CODEN (USA): IJCRGG, ISSN: 0974-4290, ISSN(Online):2455-9555 Vol.11 No.06, pp 209-223, 2018
1,2, #
3,4, #,3
Abstract : The relationship between antimicrobial properties and structure of montmorillonite (MMT) containing hexadecyltrimethylammonium bromide (HDTMA-Br) and silver (Ag) was determined. HDTMA was adsorbed at the clay interlayer by a cation exchange, through the positive head of the ammonium group. At higher surfactant loadings (100 and 200% cation exchange capacity (CEC); MH1 and MH2 samples, respectively) the prevalence of weak adsorption (Van der Waals forces) was observed; whereas below the clay CEC (50%, MH0.5) strong interactions predominated (cation exchange). These different interactions impacted on antimicrobial activity, increasing bactericidal capacity when the surfactant was more available to diffuse. For organo-montmorillonites (OMMT) and all samples with Ag, zeta potential pointed out electrical charge changes on the outer surface, respect to MMT. XPS analyses showed peaks attributed to clusters formation, silver oxidation, and Ag0 in MMT-Ag and MH0.5-Ag. The Ag0 peak was also present in MH1-Ag and MH2-Ag, the later showing an extra peak associated with AgBr. HDMTA+ and Ag adsorbed on the MMT acted synergistically against Staphylococcus aureus. This effect was less noticeable for Escherichia coli and the result was attributed to both, E. coli outer envelope which might lower the efficacy of HDMTA+ adsorbed on the MMT, and decreasing silver proportions when the surfactant loading increased. MH1-Ag presented the best bactericidal properties, showing synergistic effects against S. aureus, while maintaining activity against
E. coli compared to MMT-Ag. Understanding MMT-HDMTA-Ag efficacy contributes to the design of new antimicrobial materials for potential applications in health care. Key words : Synergistic bactericidal activity, Staphylococcus aureus, Escherichia coli, Modified montmorillonite, Hexadecyltrimethylammonium, Silver.
Mariana Blanco Massani et al /International Journal of ChemTech Research, 2018,11(06): 209-223. DOI= http://dx.doi.org/10.20902/IJCTR.2018.110627
Over the last years, considerable work has been dedicated to developing highly efficient strategies to fight bacteria. In this regard, the combination of different antimicrobials such as metal ions, nanoparticles, bacteriocins, as well as plant-derived compounds has been reported 1. The use of quaternary ammonium compounds (QAC) was also suggested as they are less susceptible to development of resistance by the bacteria
2. Particularly, hexadecyltrimethylammonium bromide (HDTMA-Br), also known as cetyltrimethylammonium bromide, showed antimicrobial effect either alone or interacting with inert or non-inert vehicles; or as a part of
2,34–6
polymers . The use of silver as antimicrobial agent has also been extensively studied .
Not only because of its large cation-exchange capacity (CEC), surface area, and swellability, but also because of its biocompatibility, montmorillonite has been used in a wide range of practical applications 7–9. The use of montmorillonite (MMT) to support different antimicrobials was previously studied for the inhibition of gram-positive and gram-negative bacteria. Its antimicrobial activity showed to be dependent on the antimicrobials used and the assayed microorganisms. That is, for QAC the antibacterial activity occurred mainly through the surfaces interactions between the ammonium compound on the MMT surface and cell envelopes, and less antimicrobial effectiveness against gram negatives was observed 7,10 . Besides for heavy metal cations exchanged in MMT, antimicrobial activity was informed to arise from both the loaded ion and the
7,11–13
cation released from the surface of the clay . Either for QACs or heavy metals, the cation excess on the
10,11
clay mineral surface led to a positive charge formation, attracting the negatively charged cell envelope . The application of antimicrobial MMT supported with Ag+, silver nanoparticles, or different QAC at varying
8,14–17
loading levels was reported . Nonetheless, to the best of our knowledge, there are no studies addressing the relationship between materials antimicrobial activity, cations loading content and their interlayer arrangements, when clay mineral involve the concomitant use of HDTMA-Br at different QAC loading levels and Ag. Such studies are to be performed in order to predict antimicrobial performance of the nanomaterials for the development of effective bactericidal carriers. Accordingly, the present work aims to obtain and characterize different loaded MMT/HDTMA and the respective MMT/HDTMA/Ag materials. XPS and zeta potential results were presented and discussed in order to elucidate clays structure relationship with the antimicrobial activity against Staphylococcus aureus ATCC 25923 and Escherichia coli ATCC 25922.
The clay mineral used was a raw Argentinean montmorillonite (MMT) (Castiglioni Pes y Cia. Lago Pellegrini, Río Negro, Argentina), with a structural formula [(Si3.89 ) (Al1.43 Fe0.26 ) O10 (OH)2]
Al0.11Mg0.30Na0.47 Ca0.08 K0.02, 18, having a cation exchange capacity (CEC) of 0.825 meq g-1 and specific surface area of 39.0
2 -1 19
mg .
Hexadecyltrimethylammonium bromide (HDTMA-Br) and precursor AgNO3 were purchased from Sigma Aldrich Co (Saint Louis, Missouri, USA).
Staphylococcus aureus ATCC 25923 (gram-positive) and Escherichia coli ATCC 25922 (gramnegative), obtained from ATCC (The American Type Culture Collection, Manassas, Virginia, USA), were grown in Mueller Hinton Broth (Britania Laboratories, Buenos Aires, Argentina) at 37°C for 16 h. Until use, all strains were maintained and stored at -20°C in 0.15 g/ml of glycerol (Cicarelli, Buenos Aires, Argentina).
Raw MMT (30 g) was dispersed in 2 L of deionized water and stirred at 60°C. Amounts of HDTMA-Br corresponding to 0.5, 1, or 2 CEC of MMT were slowly added. The mixtures were stirred for 2 h at 60°C. At the end of the reaction, the products were centrifuged (2,200 g) and the sediments were washed to free of bromide anions (tested by AgNO3). The HDTMA-MMT products or organo-montmorillonite (OMMT) samples
(referred to as MH0.5, MH1, and MH2, respectively) were dried overnight at 80°C.
To attain montmorillonite-Ag (MMT-Ag) and organo-montmorillonite-Ag (OMMT-Ag) products, 0.5 g of raw MMT and the corresponding OMMT samples were dispersed in 25 ml of AgNO3 solution (0.1 N) and stirred for 2 h at room temperature. The products obtained were washed and dried as described above; and labeled as MMT-Ag, MH0.5-Ag, MH1-Ag, and MH2-Ag.
XPS analyses were performed on a Physical Electronics PHI 5000 VersaProbe II spectrometer (Chanhassen, Minnesota, USA) with monochromatic Al Kα radiation (25W, 15 kV, 1486.6 eV).
The sample powders were pressed into small stainless steel troughs of 4 mm inner diameter and
0.5 mm depth, mounted on a multispecimen holder. The pressure in the analysis chamber was around 10-7 Pa. The following sequence of spectra was recorded: survey spectrum, C1s; O1s; Na1s; Mg2p; Al2p; Si2p;Ca2p; K2p; Fe2p; Ag3d, and C1s again to check for charge stability as a function of time and the absence of sample degradation during the analyses. The C–(C, H) component of the C1s peak of carbon was fixed at 284.8 eV to set the binding energy scale.
The rate applied to correct the charging effect was between 2.0 and 2.6 eV 20. Binding energies (BE) were determined with an accuracy of 0.1 eV. Analysis software PHI ACCESS ESCA-V6.0 F (Chanhassen, Minnesota, USA) was used for data acquisition and element quantification was based on survey spectra determined at four different positions of each sample, following the method detailed in the literature 21. The angle between the normal to the sample surface and the direction of photoelectrons collection was about 0°, the resulting analyzed area was 700 μm∓300 μm. The pass energy was set at 187.85 eV for the wide scan and 40 eV for narrow scans. In the later conditions, the full width at half maximum (FWHM) of the Ag3d5/2 peak of a standard silver sample was about 0.9 eV. Molar fractions were calculated using peak areas normalized on the basis of acquisition parameters after a linear background subtraction, experimental sensitivity factors and transmission factors were provided by the manufacturer. Elemental mole fractions were provided, excluding hydrogen which is not detected by XPS. The spectra decomposition was done using a Gaussian function, after subtraction of the linear baseline, and particularly a maximal FWHM = 2 were used for C1s decomposition. The goodness of all fits was followed by the chi-square (χ²) values, which were always below 2.00. A time period of 10 min was utilized for Ag3d analysis to prevent the photoreduction of Ag+ species.
Electrophoretic mobility was determined in water dispersions of the respective samples by micro electrophoresis (zeta potential function) using a Brookhaven 90Plus/Bi-MAS Multi Angle Particle Sizing (Brookhaven Instruments Corporation, New York, USA), operated at: λ = 635 nm, 15 mW solid state laser, scattering angle = 90º, temperature = 25ºC, and employing 10−3 M KCl as inert electrolyte and Pd electrodes.
The qualitative assay reported by Negi et al. 14 with some modifications was used to detect the primary antimicrobial activity of clays. Clay powders (about 29±6 mg) were suspended in water, deposited on blank paper disks (diameter 6.64 mm) and allowed to dry. The disks containing clays, as well as a positive control of inhibition (disk containing 50 µg of chloramphenicol, Sigma Aldrich Co, Saint Louis, Missouri, USA), were placed in Mueller Hinton agar plates inoculated separately with 107 colony-forming units (CFU) of S. aureus ATCC 25923 and E. coli ATCC 25922 and incubated at 37°C for 24 h. Antimicrobial activity was evidenced as an inhibition zone after incubation. Each determination was performed in three independent triplicates (9 times).
To examine the clays and HDMTA-Br concentrations leading to a bactericidal effect on S. aureus and
E. coli, a method similar to that reported by Sondi and Salopek-Sondi 22 was used. Approximately 105 CFU/ml of each strain were cultured in Mueller Hinton agar plates supplemented with clays or HDTMA-Br, respectively, in concentrations of 0.15 to 200 mg/ml; or 0.0003 to 0.3 mg/ml. Clay-free Mueller Hinton plates cultured under the same conditions were used as negative inhibition controls. The plates were incubated for 24 h at 37°C. MBC values were defined as the lowest concentration of the tested samples from which the absence of growth was recorded.
The proportion of elemental atomic concentrations in MMT, MMT-Ag, OMMT samples and the resultant silver clays (OMMT-Ag) deduced from the corresponding XPS analyses are summarized in Table 1.
The C1s /Si2p ratio calculated for each sample started at 0.43 for the MMT sample with zero surfactant, in agreement with previous XPS analysis of the same sample 23, and increased with the surfactant loading, to 1.85, 2.42 and 3.55 for MH0.5, MH1 and MH2 samples, respectively. The C1s/Si2p ratio was 0.60 for MMT-Ag sample, and further addition of Ag+ to OMMT samples generated an increase to 1.55, 2.14 and 3.08 for MH0.5Ag, MH1-Ag, and MH2-Ag samples, respectively. The lower C1s/Si2p ratio values obtained for OMMT-Ag samples respect to the corresponding OMMT samples indicated the competition of Ag+ with the surfactant for the external surface sites and/or a surface coverage of the OMMT by Ag+.
Table 1. Atomic proportion (molar fractions in %) of each element obtained for the indicated samples.
MMT | MMT-Ag | MH0.5 | MH1 | MH2 | MH0.5Ag | MH1Ag | MH2Ag | |
---|---|---|---|---|---|---|---|---|
C1s | 8.83 ± 0.85 | 12.23 ± 0.76 | 29.36 ± 3.27 | 35.62 ± 2.31 | 46.74 ±3.62 | 25.74 ± 4.72 | 32.28 ± 2.58 | 40.99 ± 6.42 |
N1s | 0 | 0 | 0.82 ± 0.52 | 0.79 ± 0.23 | 1.45 ± 1.22 | 1.67 ± 0.40 | 1.98 ± 0.61 | 2.68 ± 0.42 |
O1s | 57.50 ±3.95 | 56.30 ± 3.88 | 46.61 ± 2.67 | 42.18 ± 3.09 | 32.82 ± 2.88 | 48.07 ± 3.91 | 44.97 ± 0.97 | 36.98 ± 4.42 |
Na1s | 1.66 ±0.05 | 0.06 ± 0.09 | 0.12 ± 0.05 | 0.10 ± 0.06 | 0.09 ± 0.07 | 0.10 ± 0.09 | 0.09 ± 0.09 | 0.06 ± 0.06 |
Ca2p | 0.44 ± 0.07 | 0 | 0.09 ± 0.06 | 0.07 ± 0.05 | 0.07 ± 0.07 | 0.06 ± 0.06 | 0.05 ± 0.03 | 0.06 ± 0.09 |
K2p | 0.27 ± 0.10 | 0 | 0.07 ± 0.07 | 0.04 ± 0.09 | 0.05 ± 0.07 | 0.06 ± 0.10 | 0.04 ± 0.05 | 0.05 ± 0.06 |
Mg2p | 1.86 ± 0.24 | 2.10 ± 0.98 | 0.71 ± 0.58 | 0.61 ± 0.36 | 0.52 ± 0.70 | 0.49 ± 0.22 | 0.35 ± 0.29 | 0.44 ± 0.11 |
Al2p | 8.47 ± 0.78 | 7.56 ± 1.01 | 5.94 ± 0.88 | 5.62 ± 1.02 | 4.83 ± 0.64 | 6.59 ± 1.29 | 4.73 ± 0.76 | 4.05 ± 0.66 |
Si2p | 20.38 ± 0.65 | 20.24 ± 0.78 | 15.86 ± 0.85 | 14.69 ± 0.77 | 13.16 ± 0.57 | 16.59 ± 0.94 | 15.08 ± 1.19 | 13.30 ± 1.49 |
Fe2p | 0.62 ± 0.12 | 0.55 ± 0.15 | 0.36 ± 0.08 | 0.30 ± 0.06 | 0.25 ± 0.08 | 0.25 ± 0.20 | 0.18 ± 0.14 | 0.18 ± 0.16 |
Ag3d | 0 | 0.96 ± 0.17 | 0 | 0 | 0 | 0.40 ± 0.06 | 0.09 ± 0.07 | 0.10 ± 0.05 |
Br3d | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0.99 ± 0.32 |
Total | 100.03 | 100.00 | 99.94 | 100.02 | 99.98 | 100.00 | 99.84 | 99.88 |
Ag3d/Al2p | 0 | 0.13 | 0 | 0 | 0 | 0.06 | 0.02 | 0.03 |
Ag0/Al2p | 0 | 0.06 | 0 | 0 | 0 | 0.03 | 0.02 | 0.01 |
Ag+ (AgBr)/ Al2p | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0.01 |
Ag(cluster) (3 69 eV)/Al2p | 0 | 0.07 | 0 | 0 | 0 | 0.03 | 0 | 0 |
Ag+ (AgBr)/ Ag0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1.50 |
Br3d/ Al2p | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0.22 |
The MMT-Ag sample showed a little amount of interlayer remaining Na+ (Table 1) with a ratio of the molar fraction Ag3d/Na1s = 16. This high molar fraction could be associated to the presence of both cations at the MMT interlayer, and some Ag+ presence also on the external MMT surface. Sodium and Calcium were replaced according to the surfactant loading in OMMT 21 and OMMT-Ag samples, whereas Potassium was replaced irrespective of the surfactant loading.
Mg and Fe were detected in similar amounts within the error values at MMT and MMT-Ag samples, present mainly as isomorphic substitutions in the octahedral layer of the montmorillonite. The Mg and Fe amounts decrease, as those for Si and Al (Table 1), with the surfactant loading for OMMT samples indicated an increase of surfactant coating of the montmorillonite external surface. The Ag+ addition to OMMT samples generated a subsequent decrease of Mg and Fe amounts, or Mg/Si and Fe/Si ratio (Online Resource 1), pointing out the OMMT surface coverage by Ag+.
The Ag3d/Al2p ratio calculated for all OMMT-Ag samples (Table 1) indicated a decrease of Ag with the increase of surfactant loading.
The thermogravimetric analysis (TG), from 180 to 800 ºC, of same OMMT samples was performed in a previous work 24, and the actual HDTMA+ loadings obtained were 0.49, 0.90, and 1.62 meq/g clay, respectively for MH0.5, MH1 and MH2 samples. Taking these values, a calculation was performed to link the experimentally determined atomic proportions (XPS) to the actual loadings of HDTMA+. The molar ratios C/Si obtained from TG data were: 0.90, 1.66, and 2.99 respectively for MH0.5, MH1, and MH2 samples. The difference between C/Si ratios obtained by XPS and TG, were in agreement with previous data obtained by comparing the XPS area of nitrogen with TG data 24. In the afore mentioned work, the lower percentage of adsorbed surfactant determined by XPS than that obtained by TG data was assigned to the different evaluation of the Van der Waals interactions of the surfactant with MMT surface between both techniques. As a consequence, the actual loading amount of HDTMA for OMMT calculated by XPS data would be a sub-evaluation.
Quaternary ammonium (HDTMA-Br) and Ag oxidation changes due to adsorption on solid surfaces were determined through the binding energy (BE) shift by X-ray photoelectron spectroscopy analyses (Figs. 1 to 4). Table 2 resumes the position of peak maximum, FWHM and χ² of C-C and C-N bonds, obtained from deconvolution of the C1s peaks for all samples.
Figure1 -A.C1s XPS spectrum of HDTMABr. B. C1s binding energies of indicated samples
Sample | C-C | Std. dev. | FWHM | C-N | Std. dev. | FWHM | ÷² |
---|---|---|---|---|---|---|---|
MH0.5 | 284.76 | 0.05 | 1.63 | 286.50 | 0.13 | 2.26 | 1.30 |
MH1 | 284.83 | 0.07 | 1.70 | 286.63 | 0.11 | 1.47 | 1.38 |
MH2 | 284.82 | 0.09 | 1.93 | 285.74 | 0.29 | 1.30 | 1.42 |
MH0.5-Ag | 284.77 | 0.07 | 1.57 | 286.81 | 0.10 | 1.92 | 1.07 |
MH1-Ag | 284.87 | 0.10 | 1.50 | 286.74 | 0.20 | 1.67 | 1.58 |
MH2-Ag | 284.72 | 0.02 | 1.54 | 286.40 | 0.12 | 1.29 | 1.64 |
Particularly, the C1s spectra for HDTMA-Br (Fig. 1A), OMMT and OMMT-Ag samples (Table 2, and Fig. 1B) exhibited two peaks at around 284.8 and 286.3 eV, corresponding to C-C and C-N bonds, respectively
25. For OMMT samples the BE of C-C bonds were within 0.04 eV respect to that of HDTMA-Br, whereas for
21,24
BE of C-N bonds a stronger difference of 0.44 eV was found.
For OMMT-Ag samples the C1s spectrum corresponding to C-C varied within 0.15 eV respect to that of HDTMA-Br, in agreement with data found by Schampera et al. 21 for OMMT with same surfactant. The C-N peak of HDTMA-Br sample at 286.3 eV, shifted to higher BE for MH0.5-Ag and MH1-Ag samples (286.8 and
286.7 eV, respectively); whereas that of MH2-Ag sample presented a BE value similar to that of HDMTA-Br (Table 2, Fig. 1B). The shift of C-N peaks for OMMT-Ag samples towards higher BE could be associated with a change in chemical environment due to electrostatic interaction between the ammonium group (positive charge) and the MMT-Ag surface (more negatively charged than the respective MMT sample). The differences found in BE of the C1s with the increase of surfactant loading was assigned to the more complex arrangement of HDTMA and changes in the local bonding environment of the aliphatic chains 21, which seemed not to change with the Ag+ presence (Table 2).
The N1s peaks presence in OMMT samples was previously evaluated by our work group 24. The N1s peaks from HDTMA-Br and MH0.5-Ag samples; and the BE values obtained for all OMMT-Ag samples are shown in Figures 2A, 2B, and 2C, respectively.
Particularly, when the quaternary ammonium interacted with the clay in Ag presence (MH0.5-Ag sample), this peak shifted to 403.1 eV, and a second smooth and broad peak of N1s appeared at 401.2 eV (Fig. 2B) 26, with a fit of the peaks to N1s profile of χ² =1.20. Both peaks were also found for MH1-Ag and MH2-Ag samples (Fig. 2C), appearing at lower BE (402.9 and 400.5 eV; 402.6 and 399.5 eV, for MH1-Ag and MH2-Ag samples, with a fit of the peaks to N1s profile of χ² = 1.88 and 1.41, respectively).
The symmetrical peak of N1s spectrum at 402.3 eV (Fig. 2A), observed in HDTMA-Br, indicated only
24,27
one chemical status for nitrogen in the surfactant molecule . However, the smooth broadening of the N1s peak present in all OMMT-Ag samples (Fig. 2B) could be attributed to two different transitions, the first occurring around 403 eV and the second between 399.5 and 401 eV.
Figure2 -N1s high-resolution XPS spectra of A. HDTMABr and B. MH0.5-Ag sample. C. N1s binding energies of OMMT-Ag samples
The position of the bands around 403 eV, which coincided with the BE range of the quaternary nitrogen N1s band (Fig. 2B), could be assigned to nitrogen atoms of the surfactant molecules adsorbed on the surface with low energy through Van der Waals interactions (mechanism 1: surfactant molecules interaction with that previously adsorbed on the clay by the strong cation-exchange mechanism) 24 (Fig. 2C). The interaction between the positive head of HDTMA alkyl group and the clay surface shifted N1s peak from 402.3 eV towards higher BE, reaching 403.1 and 402.9 for MH0.5-Ag and MH1-Ag samples, respectively (Fig. 2C). Nevertheless, for MH2-Ag sample the shift was close to that of the surfactant itself (402.6 eV), indicating a local environment of nitrogen similar to that observed for the surfactant in bulk state, which was previously reported for HDMTA-Br load exceeding the CEC 24.
Besides, the position of the N1s bands between 399.5 and 401 eV (Fig. 2B) has previously been attributed to adsorption through cation exchange (mechanism 2) based on XPS studies, and as was earlier reported for HDTMA-MMT 24. The BE value decrease for the second N1s peak was assigned to an increase in
24,28
electron density on the nitrogen atom due to a charge transfer from the clay sheets (Fig. 2C) . This analysis was in agreement with the C1s spectra of C-N bonds (Fig. 1B).
The absence of Br3d in MH0.5 and MH1samples (Table 1) and the respective Ag+ loaded OMMT samples, indicated that this element was eliminated completely by the washing procedure performed to these samples, in agreement with previous data 24. Whilst in MH2 sample Br3d spectrum associated with the Br presence was not observed, in MH2-Ag sample an amount of 0.99 % was found (Table 1). In Figure 3 the Br3d spectra from HDTMA-Br and MH2-Ag samples are shown. Particularly, the Br3d spectrum of HDTMA-Br showed the presence of two peaks at 68.3 and 67.4 eV corresponding to the BE of Br3d 3/2 and Br3d 5/2, respectively, and keeping a peaks adjustment to the Br3d profile of χ² = 1.13. MH2-Ag sample exhibited a peak at
69.3 eV besides that located at 68.3 eV and lower peaks fit to the Br3d profile (χ² = 1.53).
Silver can form complex with HDTMA in solution 29. Moreover, loading increase of some quaternary ammonium ions onto montmorillonite surfaces affect the heavy metal adsorption 30. For the present work, the absence of silver complex with HDTMA adsorbed on MMT was verified by the absence of a 1969 cm-1 IR band (Fig. not shown), whose presence evidences the effect of Br-Ag bond on CH3 –N+ vibration 29. In contrast, this peak was recorded in MH2-Ag sample (Fig. 3 and Fig. 4; Br3d and Ag3d spectra, respectively), suggesting that both surfactant cations and ion pairs occurred in this sample, interacting with the clay, respectively by ion
24,26
exchange and sorption through weak interaction . Furthermore, the peak at 69.3 eV besides that located at
-28,31
68.3 eV, for MH2-Ag could be attributed to the crystal lattice of Br in AgBr .
Figure 3 -Br 3d high-resolution XPS spectra of HDTMABr and MH2-Ag sample
Figure 4. Ag3d high-resolution XPS spectra of OMMT-Ag and MMT-Ag samples
The Ag3d peaks of MMT-Ag and OMMT-Ag samples (Fig. 4) presented broad profiles that were fitted into two Gaussian components, assigned to different components. The peak at 368.2 eV was assigned to the
32–34
formation of metallic silver . Meanwhile, the peak around 369 eV could be attributed to either oxidized silver species (Ag2O or AgOH) intimately interacting with the clay surface or to metallic sub-nanoparticles
15,32,35
associated in small clusters .
The peak associated with metallic silver was observed in all samples. Nevertheless, that located at 369 eV was only evident for MMT-Ag and MH0.5-Ag samples (Fig. 4), decreasing the area ratios calculated with respect to the structural Al2p peak from 0.07 to 0.03, respectively (Table 1). In contrast, MH1-Ag sample showed only one peak associated with metallic Ag-Ag (Ag0) (Fig. 4). Besides, for MH2-Ag sample a peak broadening for Ag3d 5/2 was observed, indicating the presence of a new peak at 367.5 eV attributed to the formation of AgBr, in agreement with Br3d spectra (Fig. 3) 28.
24 26
Based on XPS results, and the models proposed by Naranjo et al. and He et al. , adsorption of the quaternary ammonium in OMMT-Ag at the clay interlayer by a cation-exchange mechanism (mechanism 2) through the positive head of the ammonium group could be suggested. At relative low surfactant concentration (≤ 1 CEC), intercalation could be dominant and HDMTA-Br could enter into the clay interlayer space as cation (HDTMA+), leading to a lateral monolayer, and a pseudotrilayer structure for MH0.5 and MH1 samples, respectively. Similarly, the prevalence of a weak adsorption mechanism leading to a paraffin bilayer structure
21,24,26,36
could be suggested for MH2-Ag . As will be further discussed, these results were supported by zeta potential determinations.
Zeta potential values vs pH were recorded for MMT, OMMT, and their Ag counterparts (Fig. 5A and 5B, respectively).
Figure 5 -Zeta potential of A. OMMT and B. OMMT-Ag samples
The classical negative surface charge was observed for MMT sample (Fig. 5A), originated by structural isomorphic substitutions within the clay sheets 36. A decrease of negative charge was found with the increase of
24,37
QAC, attaining a positive charge when QAC loading was ≧ CEC (Fig. 5A) , indicating not only the full neutralization of the initial MMT negative charge, but also a bilayer arrangement formed by (chain–chain) hydrophobic interactions of the surfactant for MH1 and MH2 samples, thus producing positive charge at the
36,38
external surface .
The Ag exchange into MMT (Fig. 5B), caused an increase of negative charge with respect to MMT sample, in agreement with previous data 15 and assigned to silver clusters or oxide formation as indicated in the Ag3d spectra obtained by XPS (Fig. 4). For MH0.5-Ag and MH1-Ag samples, a slight increase of negative charge and a decrease of positive charge, from pH around 5, were found as compared to MH0.5 and MH1 samples, respectively (Fig. 5A and B). However, for MH2-Ag sample the presence of AgBr and Ag0 nanoparticles (as indicated by XPS, Fig. 4 and 5) produced an increase of the positive zeta potential value with respect to MH2 sample, mainly up to pH 5.
A reduction of Ag+ to Ag0 or the presence of clusters or Ag2O as evidenced by XPS analysis (Fig. 4, Table 1), in agreement with that found by SEM analysis 8, as well as surface coordination of hydroxylated
37,39
silicon surface groups and Ag+ , could be responsible for the surface negative charge increase observed in MMT-Ag with respect to MMT sample. Similarly, the increase in negative charge in MH0.5-Ag (Fig. 5B) with respect to its OMMT counterpart could be attributed to the same chemical species (Fig. 5B, Table 1).
The slight increase of negative charge and the decrease in positive charge at pH around 5, for MH0.5Ag and MH1-Ag samples with respect to the same samples without Ag, could be assigned to the presence of Ag0 nanoparticles (isoelectric point, IEP < pH 2), in agreement with Ag3d XPS peak deconvolution (Fig. 4), which presented low negative zeta potential below pH 5, increasing with pH up to pH 8, where the particles were quite stable due to electrostatic repulsion40.
In MH2-Ag sample the increase in positive zeta potential value with respect to MH2 sample, could be assigned to the excess of cationic surfactant and the start of Br -sorption 24, with the consequent AgBr formation, as indicated by XPS spectra (Fig. 3 and 4). Due to the IEP of AgBr at pH 5 41; and to the presence of Ag0 nanoparticles, with IEP below pH 2 40, a higher positive zeta potential value in MH2-Ag with respect to MH2 sample was found up to pH 5.
ZIA determination was performed to obtain a rapid screening of samples antimicrobial activity (Fig. 6), which was further quantified by MBC determination (Table 3).
As can be seen from the activity against S. aureus and E. coli, exerted by the clay and OMMT respectively (Fig. 6A and 6B), and their Ag counterparts samples (Fig. 6C and 6D), antimicrobial activity was dependent on both the clay modifier and the sensitive microorganism used.
When assayed against S. aureus (Fig. 6A and 6C), OMMT, OMMT-Ag as well as MMT-Ag samples evidenced antimicrobial activity, in contrast to MMT sample. The increase of surfactant loading augmented inhibition areas against S. aureus, as observed for MH0.5, MH1, and MH2 samples (Fig. 6A). Furthermore, an increase in inhibitory activity upon silver addition to the clays was only evident for MMT-Ag and MH0.5Ag samples (Fig. 6C).
OMMT samples presented limited antimicrobial activity against E. coli with inhibition areas being evident only for MH2 sample (Fig. 6B). In contrast, Ag addition to MMT and OMMT imparted antimicrobial activity against E. coli to all the samples (Fig. 6D).
Figure 6 -Antimicrobial activity of the indicated clays against A.C. S. aureus ATCC 25923 and B.D.
When quantifying bactericidal activity, more concentrations of all clays were needed to kill the assayed bacteria when compared to the free surfactant (Table 3). For all OMMT samples the higher the surfactant loading, the lower the MBC. Thus, in order to kill S. aureus using MH0.5 sample, a concentration four times higher than that of MH1 sample and around ten times higher than that of MH2 sample was required (Table 3). Similarly, MH0.5 sample showed no ability to kill E. coli, whereas 50.00±21.65 and 2.50±1.08 mg/ml were needed to kill this bacterium using MH1 and MH2 samples, respectively.
In addition, when comparing the antimicrobial activity of silver-added clays with their respective counterparts, a reduction of the MBC needed to kill S. aureus upon Ag addition was observed (Table 3). A similar effect was observed against E. coli for all samples except for MH2 sample, for which MBC was not affectedbyAg addition (p≥0.05) (Table 3).
The behavior and properties of the organic MMT depend largely on the structure of the composites and the organic molecular/ion environment in the interlayer 14. OMMT antimicrobial activity found in the present work was intimately related to the surfactant availability within the clay. Thus, the increase as well as rearrangements of HDTMA+ in the clay had an effect on antimicrobial activity. For both assayed microorganisms, major antimicrobial activities were observed for MH1 and MH2, compared to MH0.5 sample. This result could be explained in terms of van der Waals interactions (mechanism 1), which were more relevant in MH1 and MH2; whereas in MH0.5 sample the surfactant mainly interacted by cation exchange (mechanism 2), as previously discussed. Weak interactions could allow HDTMA+ to be easily released from the clay to reach the cell membranes in a concentration higher than the minimum inhibitory concentration (MIC), thus giving the observed inhibitory activities (Fig. 6A and 6B) 42. This behavior was reflected in the reduction of clay concentration needed to kill bacteria when HDMTA+ loaded concentration increased over the CEC as studied by MBC assays (Table 3). Moreover having the highest proportion of HDMTA-Br and van der Waals interactions, as calculated from XPS (Table 1), MH2 showed the highest bactericidal capacity with respect to the other OMMT samples. Similarly, Parolo et al. 43 found that only smectites exchanged with an amount of surfactant greater than that of the mineral CEC exhibited suitable antibacterial activity against E. coli, attributing the inhibition effect to the surfactant from the external clay surface.
Table 3. Antimicrobial activity of the indicated samples, expressed as minimum bactericidal concentration (MBC) against S. aureus and E.coli
Sample | MBC (mg/ml) against | |
S. aureus ATCC 25923 | E. coli ATCC 25922 | |
MMT | ND | ND |
MH0.5 | 5.56±2.73a | ND |
MH1 | 1.33±0.66b | 50.00±21.65a |
MH2 | 0.50±0.15c | 2.50±1.08b |
HDTMABr | 0.0067±0.0034d | 0.042±0.016c |
MMT-Ag | 5.00±2.17a | 0.83±0.31d |
MH0.5-Ag | 0.57±0.28c | 11.11±5.46e |
MH1-Ag | 0.67±0.33c | 1.04±0.31d |
MH2-Ag | 0.28±0.14 f | 3.75±1.62b |
ND, bactericidal activity not detected; MMT, montmorillonite; MH0.5, MH1, and MH2 are MMT loaded with HDTMABr corresponding to 0.5, 1, or 2 CEC, respectively; MMT-Ag, MH0.5-Ag, MH1-Ag, and MH2-Ag are the respective silver organic montmorillonite counterparts.
a-f Different letters in the same column indicate significant differences (P˂0.05)
The antimicrobial activity of OMMT samples was also dependent on the assayed microorganism, being less effective against E. coli ATCC 25922 (Table 3). The mode of action of quaternary ammonium surfactants involves an association of the charged quaternary nitrogen with the head groups of acidic-phospholipids within the cytoplasmic or inner membrane, this allowing the hydrophobic tail integration into the hydrophobic membrane core of the bacterium and causing the cell to die 44. E. coli is a gram-negative bacterium; because this enteric bacterium inhabits the mammalian gut, it must have a cell envelope that is particularly effective at excluding some hydrophobic and hydrophilic molecules, as well as detergents such as bile salts 45. Hence, this outer envelope present in gram-negative bacteria would constitute an additional barrier interfering in HDMTA+ entrance to reach the inner cell membrane, as previously reported for QACs 3, thus increasing MBC either for the free surfactant and or OMMT (Table 3).
Also, the interaction between the clay and bacteria is important. Because the outermost surface of
44,45
bacterial cells carries a net negative charge , higher positive charges observed by zeta potential measurements upon HDMTA-Br addition to the clay in concentrations higher than the CEC, could lead to an increase in the membrane/OMMT interaction with the corresponding increase in antimicrobial activity.
The addition of Ag+ to OMMT samples was studied in order to find out whether antimicrobials targeting different molecules, and having different arrangements within the clay produced different synergistic effects against the assayed microorganisms.
For S. aureus, a marked increase in activity was observed for all samples but MH2-Ag in comparison to their OMMT counterparts (Table 3), indicating synergy of HDMTA+ and Ag in all cases, even when for MH2Ag the effect was less pronounced. The later result could be related to antagonist effects obtained when adding silver to OMMT, i.e. higher surfactant loading led to lower interchanged silver proportion (Table 1).
As previously reviewed by Durán et al. 5 silver ion and silver nanoparticle (AgNPs) activities rely on: (a) the uptake of free silver ions, followed by disruption of ATP production and DNA replication; (b) reactive oxygen species (ROS) generation by AgNPs and silver ions; and (c) direct damage to the cell membrane by AgNPs. In the present work, the presence of silver clusters in MMT-Ag, as suggested by XPS analyses (Fig. 4, Table 1), could be a source of AgNPs with the consequent increase in antimicrobial activity with respect to MMT (Table 3). Furthermore, MBC determinations showed that S. aureus presented lower sensitivity to MMT-Ag than
E. coli. This was also described for silver ions, Ag2O, and AgNPs, and was attributed to the thick peptidoglycan
4,5,46
layer in the cell wall of gram-positive microorganisms .
Besides, as above-stated, HDMTA+ was more effective in inhibiting S. aureus than E. coli due to the outer membrane present in the later bacterium. For MH0.5-Ag sample, even though an increase in activity against S. aureus and E. coli was obtained with respect to its counterpart, an opposite effect against E. coli was observed when comparing MH0.5-Ag to MMT-Ag sample (Table 3). This result could be related to the different silver proportions found in both samples (Table 1), coupled with silver and HDMTA+ mechanisms of action. Hence, S. aureus membrane disruption by HDMTA+ might allow silver ion entrance to the cell, whereas the surfactant could be retained by the selective E. coli membrane, avoiding antimicrobial synergy effects against the later organism (Table 3). Likewise, MH2-Ag, having the highest proportion of HDMTA-Br loaded on the clay and the lower proportion of Ag, mainly as AgBr, presented a similar MBC to that of MH2 and higher than that of MMT-Ag against E. coli (Table 3).
These antagonists effects led to the better activity observed for MH1-Ag sample, showing the optimal combination of silver and HDMTA+, which produced a synergy effect against S. aureus, while maintaining antimicrobial activity against E. coli (Table 3).
Unlike the present work, Savas and Hancer 8 reported failure to inhibit E. coli when using HDTMAMMT with 100% CEC loading. The result found by these authors could be attributed to OMMT concentration (25 mg/ml) below the MIC needed to inhibit the E. coli ATCC 11230 strain. In the present work, MH1 was capable of killing E. coli ATCC 25922 by using 50 mg/ml of the clay (Table 3). These authors also informed Ag+-HDMTA synergistic effects when assaying Ag+ OMMT–LDPE nanocomposite against E. coli ATCC 11230 as compared to OMMT 8; nevertheless, the comparison was performed avoiding silver MMT effects. As previously discussed in the present work, when looking for possible synergies, is critical to compare all antimicrobials in order to have a complete outlook.
XPS and zeta potential surface techniques were useful to predict cations´ rearrangements that explain the antimicrobial activity behavior of OMMT and OMMT-Ag samples.
The XPS analysis of the N1s spectra of OMMT-Ag sample showed surfactant adsorption on both the interlayer and the outer clay surface, through a cation-exchange mechanism and Van der Waals interactions, respectively. Furthermore, C1s spectra analyses established an HDTMA+ contact with the clay surface, through the positive head of the ammonium group, avoiding a direct contact between the carbon tail and silica surface.
Surface electric charge modifications on OMMT with respect to MMT sample when surfactant loading increased were attributed to pseudo trilayer and paraffin bilayer arrangements also at the outer surface.
Silver addition generated Ag0 in all OMMT samples in different proportions and species depending on the surfactant loading. For MH0.5-Ag, the presence of surfactant diminished the Ag amount with respect to MMT-Ag sample and clusters were found in both clays. For MH1-Ag and MH2-Ag samples, increasing surfactant loading also decreased the amount of Ag within the clay, MH2-Ag sample showing the presence of AgBr. For MMT-Ag and MH0.5-Ag samples, the presence of Ag clusters and Ag0 increased the negative zeta potential, whereas the opposite effect was observed for MH1-Ag and MH2-Ag with respect to MMT sample.
The antimicrobial activities of OMMT samples found in this work were intimately related to the surfactant availability within the clay. The decrease in MBC was obtained for samples having surfactant loading over the CEC and HDTMA-Br mainly interacting through weak forces. The addition of silver to OMMT produced synergy effects against S. aureus; nevertheless, this effect was not evident for E. coli. The result was attributed to the lower sensitivity of the later microorganism to HDTMA-Br coupled with the decrease in silver concentration when the surfactant loading increased within the clay.
This work contributes to the understanding of clay antimicrobial activity involving HDMTA+ and silver. This understanding, as well as the awareness of synergy effects, could help in the design of new delivery systems to fight bacteria.
MMT, montmorillonite OMMT, organic montmorillonite HDTMA-Br, hexadecyltrimethylammonium bromide CEC, cation exchange capacity MH0.5, MH1, MH2, respectively montmorillonite interchanged with 50, 100 and 200% of clay cation exchange capacity MMT-HDMTA-Ag and OMMT-Ag, montmorillonite interchanged with hexadecyltrimethylammonium bromide and silver QAC, quaternary ammonium compounds FWHM, full width at half maximum ZIA, zone of inhibition assay MBC, Minimum inhibitory bactericidal concentration CFU, colony-forming units BE, binding energy IEP, isoelectric point AgNPs, silver nanoparticles
nanoparticles using microorganisms. Mater. Sci. Pol., 2008, 26, 419–424.
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