3.1 Characteristics of initial zeolite materials
Figure 1 represents the powder diffraction patterns of the zeolite components of the composites. The diffractogram of the MFI-component (Fig. 1a) contains only maxima characteristic for this type of zeolite, while the MOR-component consists of the mordenite phase as well as the clinoptilolite phase with the predominance of the former (Fig. 1b). In the acid-modified rock (Fig. 1c), the crystallinity of the mordenite phase remains intact, whereas the degree of crystallinity of the clinoptilolite phase decreases slightly and amounts to 73% of that in original rock. The degree of crystallinity has been evaluated by the relative intensity of the analytical diffraction maxima I330 (d = 0.453 nm) and I151 + 350 (d = 0.297 nm) for mordenite and clinoptilolite, respectively. It can be assumed that partial destruction of clinoptilolite may contribute to the formation of mesoporosity in the MOR-component.
Micrographs of the components for the composites (Fig. 2) indicate the formation of nanosized particles of the metal phase. The Pd-impregnated MFI-component contains nanoparticles with a size of 7–12 nm, while in the MOR-component, Ni nanoparticles with an average size of ~ 5 nm were recorded.
The infrared spectra of the MFI and MOR-components of composite catalysts in the region of framework vibrations are shown in Fig. 3. Assignments of the main absorption bands (a.b.) are made according [37, 38]: 420 cm-1 – O − T−O bending vibration (T = Si, Al), 550–580 cm-1 – vibrations of secondary building units (SBU), 690 and 790–800 cm-1 – symmetric stretching internal and external vibrations of tetrahedra, respectively, 1025–1060 cm-1 – asymmetric stretching vibrations of bonds of tetrahedra, 1220–1225 cm-1 – asymmetric stretching vibrations of external bonds between tetrahedra.
Spectra of the samples based on MFI zeolite (Fig. 3a) are not affected by the modification procedure: all a.b. characteristic of the zeolite are well defined, retain their position in the spectra, and their intensity remains unchanged.
As in the case of synthetic MFI-based samples, the spectra of samples of natural origin (Fig. 3b), both initial and modified, contain all characteristic a.b., the intensities of which remain intact. Thus, we can speak about the preservation, on the whole, of the crystalline structure of the rock components. However, in the spectrum of dealuminated rock, the appearance of a shoulder at 920 cm-1 is observed, which is often associated with various types of structural defects [39]. This indicates insignificant amorphization of the sample, which is apparently due to the partial destruction of the clinoptilolite phase during the dealumination. Dealumination also causes a high-frequency shift of the a.b. at 1025 cm-1 in modified samples.
In the spectrum of original rock, a broadened a.b. at 550 cm-1 is observed, which narrows and shifts in the modified samples. The same was observed for another rock by Voloshyna et al. [40] and explained by the diversity of cationic composition of native rock and its homogeneity in the H-form of samples. The effect of cationic composition on the frequency of SBU vibrations in mordenite and clinoptilolite can be noticeable due to the high concentration of cationic sites in their free space. On the other hand, metal particles in the zero-valent state can also affect the SBU vibrations, restricting their motion, which leads to a high-frequency shift of this a.b. in the spectrum of the HR-2Ni sample.
3.2 Porous structure characteristics of initial materials and composite systems
The porous structure of the samples was estimated from the isotherms of low-temperature nitrogen ad(de)sorption (Fig. 4).
The shape of the isotherm of the MFI-based samples is typical for microporous adsorbents according to the IUPAC classification [41]. The proportion of micropores in these samples is > 80% (Table 2). A minor hysteresis is observed on the isotherms, the occurrence of which is explained by the slight destruction of the porous structure during the obtaining of the protonic form.
Table 2
Porous structure parameters of the samples
Samples | SBET (m2/g) | St (m2/g) | Smiсro (m2/g) | Vmicro (cm3/g) | V (cm3/g) | Vmicro/V (%) | R (nm) | RDFT (nm) |
MFI-based | | | | | | | | |
HMFI | 371 | 14.5 | 356 | 0.150 | 0.183 | 82 | 0.99 | 0.97 |
HMFI-1Pd | 332 | 11.3 | 321 | 0.136 | 0.164 | 83 | 0.99 | 0.97 |
Rock-based | | | | | | | | |
HR | 345a) | 19.1 | 326 | 0.113 | 0.205 | 55 | 1.38 | 1.17 |
HR-2Ni | 330 | 19.3 | 310 | 0.126 | 0.223 | 57 | 1.35 | 1.17 |
Binder | | | | | | | | |
α | 78.3 | 66.9 | 11.4 | 0.005 | 0.230 | 2.0 | 5.88 | 4.56 |
γ | 243 | 211 | 32.7 | 0.013 | 0.651 | 2.0 | 5.35 | 2.55 |
Composite catalytic system | | | | | | | | |
#С | 247 | 15.6 | 232 | 0.097 | 0.133 | 73 | 1.08 | 1.17 |
#С-Bα | 291 | 56.9 | 234 | 0.096 | 0.217 | 44 | 1.49 | 1.13 |
#С-Bγ | 219 | 53.2 | 165 | 0.071 | 0.170 | 42 | 1.56 | 1.17 |
a)The specific surface area for this sample was calculated using the Langmuir equation |
The isotherms of the rock-based samples have a character intrinsic to sorbents that combine micro- and mesoporosity. This is evidenced by a sharp rise at low relative pressures and the presence of a hysteresis loop at higher p/p0, respectively. The proportion of micropores in these samples is about 55%. The reason for the appearance of hysteresis with a pronounced rise in the region of high relative pressures is obviously the appearance of mesopores inside the crystallites during the dealumination procedure due to partial destruction of the structure.
The pore size distribution (Fig. 5) for the zeolite samples has three maxima: about 1 nm, 1.2 nm, and 2.6 nm. Accordingly, one can distinguish pores with a radius of 1 nm, which are classified as supermicropores [41] and predominate in the MFI-based samples, as well as narrow mesopores with a radius of about 1.2 nm, which predominate in the rock-based samples. The volume of mesopores with a radius of 2.6 nm is insignificant in both zeolites. Therefore, the secondary porosity of both zeolite components can be considered similar.
As a result of modification with metals, the parameters of the porous structure of the samples decrease compared to the original materials. At the same time, a decrease in the specific surface area of the HR-2Ni sample is accompanied by an increase in the volume of micropores and the volume of pores with a radius of ~ 1.2 nm prevailing in the rock. In this case, this increase may be imaginary and can be explained by an increase in the amount of adsorption under the influence of nickel particles, which serve as additional adsorption sites. Palladium atoms, due to their larger radius, have greater polarizability, which leads to a stronger van der Waals interaction of palladium particles with the zeolite surface [42]. Therefore, for nitrogen molecules, they are unlikely to create additional adsorption sites. For this reason, the calculation of the pore volume from the N2 adsorption isotherms in the case of palladium seems to be more adequate. The above mentioned indicates the location of metal particles in the nanopores that predominate in a particular zeolite, but in the rock-based samples, nickel is also present in zeolite micropores.
Both modifications of aluminum oxide, which were used as binders in the preparation of samples #C-Bα and #C-Bγ, show isotherms with a wide hysteresis loop. They are characteristic of mesoporous adsorbents with a small number of micropores. γ-Al2O3 has a threefold higher specific surface area compared to α-Al2O3. The average pore radius for these samples is 5–6 nm. Pores size distribution gives a wide maximum near 5 nm for α-Al2O3, and for γ-Al2O3 – a dispersion of radii in the range of 2–10 nm with a predominance of 2.5 nm radius.
Interestingly, the composite catalyst #C has worse porosity parameters than its components. The addition of a binder in the #C-Bα sample is reflected in a significant increase in the external surface area and total pore volume. The latter increases due to the addition of nanopores with radii of 2–10 nm to the porous structure (Fig. 5). In the #C-Bγ sample, the size distribution of nanopores resulting from the addition of the binder is much narrower with a maximum of about 2 nm. The larger pores present in γ-Al2O3 are obviously formed by the inter-particle space that is destroyed during the mixing process. With that, γ-Al2O3 loses a significant portion of its pore volume, which is not the case with α-Al2O3 when added to a mixture of zeolites. The observed phenomenon is explained, on the one hand, by the much higher dispersion of γ-Al2O3 compared to the dispersion of zeolite components of the composites and, on the other hand, by the close particle sizes of zeolites and α-Al2O3 [43]. The former is also the reason for the somewhat reduced micropore surface area of the #C-Bγ composite, which is due to the blockage of pore openings on the external surface of zeolite crystallites.
3.3 Catalysis
The catalysts were tested in the isomerization of linear hexane in a micro-pulse mode, and the activity was evaluated by the degree of conversion of the reagent.
The conversion of n-hexane on catalysts of the L-series, in which the zeolite components are separate layers, begins at 473 K (Fig. 6a). The lowest conversion is observed for the monometallic sample #L1, but thanks to Pd it is the most selective for C6 isomers (Fig. 6b). With increasing temperature, the isomerization selectivity on all three catalysts decreases. The addition of Ni to the MOR component (samples #L2 and #L3) obviously promotes the activation of cracking, which is reflected in the increase in conversion over these samples comparing to the #L1 sample and, accordingly, a decrease in their selectivity. In addition, there is a tendency to decrease the temperature of the maximum yield of hexane isomers (Fig. 6c) without reducing the maximum value. The effect of the addition of nickel differs depending on which catalyst layer is first exposed to hexane. Since the #L2 catalyst, which has a Pd-containing layer first, is more efficient than the other Ni-containing catalyst in this series, it can be assumed that the role of palladium is to provide initial effective dehydrogenation of alkanes, which facilitates further isomerization. Hydrogenation of the formed isomers to the final products can occur on less effective hydrogenating-dehydrogenating sites, such as nickel nanoparticles. This approach provides a basis for minimizing the content of expensive metals in composite catalysts.
As can be seen from Fig. 6c-d on the example of the formation of hexane isomers, the total effect of the two layers is not additive and exceeds their average value.
To further determine the effect of the arrangement of catalyst layers on the hexane transformation, samples #C, #C-Bα and #C-Bγ with an isotropic distribution of zeolite phases were prepared and their catalytic properties were studied (Fig. 7).
First of all, it should be noted that these catalysts, with the exception of sample #C-Bγ, showed significantly better results in the isomerization of n-hexane compared to sample #L2, the most effective catalyst of the L-series. This may indicate that the above-mentioned positive effect of the initial more efficient dehydrogenation of reagent molecules on palladium can occur not only at the macro level in the case of layering of Pd- and Ni-containing components of the composite catalyst, but also under conditions of isotropic distribution of the corresponding zeolite components in the catalyst. In the latter case, it is even more effective.
As is well known, γ-Al2O3 is widely used as a catalyst carrier and can also serve as an active catalyst due to the presence of Lewis acid sites (LAS) and a developed specific surface area, while α-Al2O3 is characterized by an order of magnitude lower concentration of LAS on the surface [43]. At the same time, in α-oxide, LAS are weak [44] and porosity is three times less developed than in γ-Al2O3 (Table 2). However, the #C-Bα sample obtained using α-aluminum oxide is significantly superior in all respects to the #C-Bγ catalyst, in which γ-Al2O3 was used as a binder (Fig. 7). Obviously, the acidic properties of γ-Al2O3 are not an advantage for hydroisomerization and hydrocracking reactions, since in these reactions the active sites are above all acidic Brønsted sites (BAS). The advantage in porosity is also lost during the preparation of the #C-Bγ composite (see subsection 3.2). Instead, this composite has a 30% smaller micropore surface area, where the active sites are located. This reduces the degree of conversion on this catalyst, as well as its selectivity (Fig. 7e), since in the micropores isomerization would be facilitated by a longer stay of the reagents in contact with the active surface.
On the composite catalyst #C-Bα, with increasing temperature, the yield of C6 isomers begins to increase, which at a maximum at a temperature of 548 K approaches the highest value for the tested catalysts – 40%. (Fig. 7b). Obviously, with an increase in the reaction temperature, there is a gradual increase in the strength of the BAS. At a temperature of 573 K, a sharp increase in the yield of cracking products С1-5 is observed (Fig. 7c), indicating the appearance of sufficiently strong sites and acceleration of the cracking reaction. On the #C-Bγ sample, these processes are much less pronounced, which cannot be explained only by the smaller micropore surface in this catalyst compared to #C-Bα. Thus, the effect of aluminum oxide modification that was used to prepare the composite catalyst may also spread to the characteristics of the acid sites of the zeolite components, probably through their interaction with the acid sites of the binder.
The maximum yield of C6 isomers on samples #C and #C-Bα (samples of the C-series with isotropic distribution of zeolite components, except for #C-Bγ) remains as high as on their Pd-containing component, sample HMFI-1Pd, but is observed at a lower temperature (Fig. 7b). At the same time, the yield of valuable dimethyl branched isomers on the composites increases by an order of magnitude compared to this component, exceeding the high yield of DMB on its other component, the HR-2Ni sample (Fig. 7d). Both composite catalysts, despite the lower Pd content and the presence of Ni, retain high selectivity for C6 isomers of their Pd-containing component (Fig. 7e). It can be concluded that such factors as Ni content and the presence of a binder in the composition affect only the activity of the catalyst, as evidenced by the divergence of the curves of the temperature dependence of the selectivity. (Fig. 7f). The highest effectiveness in the formation of hexane isomers in general, as well as dimethyl branched isomers, is demonstrated by sample #C, obtained without the use of a binder. This composite in terms of the iC6 yield is close to the bimetallic monozeolite catalyst with a similar cationic composition (0.5 wt% Ni and 0.5 wt% Pd, [33]), but, unlike the composite, the latter almost does not form DMB.