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Solvent-free hierarchization of zeolites by carbochlorination

Martin Nichterwitz , Sven Grätz , Winfried Nickel and Lars Borchardt *
Inorganic Chemistry, TU Dresden, Bergstrasse 66, D-01062 Dresden, Germany. E-mail: lars.borchardt@tu-dresden.de

Received 21st October 2016 , Accepted 22nd November 2016

First published on 22nd November 2016


Abstract

Carbochlorination, a solvent-free top-down process, is a novel pathway for the hierarchization of zeolites. In contrast to other methods no further washing steps are required. The employed method should serve as a model system for the “upcycling” of coked and deactivated zeolites accumulated by the industry. In order to establish a basic understanding of the process, zeolite H-Y was taken as a model system and a thorough investigation of important reaction parameters, like chlorination temperature, time and concentration, carbon loading, and Si/Al ratio, was performed. Under optimized conditions, we have been able to hierarchize H-Y with high yield, doubling the mesopore volume while maintaining the crystallinity and surface area.


Introduction

Zeolites are microporous, crystalline aluminosilicates that are widely used as heterogeneous catalysts,1–4 catalyst supports,5,6 ion-exchangers,7 molecular sieve membranes,8,9 in the catalytic conversion of biomass10–12 and many more advanced applications.13 Their final performance in all of the mentioned applications strongly depends on the accessibility of the active sites, which is largely affected by pore size and pore connectivity.14,15 Diffusion limitations within these pores can lead to severe issues such as hindered mass transport, pore blocking, and especially in the field of heterogeneous catalysts, the formation of coke. This causes a decreasing catalytic activity and lifetime as well as undesirable product selectivities.16 Hierarchization, the incorporation of an additional transport system into the material, can overcome these obstacles and enhance the diffusion and mass flow properties of a zeolite material.17–27 Several synthesis routes are known for hierarchical zeolites, which are usually classified as bottom-up or top-down methods.17–19,23,26,28,29 Bottom-up approaches commonly apply hard- or soft-templates, which serve as a placeholder for the future secondary porosity, directly into the synthesis of the zeolite framework.23,30 Commonly carbon nanomaterials31–35 but also organic aerogels,36 salts such as CaCO3 (ref. 37) or biological templates38 have been used as hard-templates, while structure-directing agents (SDA) such as surfactants are applied as soft-templates.39,40 Non-templating synthesis relies on aggregation of nanocrystals,41,42 the crystallization of amorphous gels43 or modification of crystal growth direction.23 However, upscaling and industrial implementation of most of these approaches is difficult due to high production costs that arise from the expensive template nanostructures, long synthesis time, including the necessary post-synthesis template removal, or the fact that some approaches are only applicable to a few zeolite structures.23,30 Top-down approaches, in turn, are based on post-synthesis treatments with acids and bases that leech either atoms (Si or Al) or fragments out of the framework, consequently creating mesopores. With dealumination44–46 by acids, and desilication47,48 by NaOH or organic hydroxides two main modification routes exist. However, many of the existing top-down methods require one or multiple washing steps, what makes this process time-consuming and waste-producing. The material loss during etching strongly depends on the applied etching agents, but it is often in the range of ∼50%.49 There are only a few publications reporting on the hierarchization preventing huge materials loss.50,51 In this respect particularly solvent-free methods have been developed allowing to synthesize and modify porous materials such as metal organic frameworks52–54 and zeolites.55

Here we present a radical new approach for the hierarchization of zeolites that is based on a one-step gas phase reaction (eqn (1) and (2)). This reaction, a carbochlorination, is known from the Kroll-process, the industrial process commonly used for the synthesis of titanium metal at temperatures between 750 and 1000 °C.56,57

 
Al2O3(s) + 3C(s) + 3Cl2(g) → 2AlCl3(g) + 3CO(g)(1)
 
SiO2(s) + 2C(s) + 2Cl2(g) → SiCl4(g) + 2CO(g)(2)

We utilized zeolite Y as model system because it is one of the most important heterogeneous catalysts in petrochemical industry, e.g. in fluid catalytic cracking (FCC) and hydrocracking.58

This approach is in addition motivated by the idea to re-use coked and deactivated zeolites accumulating after a catalytic reaction. Hot chlorine gas in combination with the deposited carbon (coke) inside the zeolite framework will lead to etching of Si and Al species (eqn (1) and (2)) and thus the generation of mesoporosity (Fig. 1). No post-synthesis washing steps are required and the yield is higher as compared to traditional top-down approaches. To study this approach systematically, defined amounts of carbon were brought into the material by infiltration and pyrolysis of furfuryl alcohol (FA). We investigated the influence of different parameters such as chlorination temperature, reaction time, carbon concentration, Si/Al ratio and chlorine concentration on the porosity, hierarchization, crystallinity, and acidity of the resulting zeolites. We have shown that a high amount of mesoporosity can be introduced while ensuring a low material loss.


image file: c6ta09145h-f1.tif
Fig. 1 Reaction scheme for solvent-free hierarchization of zeolite Y by carbochlorination.

Experimental section

Zeolite–carbon composite synthesis

5 g of commercially available zeolite H-Y (CBV 400, Zeolyst International, SiO2 to Al2O3 molar ratio: 5.1, specific surface area: 730 m2 g−1; CBV 901, Zeolyst International, SiO2 to Al2O3 molar ratio: 80, specific surface area: 700 m2 g−1) were impregnated with 2 mL solution of furfuryl alcohol (FA) and ethanol (EtOH) by mixing with mortar and pestle for 15 min. The composition of each solution is shown in Table 1. The infiltrated zeolite was carbonized under argon flow (>110 mL min−1) with several temperature steps.
Table 1 Preparation of zeolite–carbon composites
Sample Zeolite V FA/mL V EtOH/mL V (FA mzeolite−1)/mL g−1
Composite 1 (C1) HY-5 0.25 1.75 0.05
Composite 2 (C2) HY-5 0.50 1.50 0.10
Composite 3 (C3) HY-5 1.00 1.00 0.20
Composite 4 (C4) HY-80 0.25 1.75 0.05
Composite 5 (C5) HY-80 0.50 1.50 0.10
Composite 6 (C6) HY-80 1.00 1.00 0.20


Samples were treated for 2 h at room temperature, then heated for 24 h at 80 °C (heating rate 60 K h−1), further for 8 h at 150 °C (heating rate 60 K h−1) and finally for 4 h at 600 °C (heating rate: 300 K h−1).

Carbochlorination

The black zeolite–carbon-composites were flushed under argon atmosphere (150 mL min−1) for 30 min, followed by heating to the reaction temperature (heating rate 450 K h−1). Subsequently, the gas flow was changed to a mixture of 10 mL min−1 chlorine and 70 or 110 mL min−1 argon while the temperature was kept for 2 h, 4 h or 8 h, respectively. Then, the samples were cooled/heated from the reaction temperature (400–900 °C) to 600 °C under argon flow for 1 h and finally treated with 80 mL min−1 hydrogen for another 1 h. Afterwards the samples were cooled down to room temperature under argon.

Sample nomenclature

The sample name consists of its reaction parameters and has the following structure: Cα-β-γ-δ/ε, where Cα is the composite, β is the reaction temperature in °C, γ is the reaction time in h, δ is the chlorine flow in mL min−1 and ε is the argon flow in mL min−1. For example, C1-500-4-10/70 means a carbochlorination of composite 1 at 500 °C for 4 h with a gas mixture of chlorine (10 mL min−1) and argon (70 mL min−1).

Calcination

Before temperature-programmed ammonia desorption (TPAD) or inductively coupled plasma optical emission spectrometry (ICP-OES) measurements, some samples were additionally calcined under air for 6 h at 550 °C (10 K min−1).

Characterization

The argon physisorption was measured at −186 °C on an Autosorb iQ (Quantachrome Instruments) after vacuum activation at 300 °C for 16 h. Specific surface areas (SSABET) were evaluated using the multipoint BET equation according to the criteria stated from Rouquerol et al.59 Pore size distributions (PSDs) were calculated using the non-local density functional theory (NLDFT) method (adsorption branch kernel) for argon adsorbed on zeolites/silica with a cylindrical/spherical pore shape at −186 °C. This kernel was also used to calculate specific surface area (SSADFT), total pore volumes (PVDFT), micropore volume (PVmicro,DFT, dpore < 2 nm) and mesopore volume (PVmeso,DFT, dpore 2–50 nm).

Nitrogen physisorption experiments were operated at −196 °C on a Quadrasorb evo (Quantachrome Instruments). Total pore volumes (PVtotal) were determined at p/p0 = 0.95. The t-plot method (p/p0 = 0.2–0.5) was used to determine the micropore volume (PVmicro) and external surface area (SEXT). Determination of specific surface areas (SSABET) was done similar to argon physisorption. Nitrogen physisorption isotherms were measured after vacuum activation at 230 °C for 2 h.

Powder X-ray diffraction (XRD) measurements were performed on a XPERT PRO (PANanalytics) using Cu Kα radiation as fourfold determination in the 2θ range 5–50° and 0.026° step width. The crystallinity was estimated according to the standardized procedure ASTM D 3906-03.60 Therefore the area of the 15.7°, 18.7°, 20.4°, 23.7°, 27.1°, 30.8°, 31.5° and 34.2° 2θ reflections (equivalent to the [331], [511], [440], [533], [642], [822], [555] and [664] hkl planes, respectively) were taken after background subtraction in relation to the starting material HY (CBV 400, Zeolyst Int.).

Acidity was investigated with temperature-programmed ammonia desorption (TPAD) using a Belcat Basic (BEL Japan, Inc.) in the temperature range from 100 to 700 °C. Samples (around 40 mg) were activated at 500 °C (10 K min−1) for one hour under He (50 mL min−1) and then cooled down to 100 °C. After cooling the sample was loaded with pure ammonia (50 mL min−1) for 30 min. Desorption of physisorbed ammonia was performed by streaming with He (50 mL min−1) at 100 °C for 5 h. The chemisorbed ammonia was desorbed by heating the sample from 100 °C to 700 °C (10 K min−1) under constant He flow (20 mL min−1).

Thermogravimetric (TG) and mass spectroscopy (MS) measurements were carried out with STA 409 PC Luxx (NETZSCH) under synthetic air (80% N2, 20% O2) from 25 to 1250 °C with a heating rate of 5 K min−1. The amount of residual carbon (Cres) is calculated by the difference of weight loss between 400 to 800 °C from the zeolite–carbon composite to the carbochlorinated sample.

Scanning electron microscopy (SEM) images of gold sputtered samples were performed using a DSM-982 Gemini (Zeiss) with a magnification of 50[thin space (1/6-em)]000 and 6 kV acceleration voltage.

Optical emission spectroscopy (ICP-OES) measurements on an Optima 7000DV (Perkin Elmer) indicated the Si and Al content in the samples. Si ratio was measured with a radial detector (251.611 nm) and Al concentration in axial position (396.153 nm). Digestion of around 10 mg sample was performed with 150 μL HNO3, 150 μL HF and 150 μL HCl in a microwave at 130 °C (ramp: 5 min) for 15 min. Afterwards complexation with 1.5 mL saturated boric acid was realized as well in a microwave at 130 °C (ramp: 5 min) for 15 min.

Results and discussion

The proof of principle of this new hierarchization strategy is based on a commercially available zeolite H-Y which was impregnated with furfuryl alcohol. After coking, a defined gas mixture of chlorine and argon was applied to study the hierarchization process. First, the influence of chlorination temperature on porosity and textural properties of the hierarchical material is discussed. In continuing sections, the influence of carbon content, chlorination time, chlorine concentration, and Si/Al-ratio will be discussed.

Chlorination temperature

Hierarchization was performed at five different temperatures from 400 to 800 °C on carbon–zeolite-composite 2, which has a carbon content of about 7.26 w% (determined by TG-MS). All samples were treated for 4 h with a gas mixture of 10 mL min−1 chlorine and 70 mL min−1 argon. With higher reaction temperature, the hierarchization evolves and the amount of created mesopores increases. The Ar-physisorption measurement (Fig. 2) of the parent material (H-Y 5 pure) shows a type I isotherm characteristic for materials with almost exclusive microporous character. With higher chlorination temperatures the isotherms show increasing gas uptake in the p/p0 range from 0.6 to 0.8. The isotherm shape turns into type IV exhibiting a large hysteresis, which is typical for mesoporous materials. We can state that with higher chlorination temperature the total pore volume as well as the mesopore volume increases, while the micropore volume decreases. Consequently we can observe an increase in the SSAEXT as well (Table 2). This trend reaches a maximum for 700 °C with 0.40 cm3 g−1 total pore volume, but brakes down at 800 °C where the sample shows a lower total pore volume (0.29 cm3 g−1). The sample treated at 400 °C shows the lowest total pore volume (0.23 cm3 g−1) due to the high content of residual carbon within the pore network. At low temperatures (e.g. 400 °C) the etching is less efficient while at too high temperature (>800 °C) the destruction of the zeolite system becomes excessive. This effect is also reflected by the decrease of the specific surface area with the increase in chlorination temperature (Table 2).
image file: c6ta09145h-f2.tif
Fig. 2 Ar physisorption isotherms at −186 °C for samples of composite 2 (0.10 mL g−1) carbochlorinated at different temperatures. Samples: 400 °C (C2-400-4-10/70), 500 °C (C2-500-4-10/70), 600 °C (C2-600-4-10/70), 700 °C (C2-700-4-10/70), 800 °C (C2-800-4-10/70).
Table 2 Characterization data of carbochlorinated samples at different temperatures. Physisorption data derived from Ar-isotherms measured at −186 °C
Samplea Si/Alb/mol mol−1 SSABETc/m2 g−1 SSAEXTd/m2 g−1 PVtotale/cm3 g−1 PVmicrod/cm3 g−1 PVmesof/m3 g−1 HFg C XRD /% Total acidityi/mmol g−1 C res /w% Yieldk/w%
a Sample description given in Experimental section. b ICP-OES elemental analysis. c Multi-point BET-method. d t-Plot method p/p0 from 0.2 to 0.5. e Total pore volume at p/p0 = 0.95. f PVmeso = PVtotal − PVmicro. g Hierarchy factor HF = (PVmicro/PVtotal)(SEXT/SSABET).61 h % XRD intensity/HY after ASTM 3906-03.60 i Total acidity determined by TPAD. j Residual carbon (Cres) analyzed by TG; Cres = CsampleCH-Y 5 pure. k Calculated by weighing before and after carbochlorination.
H-Y 5 pure 3.0 751 72 0.33 0.29 0.12 0.015 100 0.995
C2-400-4-10/70 3.7 361 135 0.23 0.14 0.16 0.034 46 0.685 7.17 94
C2-500-4-10/70 7.0 378 169 0.37 0.13 0.27 0.050 51 0.394 2.82 76
C2-600-4-10/70 18.3 214 161 0.39 0.04 0.37 0.038 22 0.227 0.71 72
C2-700-4-10/70 13.9 189 163 0.40 0.03 0.41 0.031 19 0.195 1.28 67
C2-800-4-10/70 8.7 165 120 0.29 0.04 0.28 0.038 22 0.171 0.55 71


Verboekend et al. introduced the hierarchical factor (HF), which is defined as a product of the relative micropore volume (Vmicro/Vtotal) and the relative mesopore surface area (Smeso/SSA).61 Its purpose is to characterize hierarchization efficiency. Carbochlorination of composite 2 shows a good hierarchization performance at 500 °C with an increased HF of 0.050. As against at higher reaction temperatures the HF decreases to 0.031 for 700 °C and 0.038 for 800 °C due to an excessive introduction of mesopore volume.

Moreover, the chlorination temperature not only influences the amount of mesoporosity but also the pore size distribution of the hierarchical zeolites (Fig. 3). With an increase of reaction temperature the pore size is shifted to larger pore widths. Samples at 400 °C and 500 °C already show some pores with a diameter of 4 and 7 nm, respectively. For 600 °C, a broadening of the pore size distribution with pores from 6 to 16 nm is observed, while samples at 700 and 800 °C show two main pore sizes about 10 and 16 nm (Fig. 3b).


image file: c6ta09145h-f3.tif
Fig. 3 (a) Cumulative pore volume (b) dV(log[thin space (1/6-em)]d) pore size distribution calculated with NLDFT (adsorption branch kernel) from argon isotherms (Fig. 2).

The effect of a more intense etching reaction at higher temperatures can also be seen on SEM images. Fig. 4a shows the parent material with intact crystals. From Fig. 4b to d (corresponding to 400, 500 and 600 °C) we observe increasing leaching effects on the edges and faces of the crystals.


image file: c6ta09145h-f4.tif
Fig. 4 SEM images of carbochlorinated samples from composite 2 at temperatures from 400 to 800 °C.

Nevertheless, the particle morphology and integrity remains conserved. Fig. 4e and f (700 and 800 °C) however show heavily attacked faces and edges after the carbochlorination. This destructive effect on the zeolite framework at higher temperatures is also visible in the powder XRDs (Fig. 5), where we notice a broadening of reflexes for 400 and 500 °C and a more and more amorphous signal from 17 to 30° 2θ for the samples synthesized at 600, 700 and 800 °C. This trend can be quantified by the decreasing relative crystallinity with respect to that of H-Y 5 shown in Table 2. Although the main reflex [111] at 6° 2θ is visible in the whole temperature range, the relative crystallinity calculated from eight main reflexes according to ASTM D 3906-03 (ref. 60) (15.7°, 18.7°, 20.4°, 23.7°, 27.1°, 30.8°, 31.5° and 34.2° 2θ) decreases to 46% at 400 °C and 22% at 800 °C. The similar trend is observed for the total acidity, measured by TPAD (Fig. 6), that decreases with increasing reaction temperatures. The total acidity decreases from 69% at 400 °C, to 40% at 500 °C down to 18% at 800 °C compared to the parent material (H-Y 5 pure). In addition ICP-OES measurements state out that with increasing chlorination temperature the molar Si to Al ratio increases from 3.0 (H-Y untreated) to 18.3 (600 °C) and then decreases to 8.7 (800 °C). This implies that at lower temperatures (<600 °C) preferably Al-species are etched from the framework (dealumination). This process can be easily followed using 29Si CP-MAS NMR (Fig. S1), where a decrease of Si(nAl)-species can be observed. Furthermore, by employing 27Al CP-MAS NMR (Fig. S2) it can be shown, that the leeched aluminum is not deposited as extra-framework species but removed completely. The evidence of which is the increasing ratio of AlIVa to AlVI. At higher temperature (>600 °C) Al-species seem to be less favored and Si-species are etched in higher amount (desilication), however, there is still less Al than in the starting material. Dealumination at temperatures below 600 °C corresponds to the significant decrease of total acidity in TPAD likely caused by the elimination, of tetrahedral Al-species. Over 600 °C, the total acidity decreases further due to dealumination and more loss of Si-species (e.g. silanol-groups, threefold Si).


image file: c6ta09145h-f5.tif
Fig. 5 XRD from carbochlorinated composite 2 samples (like in Fig. 2). Diffractograms are normalized on the main reflex [111] at 6° 2θ. The absolute intensity of the [331] reflex is given on the left.

image file: c6ta09145h-f6.tif
Fig. 6 TPAD of all composite 2 samples synthesized at different temperatures and calcinated under air at 550 °C for 6.

In general with higher temperatures a stronger reaction takes place. This progress leads to decreasing residual carbon contents because more carbon is used during the reaction (eqn (1) and (2)). The composite contains 7.26 w% carbon and the concentration of residual carbon decreases from 7.17 w% at 400 °C down to 0.55 w% at 800 °C. Regarding the loss of carbon and framework species it is reasonable that the yield decreases with higher temperatures from 94 w% (400 °C) to 71 w% (800 °C).

Summing up, etching at 400 °C and 500 °C is favoured due to increased mesoporosity, HF, high yield, a moderate decrease in microporosity, total acidity and still intact crystallinity as represented in Table 2. Here it should be noticed that the increasing Si/Al ratio and the loss of acidity can even be beneficial for certain applications.

Carbon content in composite

The impact of the carbon content within the zeolite micropore framework is investigated based on three different carbon–zeolite-composites (Table 1), which were pyrolyzed with different FA loadings. These three composites C1, C2 and C3 correspond to carbon loadings of around 3.0, 7.3 and 14.1 w% carbon investigated by TG analysis, shown in Fig. S3. The N2-physisorption isotherms (Fig. S4) of the samples treated at 500 °C show type IV isotherms and an increase of mesopore volume from 0.19 (C1-500-4-10/70) to 0.30 cm3 g−1 (C3-500-4-10/70), small differences in micropore volumes and therefore also an increase of total pore volume and HF with higher carbon loadings. Further N2-adsorption for samples treated at 400 °C and 600 °C (Fig. S5 and S6) is provided in the ESI. At a temperature of 400 °C the sample with the highest carbon loading shows the lowest N2-isotherm uptake, this can be explained by the high residual carbon content in the pore network (Fig. S5). Sample C3-500-4-10/70, derived from composite 3 with 14 w% carbon loading shows the most promising results with slightly higher SSA (565 m2 g−1), pore volume (0.44 cm3 g−1), mesopore volume (0.3 cm3 g−1), hierarchy factor (0.13) and remaining total acidity (0.639 mmol g−1). This higher mesopores volume is caused by the higher carbon ratio in the composite that in turn causes a stronger leaching of framework species.

In general, we can state that higher carbon content leads to a more intense reaction and likewise slightly higher mesopore volumes and increasing HF (Table 3). Comparable to the previous section higher chlorination temperatures again increases total and mesopore volume but decreases micropore volume, total acidity, and crystallinity. The gain of mesopores at higher carbon contents results in a lower crystallinity, which was already seen in Fig. 5. All three triples (C1, C2, C3 at 400 °C, 500 °C and 600 °C) show this effect (Fig. S8). The total acidity, investigated by TPAD, shows especially for lower temperatures (400 °C: (Fig. S8), 500 °C: (Fig. 7)) no big differences, thus the loss of acidic centers corresponds mostly to the chlorination temperature and not to the carbon content. However, at 600 °C TPAD shows a certain decrease of total acidity with higher carbon contents (Fig. S9). Further characterization, presented in Table 3 shows an increasing molar Si/Al ratio with increasing carbon contents. Thus, the reaction with Al-species seems to be preferred over Si-species. For all three temperatures, the residual carbon content increases from composite 1 to composite 3, likely caused by the higher initial carbon content. In contrast, samples derived from the same composite and therefore same initial carbon loading show a diminution of residual carbon with increasing temperature. All samples were produced with high yields about 70 to 90%. Only the composite 3 sample at 600 °C (C3-600-4-10/70) shows a smaller 58% yield caused by a strong reaction and an increased loss of framework material. We can summarize that higher carbon contents lead to a higher hierarchization and therefore higher mesoporosity, total pore volume and hierarchy factor. This can be explained, by a more exhaustive leaching of Al- and Si-species corresponding to eqn (1) and (2). Whereas the crystallinity is reduced by higher carbon ratios the total acidity is retained. The SSA is preserved or even slightly increased for higher carbon contents.

Table 3 Characterization data of samples out of all three different composites (C1, C2 and C3) at 400, 500 and 600 °C. Physisorption data derived from N2-isotherms measured at −196 °C
Samplea Si/Alb/mol mol−1 SSABETc/m2 g−1 SSAEXTd/m2 g−1 PVtotale/cm3 g−1 PVmicrod/cm3 g−1 PVmesof/m3 g−1 HFg C XRD /% Total acidityi/mmol g−1 C res /w% Yieldk/w%
a Sample description given in Experimental section. b ICP-OES elemental analysis. c Multi-point BET-method. d t-Plot method p/p0 from 0.2 to 0.5. e Total pore volume at p/p0 = 0.95. f PVmeso = PVtotal − PVmicro. g Hierarchy factor HF = (PVmicro/PVtotal)(SEXT/SSABET).61 h % XRD intensity/HY after ASTM 3906-03.60 i Total acidity determined by TPAD. j Residual carbon (Cres) analyzed by TG; Cres = CsampleCH-Y 5 pure. k Calculated by weighing before and after carbochlorination.
H-Y 5 pure 3.0 798 56 0.36 0.29 0.08 0.06 100 0.995
 
C1-400-4-10/70 2.6 483 63 0.29 0.20 0.09 0.09 63 0.705 4.73 88.3
C2-400-4-10/70 3.7 370 116 0.25 0.12 0.13 0.15 46 0.685 7.17 94
C3-400-4-10/70 5.1 399 77 0.23 0.13 0.10 0.11 26 0.706 12.16 85.1
 
C1-500-4-10/70 4.9 461 105 0.36 0.17 0.19 0.11 63 0.514 2.38 89.4
C2-500-4-10/70 7.0 454 165 0.39 0.12 0.27 0.11 51 0.394 2.82 77.8
C3-500-4-10/70 4.9 565 235 0.44 0.14 0.30 0.13 27 0.639 6.85 72.1
 
C1-600-4-10/70 6.6 164 59 0.23 0.04 0.19 0.07 30 0.526 0.83 83.6
C2-600-4-10/70 18.3 275 156 0.42 0.05 0.37 0.07 22 0.227 0.71 72.2
C3-600-4-10/70 11.9 509 302 0.54 0.09 0.45 0.10 20 0.215 5.66 57.5



image file: c6ta09145h-f7.tif
Fig. 7 TPAD of all three composite samples after carbochlorination at 500 °C and calcination. C1-500-4-10/70 (red), C2-500-4-10/70 (blue), C3-500-4-10/70 (green).

Chlorination time

Fig. S10 shows the N2-physisorption isotherms of samples prepared from composite 2 that have been carbochlorinated at 400 °C and 500 °C for 2, 4, and 8 h, respectively. The N2-isotherms at 400 °C and 500 °C are nearly superimposed. Similar result can also be seen for the samples at 600 °C (Fig. S11).

Thus, the reaction time seems to have no significant influence on the porosity (Fig. S10) and acidity (Fig. S11), as TPAD and N2-adsorption show similar values (Table 4). The XRD measurements (Fig. S13) show comparable crystallinity for samples synthesized at 500 °C or 600 °C for 2 h and 4 h, respectively. Nevertheless to long reaction times lead to decreasing crystallinity and HF, as seen for 8 h at 500 °C (C2-500-8-10/70). In contrast the 400 °C samples show an increase of total acidity and crystallinity from 4 h to 8 h reaction time. A possible reason can be the reinsertion of Al-species in the framework over time under this relatively mild conditions and therefore the rebuilding of acidic sites, as the Si/Al ratio increases similar to the total acidity. The yields are comparable for different reaction times at the same reaction temperature, whereas the residual carbon content decreases with increasing reaction time. All material characteristics are summarized in Table 4.

Table 4 Characterization data of samples synthesized at 400, 500 and 600 °C for different reaction times. Physisorption data derived from N2-isotherms measured at −196 °C
Samplea Si/Alb/mol mol−1 SSABETc/m2 g−1 SSAEXTd/m2 g−1 PVtotale/cm3 g−1 PVmicrod/cm3 g−1 PVmesof/m3 g−1 HFg C XRD /% Total acidityi/mmol g−1 C res /w% Yieldk/w%
a Sample description given in Experimental section. b ICP-OES elemental analysis. c Multi-point BET-method. d t-Plot method p/p0 from 0.2 to 0.5. e Total pore volume at p/p0 = 0.95. f PVmeso = PVtotal − PVmicro. g Hierarchy factor HF = (PVmicro/PVtotal)(SEXT/SSABET).61 h % XRD intensity/HY after ASTM 3906-03.60 i Total acidity determined by TPAD. j Residual carbon (Cres) analyzed by TG; Cres = CsampleCH-Y 5 pure. k Calculated by weighing before and after carbochlorination.
H-Y 5 pure 3.0 798 56 0.36 0.29 0.08 0.056 100 0.995
 
C2-400-4-10/70 3.7 370 116 0.25 0.12 0.13 0.155 46 0.685 7.17 94.0
C2-400-8-10/70 2.9 381 87 0.24 0.14 0.10 0.137 67 0.882 7.63 99.3
 
C2-500-2-10/70 7.7 335 98 0.35 0.10 0.25 0.081 42 0.406 1.67 76.3
C2-500-4-10/70 7.0 454 156 0.39 0.12 0.27 0.110 51 0.394 2.82 77.8
C2-500-8-10/70 n.a. 381 182 0.42 0.08 0.34 0.093 35 0.393 1.72 72.6
 
C2-600-2-10/70 15.8 228 158 0.44 0.04 0.40 0.066 22 0.242 1.45 69.2
C2-600-4-10/70 18.3 275 156 0.42 0.05 0.37 0.070 22 0.227 0.71 72.2


Chlorine concentration

Few investigations with different chlorine concentration were performed. Higher chlorine concentration leads to a stronger hierarchization with an increased total and mesopore volume (Fig. S14). However, we can also observe a decreased crystallinity and a lower total acidity of the samples (Fig. S15 and S16). All characterization data is provided in ESI (Table S1).

Si/Al ratio

In addition to the parameters discussed above we also investigated the influence of the Si/Al ratio on the chlorination process. With a Si/Al ratio of 40, the HY-80 presents a steep increase in this parameter but it inherently possesses a few mesopores owing to the fabrication process. Due to the decreased aluminum content, the hierarchization requires higher temperatures. This is in accordance with findings from the ICP-OES (Table 2). In the experiments, beneficial effects on the adsorption behavior can be observed at 800 °C to 900 °C (Table 5 and Fig. S17). Temperatures higher than these lead to an excessive destruction of the zeolite network and hence a drastic decrease in surface area and pore volume of the material. The impact of the reduced aluminum content can also be observed in the TPAD measurements. Where the HY-5 loses nearly 83% of its acidity during the treatment at 800 °C the HY-80 loses only 28% under the same conditions. More interestingly, even at the higher temperatures, the zeolite maintains most of its crystallinity (Table 5 and Fig. S18). This is in sharp contrast to HY-5 (Fig. 5).
Table 5 Characterization data of the H-Y 80 samples. Physisorption data derived from N2-isotherms measured at −196 °C
Samplea Si/Alb/mol mol−1 SSABETc/m2 g−1 SSAEXTd/m2 g−1 PVtotale/cm3 g−1 PVmicrod/cm3 g−1 PVmesof/m3 g−1 HFg C XRD /% Total acidityi/mmol g−1 C res /w% Yieldk/w%
a Sample description given in Experimental section. b ICP-OES elemental analysis. c Multi-point BET-method. d t-Plot method p/p0 from 0.2 to 0.5. e Total pore volume at p/p0 = 0.95. f PVmeso = PVtotal − PVmicro. g Hierarchy factor HF = (PVmicro/PVtotal)(SEXT/SSABET).61 h % XRD intensity/HY after ASTM 3906-03.60 i Total acidity determined by TPAD. j Residual carbon (Cres) analyzed by TG; Cres = CsampleCH-Y 5 pure. k Calculated by weighing before and after carbochlorination.
H-Y 80 pure 34.6 738 143 0.45 0.24 0.21 0.103 100 0.108
 
C5-500-4-10/70 n.a. 582 109 0.44 0.23 0.21 0.096 76 0.097 5.09 98.6
C5-600-4-10/70 n.a. 585 99 0.44 0.24 0.21 0.086 76 0.081 4.55 98.4
C5-800-4-10/70 46.1 617 240 0.53 0.19 0.34 0.130 76 0.078 1.17 88.9
C5-900-4-10/70 48.0 736 244 0.55 0.20 0.35 0.120 97 0.059 0.87 84.0
C5-1000-4-10/70 n.a. 397 181 0.40 0.09 0.31 0.100 70 0.046 0.14 79.3
 
C4-800-4-10/70 50.0 753 218 0.50 0.22 0.28 0.121 92 0.057 0.52 91.0
C5-800-4-10/70 46.1 617 240 0.53 0.19 0.34 0.130 76 0.078 1.17 88.9
C6-800-4-10/70 38.5 817 288 0.68 0.22 0.47 0.111 87 0.055 1.48 73.8


A variation of the carbon content was undertaken in the same fashion as for the HY-5, the results of which are presented in the lower half of Table 5. These three composites C4, C5 and C6 correspond to carbon loadings of around 3.6, 6.5 and 9.3 w% carbon as determined by TG analysis (Fig. S19). The N2-physisorption isotherms (Fig. 8) for the samples treated at 800 °C show type IV isotherms and an increase of mesopore volume from 0.28 (C4-800-4-10/70) to 0.47 cm3 g−1 (C6-800-4-10/70) and therefore also an increase of total pore volume with higher carbon loadings. Sample C6-500-4-10/70, derived from composite 6 with 9.3 w% carbon loading shows the most promising results with a higher SSA (817 m2 g−1), pore volume (0.68 cm3 g−1), mesopore volume (0.47 cm3 g−1), hierarchy factor (0.111) and remaining total acidity (0.055 mmol g−1). The higher carbon ratio in the composite causes a stronger leaching of framework species and thereby creates a higher mesopore volume. In contrary to the HY-5 samples the crystallinity of all 3 samples remains on a high level (Fig. 9) and the acidity only drops to 51% (C6-800-4-10/70) to 72% (C5-800-4-10/70) of the parent zeolite with no clear trend visible in these samples (Fig. S20). ICP-OES shows a lower Si/Al ratio with increasing carbon contents (Table 5) level. It can be deduced that at higher carbon loadings the leachable aluminium species are depleted and therefore the leeching silica species takes place and reduces the Si/Al ratio. This trend correlates with the yield of the three samples which is between 91% (C4-800-4-10/70) and 73.8% (C6-800-4-10/70). For all three different temperatures, the residual carbon content increases from composite 4 to composite 6 caused by the higher initial carbon content. We can summarize that higher carbon contents lead to higher hierarchization and therefore higher mesoporosity, total pore volume. Compared to HY-5 the crystallinity is mostly retained after the treatment and the SSA is kept or even increased for higher carbon contents.


image file: c6ta09145h-f8.tif
Fig. 8 N2-Isotherms at −196 °C of samples at 800 °C from different zeolite–carbon composite red (C4-500-4-10/70), blue (C5-500-4-10/70), green (C6-500-4-10/70).

image file: c6ta09145h-f9.tif
Fig. 9 XRD of carbochlorinated composite samples. Diffractograms are normalized on the main reflex [111] at 6° 2θ. The absolute intensity of the [331] reflex is given on the left.

Conclusions

As the first proof of principle, we presented a new top-down synthesis route for hierarchical zeolite Y. The process of carbochlorination has no need for any solvents and can be executed in a one-step reaction.

The herein used zeolite/carbon composite material should serve as a model system for coked and deactivated zeolite Y. It was the scope of this research to elucidate the hierarchization process in-depth, rather than screening different zeolite types or giving potential applications for hierarchical zeolites.

Our experiments show that carbochlorination temperature and carbon loading are the most influencing parameters to tune the properties of hierarchical zeolite. The insights obtained from the experiments with HY-5 could be adapted to the different Si/Al ratio of HY-80 as well, by changing the treatment temperature.

A chlorination temperature of 500 °C (HY-5) or 800 °C (HY-80) respectively and high carbon content was best with respect to generated mesoporosity, with only a moderate loss in total acidity and retained crystallinity.

The best results were obtained with HY-80, where the treatment leads to a doubling of the pore volume while the surface area and crystallinity of the material could be maintained.

Carbochlorination yields materials with a 1.5 to 1.75 times higher hierarchy factor (HF) and around 40 to 70 w% of initial total acidity with a yield from 70 to 94 w% compared to an industrially available zeolite Y material. We can state the following findings.

(1) Higher carbochlorination temperatures lead to a stronger hierarchization with higher hierarchy factors and meso-/micropore volume ratios, reduced crystallinity, decreased SSA, and lower total acidity.

(2) The Si/Al ratio plays a major role in the carbochlorination behavior of zeolites, with higher ratios making for a higher crystallinity and meso-/micropore volume ratios, a similar or higher SSA, and a lower total acidity.

(3) Higher initial carbon contents lead to stronger hierarchization.

(4) Increasing reaction time did not significantly impact porosity, total acidity, SSA or yield. Only some differences in crystallinity and residual carbon occur.

Acknowledgements

We gratefully acknowledge the Federal Ministry of Education and Research (Bundesministerium für Bildung und Forschung, BMBF) for support of the Mechanocarb project (award number 03SF0498). The authors acknowledge Anja Werner for support with TPD measurements and Silvia Paasch for support with the NMR measurements.

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Footnotes

Electronic supplementary information (ESI) available: Further material characterization. See DOI: 10.1039/c6ta09145h
Both authors contributed equally.

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