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Research paper Matrix dependent changes in metachromasy of crystal violet in Langmuir-Blodgett films Ashis Shil a , Mitu Saha a , Chandan Debnath b , S.A. Hussain a , D. Bhattacharjee a,a Thin Film and Nanoscience Lab, Department of Physics, Tripura University, Suryamaninagar, Tripura 799022, India b Department of Physics, MBB College, Agartala, West Tripura 799004, India article info Article history: Received 29 July 2016 In final form 8 October 2016 Available online 21 October 2016 Keywords: Crystal Violet (CV) Metachromasy Langmuir-Blodgett (LB) Films Isotherm Spectroscopy abstract This communication reports the effect of building matrices and nano clay platelets on the aggregation pattern of a water soluble cationic fluorescent dye Crystal Violet (CV) in Langmuir-Blodgett (LB) Films. When stearic acid (SA) was used as a building matrix, pressure induced changes in metachromasy was observed in the SA-CV complex LB films with a characteristic J-band formed at the longer wavelength side. On the other hand, clay incorporated hybrid LB films showed high degree of control over H- dimeric band. Isotherm characteristics, Brewster Angle Microscopic (BAM) images, UV–vis absorption and fluorescence characteristic studies were employed to investigate this result. Ó 2016 Elsevier B.V. All rights reserved. 1. Introduction Several dyes show Metachromasy in solid state, in ultrathin films, in the staining of biological tissues and even in solution. Metachromasy is a change in the shape of the absorption spectrum and the color of the dye with concentration or adsorption but with no chemical change in the dye itself [1]. This phenomenon can be seen in concentrated and even in dilute aqueous solutions of crys- tal violet (CV). In dilute aqueous solution of CV, UV–vis absorption spectrum shows intense band with peak at 590 nm and a shoulder at 550 nm [2]. The 590 nm peak is due to the presence of mono- meric sites. With increasing solution concentration, 550 nm shoul- der becomes intense and the 590 nm absorption band reduces to a shoulder. At higher concentration the 550 nm peak is further blue shifted [3]. The change in the spectrum is due to the aggregation of the dye molecules into dimmers and higher order aggregates. For dimeric sites, the absorption peak is at 550 nm. For higher order aggregates it is further blue shifted [4]. CV is soluble in water because it is an ionic compound. The dye ions themselves, how- ever, are made up of large hydrophobic groups, and the charge is delocalized over most of the molecule. Thus, even at relatively low dye concentrations, the ions have a tendency to aggregate to minimize the interaction with water molecules, and the resulting p-electron interactions cause the aggregates to have a different absorption maxima [5]. A similar effect is responsible for Metachromasy of dyes when adsorbed on a preformed oppositely charged Langmuir monolayer at the air-water interface by electro- static interactions [6]. A complex/hybrid Langmuir monolayer is thus formed at the air-water interface which can be transferred onto solid substrates to form mono- and multilayer Langmuir Blod- gett (LB) films [6–10]. Depending on the various film forming parameters and molecular organizations in the LB films various kinds of dye Metachromasy were observed [11]. Red shifted absorption band with respect to the monomer absorption band is generally referred to as J-band formed due to J-type molecular aggregates. H-aggregates result in the blue shifted absorption band with respect to the monomer and it generally leads to the forma- tion of H-dimmer resulting in the quenching of fluorescence inten- sity [12–14]. It reduces the fluorescence efficiency of a biological stainer. On the other hand H-aggregation of CV shows higher opti- cal coefficients for third order nonlinear susceptibility and is used to study non-linear optical phenomena [15]. It may be mentioned in this context that several works reported the incorporation of water soluble ionic dyes into LB films and studied their character- istics. Aggregation behavior of a water soluble cationic dye Nile Blue A (NB) onto the inorganic nano clay sheets Laponite was investigated by LB technique [16]. H-aggregation of water soluble anionic dye merocyanine 540 (MC540) mixed with amphiphilic Octadecylamine (ODA) in LB films fabricated by co-spreading method was also reported [17]. Interaction of water soluble anionic dye Congo Red (CR) and cationic surfactant CTAB in presence of Ag + ions and AgNPs was investigated and found that CR formed stable complex in presence of AgNPs [18]. http://dx.doi.org/10.1016/j.cplett.2016.10.027 0009-2614/Ó 2016 Elsevier B.V. All rights reserved. Corresponding author. E-mail address: [email protected] (D. Bhattacharjee). Chemical Physics Letters 665 (2016) 76–84 Contents lists available at ScienceDirect Chemical Physics Letters journal homepage: www.elsevier.com/locate/cplett

Matrix dependent changes in metachromasy of crystal violet ... · Research paper Matrix dependent changes in metachromasy of crystal violet in Langmuir-Blodgett films Ashis Shila,

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Page 1: Matrix dependent changes in metachromasy of crystal violet ... · Research paper Matrix dependent changes in metachromasy of crystal violet in Langmuir-Blodgett films Ashis Shila,

Chemical Physics Letters 665 (2016) 76–84

Contents lists available at ScienceDirect

Chemical Physics Letters

journal homepage: www.elsevier .com/locate /cplet t

Research paper

Matrix dependent changes in metachromasy of crystal violet inLangmuir-Blodgett films

http://dx.doi.org/10.1016/j.cplett.2016.10.0270009-2614/� 2016 Elsevier B.V. All rights reserved.

⇑ Corresponding author.E-mail address: [email protected] (D. Bhattacharjee).

Ashis Shil a, Mitu Saha a, Chandan Debnath b, S.A. Hussain a, D. Bhattacharjee a,⇑a Thin Film and Nanoscience Lab, Department of Physics, Tripura University, Suryamaninagar, Tripura 799022, IndiabDepartment of Physics, MBB College, Agartala, West Tripura 799004, India

a r t i c l e i n f o a b s t r a c t

Article history:Received 29 July 2016In final form 8 October 2016Available online 21 October 2016

Keywords:Crystal Violet (CV)MetachromasyLangmuir-Blodgett (LB) FilmsIsothermSpectroscopy

This communication reports the effect of building matrices and nano clay platelets on the aggregationpattern of a water soluble cationic fluorescent dye Crystal Violet (CV) in Langmuir-Blodgett (LB) Films.When stearic acid (SA) was used as a building matrix, pressure induced changes in metachromasy wasobserved in the SA-CV complex LB films with a characteristic J-band formed at the longer wavelengthside. On the other hand, clay incorporated hybrid LB films showed high degree of control over H-dimeric band. Isotherm characteristics, Brewster Angle Microscopic (BAM) images, UV–vis absorptionand fluorescence characteristic studies were employed to investigate this result.

� 2016 Elsevier B.V. All rights reserved.

1. Introduction

Several dyes show Metachromasy in solid state, in ultrathinfilms, in the staining of biological tissues and even in solution.Metachromasy is a change in the shape of the absorption spectrumand the color of the dye with concentration or adsorption but withno chemical change in the dye itself [1]. This phenomenon can beseen in concentrated and even in dilute aqueous solutions of crys-tal violet (CV). In dilute aqueous solution of CV, UV–vis absorptionspectrum shows intense band with peak at 590 nm and a shoulderat 550 nm [2]. The 590 nm peak is due to the presence of mono-meric sites. With increasing solution concentration, 550 nm shoul-der becomes intense and the 590 nm absorption band reduces to ashoulder. At higher concentration the 550 nm peak is further blueshifted [3]. The change in the spectrum is due to the aggregation ofthe dye molecules into dimmers and higher order aggregates. Fordimeric sites, the absorption peak is at 550 nm. For higher orderaggregates it is further blue shifted [4]. CV is soluble in waterbecause it is an ionic compound. The dye ions themselves, how-ever, are made up of large hydrophobic groups, and the charge isdelocalized over most of the molecule. Thus, even at relativelylow dye concentrations, the ions have a tendency to aggregate tominimize the interaction with water molecules, and the resultingp-electron interactions cause the aggregates to have a differentabsorption maxima [5]. A similar effect is responsible for

Metachromasy of dyes when adsorbed on a preformed oppositelycharged Langmuir monolayer at the air-water interface by electro-static interactions [6]. A complex/hybrid Langmuir monolayer isthus formed at the air-water interface which can be transferredonto solid substrates to formmono- andmultilayer Langmuir Blod-gett (LB) films [6–10]. Depending on the various film formingparameters and molecular organizations in the LB films variouskinds of dye Metachromasy were observed [11]. Red shiftedabsorption band with respect to the monomer absorption band isgenerally referred to as J-band formed due to J-type molecularaggregates. H-aggregates result in the blue shifted absorption bandwith respect to the monomer and it generally leads to the forma-tion of H-dimmer resulting in the quenching of fluorescence inten-sity [12–14]. It reduces the fluorescence efficiency of a biologicalstainer. On the other hand H-aggregation of CV shows higher opti-cal coefficients for third order nonlinear susceptibility and is usedto study non-linear optical phenomena [15]. It may be mentionedin this context that several works reported the incorporation ofwater soluble ionic dyes into LB films and studied their character-istics. Aggregation behavior of a water soluble cationic dye NileBlue A (NB) onto the inorganic nano clay sheets Laponite wasinvestigated by LB technique [16]. H-aggregation of water solubleanionic dye merocyanine 540 (MC540) mixed with amphiphilicOctadecylamine (ODA) in LB films fabricated by co-spreadingmethod was also reported [17]. Interaction of water soluble anionicdye Congo Red (CR) and cationic surfactant CTAB in presence of Ag+

ions and AgNPs was investigated and found that CR formed stablecomplex in presence of AgNPs [18].

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A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84 77

Crystal Violet (CV, (tris[p-(dimethylamino)phenyl]methyl) hasbeen the subject of interest in various fields of science due to itsmolecular structure, electronic states and the relaxation dynamicsof the electronic states and good optical properties in the solidstate [19–21]. It is also used as a biological stainer [21], dermato-logical agent [22] and considered as a drug for use in photody-namic therapy [23–25]. Being cationic, it can interact withnegatively charged cell membrane surfaces and can enter into cellsand concentrate in cytoplasm [26]. CV is carcinogenic and catego-rized as a recalcitrant molecule [27,28]. It is also widely used totest Gram-positive and Gram-negative bacteria [29,30]. CV is alsoused as a fluorescent tracer. It has a large molecular hyperpolariz-ability [31]. This important optical property has made this dye aninteresting element for NLO – experiments [19,31] and near-fieldspectroscopy [32].

Smectite clay such as Laponite (inorganic sheet-like naturalmineral) has its potential applications over the few years, due toits high aspect ratio, unique optical, thermal, mechanical proper-ties, high Cationic Exchange Capacity (CEC), special swelling prop-erties, large surface areas, surface reactivities, adsorptiveproperties, colloidal size, permanent structural charge, high viscos-ity and transparency in solution, etc. [33,34]. They are generallyused as spacer/inert modifiers and film-forming agents with amaz-ing properties. Recently organo-clay hybrid films have varioustechnological applications due to their unique semiconducting,conducting, non-linear, dielectric properties [35,36].

In the present communication detailed investigations havebeen carried out to investigate the controlling of aggregates inthe ultra-thin films of CV fabricated by Langmuir-Blodgett tech-nique. Effect of nano clay platelets and ionic nature of the surfac-tants in controlling the aggregation of CV in the LB films havealso been investigated.

2. Experimental section

2.1. Chemicals

Crystal Violet (CV), Stearic Acid (SA) and Octadecylamine (ODA)were purchased from Aldrich Chemical Co. and used as received.Solvent chloroform (SLR, India) was of spectroscopic grade andits purity was checked by fluorescence spectroscopy before use.The clay mineral Laponite used in this study was obtained fromthe source clays repository of the clay minerals society.

2.2. Instruments

Surface pressure vs. area per molecule (p-A) isotherm measure-ments of complex/hybrid Langmuir monolayers and preparation ofmono- and multilayered LB Films were done by a commerciallyavailable Langmuir-Blodgett film deposition instrument (Apex-2006C). The Brewster Angle Microscope (BAM) images of complex/hybrid films were taken by a commercially available in-situ Brew-ster Angle Microscope (Accurion, nanofilm_EP4) attached to a KSVLangmuir-Blodgett instrument. Ultra-pure Milli-Q (18.2 MO-cm)water was used for the aqueous subphase of the Langmuir trough,for the preparation of aqueous clay dispersion also used in the Lang-muir trough and for the preparation of aqueous solution of CV. Aqu-eous clay dispersion was prepared at various clay concentrationsranging from 10 to 80 PPM. Aqueous clay dispersion was stirredfor 24 h and then sonicated for 30 min prior to use. The temperaturewasmaintainedat 24 �C throughout the experiment.UV–vis absorp-tion and fluorescence spectra were recorded by UV–vis absorptionspectrophotometer (Lambda 25, Perkin Elmer) and Fluorescencespectrophotometer (LS-55, Perkin-Elmer) respectively. The quartzand silicon substrates used for LB filmpreparationswere thoroughly

cleaned prior to use. The substrates were first of all cleaned withsoap solution for removal of grease/dirt. Then the slideswere treatedwith chromic acid for 30 min and washed with de-ionized water.Further they were rinsed by acetone followed by chloroform andthen stored in an oven for drying. Atomic Force Microscopic (AFM)image of ODA-Clay-CV hybrid LB monolayer was taken in air witha commercial AFM system (Innova AFM system, Bruker AXS PteLtd.). AFM image was obtained in intermittent-contact (‘taping’)mode. Typical scan area was 2 � 2 lm2. Monolayer on Si wafer sub-strate was used for the AFM measurement. Experiment was per-formed at room temperature (24 �C). Relative humidity was keptunder 60% (non-condensing). The pH of the subphasewas kept fixedat 6.5 in equilibrium with atmospheric carbon dioxide throughoutthe experiments.

2.3. Methods

For surface pressure vs. area per molecule (p-A) isotherm stud-ies and for the recording of BAM images, first of all stock solutionsof SA (0.5 mg/ml) and ODA (1 mg/ml) were prepared using Spec-troscopic grade chloroform. Stock solution of CV was prepared bydissolving it into ultra-pure Milli-Q water (10�4 M). For the studiesof p-A isotherms and LB films preparations, the total volume of thesubphase was kept fixed at 400 ml in all the cases.

To record the p-A isotherm of pure SA monolayer at the air-water interface, the subphase of the Langmuir trough was filledup with Milli-Q water and then 60 ll of chloroform solution ofSA was spread on the aqueous subphase of the Langmuir troughby using a micro-syringe. After waiting for sufficient time to evap-orate the solvent, the barrier of the Langmuir trough was com-pressed slowly to study the isotherm characteristics.

For the p-A isotherm studies of SA-CV complex monolayer, firstof all SA-CV complex Langmuir monolayer was prepared at the air-water interface of the Langmuir trough. For this purpose 2000 ll ofaqueous solution of CV (10�4 M) was dissolved in the aqueous sub-phase of the Langmuir trough and then 60 ll of chloroform solu-tion of SA was spread on the aqueous subphase. Being cationicCVmolecules interacted electrostatically with the anionic SA mole-cules and formed SA-CV complex Langmuir monolayer at the air-water interface. After waiting for sufficient time (1 h) to completethe reaction, the monolayer was compressed slowly to obtain p-Aisotherm. The complex monolayer at the air water interface wasalso transferred onto solid substrates at different surface pressures(10, 15, 18, 20 and 25 mN/m) to form monolayer LB films. Liftingspeed was kept at 5 mm/min.

To incorporate anionic nano clay platelets in the LB films, first ofall aqueous clay dispersionswere prepared at various PPM clay con-centration (namely 10–80 PPM). The aqueous clay dispersion wasstirred overnight followed by 30 min sonication prior to use inthe Langmuir trough. Preformed Langmuir monolayer of cationicODA molecules was prepared for the adsorption of anionic nanoclay platelets onto the ODAmonolayer by electrostatic interactions.Thus ODA-Clay hybrid Langmuir monolayer was formed at the air-water interface. For the preparation of ODA-Clay-CV hybrid mono-layer, 2000 ll of aqueous solution of CV (10�4 M) was mixed withthe aqueous clay dispersion (various clay PPM concentrationsnamely 80–10 PPM) and sonicated prior to use in the Langmuirtrough. Being cationic CV molecules interacted electrostaticallywith anionic nano clay platelets and got adsorbed onto the nanoclay platelets. Thus Clay-CV hybrid molecules were formed in theaqueous dispersion of the Langmuir trough. When cationic ODAmolecules were spread at the air-water interface of the Langmuirtrough, then CV tagged nano clay platelets were further adsorbedonto the preformed cationic ODA monolayer and thus ODA-Clay-CV hybrid monolayer was formed at the air-water interface. Afterwaiting for sufficient time (1 h) to complete the reaction, the hybrid

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monolayer was compressed slowly to obtain p-A isotherm. Thehybrid monolayer was also transferred onto solid substrates at adesired surface pressure to form mono- and multilayered LB films.

3. Results and discussion

3.1. Molecular structure and area of the CV

Inset of Fig. 1(a) shows the molecular structure of CV. One catio-nic charge is associated with the N+ ions. In the solution as well asin the solid phase CV form planer structure and the molecular areaof CV was found to be 1.2 nm2 [37]. SA-CV complex molecule wasformed when anionic head group of SA molecule was attachedelectrostatically to the N+ cation of the CV molecule. This is alsoshown in the inset of Fig. 1(a). At the air-water interface of theLangmuir trough when SA-CV complex monolayer was formed, ifCV molecules lying flat at the air-water interface of the Langmuirtrough, area per molecule would have been of the order of1.2 nm2. Any deviation of this area per molecule indicates the tiltedorientation of the CV molecules in the complex monolayer at theair-water interface. The area per molecule of any monolayer canbe calculated from the surface pressure vs. area per molecules(p-A) isotherm characteristics curve. It was discussed in Sec-tion 3.2, that the area per molecule at any surface pressureremained far below 1.2 nm2, which is the area per molecule ofCV in lying flat conformation. It strongly indicated the tilted orien-tation and even vertical orientation of CV molecules at higher sur-face pressure.

3.2. p-A isotherm studies of SA and SA-CV complex monolayer at theair-water interface

Fig. 1(a) shows the p-A isotherm characteristic studies of theLangmuir monolayer of pure SA (graph-I) and SA-CV complex

Fig. 1. [a] p-A isotherms of (i) SA monolayer, (ii) SA-CV complex monolayer

(graph-II). The p-A isotherm of pure SA monolayer showed a riseof surface pressure with decreasing area per molecule and hasthe characteristic kink at 25 mN/m known as lateral transitionpressure for long-chain fatty acids. The lift-off area of SA was foundto be 0.276 nm2 determined by the method described by Ras et al.[38]. The molecular areas of 0.23 nm2 and 0.21 nm2 at surface pres-sures 15 mN/m and 25 mN/m of SA isotherm are in good agree-ment with the reported results [39]. The p-A isotherm ofcomplex SA-CV monolayer showed a larger lift off area(0.37 nm2) that of pure SA monolayer, which was the clear evi-dence of the formation of SA-CV complex monolayer at the air-water interface. At about 18 mN/m surface pressure, there was aphase transition which was due to the orientation of the complexmolecules at the air-water interface. This orientation might leadto different types of molecular organizations in the ultrathin films.At 15 mN/m surface pressure the area per molecule of the complexmonolayer became 0.25 nm2 which was greater than the area permolecule of pure SA monolayer (0.23 nm2) at the surface pressure,but far below the area per molecule of CV when it was lying flat atthe air-water interface (1.2 nm2). At lower surface pressurealthough the lift of area (per molecule) of the complex monolayerwas to some extent larger (0.37 nm2) but still it was much smallerthan the 1.2 nm2 area per molecule of CV in lying flat conforma-tion. It indicated that in the complex monolayer, CV moleculesdid not lying flat at the air-water interface rather it formed tiltedorientation. At 25 mN/m surface pressure, the area per moleculeof the complex monolayer was 0.22 nm2 which was almost equalto the area per molecule of pure SA monolayer. It indicated almostvertical orientation of the CV molecules in the complex monolayer.When this monolayer was transferred onto solid substrates at dif-ferent surface pressures to form LB monolayer, CV molecules werestacked keeping their vertical orientation and tilted orientationrespectively. The organization of CV molecules in the LB monolayerlifted at lower and higher surface pressures are schematicallyshown in Section 3.4.

; [b] C-p graphs of pure SA monolayer and SA-CV complex monolayer.

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A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84 79

3.3. Compressibility studies of complex monolayer at the air-waterinterface

The compressibility can be extracted from the p-A isotherms ofthe Langmuir monolayer at the air-water interface. It is often usedto characterize the nature of a monolayer’s stable phases and hasbeen correlated with particular phase behavior. Compressibility(C) is calculated using the following standard thermodynamic rela-tion in two dimensions C = �(1/A)(dA/dp), where A is the area permolecule at the indicated surface pressure ‘p’ [40,41]. Differentphases of Langmuir monolayer are reflected as peaks in the com-pressibility vs. surface pressure (C–p) curve. The presence of a peakin the curve represents the inherent phase transitions involved inthe system. Fig. 1(b) showed the C-p curve of pure SA monolayerand SA-CV complex monolayer at the air-water interface and cal-culated from the data of compression isotherms. At the lower sur-face pressure region of 0–15 mN/m, both the curves showedcompressible in nature but complex monolayer showedmore com-pressible than the pure SA monolayer. In the complex monolayer asharp peak in the 18–22 mN/m surface pressure region indicated aphase transition which was absent in pure SA monolayer. This wasalso confirmed from isotherm characteristic studies. In SA mono-layer a small peak in the C-p curve at 25 mN/m surface pressureindicated the starting of the solid phase. In the complex monolayerthe sharp phase transition led to the orientational change and com-pact molecular packing. The change in the photophysical behaviorin the light of this phase transition has been discussed later in thesection UV–vis absorption spectra.

3.4. Schematic representation of CV molecules in the complex LBmonolayer

When the complex LB monolayer was lifted at higher surfacepressure of 25 mN/m, the stacking of vertically oriented CV mole-cules is shown schematically in Fig. 2 (H-aggregate). In the mono-layer film this types of molecular stacking leads to the formation ofH-aggregates [16]. H-aggregates generally form H- dimeric sites. Itgives high energy H-dimeric band in the UV–vis absorption spec-trum. On the other hand, CV molecules lying in a tilted orientationin the complex LB monolayer when lifted at a lower surface pres-sure Fig. 2 (J-aggregate). Stacking of tilted CV molecules in the LBmonolayer most favorably forms J-aggregate [42]. It leads to thelonger wavelength J-band in the UV–vis absorption spectrum.UV–vis absorption spectra of these films have been discussed inSection 3.6.

Fig. 2. Schematic representation of SA-CV complex LB films lifted a

3.5. In-situ Brewster Angle Microscopic (BAM) images of SA-CVcomplex monolayer at the air-water interface

The phase behavior of the complex monolayer at the air-waterinterface is the most important aspect, which can be investigatedby BAM images [43,44]. With increasing surface pressure, domainsof different sizes and shapes are observed in the Langmuir mono-layer indicating phase transition and formation of micro-domainsat the air-water interface. In this investigation BAM images havebeen used for the direct visualization of micro-domains and mor-phological information of SA-CV complex monolayer formed atthe air-water interface. After spreading chloroform solution of SAon the Langmuir trough containing desired amount of CV aqueoussolution and then compressing the monolayer, BAM images weretaken at different surface pressures namely (a) 15 mN/m, (b)18 mN/m, (c) 20 mN/m and (d) 25 mN/m as shown in Fig. 3. Image(a) shows the presence of large number of small dimensional circu-lar domain at the air-water interface. In some cases few circulardomains were attached to form a chain like structure. At 18 mN/m surface pressure, image (b) shows a large number of linear wormlike structure formed by the linear combination of circulardomains. At 20 mN/m surface pressure, image (c) shows highlyconcentrated large dimensional circular domains. Linear arrays ofthe circular domains are also observed. At higher surface pressureof 25 mN/m, image (d) shows a highly concentrated closed packstructures indicating the attainment of solid phase. From theBAM images it becomes evident that the monolayer film at theair-water interface has gone through a phase transition just above20 mN/m surface pressure. This was also supported by the p-A iso-therms and compressibility studies of the complex monolayer atthe air-water interface. UV–vis absorption studies discussed latershowed clearly the changes in the aggregation pattern before andafter the phase transition.

3.6. UV–vis absorption spectra of SA-CV complex Langmuir-Blodgett(LB) film

UV–vis absorption spectrum of CV in aqueous solution consistsof two absorption bands arising due to p-p⁄ transitions [45]. Alonger wavelength absorption band with intense peak at 590 nmis the monomeric band while the band at 550 nm is assigned asH-dimeric band.

Fig. 4(a) shows the normalized UV–vis absorption spectra of theaqueous solution of CV (10�5 M) and SA-CV complex LB monolayerfilms lifted at different surface pressures namely 10, 15, 18, 20 and

t [a] 20 mN/m surface pressure; [b] 25 mN/m surface pressure.

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Fig. 3. BAM images for SA-CV complex Langmuir monolayer taken at different surface pressures namely (a) 15 mN/m, (b) 18 mN/m, (c) 20 mN/m and (d) 25 mN/m. Scale barrepresents 20 lm.

80 A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84

25 mN/m. These surface pressures have been chosen as theremight have been some orientational/organizational changes ofthe molecules in the LB films at these surface pressures, as wouldbe inferred from the isotherm characteristic studies, compressibil-ity studies, schematic representation and BAM images.

UV–vis absorption spectrum in aqueous solution of CV (10�5 M)shows highly intense monomeric band at 590 nm and weak humpof H- dimeric band at 550 nm. Even at much lower concentrationsof CV (10�7 M) in aqueous solution a small hump of H-dimericband was found at 550 nm (figure not shown). Generally at suchlow concentration dimeric band does not exist. But with increasingsolution concentration this band increased and in solid state of theLB film this band became highly intense and blue shifted. As dis-cussed by several authors [4] the origin of this band is due to theformation of dimer and higher order aggregates. The existence ofthis band even at very low concentration in the aqueous solutionmay be due to the planer structure of the molecule. It favoursthe closer association of several CV molecules even at very lowconcentration in the aqueous solution.

Films lifted at 10 and 15 mN/m surface pressures showed abroad band with two overlapping peaks at around 610 nm and540 nm. At 18 and 20 mN/m surface pressures, the UV–vis absorp-tion spectra showed intense longer wavelength band with peak at610 nm and comparatively low intense band with high energyshoulder at 540 nm. However for the LB film fabricated at25 mN/m surface pressure an intense high energy band at540 nm along with a weak hump at 610 nm was observed. Thesharp changes in the UV–vis absorption spectra of the LB mono-layer film lifted at 20 mN/m surface pressure and 25 mN/m surfacepressure was an indication of pressure induced organizationalchanges of the complex monolayer. As discussed schematically inSection 3.1, in the LB monolayer lifted at higher surface pressure,stacking of CV molecules formed H-dimeric sites. Whereas in theLB monolayer lifted at lower surface pressure, J-aggregationbecame predominant. This thesis has also been confirmed fromp-A isotherm, C-p characteristics studies and BAM images. Thus

intense H-dimeric band was found in the UV–vis absorption spec-trum of complex LB monolayer lifted at 25 mN/m surface pressure.Another interesting point to note is that in the LB films lifted at20 mN/m surface pressure, there was a shifting of about 20 nmin the longer wavelength UV–vis absorption band with respect tothe monomeric band at 590 nm. Gaussian deconvolution of thetwo peaks showed sharp intense longer wavelength band withpeak at 610 nm (Fig. 4b). This is the characteristic feature of theJ-band [41].

Inset of Fig. 4(a) shows the layer effect of SA-CV complex LBfilms lifted at 20 mN/m surface pressure. From the graph it wasobserved that, with increasing layer number, the intensity of highenergy H-dimer band was also increased. It may be that withincreasing layer number, orientational changes of the complexmolecules took place resulting in the favorable condition forincreased H-dimeric sites.

3.7. Effect of nano clay platelets Laponite in controlling the H-dimerformation of CV

3.7.1. Inclusion of nano clay platelets in aqueous solutionAnionic nano clay platelets Laponite has a plate like structure

with a large surface charge density [46]. As a result, cationic CVmolecules were adsorbed on the surface of anionic nano clay plate-lets by electrostatic interactions and formed hybrid molecules [16].Effect of clay on the UV–vis absorption spectra of CV molecules hasbeen investigated both in the aqueous solutions and in the LB films.

Fig. 5 shows the UV–vis absorption spectra of CV in aqueousclay dispersion having clay concentrations varying from 10 to80 PPM along with the pure aqueous solution. As discussed earlier,aqueous solution absorption spectrum consists of intense mono-meric peak at 590 nm along with H-dimeric shoulder at 550 nm.At lower clay concentration of 10 PPM, monomeric peak wasreduced to a weak shoulder and an intense high energy band withpeak at 525 nm was observed. As discussed earlier, this blueshifted band at 525 nm was originated due to higher order aggre-

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Fig. 4. [a] UV–vis absorption spectra of monolayer SA-CV complex LB films lifted at different surface pressures namely 10 mN/m, 15 mN/m, 18 mN/m, 20 mN/m and 25 mN/m. Inset shows UV–vis spectra of different layered LB films lifted at 20 mN/m surface pressure. [b] Deconvolution spectra of UV–vis absorption spectra of monolayer SA-CVcomplex LB films at 20 mN/m surface pressure.

A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84 81

gates [4]. With increasing clay concentration the 525 nm band wasagain red shifted and at higher clay concentration of 80 PPM thisband coincided with the dimeric band at 550 nm. The intensitywas also reduced while the intensity of the monomeric band wasincreased to a considerable amount. It is clearly evident from thisspectral data that at higher clay concentration, due to the presenceof large number of nano clay platelets, CV molecules wereadsorbed onto a large number of clay platelets thus reducing thechances of higher order aggregates. While at lower clay concentra-tion chances of aggregating of large number of CV molecules ontothe few clay platelets increased and thus forming the higher orderaggregates. Also at higher clay concentration, intensity of mono-meric band with peak at 590 nm is also appreciable. It indicatedthe existence of monomeric species of CV molecules.

3.7.2. In-situ Brewster Angle Microscopic images of ODA-Clay-CVhybrid monolayer at the air-water interface

BAM images of the ODA-Clay-CV hybrid Langmuir monolayerwere taken at a surface pressure of 10 mN/m and at differentPPM of clay concentrations in the aqueous subphase. Fig. 6 showsthe BAM images at (1) 10 PPM, (2) 30 PPM, (3) 50 PPM and (4)80 PPM clay concentrations in the aqueous subphase.

Unlike the BAM images of SA-CV complex Langmuir monolayer,in this case, distinct circularly shaped domains were observed. At10 PPM clay concentration the domains were smaller in size. How-ever with increasing clay concentration the domains became largerin size and density of domains were also increased. From the dis-tinct dissimilarities in the BAM images before and after inclusionof clay platelets, it became clearly evident that inclusion of clayplatelets affected the molecular organizations in the Langmuir

monolayer at the air-water interface. Laponite has plate like struc-ture having dimension varying from 25 nm to 30 nm. However thecircular domains as observed in the BAM images have severalmicrometer dimensions. Therefore it became evident that severalODA-Clay-CV hybrid molecules aggregated to form microcrys-talline circular domains. The circular plate like Laponite clay plate-let has clear influence in the formation of circular domains asshown in the BAM images. The nature of the aggregated speciescould not be ascertained from the BAM images however UV–visabsorption and Fluorescence spectroscopic studies discussed inthe next section clearly showed the nature of the aggregatedspecies.

3.7.3. UV–vis absorption spectra of ODA-Clay-CV hybrid Langmuir-Blodgett (LB) film

Fig. 7(a) shows the normalized UV–vis absorption spectra of theODA-Clay-CV hybrid monolayer LB films prepared at different clayconcentrations of 80–10 PPM in the aqueous subphase of the Lang-muir trough. The surface pressure of lifting was kept fixed at10 mN/m.

The UV–vis absorption spectrum of monolayer LB film preparedat 10 PPM clay concentration showed two distinct overlappingbands with peaks at 590 nm and 550 nm. The two bands have beenassigned as monomer and H-dimer. There was no shifting of thepeak positions unlike that in case of SA-CV complex LB films. Withincreasing clay concentrations, dimeric band reduced in intensitywhile intensity of monomeric band increased. At 80 PPM clay con-centration, the monomeric peak at 590 nm became intense and thedimeric band was totally absent. Thus it was clearly observed thatinclusion of clay platelets in the LB film, could control the dimeric

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Fig. 5. UV–vis absorption spectra of aqueous solution of CV at different PPM clayconcentration (from 10 to 80 PPM clay concentration).

82 A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84

band and increased the monomeric species. It might be that athigher clay concentration, CV molecules got adsorbed onto a largenumber of clay platelets and relatively less number of CV

Fig. 6. BAM images of ODA-Clay-CV hybrid Langmuir monolayer taken at different PPMfor all the cases. Scale bar represents 20 lm.

molecules got adsorbed on a single clay platelet and thus reducingthe chances of formation of aggregates of CV molecules on a singleclay platelet. Inset of Fig. 7(a) shows the plot of the ratio of inten-sity of dimeric and monomeric bands vs. Clay concentration (PPM)of monolayer LB films. It shows the presence of a larger number ofdimeric species in the monolayer LB film prepared at lower PPMclay concentration. With increasing PPM clay concentration mono-meric band increased in intensity.

Fig. 7(b) shows the UV–vis absorption spectra of different lay-ered (1–11) layer ODA-Clay-CV LB films prepared at 80 PPM clayconcentration. With increasing layer number dimeric band at550 nm was observed along with the intense monomeric peak at590 nm. It might be that with increasing layer number, stackingand overlapping of CV tagged clay platelets occurred in the LB filmsresulting in the changes in the molecular organizations. Thusdimeric species increased.

3.7.4. Fluorescence spectra of ODA-Clay-CV hybrid LB films lifted atdifferent PPM clay concentrations

In an aqueous solution, CV fluoresces weakly due to rapid rota-tion of its phenyl rings which results a fast relaxation process andprovides a non radiative decay path for the excited singlet state[17]. The fluorescence intensity increases when the dye is presentin rigid media and when it is bound to the polymer like substratesand surfactants [20]. CV in a rigid media gives emission at around620 nm and with increasing concentration of a surfactant, it isslightly shifted to 630 nm. Again the formation of H-dimer of dyemolecules in the ultra-thin films reduces its fluorescence intensitygreatly. So the controlling of H-dimer formation of the dye mole-cules in the ultra-thin film becomes utmost important.

Fig. 8 shows the fluorescence spectra of ODA-Clay-CV hybrid LBfilms lifted at different PPM clay concentrations varying from10 to80 PPM. From the figure it was observed that at 80 PPM clay con-centration, the fluorescence intensity became maximum indicatingthe predominance of monomeric sites in the ODA-Clay-CV hybridLB film. With decreasing PPM clay concentration, the dimeric bandincreased which reduced the fluorescence intensity as observed

clay concentrations (10–80 PPM). The surface pressure remained fixed at 10 mN/m

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Fig. 7. UV–vis absorption spectra of [a] ODA-Clay-CV hybrid monolayer LB films lifted at different PPM clay concentrations (10–80 PPM). Inset shows a plot of the ratio ofintensity of dimeric and monomeric bands vs. clay concentration (PPM). [b] Different layered ODA-Clay-CV hybrid LB films lifted at 80 PPM clay concentration.

Fig. 8. Fluorescence spectra of ODA-Clay-CV hybrid monolayer LB films lifted atdifferent PPM clay concentrations (10–80 PPM).

A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84 83

form the graphs and showed a minimum intensity at 10 PPM clayconcentration.

4. Atomic force microscope

Fig. 9 shows the AFM image of ODA-Clay-CV hybrid monolayerLB film deposited onto smooth silicon substrate. The surface pres-sure was maintained at 10 mN/m. The Laponite nano clay plateletsare clearly visible in the AFM image. The surface coverage is morethan 90%. The dimensions of ODA and CV are beyond the scope ofthe resolution. AFM image gives clear visual evidence of the inclu-sion of nano clay platelets in the hybrid monolayer and thus forma-tion of ODA-Clay-CV hybrid LB film.

5. Conclusion

In conclusion, our results showed the effect of building matricesand nano clay platelets on the aggregation pattern of CV moleculesin the LB films resulting in metachromasy. At particular surfacepressures of SA-CV complex monolayer, CV molecules were orga-nized to form J-aggregates. This was happened at the phase transi-tion surface pressure of the complex monolayer as was observedfrom the p-A isotherm studies. The longer wavelength sharp J-band was found in the UV–vis absorption spectra of the complexfilm. When nano clay platelets were incorporated in the LB film,then at high clay concentration, only monomeric species wereavailable. This was inferred from the existence of intense mono-meric absorption peak at 80 PPM clay concentration in the clayincorporated LB film. At such higher clay concentration, dimericspecies of CV molecules remained absent in the LB film. Itincreased the fluorescence intensity as observed from the fluores-cence spectroscopic studies. Thus clay incorporated LB film of CV

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Fig. 9. Atomic Force Microscopic (AFM) image of ODA-Clay-CV hybrid monolayerLB film lifted at 80 PPM clay concentration.

84 A. Shil et al. / Chemical Physics Letters 665 (2016) 76–84

can be used as an efficient fluorescent tracer and biological fluores-cent stainer.

Acknowledgement

The authors are grateful to DST, Govt. of India for financial sup-port to carry out this research work through FIST DST project Ref.SR/FST/PSI-191/2014. The author SAH is grateful to DST, for finan-cial support to carry out this research work through DST, Govt ofIndia project Ref. No. EMR/2014/000234; dated 17.03.2015. Mr.Chandan Debnath is grateful to UGC-NERO, Govt. of India for finan-cial support through UGC project (Ref. No. F.5-378/2014-15/MRP/NERO/2235). Ms. Mitu Saha is grateful to DST for financial supportto carry out this research work through Women Scientist Project(Ref. No. SR/WOS-A/PM-1034/2014).

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