2.2. Material Characterization
The raw material used for the synthesis of BN-Ag
0 catalyst was natural BN. Its mineralogical composition is presented in
Table 1. BN raw material has a high content of montmorillonite. For this reason, it is a suitable candidate for obtaining adsorbents with catalytic activity that can be effective in destruction of industrial pollutants.
Natural and chemically modified clays were characterized by the following analysis: EDX, SEM, BET, TPD, XRD and FTIR.
The particle morphology of the surface was investigated by scanning electron microscopy which is presented in
Figure 1.
The morphological analysis of the raw material (
Figure 1a,c,e,g,i) reveals the presence of large, clearer particles, which may correspond to the presence of quartz, highlighted by DRX analysis. The morphological analysis of BN-Ag
0 (
Figure 1b,d,f,h,j) shows the presence of small clearer particles, with smooth surfaces. The surface morphology of the modified bentonite is different from the raw material, by presenting grain-like particles with a fluffy appearance, revealing its extremely fine plate-like structure. The surface has become more porous by the binding of Ag
+ ions in the interlayers of clay. A decrease in the particle size of the BN-Ag
0 is clearly visible, the nanoparticles having the tendency to form aggregates.
The results obtained by EDX analysis in six distinct points, for the raw material, respectively for the chemically modified bentonite presented in
Figure 2.
Incorporation of Ag+ ions was confirmed by EDX. Ag was found in all six points analyzed. Its weight was in the range of 0.5–2.9%. The second area analyzed presented the largest amount, followed by area one with 2.2%.
The pore size distribution curves of indigenous natural clay and of chemically modified clay are presented in
Figure 3. The natural clay contains mainly meso and micropores, this variation could be explained by the presence in the structure of different minerals with different characteristics. The chemically modified natural clay (
Figure 3b) also contains meso and micropores in its structure. The increase in height of the peaks characteristic of the distribution curves in the mesoporous region highlights the formation of a large number of mesopores (2–50 nm).
In
Figure 4, the isotherms obtained for BN compared to BN-Ag
0 are shown. They are similar in shape. According to IUPAC classification [
25] of adsorption isotherms, the isotherms obtained are similar to those of type IV and show a hysteresis corresponding to the formation of pore aggregates in the form of slits and of variable sizes.
The specific surface areas of the natural clay and of chemically modified clay BN-Ag
0 are presented in
Table 1. By chemical modification, the specific surface area of the clay decreases from 25.80 m
2/g to 24.29 m
2/g according to
Table 2.
The values of total surface acidity for BN and BN-Ag
0 obtained and presented in
Table 2, are in accordance with the theories developed in the literature, the surface acidity being influenced by the number of protons in the interleaving solution.
The NH
3-TPD profiles for BN and BN-Ag
0 are shown in
Figure 5. From this figure, it can be determined that NH
3 molecules are now fixed on active material sites. From the profile of the forks, it can be concluded that between the acidic active sites of the material and the weakly basic NH
3 molecules, weak bonds have been created that can break relatively easily when the temperature increases. This is also the interest pursued to be able to use the materials in adsorption–desorption processes. The incorporation of Ag probably also led to an increase in the acidity of the material. The structural changes during preparation lead to the partial or total destruction of the octahedral layers in the crystalline structure, which immediately results in an increase in Lewis acidity—attributed to surface cations. During the preparation, in order to establish the balance at the charge level, the protons in the ion exchange solution replace the exchange interlamellar cations. These protons contribute to increasing the surface acidity. It is also possible that the protons in the marginal -OH groups of the octahedra become more labile due to structural deformations due to ion exchange, which also leads to an increase in Brønsted acidity. In the case of the adsorption of basic gases (ammonia), it is important that the adsorbent has a surface acidity as high as possible for the best efficiency of the adsorption process.
The mineralogical data obtained and presented in
Figure 6, are similar to other results published in the literature for exploited natural bentonites [
26], being composed mainly of montmorillonite and non-clay minerals such as cristobalite and quartz. The results of the XRD analysis indicate that the crystallinity of BN increases with chemical modification. According to the XRD diffractograms shown in
Figure 6, the presence of silver in the clay structure can be observed at the value of 2 θ of 27°. According to the XRD analysis, the mineralogical composition of BN-Ag
0 is presented in
Table 3.
The crystal lattice of the synthesized material is not destroyed, it is partially preserved, and the non-clay fractions do not change.
FTIR analysis reveals the differences that occur in the chemical structure of clays after the chemical modification process. Depending on the variations in the wave number, the free cations as well as the cations in the interlamellar space are highlighted. They occur due to interactions that took place in the clay matrix during the chemical modification process.
In
Figure 7, the FTIR spectra corresponding to BN and to BN-Ag
0 are presented. It is observed that the FTIR spectra contain bands characteristic of smectite clays. The intense bands that appear in the spectrum are assigned to the following groups of molecules: 3735 cm
−1 corresponds to AlAlOH vibration coupled with AlMgOH and SiO-H vibration; 3655 and 1650 cm
−1 correspond to the interlamellar water absorption bands (H-O-H); 1000 cm
−1 corresponds to the elongation vibration of -Si-O; 800 cm
−1 corresponds to -Si-O vibrations in various modified forms of silica, Si-O-Al vibrations in lamellar silicates and (Al, Mg) -O-H; 475 cm
−1 corresponds to -Si-O-Al and Si-O-Mg coupled with OH vibrations or Si-O vibrations.
Ag incorporation was confirmed by EDX, DRX as previously presented, and FTIR analysis which revealed the appearance of a new bands at 480–510 cm−1, 780–805 cm−1 and 1050–1060 cm−1.
2.3. Bacterium Characterization
The characterization of the
ISO SS strain was performed by Gram staining, colony cultural characteristics (appearance, shape, color), oxidase test (
Table 4) and spectral analysis using FTIR technique. Recording spectra obtained from isolated bacteria in a usual nutrient agar medium, was accomplished by transferring a portion of the colony with sterile instruments, to avoid contamination of the samples.
The structural and compositional characteristics of isolated pure bacterial strains derived from the anaerobic stabilized sludge were identified using the FTIR technique. It is known that the cell membrane spectra contain the main modes of vibration of lipopolysaccharides and proteins. Each spectrum recorded for isolated strains was mathematically processed (the second derivative was used, which allows the highlighting of “hidden” maxima) [
27]. In
Figure 8 it can be observed that in the spectra for the strain isolated in the 900–1530 cm
−1 range, the characteristic bands of the sludge and of the nutrient medium (Gelose) are not found, as presented in (
Table 5).
For the correct evaluation of the spectral data, additional untreated sludge samples (N) as well as additional sterilized sludge samples (NS) were subjected to analysis (
Figure 9a). The second order derivatives of Geloza G nutrient medium (
Figure 9b), of N (
Figure 9c) and of NS (
Figure 9d) were obtained following additional sterilization by autoclaving, respecting standardized procedures.
Figure 9a shows that the ATR spectrum for the NS slurry differs substantially from the spectrum of the N sludge (in which the microorganisms are viable) in the spectral range of 2000–550 cm
−1. This finding is confirmed by the derivation of the second order derivative of the original spectra of gelatin, N and of the additional sterilized NS by autoclaving. Therefore, it can be argued that in the spectral range of 2000–550 cm
−1 the differences between the spectra of each bacterial strain investigated can be identified. The spectral range chosen is different from the one used in the literature [
32].
Figure 9b shows major differences between the N-sludge spectra and the extra treated N-autoclave in two distinct domains 550–875 cm
−1 (I) and respectively 990–633 cm
−1 (II). Since the fingerprint domain is considered by most authors [
29,
32,
33] to be attributed to the range of 1800–550 cm
−1, we propose to analyze in more detail the spectra of isolated
ISO SS in this spectral domain. In the first domain (I), the bands are mainly caused by carbon bonds. The maxima in the region of 586 cm
−1 corresponds to the deformation vibrations of the CH bonds outside the plane. The second domain II, specific for N and NS sludge (
Figure 9c,d), has two particularities at 1537 cm
−1 and 1560 cm
−1, which correspond to the Amide II groups.
The ATR spectra were studied in the 550–1800 cm
−1 range, in order to characterize isolated bacterial strain in terms of molecular structure. The purpose of these analyzes was to identify the fingerprint of the bacterial strain that remained resistant to the applied treatment. Because in the 550–800 cm
−1 range, there were no well-defined particularities, the field of investigation was reduced to 900–1700 cm
−1. Because the results of the investigations of isolated peculiar strains do not interfere with the nutritive medium on which the isolated strains were grown, the spectral characteristics of G-gel (nutrient medium for isolated strains) were also identified (
Figure 9b). The assignment of the main FTIR absorption bands for nutrient agar (G) medium, anaerobic stabilized treatment sludge (N) and anaerobically stabilized anaerobic treatment sludge by autoclaving (NS) is synthesized in
Table 6. The assignment of the main ATR absorption bands of the agar nutrient (G) is used only to avoid possible overlapping of the bands.