Joel E.
Schmidt
a,
Dan
Xie
b and
Mark E.
Davis
*a
aChemical Engineering, California Institute of Technology, Pasadena, CA 91125, USA. E-mail: mdavis@cheme.caltech.edu
bChevron Energy Technology Company, Richmond, CA 94802, USA
First published on 27th July 2015
There are several distinct two-dimensional zeolite building layers that can condense through different stacking arrangements of the layers to form various three-dimensional framework materials. All known building layers are dense layers in that they do not contain 8-membered ring (MR) or larger pores perpendicular to the two-dimensional layers. Herein, we report a new material (CIT-10) that consists of a two-dimensional layer (termed “rth” layer) that contains an 8 MR perpendicular to the layer. Calcination of CIT-10 forms pure-silica RTH (SSZ-50). CIT-10 can be pillared to form a new framework material with a three-dimensional pore system of 8 and 10 MRs, denoted CIT-11, that can be calcined to form a new microporous material, denoted CIT-12.
In a topotactic condensation, a three-dimensional (3D) framework structure is formed from a two-dimensional (2D) layered silicate by condensation of surface silanol groups (Si-OH), releasing water. Some of the initial framework materials prepared via topotactic condensation were FER, formed from the layered precursor denoted PREFER,15 and MWW, formed from the layered precursor MCM-22(P).16 After these pioneering efforts, several additional frameworks have been prepared using topotactic condensation, and they include (layered precursor given in parentheses): AST (β-helix-layered silicate),17CAS-NSI intermediate (EU-19, NU-6(1)),18–20CDO (PLS-1, RUB-36),19,21FER (PREFER),15MTF (HPM-2),22MWW (MCM-22),16PCR (IPC-4 prepared by disassembly of UTL),23RRO (RUB-39),24RWR (RUB-18)25 and SOD (RUB-15).26 The layered materials that form 3D frameworks can be built by different stacking arrangements of a few 2D building layers (such as CAS, FER, HEU, MWW and RWR).8,9 Additionally, methods have been developed to prepare MFI nanosheets that are a single unit cell thick,27,28 however, this material generally is not considered to be a building layer.29
The silanol groups of the layered zeolite precursors can also be used to prepare larger pore materials through a pillaring process. This process normally uses dichlorodimethylsilane or diethoxydimethylsilane to react with the silanol groups to form pillars that are coordinated to two methyl groups (or two hydroxyl groups after calcination). This process is typically carried out in acidic media under hydrothermal conditions. Some of the layered materials that have been pillared include PREFER, MWW(P), PLS-1, MCM-47, RUB-36, RUB-39 and Nu-6(1).8,30,31 Additionally, related strategies to prepare porous materials include delamination or exfoliation. Recently, it has also been shown to be possible to introduce catalytic activity in the pillars.32,33 Excellent reviews of the above strategies are available.8,9
All of the previously reported layered zeolite precursors are dense layers, that is, they contain no pores (8-membered ring (MR) or larger) that are perpendicular to the layers. The MWW layer contains a sinusoidal 10 MR channel parallel to the ab-plane, but it is still dense as this channel is not perpendicular to the layer. However, the nanosheets of MFI that are single unit cell thick do contain a 10 MR perpendicular to the layer, a medium size pore.27 We recently reported a method to prepared high-silica heulandite (denoted CIT-8) via topotactic condensation from a layered precursor (denoted CIT-8P), that was prepared using a diquaternary organic structure directing agent (OSDA) in fluoride-mediated syntheses.34 In that case, the building layer that forms CIT-8 (HEU) is the same as that of RUB-41 (RRO), but is formed from a different stacking of the HEU building layer: AA stacking gives the RRO structure while AA′ stacking (where the A′-layer is related to the A-layer by a 180 degree rotation) gives the HEU structure.25 CIT-8 was prepared from fluoride-mediated, aluminosilicate inorganic conditions across a relatively narrow composition range. It is interesting to note with this material that the OSDA used was considerably larger than what is normally found in preparing topotactic materials such as piperdines,15 as well as methyl, ethyl and propyl substituted ammoniums.31
In the absence of aluminium, we have found conditions to prepare the layered precursor to pure-silica RTH, denoted CIT-10. This layered material can be directly calcined to prepare pure-silica RTH (SSZ-50 (ref. 35)) or can be pillared, leading to a new microporous material (denoted CIT-11), that is stable to calcination (calcined material denoted CIT-12). CIT-10 is a layered material composed of a new type of 2D building layer (termed “rth”, according to the nomenclature defined in ref. 9) containing an 8 MR channel going through the layer (8 MR pore dimensions of 5.6 × 2.5 Å). The discovery of CIT-10 adds a new group of layered zeolite precursors and is the first to contain an 8 MR through the 2D layer. Pure-silica RTH is now the sixth known microporous material that can be obtained by both direct synthesis and topotactic condensation.
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Fig. 2 PXRD of CIT-10 (lower) and calcined CIT-10 (pure silica RTH, upper) with selected crystallographic indicies. |
To determine the mechanism of formation of pure-silica RTH, the materials were studied using 13C CPMAS NMR, 29Si MAS and CPMAS NMR and variable temperature PXRD. The 13C CPMAS NMR of CIT-10 (Fig. 4) shows that the diquat OSDA was occluded intact in the material. It is interesting to note that many of the peaks in this spectrum are split, indicating that otherwise equivalent carbon atoms are present in non-equivalent environments; this has been previously reported in layered materials.10 The 29Si MAS and CPMAS NMRs of CIT-10 are shown in Fig. 5. CIT-10 was studied using CPMAS NMR in addition to MAS NMR to confirm the resonances (organic-containing materials often exhibit a poor signal-to-noise ratio). In the as-made material there are three resonances at −113, −107 and −102 ppm with approximate area ratios of 8:
5
:
3. The signals at −113 and −107 ppm are assigned to Q4 silicon, Si(OSi)4 coordination, while the signal at −102 ppm is assigned to Q3 silicon, Si(OSi)3(OH) coordination. The presence of Q3 silicon is expected in a layered material. The ratio of Q3/(Q3 + Q4) silicon in the as made material is 0.23, which is very close to the theoretical value of 0.25 (see the ESI Fig. S1† for additional details). Upon calcination, the 29Si MAS NMR spectrum no longer shows the presence of any Q3 silicon and instead shows 3 resonances in the Q4 region at −116, −114 and −109 ppm, with area ratios of 1
:
2
:
1. These area ratios agree with the crystal structure of RTH, as it contains 4 independent T-sites.
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Fig. 4 13C NMR of the diquat in D2O (lower, methanol added as an internal standard), 13C CPMAS NMR of CIT-10 showing the occluded diquat (middle) and 13C CPMAS NMR of CIT-11 (upper). |
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Fig. 5 29Si (a) MAS NMR of CIT-10, (b) CPMAS NMR of CIT-10, (c) MAS NMR of pure-silica RTH prepared by calcination of CIT-10, (d) MAS NMR of CIT-11 and (e) MAS NMR of CIT-12. |
The structural mechanism of condensation was determined by using variable temperature PXRD as well as RED. The variable temperature PXRD of CIT-10 is shown in Fig. 7. When compared with the PXRD patterns of RTH in Fig. 2 (labelled with the crystallographic indices), it is apparent that peak positions for hk0 reflections remain during heating, while the peak positions for the hkl (l ≠ 0) reflections are shifted to higher 2θ angles (i.e., lower d-spacing). This result indicates that the 3D RTH structure forms via topotactic condensation along the c-axis, and that the a and b axes are intact in the layered material. The structural change was further confirmed by studying CIT-10 using RED (Fig. 6). The RED clearly shows that CIT-10 is ordered in the a and b directions (indicated by clearly defined diffraction spots), but that some disorder is present in the c direction (indicated by diffraction streaks between diffraction spots). Thus, results from using both techniques confirm that CIT-10 contains 2D sheets in the a and b directions that are separated by a disordered organic in the c direction.
The TGA data are consistent with the condensation temperature observed in the variable temperature PXRD. In the variable temperature PXRD, the structure of the layered material is intact until 330 °C, then the low angle peak corresponding to the 001 direction abruptly disappears. This reflection is absent at the PXRD pattern taken at 380 °C, then begins to emerge around 430 °C. From the TGA trace in Fig. 8, a sharp mass loss occurring around 375 °C is seen, and is in the same temperature range where the low angle peak disappeared in the variable temperature PXRD. The rapid change observed with RTH is in contrast to the TGA trace and structural changes observed with CIT-8P (layered precursor to HEU) where a gradual shift in position of the low-angle peak was observed along with the gradual decrease in mass.34
A detailed analysis of the structural changes occurring during the topotactic condensation process for RUB-39 have been reported as a series interconnected endothermic (OSDA decomposition and condensation of silicate layers) and exothermic (OSDA combustion) processes that are dominated by combustion of the OSDA.44 It was found that as soon as the OSDA was removed, the condensation occurred. Attempts to stabilize the intermediate material were not successful. The sharp mass loss over a narrow temperature range observed with CIT-10 is similar to what is reported with RUB-39, and for the latter the loss was ascribed to a fast series of connected processes that include OSDA decomposition and combustion as well as condensation of the silicate layers.
CIT-10 has an 8 MR channel running through the layer along the c axis, with dimensions of 2.5 × 5.6 Å. As the structure condenses along the c-axis, a second 8 MR channel system running through the a-axis is formed, and a cavity is created at the intersection of the two 8 MR channels, forming the RTH framework structure. The condensation process is shown schematically in Fig. 9. As the schemes in the figure depict, the RTH layer is actually a half unit cell thick compared to the final RTH framework unit cell.
Table 1 shows the comparisons of the d-spacing corresponding to the first and most intense PXRD peak for known 2D layered materials, and the corresponding d-spacing shrinkage after topotactic condensation to form 3D framework materials. In most of the cases (including CIT-10) the d-spacing shrinkage due to topotactic condensation is around 2 Å, an observation that has been discussed by Roth et. al.46 It is also interesting to note that although the OSDAs used to make CIT-10 and CIT-8P are very similar, the latter demonstrated a d-spacing contraction nearly twice that of the former.
2D zeolite | d-spacing (Å) | 3D zeolite | Corresponding d-spacing (Å) | d-spacing shrinkage (Å) | Ref. |
---|---|---|---|---|---|
CIT-10 | 11.8 | Siliceous RTH | 9.8 | 2.0 | This work |
RUB-36 | 11.1 | RUB-37 (CDO) | 9.2 | 1.9 | 45 |
MCM-22P | 26.9 | MCM-22 (MWW) | 24.9 | 2.0 | 16, 46 |
HMP-2 | 17.5 | MCM-35 (MTF) | 15.4 | 2.1 | 22 |
RUB-39 | 10.8 | RUB-41 (RRO) | 8.7 | 2.1 | 24 |
R-RUB-18 | 9.1 | RUB-24 (RWR) | 6.8 | 2.3 | 25 |
EU-19 | 11.5 | EU-20 (CAS-NSI) | 8.3 | 3.2 | 19 |
PREFER | 13.1 | FER | 9.4 | 3.7 | 15 |
CIT-8P | 12.8 | CIT-8 (HEU) | 8.9 | 3.9 | 34 |
In attempting to pillar CIT-10, a wide range of conditions were explored including acid type and concentration, aqueous versus ethanolic acid, silane source, and reaction temperature and time. The optimal conditions to pillar CIT-10 were found to be 1.25 M HCl in ethanol with either dichlorodimethylsilane or diethoxydimethylsilane at 175 °C for 24 hours. Other conditions lead to what appeared to be pillared materials (based on PXRD), but these materials exhibited very weak X-ray reflections. We interpret these results as indicating framework destruction, and these solids were often not stable to calcination. This phenomenon has been observed before, i.e., that acidic ethanol is the only effective medium to carry out pillaring. It has been postulated that the reason for this is that effective pillaring takes place when the rate of removal of OSDA is well matched by the rate of silylation.30 It should be noted that while we made no special efforts to preclude trace amounts of water in these syntheses (such as working in a glovebox or using a Schlenk line), the water content was likely very low.
The X-ray diffraction results of pillared CIT-10 are shown in Fig. 10. As can be observed from the PXRD patterns, pillaring causes a shift in the most intense reflection from 7.5° 2θ in CIT-10 to 6.8° 2θ in CIT-11 (i.e., 1.1 Å expansion). This peak continues to shift to 7.7° 2θ in CIT-12 (after calcination). The 13C CPMAS NMR of CIT-11 (Fig. 4) shows that the majority of the organic was removed under acidic conditions (while CPMAS NMR is not quantitative this was confirmed by TGA, shown in Fig. 8). This result was expected as a change in color of the acidic medium was observed. The strong resonance observed near −1 ppm is consistent with (CH3)2Si carbon that is expected from the pillaring. (Prior to NMR analysis it was necessary to degas the material under vacuum at 150 °C to remove any residual ethanol or acetone.) The TGA analysis of CIT-11 (Fig. 8) shows several distinct mass loss regions. The first mass loss of 5% is attributed to the loss of water and possibly residual ethanol or acetone (material was dried in air at 100 °C prior to analysis but not under vacuum as was done with the NMR sample). The second sharp mass loss begins around 300 °C, and is attributed to removal of residual organic (present in 13C CPMAS NMR). There is a third, distinct region of mass loss that begins around 500 °C and is attributed to combustion of the Si–CH3 groups to form hydroxyl groups.
The 29Si NMR spectra are consistent with a pillared material (Fig. 5). In CIT-10, both Q4 and Q3 silicon environments are observed, consistent with a layered material (vide supra). In the pillared material, CIT-11, 29Si NMR resonances are observed at −113.5, −108.4, −104.5 and −15.3 ppm with approximate area ratios of 20:
8
:
2
:
5. The resonances at −113.5 and −108.4 are assigned to Q4 silicon and the resonance at −104.5 is assigned to residual Q3 silicon. The Q3/(Q3 + Q4) ratio in the pillared material is 0.07, a significant decrease from 0.23 in CIT-10, indicating that a substantial amount of Q3 species have been consumed in linking the layers of the material. The resonance at −15.3 is assigned to bridging silanol groups bonded to two methyl groups, that is Si(CH3)2(OSi)2 coordination. The ratio of (Q2 + Q3)/(Q2 + Q3 + Q4) is 0.25, consistent with the expected value from the RTH layer (see ESI†). Upon calcination the material exhibits a broad resonance around −110 ppm. A single broad resonance has been observed in other pillared, calcined materials such as PLS-4.47 No obvious peak for Q2 silicon can be seen near −90 ppm, but it is likely obscured by the much broader resonance.
The structure of CIT-11/12 is a 3D pore system consisting of 8 and 10 MRs, shown in Fig. 9. The 8 MR running the in the c-direction perpendicular to the RTH layer remains intact. The pillars form two new ring sizes as the previous 8 MR along the a-direction expands to a 10 MR and the 6 MR along the b-direction expands to an 8 MR. This means that the previous 2D ring system in RTH expands be a 3D ring system in CIT-11/12.
The pore system of CIT-12 was confirmed using argon adsorption. The results from this analysis are shown in Fig. S2† compared to pure-silica RTH as well as zeolite 5A and pure-silica BEA. We chose to plot all of these isotherms on the same graph as the shape of the isotherm in the low pressure regime is an indication of the pore size distribution. The comparison of the low pressure region of the argon adsorption isotherms indicates that this material has a pore system that has expanded compared to pure-silica RTH (8 MRs) but is smaller than pure-silica BEA (12 MRs), consistent with the structure solution.
Footnote |
† Electronic supplementary information (ESI) available: Figure of the RTH-type layer with T-site labels and log-plot high resolution argon adsorption isotherms. See DOI: 10.1039/c5sc02325d |
This journal is © The Royal Society of Chemistry 2015 |