Figure 1 shows the powder XRD patterns of B-MWW(P) and the as-synthesized Mg-DML-x (x = 100–180) samples prepared in this study. The B-MWW(P) exhibited the low-angle XRD peaks at 2θ = 7.4°, 8.1°, and 9.9° corresponding to (100), (101), and (102) reflections of MWW-type materials, respectively [16]. However, as the hydrothermal temperature increased to 140°C, the intensities of these characteristic peaks continuously decreased and broadened, which are similar to the XRD pattern of delaminated MWW analogue, such as ITQ-2 [17]. In addition, these MWW-type characteristic peaks were completely disappeared at higher temperatures of 160 and 180°C, and some other characteristic peaks at 2θ = 36° and 61°, which are in good agreement with the XRD pattern of magnesium silicate, were emerged [18, 19]. In all Mg-DML-x samples, however, the formation of MgO, represented by the intense XRD peaks at 2θ = 42° and 62°, was not observed [20].
The physical transformation from 3D MWW structure to 2D delaminated layers was further characterized by N2 sorption experiments. As shown in Fig. 2a, the N2 adsorption-desorption isotherms of calcined B-MWW were similar to those of type I microporous solids, while those of Mg-DML-x (x = 100–180) were changed to type IV mesoporous materials as the hydrothermal temperature increased. This is well corresponded to the appearance of an H3-type adsorption-desorption hysteresis loop of Mg-DML-180, indicating the generation of interparticle void spaces between parallel plates. In addition, the external surface areas of Mg-DML-x (x = 100–180) steadily increased with rising hydrothermal temperatures, which is also a typical characteristic of delaminated materials (Fig. 2b and Table 1) [21]. The delamination of MWW layers was also accompanied by the increase in average pore diameter and pore volume as shown in Fig. S1 and Table 1. In contrast to the increase of the external surface area, the micropore area of Mg-DML-x drastically decreased, reaching zero as the hydrothermal temperature increased to 180°C. This is consistent with the disappearance of XRD peaks corresponding to non-porous magnesium silicate as shown in Fig. 1.
Table 1
Physicochemical properties of B-MWW and Mg-DML-x (x = 100–180)
Catalyst | ICP elemental analysis | | N2 sorption analysis |
Si/Mg | Si (wt.%) | Mg (wt.%) | B (wt.%) | BET surface area (m2 g− 1) | Total pore volume (cm3 g− 1) |
Total | Micropore | External |
B-MWW | - | | - | 1.8 | 477 | 452 | 25 | 0.364 |
Mg-DML-100 | 22 | 43 | 1.7 | 1.2 | 533 | 422 | 111 | 0.458 |
Mg-DML-120 | 36 | 44 | 1.1 | 1.1 | 475 | 360 | 115 | 0.538 |
Mg-DML-140 | 18 | 47 | 2.3 | 0.6 | 297 | 158 | 139 | 0.690 |
Mg-DML-160 | 11 | 48 | 3.7 | 0.1 | 143 | 4 | 139 | 0.679 |
Mg-DML-180 | 9 | 50 | 4.7 | 0.1 | 127 | 0 | 127 | 0.744 |
The transformation of MWW crystals to delaminated layers and magnesium silicate layers through the hydrothermal treatment was monitored in SEM images (Fig. 3). The thick and plate-like crystals of B-MWW were transformed to thinner layers-like crystals as the hydrothermal temperature increased. Meanwhile, very small and thin layers, likely corresponding to magnesium silicate, began to form on the surface of MWW crystals, becoming predominant at temperatures higher than 160°C [22, 23]. As shown in Fig. S2, the IR absorption band corresponding to terminal hydroxyls and defect hydroxyls on B-MWW increased as the hydrothermal temperature of Mg-DML-x increased. This also suggests the structural evolution of Mg-DML-x from 3D MWW to 2D layers having silanol groups on their surface. The transformation from B-MWW to magnesium silicate also further confirmed by the uniform distribution of Mg species on the STEM-EDS images of Mg-DML-x catalysts, whose Mg contents varied from 1.2 to 4.7 wt.% as hydrothermal temperature increases from 100 to 180°C (Fig. 4), which were closed to the values calculated from ICP elemental analysis (Table 1). However, the contents of Mg on Mg-DML-x were much lower than those of other transition metal-incorporated DMLs, such as Ni-, Co-, and Zn-DMLs reported in our previous works [24, 25].
The state of Mg species on Mg-DML-x (x = 100–180) were characterized by UV-DRS (Fig. 5a). The formation of magnesium silicates on Mg-DML-x was confirmed by the observation of UV absorption bands at 221 and 256 nm, whose intensity increases with the increase of hydrothermal temperature [26, 27]. Additionally, the broad UV absorption band at 340 nm also steadily increased and red shifted with the rise in the hydrothermal temperature, attributed to the formation of silica nanoparticles [28]. The chemical states of Mg in Mg-DML-x were further characterized by FT-IR spectroscopy in the structural region of 500 to 1600 cm− 1 (Fig. 5b). The IR absorption bands of B-MWW were observed at 560, 610, 810, 1085, 1250, and 1390 cm− 1, typical framework vibrations of the MWW-type structures [29]. The bands at 560 and 610 cm− 1, originated from the double six-ring in MWW structure, were continuously decreased as the increase of hydrothermal temperature [23]. Notably, these characteristic IR bands for MWW structure were not observed on Mg-DML-180, indicating that MWW framework had almost degraded to amorphous layer at this high temperature. Meanwhile, additional bands at approximately 667 and 1025 cm− 1, corresponding to Mg–OH and Si–O–Mg, respectively, were continuously increased. This also indicates the formation of magnesium silicates on the surface region of 2D Mg-DML-x as seen in SEM images (Fig. 3). In line with the observation of UV absorption band for silica nanoparticles on Mg-DML-160 and Mg-DML-180, the intensity of IR absorption band at 803 cm− 1, representing Si–O–Si symmetric stretching vibrations, also increased in these catalysts. The increase of silica nanoparticles on Mg-DML-160 and Mg-DML-180 was further corroborated by the generation of intense peak at 3671 cm− 1 in Fig. S2, corresponding to the stretching mode of hydroxyl groups.
The formation of magnesium silicate in Mg-DML-x (x = 100–180) was investigated by 29Si MAS NMR spectroscopy (Fig. 5c). The borosilicate B-MWW has distinct peaks at − 105 and − 112 ppm, corresponding to Q4(nB) signals, which is similar to the spectrum of low silica (Si/Al = 9) aluminosilicate MCM-22 zeolite [30]. However, the intensity of these two peaks was gradually decreased with increasing hydrothermal temperature, while a new peak at − 98 ppm, corresponding to Q3 signal of talc-like species, emerged [31]. This observation is consistent with the evolution of Si–O–Mg band in FT-IR spectra shown in Fig. 5b. Additionally, the Q4 signal at − 112 ppm was still observed on the samples prepared at high temperature (140–160°C) of hydrothermal treatment. This also correlates well with the increase of IR absorption band (803 cm− 1) representing Si–O–Si symmetric stretching vibrations (Fig. 5b).
The valence state of the elements in Mg-DML-x (x = 100–180) was characterized by XPS analysis. As shown in Fig. 6a, Mg 2p signals were deconvoluted into two peaks (Peak I and II) at approximately 49.9 and 50.5 eV, corresponding to magnesium silicate and MgO, respectively [32]. In line with the elemental analysis results in Table 1, the overall intensity of Mg 2p signals increased proportionally with the hydrothermal temperature (Table S1), which is due to the increasing Mg contents in solid samples. Furthermore, while the proportion of magnesium silicate were grown until Mg-DML-160, Mg-DML-180 showed the highest proportion of MgO (Table S1). This can be explained by the higher thermodynamic stability of MgO at such high hydrothermal temperature. In Fig. 6b, the evolution of Peak I, assigned to Si–OH with the increase in intensity corresponding to hydrothermal temperature was observed in Si 2p region, which aligns with the OH-IR results mentioned above. Additionally, Peak II at 103.6 eV in Si 2p XPS and Peak III at 533.5 eV in O 1s XPS spectra, corresponding to Si4+ and O2− in Si–O–Mg, respectively, both increased proportionally to hydrothermal temperature up to 160°C. However, in Mg-DML-180, the proportion of Si–O–Mg was lower than in Mg-DML-160, which is consistent with Mg 2p XPS results.
The basic properties of Mg-DML-x (x = 100–180) originating from the substitution of B by Mg were investigated by CO2 TPD (Fig. 7). The CO2 TPD profiles can be categorized into three temperature regions, i.e., 50–250°C, 250–550°C, and 550–800°C, corresponding to CO2 desorption from weak, intermediate, and strong base sites, respectively. With the increase of hydrothermal temperature up to 160°C, the concentration of strong base sites increased. In addition, the desorption of CO2 from weak base sites was shifted to higher temperature region, indicating the enhancement in the strength of weak base sites compared to the other Mg-DML samples. This can be attributed to the increased concentration of framework Mg species as discussed in structural IR and Mg 2p XPS (Figs. 5b and 6a). Unlike the other catalysts, Mg-DML-180 exhibited intermediate base sites, which is a typical base strength of MgO [14].
The catalytic properties of basic Mg-DML-x (x = 100–180) catalysts were investigated by Knoevenagel condensation of benzaldehyde with malononitrile as a test reaction. As shown in Fig. 8a, the conversions of benzaldehyde over all Mg-DML catalysts increased linearly as a function of reaction time, indicating that the product yield is not limited by the thermodynamic equilibrium of the reaction. Here, benzylidenemalononitrile was the only product observed in all experiments. The conversions of benzaldehyde at 96 h of reaction time increased following the hydrothermal temperature of Mg-DML-x (x = 100–180). Although Mg-DML-160 exhibited the higher conversion of benzaldehyde up to 48 h, Mg-DML-180 prevailed at the end of the reaction. This can be rationalized by the presence of intermediate base sites on Mg-DML-180, which is more favorable for catalyzing Knoevenagel condensation [33]. As shown in Fig. 8b, Mg-DML-180 exhibited good reusability as evidenced by the stable benzaldehyde conversion of 72–77% during 5 repeated uses after regeneration. This can be attributed by the 2D crystal morphology of this catalyst, which is favorable for removal of carbonaceous deposits through simple washing with organic solvent.