental contaminants, such as humid air. Such contaminants are external factors that might affect the crystal structure. In addition to the clean synthesis in the ow cell, synthesis in the QCM cell enables an exact determination of the SURMOF mass by applying the Sauerbrey equation34 (Fig. 2). The structures of the SURMOF thin lms grown on the QCM substrates were monitored by ex situ X-ray diffraction (XRD; see Supplementary Fig. 2).
Using this approach, the loading of cyclohexane by thin MOF lms of specic thicknesses was studied (Fig. 3). The cyclohexane loading relative to the SURMOF mass was found to be independent of the SURMOF thickness (Fig. 3a), showing that the SURMOF is homogenous. A relative cyclohexane loading of B0.26 g cyclohexane per 1 g (activated) HKUST-1 was determined, which corresponds to a capacity of 33 cyclohexane molecules per HKUST-1 unit cell. The time-dependent uptake curves (Fig. 3b and Supplementary Fig. 3) were used to determine the quantitative mass transfer into the thin SURMOF lms. The time constants of the uptake processes were determined by tting the experimental data with equation (1), resulting in reasonable ts (see Supplementary Fig. 3). The time constant of uptake versus lm thickness (Fig. 3c) revealed a clear quadratic increase in uptake time with increasing lm thickness. This observation directly shows that the mass transfer of cyclohexane into the HKUST-1 SURMOF is not inuenced by surface barriers, but it is almost exclusively determined by intracrystalline diffusion. This was also demonstrated by plotting the normalized uptake versus the normalized time (that is, time divided by the square of the lm thickness), resulting in coinciding plots (Fig. 3d). By using equation (2) and neglecting the surface barriers, the cyclohexane diffusivity was determined to be 6 10 13 m2 s 1 (Fig. 3c).
From the data in Fig. 3c, we estimated a lower limit of surface permeability, that is, the maximum inuence of the surface barrier. Using t44tsurface barrier l/a, we obtained a lower limit
of B10 5 m s 1 for surface permeability a. As the relative inuence of the surface barriers decreased with increasing crystal size, we concluded that surface barriers have vanishing inuence on the mass transfer in pristine and defect-free MOF powders, which typically consist of large 1100 mm crystals. Owing to the similarities in their pore spaces, this conclusion can probably be generalized to most MOF structures.
Origin of surface barriers. In order to obtain a better understanding of what causes surface barriers in MOFs, the thin MOF lms, which exhibited no evidence of surface barriers, were modied using different procedures (Fig. 4). A pristine SURMOF was immersed for 10 min in the solution (0.15 M copper(II)acetate and 0.1 M BTC in pure ethanol) used for the solvothermal synthesis of powder HKUST-1 MOFs. An increase in mass was observed (see Supplementary Fig. 4), indicating that MOF crystallites grew on top of the SURMOF lm. Cyclohexane
4 NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications
& 2014 Macmillan Publishers Limited. All rights reserved.
NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5562 ARTICLE
uptake by this sample was greater than the uptake by the SURMOF alone, and the uptake was also slightly slower (both by a factor of B1.2, Fig. 4a). However, a signicant deceleration of the mass transfer was not observed. This observation provides strong evidence that surface barriers are not caused by the solvothermal synthesis conditions.
The impact of environmental conditions was investigated by exposing a pristine SURMOF to air at 298 K and 30% relative humidity for 30 min. A decrease in the adsorption capacity and a signicant deceleration of the uptake process were observed (Fig. 4b). After exposing the SURMOF to air for another 24 h, a further decrease in the adsorption capacity and mass transfer was observed. By exposing a pristine SURMOF to water vapour for only a short time (10 and 30 s), we showed that water is responsible for the decrease in and dramatic retardation of uptake (Fig. 4c).
A quantitative analysis of the uptake curves in Fig. 4b,c) shows that, in both cases, the uptake rates decreased by a factor of B30.
Although exposure to water-containing air and water vapour had dramatic effects on mass transfer, the changes in crystallinity as monitored by XRD were minor (see Supplementary Fig. 5). Therefore, we concluded that exposure to water vapour mainly affects the crystal structure at the outer surface and not the bulk of the crystalline lm, and that this destruction creates the surface barriers. One might generalize that water is responsible for causing surface barriers in all non-water-stable MOFs, the majority of MOFs.
DiscussionPrevious studies35,36 have shown that the transport resistance of surface barriers results from a total blockage of the pore entrances and that the uptake and release occurs by detours via unblocked pores, which remain fully opened. This means water molecules destroy the MOF structure close to the crystal surface, resulting in blocked pore entrances that have to be bypassed by the guest molecules during the mass transfer, causing the additional mass transfer resistance referred to as surface barriers. As a direct result of this model, the activation energy of the surface barrier equals the activation energy of the diffusion in the lm. By using equation (2) and neglecting the diffusion term, the surface permeabilities a of both SURMOF lms exposed to air or water vapour can be calculated to roughly 10 7 m s 1. By adapting equation (2) from ref. 35 to HKUST-1, which has an isotropic pore system, the fraction of open pore entrances popen can be
calculated by popen 12l/5 a/D, with l denoting the distance
between the pores (here: l 1.3 nm27), resulting in popen 0.05%.
This means most of the pore entrances are blocked and only one out of 2,000 pore entrances remains open.
In conclusion, the mass transfer in HKUST-1 MOFs was investigated in detail using thin, quasi-epitaxial grown lms (SURMOFs) with different thicknesses and by studying the uptake of a prototype probe molecule, cyclohexane, using QCM. For pristine SURMOFs, the time for cyclohexane uptake increased quadratically with lm thickness, indicating that the mass transfer is controlled by intracrystalline diffusion rather than by surface barriers. This observation demonstrates that, in contrast to common belief, surface barriers are not intrinsic properties of MOFs. Furthermore, exposing the MOF to air or water vapour creates surface barriers. Our results demonstrate that clean, particularly water-free, synthesis and storage are crucial for obtaining MOFs with high mass transfer rates.
Methods
Synthesis of powder HKUST-1 MOF. Powder HKUST-1 was solvothermally synthesized by mixing 0.30 g (1.5 mmol) copper(II) acetate and 0.21 g (1 mmol)
BTC in 12 ml pure ethanol in a sealed glass bottle37. The reagents were mixed and dissolved in ultrasonic bath for 30 min, followed by heating at 65 C for 2 days and cooling down to room temperature. The resulting powder was washed with pure ethanol and dried in nitrogen. By comparing with the simulated XRD of HKUST-1, the recorded XRD shows that powder HKUST-1 was synthesized (Supplementary Fig. 1)27. Finally, powder HKUST-1 suspension in ethanol was prepared and spin-coated on the MHDA-functionalized QCM sensor.
SURMOF synthesis and cyclohexane uptake experiments. The HKUST-1 SURMOF synthesis was performed in situ in the QCM cell by subsequently pumping the metal and linker solutions as well as pure ethanol through the QCM cell. For the rst data point shown in Fig. 2, the synthesis of the HKUST-1 SURMOF was interrupted after 30 cycles. The mass density of the synthesized SURMOF was determined to be 7.9 mg cm 2, yielding a SURMOF thickness of 52 nm for a mass density of the ethanol-soaked HKUST-1 of 1.53 g cm 3. Note that the density of the activated framework amounts to 0.98 g cm 3 (ref. 27), which has to be augmented by the density of ethanol contained in the pores. This value amounts to 0.56 g per 1 g HKUST-1 MOF38. After activating the sample at 65 C in a ow of pure argon (with a ow rate is 100 ml min 1) overnight, the uptake of the guest molecules was studied again with the QCM. The initially pure argon was switched to an argon ow passing through liquid cyclohexane at room temperature (298 K), resulting in argon ow with a cyclohexane partial pressure of 130 mbar. The cyclohexane uptake by the 52-nm-thick HKUST-1 SURMOF is shown in Supplementary Fig. 3a.
After the cyclohexane uptake experiments using the 52-nm-thick SURMOF lm were performed, the SURMOF synthesis was continued in situ for additional 40 cycles. The sample thickness was recorded by QCM, resulting to an overall sample thickness of 110 nm (see Fig. 2). After activating the sample, the uptake of cyclohexane was studied (see Supplementary Fig. 3b). Subsequently, the SURMOF synthesis was continued and the cyclohexane uptake was again investigated. In this way, the cyclohexane uptake by the HKUST-1 SURMOF was investigated for seven different thicknesses, that is, for lm thicknesses of 52, 110, 190, 260, 340, 490 and 690 nm, see Supplementary Fig. 3. The syntheses as well as the uptake experiments were performed at a temperature of 303 K. All uptake experiments were repeated at least twice for calculating the average value and the s.d. After all uptake experiments were completed, the sample quality was checked by out-of-plane XRD and scanning electron microscopy (SEM), see Supplementary Fig. 2. The SEM images show a smooth and homogenous lm without visible defects.
It has to be stated that, at the experimental set-up, the volume in the QCM cell is 40 ml and the argon ow rate is 100 ml min 1. It takes therefore B0.024 s until the cyclohexane partial pressure in the QCM cell is established when switching from pure argon to cyclohexane-enriched argon. Hence, the time constants(see Fig. 3c) are corrected by this value.
References
1. Zhou, H. C., Long, J. R. & Yaghi, O. M. Introduction to metal-organic frameworks. Chem. Rev. 112, 673674 (2012).
2. Farha, O. K. et al. Metalorganic framework materials with ultrahigh surface areas: is the sky the limit? J. Am. Chem. Soc. 134, 1501615021 (2012).
3. Lu, W.-G., Zhong, D.-C., Jiang, L. & Lu, T.-B. Lanthanide coordination polymers constructed from Imidazole-4,5-dicarboxylate and sulfate: syntheses, structural diversity, and photoluminescent properties. Cryst. Growth Des. 12, 36753683 (2012).
4. Gu, Z.-G. et al. Construction of metal-imidazole-based dicarboxylate networks with topological diversity: thermal stability, gas adsorption, and uorescent emission properties. Crystal Growth Design 12, 21782186 (2012).
5. Vermoortele, F. et al. Tuning the catalytic performance of metal-organic frameworks in ne chemistry by active site engineering. J. Materials Chem. 22, 1031310321 (2012).
6. Tan, Y. X., He, Y. P. & Zhang, J. Tuning MOF stability and porosity via adding rigid Pillars. Inorg. Chem. 51, 96499654 (2012).
7. Purewal, J. J. et al. Increased volumetric hydrogen uptake of MOF-5 by powder densication. Int. J. Hydrogen Energy 37, 27232727 (2012).
8. Choi, S., Watanabe, T., Bae, T. H., Sholl, D. S. & Jones, C. W. Modication of the Mg/DOBDC MOF with amines to enhance CO2 adsorption from ultradilute gases. J. Phys. Chem. Lett. 3, 11361141 (2012).
9. Li, J.-R., Sculley, J. & Zhou, H.-C. Metalorganic frameworks for separations. Chem. Rev. 112, 869932 (2011).
10. Lee, J. et al. Metal-organic framework materials as catalysts. Chem. Soc. Rev. 38, 14501459 (2009).
11. Kreno, L. E. et al. Metalorganic framework materials as chemical sensors. Chem. Rev. 112, 11051125 (2011).
12. Xu, C. et al. Hydrogen permeation and diffusion in densied MOF-5 pellets. Int. J. Hydrogen Energy 38, 32683274 (2013).
13. Saha, D., Wei, Z. & Deng, S. Hydrogen adsorption equilibrium and kinetics in metalorganic framework (MOF-5) synthesized with DEF approach. Sep. Purif. Technol. 64, 280287 (2009).
NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications 5
& 2014 Macmillan Publishers Limited. All rights reserved.
ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms5562
14. Zhao, Z., Ma, X., Li, Z. & Lin, Y. S. Synthesis, characterization and gas transport properties of MOF-5 membranes. J. Memb. Sci. 382, 8290 (2011).
15. Zhao, Z. X., Li, Z. & Lin, Y. S. Adsorption and diffusion of carbon dioxide on metal-organic framework (MOF-5). Ind. Eng. Chem. Res. 48, 1001510020 (2009).
16. Karger, J. et al. Unprecedented insight into diffusion by monitoring the concentration of guest molecules in nanoporous host materials. Angew. Chem. Int. Ed. 45, 78467849 (2006).
17. Heinke, L. et al. Assessing guest diffusivities in porous hosts from transient concentration proles. Phys. Rev. Lett. 102, 065901 (2009).
18. Sholl, D. S. Metal-organic frameworks: a porous maze. Nat. Chem. 3, 429430 (2011).
19. Micke, A., Bulow, M. & Kocirik, M. A nonequilibrium surface barrier for sorption kinetics of p-Ethyltoluene on ZSM-5 molecular sieves. J. Phys. Chem. 98, 924929 (1994).
20. Karger, J., Ruthven, D. M. & Theodorou, D. N. Diffusion in Nanoporous Materials (Wiley-VCH, 2012).
21. Barrer, R. M. Zeolites and Clay Minerals as Sorbents and Molecular Sieves (Academic Press, 1978).
22. Shekhah, O., Liu, J., Fischer, R. A. & Wll, C. MOF thin lms: existing and future applications. Chem. Soc. Rev. 40, 10811106 (2011).
23. Munuera, C., Shekhah, O., Wang, H., Wll, C. & Ocal, C. The controlled growth of oriented metal-organic frameworks on functionalized surfaces as followed by scanning force microscopy. Phys. Chem. Chem. Phys. 10, 72577261 (2008).
24. Heinke, L. & Wll, C. Adsorption and diffusion in thin lms of nanoporous metal-organic frameworks: ferrocene in SURMOF Cu2(ndc)2(dabco). Phys.
Chem. Chem. Phys. 15, 92959299 (2013).25. Zybaylo, O. et al. A novel method to measure diffusion coefcients in porous metal-organic frameworks. Phys. Chem. Chem. Phys. 12, 80928097 (2010).
26. Heinke, L. et al. Photoswitching in two-component surface-mounted metal-organic frameworks: optically triggered release from a molecular container. ACS Nano 8, 14631467 (2014).
27. Chui, S. S. Y., Lo, S. M. F., Charmant, J. P. H., Orpen, A. G. & Williams, I. D. A chemically functionalizable nanoporous material Cu-3(TMA)(2)(H2O)(3)(n). Science 283, 11481150 (1999).28. Schlichte, K., Kratzke, T. & Kaskel, S. Improved synthesis, thermal stability and catalytic properties of the metal-organic framework compound CU3(BTC)(2). Micropor. Mesopor. Mater. 73, 8188 (2004).
29. Alaerts, L. et al. Probing the Lewis acidity and catalytic activity of the metal-organic framework Cu-3(btc)(2) (BTC benzene-1,3,5-tricarboxylate).
Chemistry 12, 73537363 (2006).30. Plaza, M. G. et al. Propane/propylene separation by adsorption using shaped copper trimesate MOF. Micropor. Mesopor. Mater. 157, 101111 (2012).
31. Chmelik, C. et al. Adsorption and diffusion of alkanes in CuBTC crystals investigated using infra-red microscopy and molecular simulations. Micropor. Mesopor. Mater. 117, 2232 (2009).
32. Dosseh, G., Xia, Y. D. & Alba-Simionesco, C. Cyclohexane and benzene conned in MCM-41 and SBA-15: connement effects on freezing and melting.J. Phys. Chem. B 107, 64456453 (2003).33. Shekhah, O., Wang, H., Zacher, D., Fischer, R. A. & Wll, C. Growth mechanism of metalorganic frameworks: insights into the nucleation by employing a step-by-step route. Angew. Chem. Int. Ed. 48, 50385041 (2009).
34. Sauerbrey, G. Verwendung von Schwingquarzen zur Wagung dnner Schichten und zur Mikrowagung. Zeitschrift Fur Physik 155, 206222 (1959).
35. Heinke, L. & Karger, J. Correlating surface permeability with intracrystalline diffusivity in nanoporous solids. Phys. Rev. Lett. 106, 074501 (2011).
36. Hibbe, F. et al. The nature of surface barriers on nanoporous solids explored by microimaging of transient guest distributions. J. Am. Chem. Soc. 133, 28042807 (2011).
37. Zhuang, J.-L., Ceglarek, D., Pethuraj, S. & Terfort, A. Rapid room-temperature synthesis of metalorganic framework HKUST-1 crystals in bulk and as oriented and patterned thin lms. Adv. Funct. Mater. 21, 14421447 (2011).
38. Van Assche, T. R. C. et al. High adsorption capacities and two-step adsorption of polar adsorbates on copperbenzene-1,3,5-tricarboxylate metalorganic framework. J. Phys. Chem. C 117, 1810018111 (2013).
Acknowledgements
L.H. is indebted to the Baden-Wrttemberg Stiftung for the nancial support of this
research project by the Eliteprogramme for Postdocs. Z.G. is grateful for a PhD fel
lowship donated by the China Scholarship Council (CSC).
Author contributions
All authors contributed to writing the manuscript and have approved the nal version of
the manuscript. L.H. planned and performed the experiments. Z.G. synthesized and
characterized the powder MOFs. C.W. was involved in planning the experiments.
Additional information
Supplementary Information accompanies this paper at http://www.nature.com/naturecommunications
Web End =http://www.nature.com/
http://www.nature.com/naturecommunications
Web End =naturecommunications Competing nancial interests: The authors declare no competing nancial interests. Reprints and permission information is available online at http://npg.nature.com/reprintsandpermissions/
Web End =http://npg.nature.com/
http://npg.nature.com/reprintsandpermissions/
Web End =reprintsandpermissions/
How to cite this article: Heinke, L. et al. The surface barrier phenomenon at the loading
of metal-organic frameworks. Nat. Commun. 5:4462 doi: 10.1038/ncomms5562 (2014).
6 NATURE COMMUNICATIONS | 5:4562 | DOI: 10.1038/ncomms5562 | http://www.nature.com/naturecommunications
Web End =www.nature.com/naturecommunications
& 2014 Macmillan Publishers Limited. All rights reserved.
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer
Copyright Nature Publishing Group Jul 2014
Abstract
Loading with guest molecules is a crucial step for most applications of porous materials. For metal-organic frameworks, which are one of the most intensely investigated classes of porous materials, the experimentally determined rate of mass transfer into the material may vary by several orders of magnitude for different samples of the same material. This phenomenon is commonly attributed to the presence of so-called surface barriers, which appear to be omnipresent but poorly understood. Here we quantitatively study this phenomenon with a quartz crystal microbalance, using well-defined, highly crystalline, epitaxially grown thin films of metal-organic frameworks as a model system. Our results clearly demonstrate that surface barriers are not an intrinsic feature of metal-organic frameworks, as pristine films do not exhibit these limitations. However, by destroying the structure at the outer surface, for instance by exposure to air or water vapour, surface barriers are created and the molecular uptake rate is reduced.
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer