Polymer 99 (2016) 614e622 Contents lists available at ScienceDirect Polymer journal homepage: www.elsevier.com/locate/polymer Role of the OH and NH vibrational groups in polysaccharidenanocomposite interactions: A FTIR-ATR study on chitosan and chitosan/clay films C. Branca*, G. D'Angelo, C. Crupi, K. Khouzami, S. Rifici, G. Ruello, U. Wanderlingh Department of Physics and Earth Sciences, University of Messina, Viale Stagno D'Alcontres 31, 98166 Messina, Italy a r t i c l e i n f o a b s t r a c t Article history: Received 2 May 2016 Received in revised form 25 July 2016 Accepted 29 July 2016 Available online 30 July 2016 Attenuated Total Reflectance Fourier Transform Infrared (ATR-FTIR) spectroscopy was used to examine the impact of hydrogen bonding on the reactive amine and hydroxyl groups of chitosan. Measurements were performed on powder and film samples hydrated under different conditions. To resolve the individual OH and NH bands that overlap in the region between 3000 and 3800 cm1, the spectra were deconvoluted using a Gaussian curve fitting method. By analyzing the changes recorded for each Gaussian component along the dehydration process of the films at different pH values, a band assignment was proposed. This assignment was then used to analyze the ATR-FTIR spectra of the chitosan/ montmorillonite composites. The changes induced by the presence of the clay were ascribed to particular mechanisms of interaction that involve the active sites of the clay and the amino or hydroxyl groups of chitosan. The comparison between the FTIR and the XRD data, evidenced that these mechanisms are intimately controlled by the type of nanostructures that are formed depending on the clay content. © 2016 Elsevier Ltd. All rights reserved. Keywords: Chitosan Montmorillonite FTIR-ATR spectroscopy 1. Introduction Naturally occurring polymers are extensively used as biocompatible and biodegradable materials and their importance will increase further in the future because of the growing urgency to develop new bio based products. Most of the biopolymers are based on biodegradable starch polymers, such as chitosan. Chitosan is the only natural cationic polysaccharide derived from chitin through a deacetylation process to obtain a linear structure of glucosamine and N-acetylglucosamine linked in a b-1,4 manner. The chemically active groups in the chitosan structure are the free amine groups, located in the C2 position of the glucose residue in the polysaccharide chain, and the hydroxyl groups, that can be both modified and involved in hydrogen or electrostatic bonding [1e3]. The amine groups can be easily protonated in acid environment making chitosan soluble in aqueous acid solutions. Thanks to its high biocompatibility, non toxicity, antifungal and antimicrobial activities, chitosan is used for a broad range of applications including drug carriers, food packaging films, bone substitutes and so on [4e11]. However, its applications are limited because of the * Corresponding author. E-mail address: cbranca@unime.it (C. Branca). http://dx.doi.org/10.1016/j.polymer.2016.07.086 0032-3861/© 2016 Elsevier Ltd. All rights reserved. high moisture permeability and brittleness. The combination of chitosan with clay nanofillers, such as montmorillonite, has proved to be an effective method to overcome this limit creating new nanocomposites showing improved mechanical, thermal and barrier properties usually even at very low concentrations [12e21]. Montmorillonite (hereafter MMT) is a hydrated alumina-silicate layered clay made up of two silica tetrahedral sheets fused to an edge-shared octahedral sheet of aluminum hydroxide. It is well suitable for reinforcement purposes since it has a high surface area, large aspect ratio (50e1000), and platelet thickness of 10 Å [22e24]. Due to the relatively weak forces between the layers of MMT, water and other polar molecules can enter between the unit layers, causing the lattice to expand in the thickness direction. Although several studies are reported in literature about chitosan-clay composites, the overall understanding of the interactions underlying the formation of composite films still remains elusive. It is generally reported that the incorporation of montmorillonite induces electrostatic interactions between the negatively charged groups of the clay and the positively charged eNHþ 3 groups of chitosan [12,13,15,17]. However, controversial results are reported in literature [12,13,15,17,19,21] about the dependence on the clay content shown by many properties of the polymer/clay composites, such as tensile strength, elongation and swelling. C. Branca et al. / Polymer 99 (2016) 614e622 615 Considering that interactions between different components are governed by a variety of chemical bonds, the study of the vibrational properties can provide a valuable tool to understand the nature of the interactions that strongly affects the properties of the final products. In the present work, by ATR-FTIR spectroscopy, we investigated the role played by the OH and NH groups of chitosan in the formation of an hydrogen bonded network and how this is modified by the presence of a nanocomposite structure. Measurements were performed for chitosan powder, dry and hydrated films, and chitosan/montmorillonite nanocomposite films at different clay content. In particular, the time evolution of the absorption spectra of the chitosan films, hydrated at different pH values, were carefully monitored along the dehydration process. Infrared spectra were recorded in the mid-ir region focusing the attention on the stretching region that was deconvoluted using a Gaussian curve fitting method. The novelty of the present work lies in a comprehensive vibrational analysis of the spectral features of chitosan under different environmental conditions that allowed a separation and identification of the intramolecular OH and NH stretching components. The assignment of these modes, usually reported as overlapping bands in the region 3000e3800 cm1, was crucial to get insights into the existing correlation among mechanisms of interaction between chitosan and clay, swelling properties and different architectures of nanostructures. XRD mounts were obtained by pipetting a small amount of the solutions onto glass plates. Silicon powder was added to the spread solution, thus Silicon peak was used as a reference, in order to shift spectra to the correct position and eliminate possible mistakes due to incorrect vertical positioning of the sample. The solvent was then removed by evaporation under nitrogen flux and the dry samples were stored at 35 C. The drying of the XRD mounts was performed at the same nitrogen flux and time duration for all the samples to guarantee the comparability of XRD results. 2. Experimental where We and Wd are the weights of the sample at equilibrium and in the dry state, respectively. 2.4. Swelling Dry chitosan films were immersed in water solutions at different pH values, 3 and 11, and stored at 25 C. In order to avoid any structural alteration of the phyllosilicate, all the chitosan-clay films were swollen at pH 6. After the removal of the excess surface water by filter paper, the weights of the samples were measured at various time intervals. The weighing was continued until equilibrium swelling was attained. Each swelling experiment was repeated three times, and the average values were reported. The equilibrium degree of swelling (EDS) was calculated as follows: EDSð%Þ ¼ We Wd *100 Wd (1) 2.1. Materials Low molecular weight chitosan (CS) (Cat. No. 448869, 190e310 kDa) and montmorillonite K10 were purchased by Sigma Aldrich. MMT employed in this study has a CEC of 70e100 meq/ 100 g. We used montmorillonite for its unique intercalation/exfoliation characteristics that can lead to platelets with very high stiffness and strength when dispersed in a polymer matrix. All the reagents were analytical grade and used without further purification. 2.2. Sample preparation Chitosan was dissolved in 1% acetic acid solution, magnetically stirred for 24 h at 40 C. The pH of the polysaccharide solution was adjusted to 5 with NaOH in order to avoid any structural alteration of the phyllosilicate. We obtained a final concentration of 1.6% (w/ v). Prior to the addition of clay, an aliquot of the solution was cast on a Teflon dish and left overnight for drying in an oven at 30 C. The sample, labeled “as prepared film”, was kept in a desiccator before characterization. Two clay suspensions were prepared and slowly added to two aliquots of the chitosan solution in order to obtain two physical mixtures with a clay concentration of 2.5 wt% and 5 wt% based on chitosan. For simplicity, these samples were labeled as CSM2.5 and CSM5. The mixtures were stirred for 2 days, then poured onto a Teflon surface and dried in an oven at 30 C. Finally, they were peeled off, washed with bistilled water until free from acetate, and stored in a desiccator until the tests were done. 2.5. ATR-FTIR FTIR spectra were recorded at room temperature in the mid IR range (400e4000 cm1) on a Bruker Vertex 80V FTIR spectrometer equipped with a Bruker Platinum ATR accessory with a single reflection diamond crystal. Each spectrum was averaged over 128 scans with a resolution of 2 cm1. A background scan was recorded prior to the measurement and subtracted from the sample spectra. The ATR correction to each spectrum was applied using the OPUS software (Bruker optics). The spectra were normalized to the same area and compared to each other. Measurements were performed on powder, dry films and hydrated films. In this latter case, the films were placed on the ATR diamond and exposed to the dynamic vacuum of a diffusion pump 2.3. X-ray diffraction (XRD) The diffractograms of the samples were recorded at room temperature using a D8-ADVANCE Bruker diffractometer in BraggBrentano geometry using the Cu line l ¼ 1.542 Å. Each scan covered 2q from 2 to 12 with a step size of 0.02 , 1 s per step. Fig. 1. A 3-D frequency-time-intensity plot for the dehydration process of a chitosan film. 616 C. Branca et al. / Polymer 99 (2016) 614e622 at room temperature for fixed times to monitor the dehydrationinduced conformational changes. Spectra were recorded every 30 s initially and then every 2 min to 1 h. As an example, in Fig. 1 a 3D plot for the dehydration process of a chitosan film is reported. In order to separate the OH and NH vibrational groups overlapping in the region between 3000 and 3800 cm1, a deconvolution of this spectral region into Gaussian components was performed. According to the usual procedure, we started with two components and then increased the number until the deconvolution was significantly improved. We used a curve-fitting procedure using Peakfit software with all fit parameters having a 95% confidence interval. To avoid any ambiguity as to the number of components, we monitored both c2 and the residual sum of squares (RSS) and selected the number of Gaussian components that minimized both the parameters. No constraint was imposed on the fitting parameters. To avoid any distortion of the band shape resulting from an incorrect background subtraction, the whole region down to 1800 cm1 was deconvolved. It was observed that for all the recorded spectra the same number of components were required to satisfactorily reproduce the spectral profiles. After the deconvolution was completed, the Gaussian components below 3000 cm1 were subtracted from each spectrum. Such a procedure evidenced the presence of six components in the region between 3000 and 3800 cm1. This result is fully consistent with the previsions about the presumed minimum number of components based on literature data according to which at least four components are expected (two for the primary amine group, one for the secondary and at least one for the hydroxyl group). 3. Results and discussion Fig. 2. (a) Equilibrium swelling degree of chitosan film at different pH values; b) Equilibrium swelling degree of chitosan film and its composites at pH 6. overlap in the same spectral region and, as a consequence, a clear assignment of these modes is not trivial. The strategy followed in this work to overcome this problem involved the use of a curve fitting procedure and the analysis of chitosan under different forms. To start with, the ATR-FTIR spectrum of the dry “as prepared” chitosan film was compared to that of the chitosan powder. As one can see from Fig. 3, both spectra present three main spectral regions: i) a broad asymmetric band between 3400 and 2500 cm1 encompassing the CH stretching modes at around 2927 and 2873 cm1 and, at higher wavenumbers, the overlapped OeH and NeH stretching vibrations; ii) a region between 1700 and 1200 cm1 characteristic of the amide groups; iii) a strong absorption region between 800 and 1200 cm1 characteristic of the (a) (b) C-O-C Transmittance (a.u.) Transmittance (a.u.) As a preliminary phase, we investigated the swelling properties of the prepared samples. They all swelled very rapidly and reached equilibrium within half an hour. Confirming data from literature, the chitosan films swelled to a larger degree at the lowest pH values, see Fig. 2(a). The increased swelling in acidic condition is generally ascribed to the presence of more protonated amino groups that induce electrostatic repulsions between the polymer segments. As pH increases, amino groups become deprotonated and repulsions recede [25,26]. In the following, the relationship between swellability and pH will be examined more closely with respect to changes in the vibrational properties of some specific functional groups. For what concerns the polymer-clay composites, the presence of the clay induces a reduction in the swelling property with respect to the chitosan film at the same pH of 6, see Fig. 2(b). This is reasonable since it was proved that the dispersion of nanofillers into a polymer matrix introduces breakable physical crosslinks based on noncovalent interactions [18,27e31]. Consequently, a denser structure with a reduced swelling capability has to be expected. However this effect is not linearly dependent on the clay content; in fact, as shown in Fig. 2(b), the EDS (%) reached a minimum for a clay concentration of 2.5% and then increased by further increasing the clay content. This result suggested that, depending on the number of amino and hydroxyl groups involved in the chitosan-clay interaction, peculiar nanostructures with different hydrogen bonding network were likely to be formed. In this frame, ATR-FTIR spectroscopy can give valuable information since it is particularly sensitive to the conformational changes and reorganization of intra and intermolecular hydrogen bonds involving the active groups of the compounds. In the present work, we analyzed first the absorption spectra of chitosan and then those of the chitosan/clay composites, focusing the attention on the OH and NH stretching vibrations. This kind of study is rather complex and challenging since the amino and hydroxyl groups 1555 1590 (a) (b) C-H 1400 1500 1600 -11700 Wavenumber (cm ) N-H, O-H 500 1000 1500 2000 2500 3000 3500 4000 -1 Wavenumber (cm ) Fig. 3. FTIR-ATR spectra of chitosan powder (a) and dry “as prepared” chitosan film (b). The inset shows a magnification of the amide region. C. Branca et al. / Polymer 99 (2016) 614e622 chitosan saccharide structure. Peaks at similar locations were observed by several groups working on chitosan and its derivatives [15,25,30e37]. The main differences between the film and the powder spectra are visible in the amide region, see inset of Fig. 3, where for the chitosan powder the characteristic peaks of amide I, amide II and amide III are located at 1650 cm1, 1590 cm1 and 1317 cm1, respectively [32,33]. The peaks at 1375 cm1 and 1420 cm1 are assigned to the CH3 symmetrical deformation mode [38,39]. For the “as prepared” film, the effects of protonation of the amine functionalities in the acidic medium are evident. In fact, protonation gives rise to two peaks both attributed to NHþ3 groups, namely the antisymmetrical deformation that overlapped the amide I band at 1646 cm1, and the symmetric deformation (dNH3) at 1555 cm1 [13,36]. Significant differences in the spectral profiles of the powder and the film appear also in the stretching region, see Fig. 4(a) and (b). To better quantify these changes, a deconvolution in Gaussian lineshapes, also displayed in the same figures, was performed. In Table 1 the values of the central frequencies of the Gaussian components together with the integrated areas are reported. Each of these components was numbered from A to F, as reported in the table, and we will use this nomenclature in the discussion that follows. Notwithstanding previous studies, performed by using similar approaches, often resulted in a controversial identification of the spectral components in this stretching region, there is a general agreement on the assignment of the high frequency side to the vibrational stretching of the hydroxyl groups, and of the low frequency one to the amine stretching mode [40e44]. In order to assign each of these components to a specific vibrational group, the FTIR-ATR spectra of chitosan films at different hydration degree and pH were also recorded and analyzed. In fact, it is reasonable to expect that the OH and NH groups are involved to a different extent in the protonation and hydration processes and that this is reflected into some spectral changes. For this reason, starting from an hydration level corresponding to h z 1.1 (h ¼ g H2O/g dry chitosan) at pH 3 and 11, we monitored the time evolution of the ATR-FTIR spectra along the dehydration process by comparatively analyzing the changes exhibited in the amide and stretching band. In the following, for sake of clarity, only the spectra corresponding to three dehydration times are reported: tdehyd ¼ 0, Absorbance (a.u.) a) b) 2800 3200 3600 -1 Wavenumber (cm ) Fig. 4. Spectral deconvolution for the chitosan powder (a) and “as prepared” dry film (b) into Gaussian components. The experimental data are reported as squares; the best fit is reported as a continuous line together with the single Gaussian contributions (dashed lines). 617 Table 1 List of peak frequencies and integrated areas of the deconvoluted bands in the region 2800e3700 cm1 for the chitosan powder and the “as prepared” film. Sample Peak Powder A B C D E F 3094 3223 3294 3358 3422 3550 Area% Sample Peak 19.0 26.5 11.0 5.4 31.7 6.4 As prepared film A B C D E F Area% 3075 3225 3292 3355 3424 3564 26.4 25.9 6.3 4.8 31.2 5.4 hydrated sample, tdehyd ¼ 4 min, partially hydrated sample, and tdehyd ¼ 24 h fully dried sample. The ATR spectra reported in Figs. 5(a) and 6(a) show the dehydration evolution in the amide region for chitosan films at pH 11 and pH 3, respectively. For comparison, the spectrum of the dry “as prepared” film is also reported as dashed line. The plots b, c and d of Figs. 5 and 6 show the Gaussian deconvolution of the same spectra in the high frequency region. With reference to the amide region, what emerges at first sight from these plots is that, whereas at pH 11 the effects of hydration seem to be reversible, at pH 3 these effects modify permanently the spectral profiles. This qualitative observation is confirmed by the analysis of the frequency shifts observed for the two bands with increasing dehydration degree at pH 3 and 11, see Fig. 7(a) and (b). The frequency values corresponding to the dry “as prepared film” are also reported as dashed lines. As can be inferred from Fig. 7, at pH 11 (circle symbols), after a slight frequency upshift determined by the initial hydration of the film, both the bands moved back to the positions before the swelling. On the contrary, at pH 3 (square symbols), the hydration of the film induced a significant downshift in both peaks that increased further in the first hour of dehydration and then levelled off. This behavior can be explained in terms of a protonation effect. In fact, under acidic conditions, because of the excess of Hþ, we expect a further protonation of both the amine and the carbonyl groups at the oxygen with a consequent downshift of the corresponding bands. This is more evident as the dry state is approached because of the antagonist “deprotonation” effect of water. However, the larger downshift observed at pH 3 for the lower frequency component, ~17 cm1, suggests an higher involvement of the amine groups rather than the carbonyl ones in the hydration process. This is in agreement with previous observations according to which the higher swelling degree of chitosan film in acidic pH is attributed to the presence of the ionic eNH3þ groups that cause the migration of counter ions into the hydrogel favoring water uptake [26]. Starting from these observations, we have analyzed the effects of the hydration/dehydration process on the peak positions and on the fractional areas for the Gaussian components in which the stretching region was deconvolved. Let's start with the component labeled as E. Comparing Table 1 with Table 2, no change for this component is observed between the powder and the film, whereas, as a result of hydration, a significant downshift and an increase of the percentage area is evident for any pH value. These variations suggest that, in agreement with previous studies [45e47], this component can be associated to the more solvent exposed hydroxyl groups of chitosan that tend to form hydrogen bonds with the water molecules rather than OHeOH or NHeOH bonds within the polysaccharide itself. Considering that the lower the pH, the higher the swelling and, hence, the more the OH groups that are solvent exposed, it is not surprising observing that the redshift for the E component is higher under acidic conditions. Along the subsequent dehydration process, tdehyd=0 tdehyd=24 h 1520 1560 1600 1640 -1 Absorbance (a.u.) Wavenumber (cm ) 1680 2800 3200 tdehyd=0 3200 3600 -1 Wavenumber (cm ) tdehyd=4 min c) b) 2800 Absorbance (a.u.) a) Absorbance (a.u.) C. Branca et al. / Polymer 99 (2016) 614e622 Absorbance (a.u.) 618 3600 2800 -1 tdehyd=24 h d) Wavenumber (cm ) 3200 3600 -1 Wavenumber (cm ) a) tdehyd=0 tdehyd=24h Absorbance (a.u.) Absorbance (a.u.) Fig. 5. FTIR-ATR spectra of chitosan film initially hydrated at pH 11 recorded for increasing times of dehydration. Plot a) shows the evolution of the spectra (solid lines) in the region 1500e1700 cm1 monitored at (from top to bottom) tdehyd ¼ 0, 4 min and 24 h. For comparison the spectrum of the “as prepared film” before swelling is also reported as dashed line. Plots b), c) and d) show the Gaussian deconvolution of the same spectra in the region 2700e3800 cm1. 1480 1520 1560 1600 1640 1680 -1 2800 tdehyd=4 min 2800 3200 -1 Wavenumber (cm ) 3600 Absorbance (a.u.) Absorbance (a.u.) Wavenumber (cm ) c) b) tdehyd=0 3200 tdehyd=24 h d) 2800 3600 -1 Wavenumber (cm ) 3200 3600 -1 Wavenumber (cm ) Fig. 6. FTIR-ATR spectra of chitosan film initially hydrated at pH 3 recorded for increasing times of dehydration. Plot a) shows the evolution of the spectra (solid lines) in the region 1500e1700 cm1 monitored at (from top to bottom) tdehyd ¼ 0, 4 min and 24 h. For comparison the spectrum of the “as prepared film” before swelling is also reported as dashed line. Plots b), c) and d) show the Gaussian deconvolution of the same spectra in the region 2700e3800 cm1. the position of this component shifts to higher frequencies suggesting the occurrence OH bond contraction related to the progressive decrease in the number of neighboring water molecules. However, it is interesting observing that the extent of this bond contraction is strongly dependent on pH; in fact, whereas for the totally dehydrated sample at pH 3, the frequency of the E component is about 10 cm1 higher than that observed for the “as prepared film”, for the sample dehydrated at pH 11, it is practically the same. Indeed, at pH 11, almost all the components are located at the same frequencies of the “as prepared film”, thus confirming the observation made for the amide region about the reversibility of the hydration/dehydration process under basic conditions. Contrary, the differences observed in the dry state at pH 3 suggest the occurrence of deep and permanent changes in the polymeric network after swelling in acidic conditions. In particular, the hypothesized higher contraction of the OeH bond at pH 3, can be 1550 1540 1530 1300 tdehyd (min) 1400 -1 Peak frequency (cm ) 0 b) 1648 1644 1640 1636 1632 1628 0 1300 tdehyd (min) 1400 Fig. 7. Peak frequency shifts for the deformation (a) and amide I (b) band as a function of the dehydration time, tdehyd for chitosan films hydrated at pH 3 (squares) and pH 11 (circles). The values corresponding to the dry “as prepared film” are also reported as dashed arrows for comparison. Table 2 List of peak frequencies and integrated areas of bands in the region 2800e3700 cm1 for the chitosan film hydrated at pH 3 and pH 11 for different dehydration times. tdehydr ¼ 0 (h ¼ 1.1) tdehydr ¼ 4 min tdehydr ¼ 24 h (dry) Peak (cm1) Area (%) Peak (cm1) Area (%) Peak (cm1) Area (%) 25.9 27.8 4.1 1.2 39.2 1.8 3065 3217 3292 3354 3413 3578 28.0 27.4 4.0 2.1 37.1 1.4 3053 3222 3292 3355 3434 3581 39.2 25.2 3.1 4.2 27.1 1.2 24.0 26.1 4.8 2.7 37.1 5.3 3084 3222 3292 3356 3417 3567 23.9 26.2 4.9 3.8 36.0 5.2 3083 3223 3294 3354 3422 3568 24.2 26.2 6.3 5.1 31.8 6.4 pH3 A 3072 B 3215 C 3290 D 3354 E 3408 F 3577 pH11 A 3085 B 3222 C 3294 D 3356 E 3415 F 3568 ascribed to an excess of negative ions gathered around the NHþ 3 ions that, reducing the repellency among positive ions, favor the folding of the polymer chains. The behavior of the E component presents some analogies with that observed for the B component. In particular, for the sample hydrated at pH 3, a shift to a lower frequency and an increase of the area for this component can be observed. Moreover, along the dehydration, it moves again to higher frequencies tending to values close to those measured for the “as prepared” chitosan film. This similarity suggests the idea that also this component could be assigned to stretching vibrations involving hydroxyl groups of chitosan. However, the fact that at pH 11, both the hydration and dehydration process does not induce any significant change in the spectral characteristics of this component, suggests that the hydroxyl groups involved in this stretching vibration are those deeply buried inside the polymer coil that are accessible to solvent only after a strong swelling of the polysaccharide. For what concerns the A component, it resulted to be the most sensitive to pH changes. In particular, after the powder was treated 619 in an acidic solution to prepare the film, a strong downshift, of about 20 cm1, and a decrease in the integrated area was observed for this component, see Table 1. The subsequent hydration of the “as prepared film” caused slight changes at pH 3 and a marked frequency Given these findings, we hypothesized to assign this component to the stretching vibration of primary amine groups, the most sensitive to pH changes, and to relate its frequency shifts to the higher or lower upshift, with a reduction in the integrated area, at pH 11, see Table 2. Along the dehydration process at pH 3, a new strong peak downshift, associated with a consistent increment in the integrated area, is observed for this component. Contrary, at pH 11 the dehydration seems to have no effect. Degree of protonation. More precisely, the positioning of this component is the result of two competitive processes; the deprotonation from the water molecules, that is the dominant effect for the most hydrated samples, especially for those under basic conditions, and the protonation of the amine groups at pH 3 that obviously predominates in the dry state. The F component deserves a particular discussion. Differently from all the others components associated to functional groups of chitosan, in our opinion it has to be attributed to water molecules absorbed in the inner polymer and tightly bound to chitosan. The presence of some residual water is widely reported in literature [45e47]. The behavior observed for this component along the initial film preparation and the following hydration/dehydration process, is fully consistent with the hypothesis of a progressive hydrogen bond weakening that involves the water molecules. The fact that this effect results more marked under acidic conditions, that is when the chitosan segments are loosened out, and that this component is located, for the dried sample at pH 3, at the same frequency observed for liquid water supports our hypothesis. Finally, for what concerns the components C and D, whereas their peak frequencies are practically the same at any experimental condition, some changes are observed for the corresponding integrated areas. In particular, in the “as prepared” film, a strong decrease in the area of the component C is observed in comparison to the powder. Taking in mind that the strongest variation observed along the film preparation involved the A component, we hypothesize that it could be assigned to primary amine groups not involved in protonation. Finally, even if the recorded observations are not sufficient to give a clear indication, we can assign the D component to the secondary amine group by exclusion. Given these findings, we proceeded, following the same criteria, to analyze the spectra for the chitosan/clay nanocomposites. In Fig. 8 the ATR spectrum of the “as prepared” chitosan film is (a) (b) (c) (d) Transmittance (a.u.) a) 1560 Transmittance (a.u.) -1 Peak frequency (cm ) C. Branca et al. / Polymer 99 (2016) 614e622 1548 1555 1500 1600 (b) (c) (d) 1700 -1 Wavenumber (cm ) 500 1000 1500 2000 2500 3000 3500 4000 -1 Wavenumber (cm ) Fig. 8. ATR-FTIR spectra of MMT (a), CSM5 (b), CSM2.5 (c) and “as prepared” (d) film. An enlargement of the amide region for the chitosan film and its nanocomposites is also reported. C. Branca et al. / Polymer 99 (2016) 614e622 compared to the spectra of the polymer/clay composites at different clay content prepared under the same conditions. The spectrum of MMT is also reported. This latter is characterized by typical bands responsible for the HeOeH stretching, 3426 cm1, and the bending mode, 1636 cm1, of the adsorbed water. The peak at 3626 cm1 is typical for AleAleOH stretching vibrations whereas the sharp peak at 1038 cm1 is assigned to SieO stretching vibrations. Finally, the peak at 795 cm1 corresponds to quartz symmetrical stretching [13,17,48,49]. Because a relatively tiny amount of MMT was added, the ATRFTIR spectra of the chitosan/MMT composites present all the vibrational peaks typical of chitosan. In the range between 950 and 1200 cm1 the characteristic bands of chitosan and MMT overlap, giving rise to more intense bands for both the nanocomposite samples. Major differences in peak position and intensity were detected in the spectral regions between 1200e1750 and 3000e3700 cm1, and for this reason they were analyzed in more details. As shown in the inset of Fig. 8, for the film containing 5% MMT, the frequency of the deformation vibration (dNH3), located at 1555 cm1 in the “as prepared film”, shifts towards a lower frequency, 1548 cm1. According to previous studies [13,15,30,48], this shift is a signature of the intercalation of the biopolymer into the silicate galleries, whose extent depends on the clay content. The intercalation is favored, especially under acidic conditions, by the electrostatic interactions between the negative charges on the clay surface and the positive charges of chitosan. In order to verify this hypothesis, the chitosan-clay films were analyzed by XRD and the results are shown in Fig. 9. The XRD patterns of MMT and of the “as prepared” chitosan film were also recorded as reference. MMT presents a diffraction peak at 2q z 8.8 , corresponding to a d001 spacing of about 10 Å. In agreement with previous investigations [12,17], the basal plane of MMT disappears in the XRD pattern of the nanocomposite film at the lowest clay content (2.5%), indicating the presence of a disordered structure. At a higher clay content, 5%, a broaden shoulder was detected in the 2q range between 3.3 and 5.6 . This was much lower than that of pristine MMT, suggesting that, consistently with the infrared findings, intercalation occurred together with some exfoliation [12,17,29]. It's reasonable expecting that the different nanostructures modify the network of electrostatic interactions between chitosan and MMT. Consequently, some changes on both the OH and NH stretching modes are likely to happen. For this reason, following the same criteria used for the chitosan films, a deconvolution of the absorption spectra for the nanocomposite films was performed between 2800 and 3700 cm1, see Fig. 10. The peak frequencies and the corresponding areas resulting from deconvolution are presented in Table 3. Intensity (a.u.) a) b) Intercalated nanocomposites c) d) 3 4 5 6 7 2θ (degree) 8 9 Exfoliated nanocomposites Fig. 9. XRD patterns of (a) MMT, (b) CSM5, (c) CSM2.5, and (d) chitosan film; a schematic drawing of the different nanostructures formed is also reported. a) Absorbance (a.u.) 620 b) 2800 3200 3600 -1 Wavenumber (cm ) Fig. 10. Gaussian deconvolution of the ATR-FTIR spectra for the CSM2.5 (plot a) and the CSM5 (plot b) nanocomposite film. Table 3 List of peak frequencies and integrated areas of bands in the region 2800e3700 cm1 for the “as prepared” chitosan film, and the chitosan/clay films with 2.5% and 5% of MMT. A B C D E F As prepared CS film CSM2.5 Peak (cm1) Area (%) Peak (cm1) Area (%) Peak (cm1) Area (%) 3075 3225 3292 3355 3424 3564 26.4 25.9 6.3 4.8 31.2 5.4 3074 3223 3292 3354 3424 3562 27.1 27.2 5.1 5.0 30.1 5.5 3070 3228 3292 3352 3430 3568 29.7 25.8 6.6 6.1 28.8 3.0 CSM5 As for the chitosan, the deconvolution, performed leaving all the fitting parameters free, evidenced the presence of six Gaussian components that we labeled using the same nomenclature as before. For what concerns the peak frequencies, it can be observed that whereas the components B, E and F move to higher frequencies, the component A shifts to a lower one; moreover, also for the nanocomposites, the components C and D result unchanged with respect to the “as prepared” chitosan film. Consistently with the observed frequency shifts, the incorporation of the clay determined a decrease of the integrated area for the components B, E and F and in an increase for the A component. Taking into mind that the component A was attributed to protonated amine groups, the observed downshift is fully consistent with the formation of hydrogen bonds between the NHþ 3 groups of chitosan and the negatively charged sites on the clay surface. Since, as above reported, the swelling properties of the chitosan film are ruled by to the presence and the mobility of protonated amine groups, the involvement of these groups in hydrogen bonding with the clay implies a reduction, in comparison to neat chitosan, in the water sorption capability, as confirmed by our observations, see Fig. 2. This behavior is in agreement with that reported by Abdollahi et al. [17] according to which the nanocomposites exhibit a lower swelling capability. Moreover, they observed a minimum in the water sorption for the nanocomposite containing 3% MMT; also this result agrees very well with our experimental observations, see Fig. 2. This result is quite surprising since, if the reduced water sorption were just up to the reduced number of protonated amine groups, we should expect a higher swelling at the lowest clay C. Branca et al. / Polymer 99 (2016) 614e622 concentration, that is when the number of protonated amine groups not involved in hydrogen bonding is higher. This contradiction can be solved if we take into account the different network structures formed depending on the clay content. When intercalation occurs, the chitosan chains are forced to stretch along the clay galleries; this arrangement increases the surface of interaction favoring the electrostatic interactions between the NHþ 3 groups and the clay platelet. At the same time, the elongation of the chain tends to weaken and, eventually, to brake the bonds between the OH groups of chitosan. This hypothesis is consistent with the FTIR results showing a blueshift, and a concomitant area decrease, for the components B, and E both assigned to the hydroxyl groups of chitosan. These groups are thus available to bind with the water molecules entering into the clay galleries. Contrary, in presence of a complete exfoliation or homogeneous dispersion of the clay platelets, the OH groups of chitosan are likely involved in both intra and intermolecular bonds between adjacent chitosan molecules. In such a configuration, the chains form of a highly crosslinked network for which a reduced swelling is expected. 4. Conclusions We have presented a systematic investigation of the vibrational spectra of chitosan under different forms and solvent conditions. By applying a deconvolution analysis of the ATR-FTIR spectra in the region 3000e3800 cm1, the OH and NH stretching vibrational modes were differentiate and identified. The assignment was based on the analysis of the changes in peak position and integrated areas of the Gaussian components upon variation of the hydration and pH conditions of the chitosan film. Starting from this assignment, the vibrational spectra of chitosan/montmorillonite nanocomposites at different clay content were analyzed. The clay concentrations were accurately chosen in order to realize, as evidenced by XRD data, exfoliated and intercalated nanostructures. The observed changes in the spectral features of the OH and NH stretching components revealed a strong influence of the architecture of the nanocomposites on the network of electrostatic interactions between chitosan and MMT. A direct consequence is that the water sorption capability for the nanocomposites, cannot be exclusively ascribed to the presence and mobility of the protonated amino groups. It was found that at the highest clay content investigated, the intercalation of chitosan inside the clay galleries, reduces the intra and intermolecular hydrogen bonding involving the hydroxyl groups of the chitosan chains; the OH groups are thus available to make hydrogen bonds to water molecules entering inside the gallery. 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