Effect of Structure and Chemical Activation on the Adsorption Properties of Green Clay Minerals for the Removal of Cationic Dye

In this study, natural clay minerals with green appearance were treated with sulfuric acid. Mass percentage of acid (wt%), temperature (T), contact time (t) and liquid-to-solid mass ratio (R) are used as the prevailing factors that determine the extent of acid-activation. The values of these factors range from 15–50%, 60–90 °C, 1.5–6 h and 4–7, respectively. The study has focused on the structural changes as well as textural characteristics of the clay. Three activated clay samples were prepared under different treatment conditions. The samples were characterized using X-ray powder diffraction (XRD), fourier transform infrared (FTIR), scanning electron microscope (SEM), chemical analysis and N2 adsorption techniques. Characterization of the treated clay minerals exhibited significant structural changes to a greater extent of acid-activation, from being partially crystalline to being amorphous silica. The surface area and total pore volume of clay increased proportionally with the level of acid treatment. The average pore diameter behaved differently. During the strong acid treatment, a large increase in pore volume and the enlargement of the pore size distribution were observed. This suggests that considerable structural changes and partial destruction may have occurred in this condition. The removal of methylene blue, used as cationic dye, from aqueous solution by the batch adsorption technique on three prepared acid-activated clay samples was studied. The Langmuir model was found to agree well with the experimental data.


Introduction
Clays and clay minerals are of significant interest because of their interesting characteristics that make them suitable for industrial applications. They have been accepted as one of the most appropriate low-cost adsorbents and common component in different industrial applications [1][2][3][4][5][6][7]. Among the various types of clays, bentonite is more popular. Its physicochemical and adsorption properties depend on the montmorillonite content, the crystalline structure of the clay minerals that constitute them and the nature of the inter-layer cations [8,9]. In order to eliminate impurities and different exchangeable cations from clay minerals and to prepare a well-defined material for use as catalyst and adsorbent, various activations have been used, most often with inorganic acids [10][11][12][13]. Indeed, the treatment with minerals acids significantly changed their textural characteristics. This can expand their applications to include environmental protection [14,15], catalytic cracking of petroleum [16], catalyst supports in many chemical processes and detergent

Materials
All the required chemicals used in this work were of analytical grade. Sulfuric acid H 2 SO 4 and Methylene blue (MB) were purchased from Sigma-Aldrich chemicals (Saint Louis, MO, USA). The formula of MB is C 16 H 18 N 3 SCl·2H 2 O, the molecule is positively charged and its aromatic moiety is planar.
A MB stock solution of mass concentration 1 g/L was prepared by dissolving 1 g of dye in double distilled water in 1000 mL volumetric flask. Other required solutions with various dye concentrations in the range of 10 mg/L to 120 mg/L, were prepared by serial dilution. The pH of solutions was adjusted using 0.1 M solution of HCl or NaOH. The structural formula of methylene blue is given in Figure 1.

Adsorption Studies
In this section, batch adsorption technique is used. Appropriate clay quantity of 200 mg was added in 250 mL conical flask to solutions of MB of different initial concentrations and stirred by magnetic hot plate stirrer with 10 positions of model MS-H-S10 (Scilogex, Rocky Hill, NJ, USA) at the rate 300 rpm and at temperature 20 • C. The time required to attain equilibrium was predetermined previously based on some experiments of kinetic study and estimated to be 60 min. To ensure that the time chosen was enough to reach equilibrium, all experiments were conducted at 1.5 h. Once the dye solutions had reached equilibrium, the suspensions were separated by centrifugation within 30 min at the rate of 3000 rpm using centrifuge of type 80-2C (Xiangtian, Jiangsu, China), for further analysis of the dye concentrations. The residual concentration of the dyes was determined using a UV-visible spectrophotometer of model UV-1700 (Shimadzu corporation, Kyoto, Japan) at 665 nm. The pH of the solutions for adsorption experiments was set to 7 and controlled using a pH-Meter of type Basic 20 + (Crison instruments, Barcelona, Spain). The temperature of experiments was maintained at 20 • C and its control was performed using a thermostatically controlled incubator.
The amount of MB adsorbed q e (mg/g) was calculated from the difference between the initial and equilibrium MB concentrations and is given by: C e (mg/L) is the concentration of adsorbate at equilibrium; C 0 (mg/L) is the initial concentration of adsorbate; m (g) is the mass of the adsorbent; and V (L) is the volume of the solution.

Preparation and Purification of the Adsorbent
The starting material is clay collected from the deposit of "Djebel Aïdoudi" of "Hamma," located in south Tunisia, at the east of Gabes town. The raw material contained, in addition to the mineral phases, impurities which can be reduced or eliminated completely by applying a purification protocol. After collection and before use for activation, the raw material is purified by sedimentation. This is achieved by suspending the crude lumps in distilled water at mass ratio 1:10 (clay:water). The mixture was stirred very vigorously to ensure efficient mixing and then sieving was carried out three times through a sieve of different mesh size and particles smaller than 43 µm were collected. Then, the suspended particles were recovered after allowing coarser mineral particles to settle. Finally, the water is siphoned off and the clay is dried in an air oven at 60 • C.

Preparation and Analysis of Oriented Aggregates of Clay
Oriented aggregate specimens of clay were carried out using the standard procedure of Brown and Brindley [33] according to the following steps [36]: a few gram of finely ground clay was added to a vessel containing distilled water and then the mixture was stirred and allowed to stand. After a few minutes, the heavy and/or coarse fractions are separated by decanting. Only clay grains that remain suspended in the liquid are removed using a pipette. The liquid was extended on a horizontal glass slide to obtain a well oriented regular deposit, then left to dry in open air. Three oriented clay specimens were prepared; the first one was analyzed in normal state. The normal state of the material refers to the raw material, merely freed from its coarse fraction by sedimentation and keeping the clay fraction in its natural state (without changing the interlayer space by ion exchange). This sample was used as the reference to judge the movements caused by other treatments. The second one is subjected to ethylene glycol vapor in a desiccator for 24 h (glycolated aggregate), this treatment leads to the swelling of smectites. The last one is heated in an oven for one hour at a temperature of 500 • C. This heating can destroy kaolinite and keep chlorite. After this treatment, the minerals of smectite group are dehydrated irreversibly and interlayer space will be blocked to 10 Å.

Acid Activation of Raw Material
Clay mineral was treated with sulfuric acid. According to previous works [12] and preliminary tests, it was shown that the particle size of the solid had no significant effect on the kinetics of the activation or the pore properties of clay particles when the dimensions were equal to or less than 40 µm. Moreover, it was found that the agitation does not have much effect on the kinetics of the acid attack from certain values. Hence, the stirring has been adjusted to the maximum value of a laboratory stirrer in order to ensure the homogenization of the reaction mixture. Consequently, this study was conducted using only four major factors: the strength of acid (wt%), the reaction temperature (T), the reaction time (t) and the liquid to solid mass ratio (R).
Based on preliminary tests and from the literature review [12], samples were prepared according to the following ranges: Temperature (60-90 • C), contact time (1.5-6 h), liquid/solid mass ratio (4-7) and mass percentage of acid (15-50%). It was shown that the selected ranges of these factors, are appropriate to investigate the effect of acid activation on raw material and efficient to make difference in activation degree between the samples. Three activated clay samples were prepared: the first sample (S 1 ) was prepared under low conditions (wt = 15%, T = 60 • C, t = 1.5 h, R = 4), the second sample (S 2 ) was activated at average conditions (wt = 32.5%, T = 75 • C, t = 3.75 h, R = 5.5), while the last sample (S 3 ) was prepared under strong conditions (wt = 50%, T = 90 • C, t = 6 h, R = 7).
A series of treatment steps were used for the acid-treatment of clay. Experiments were carried out with sulfuric acid in a jacketed glass reactor equipped with a thermometer, a reflux condenser and a stirrer. Each sample was prepared according to the following procedure: 100 g of raw clay, with a particle size less than 40 µm, was mixed with an appropriate aqueous solution of H 2 SO 4 . The slurry was stirred at maximum speed by a laboratory agitator of type Kirk 210 (Bicasa, Monza Brianza, Italy). Then, slurry was air-cooled and filtered with a glass fibber. The filter cake was washed with distilled water several times until the wash water was neutral with no trace of sulphate. The pH of the filtrate is monitored by universal pH test strips.
Finally, the clay product was dried in an oven at 70 • C for 48 h until the weight remains constant. The freshly prepared dry sample was crushed into powder by a mortar. Then the activated clay was sieved before use according to U.S. standard sieve designations (Afnor nF-11504). All the activated clay samples (S 1 , S 2 and S 3 ) were prepared with the same described procedure.

Characterization
The mineralogical compositions were determined by the techniques of X-ray powder diffraction (XRD) using Philips Panalytical X' Pert PRO powder diffractometer (Almelo, The Netherlands) equipped with X' Celerator detector and with cobalt K α radiation (λ = 1.789 Å). Tension and current were set to 40 kV and 40 mA respectively. Scans were collected between 3 and 60 • 2θ angular range at steep angle of 0.017 • . Orientated aggregate samples were scanned from 3 • to 35 • 2θ angular range at 1 • /min with a scanning step of 0.01 • /step. The clay fraction was maintained at three different conditions (1 to 3); 1: untreated (natural state), 2: after treatment with ethylene glycol vapors in a desiccator for 24 h at 60 • C, 3: after heating at 500 • C for 1 h. The micromorphological features of the samples before and after activation were studied using a scanning electron microscope (SEM) of type Philips XL30 ESEM (Leuven, Belgium) operating with up to 30 kV acceleration voltage field emission gun. Sample clays fragments were previously coated with a thin layer of gold before proceeding to morphological observations. The Fourier transform infrared spectroscopy (FT-IR) was applied using a Perkin-Elmer 983 G IR-spectrometer (Bridgeport, CT, USA) equipped with IR source, KBr beam splitter and DTGS KBr detector. Prior to analysis, samples were lightly ground using a mortar and pestle and sieved again through the 45 µm sieve. This was done to minimize the scattering, distortion and peak broadening of IR radiation due to larger-sized particles that may have resulted from agglomeration during drying. The spectra were recorded in the spectral range from 4000 to 250 cm −1 . Quantitative chemical analysis of raw material (S 0 ) and acid-activated clays were performed using atomic absorption spectrometer (AAS) of type NOVAA 400 (Analytik Jena AG, Jena, Germany) and X-ray fluorescence (ARL ® 9800 XP spectrometer, Thermo ARL, Ecublens, Switzerland). By X-ray fluorescence, the loss on ignition (LOI) content of dried and powdered clay sample was attributed to the release of water and was measured by calcinations at 975 • C. Then the dried clay samples were mixed with lithium-tetraborate and lithium iodide and the mixture was fused in a Pt crucible and moulded to a glass disk for chemical analysis.N 2 adsorption/desorption isotherms were measured using Quantachrome Autosorb AS1C (Quantachrome Instruments, Boynton Beach, FL, USA) equipment at liquid nitrogen temperature of −196.15 • C. Before adsorption measurements, the samples were degassed in vacuum at 300 • C for more than 3 h to remove any adsorbed contaminants from the surface and pores of the samples. The Brunauer-Emmett-Teller (BET) method was used to determine the surface areas and pore volume of samples and the pore size distribution was calculated using the BJH method based on the nitrogen adsorption or desorption data.

Results and Discussions
After acid-activation, clays underwent chemical analysis and textural characterizations. The expected results obtained by acid-activated clays (S 1 , S 2 , S 3 ) were compared to those found by raw material (S 0 ). For full description of the mineralogical composition of clay materials and to understand the structure changes, it is required first to determine the nature of the various impurities contained in each sample. The reflections of phyllitic phases were then established.

Determination of Non-Clay Minerals
It should be noted that the quantification of non-clay mineralsfound in the clays by XRD alone was difficult, since some components are hardly detectable by X-ray. Thesenon-clay minerals in the raw material were marked by different peaks. An X-ray diffraction pattern of raw clay mineral (S 0 ) is shown in Figure 2. Quartz appeared as major non-clay minerals by the reflection peaks observed at d = 3.34; 2.28; 2.13; 1.819 Å and d = 4.26 Å. Other non-clay minerals are also detected, such as the calcite at 3.858; 3.04; 1.915, 1.878 Å and gypsum at 2.09 Å. It is remarkable that the non-clay minerals were still present even after purification. This is probably due to their fine particle size which makes their complete separation impossible during clay pre-treatment. Figure 3 presents the morphologies of raw material (S 0 ) and the acid-activated clay prepared at strong condition (S 3 ) observed by SEM. In agreement with the results obtained from XRD patterns, very large aggregates appeared on SEM images of the raw material ( Figure 3a) (size up to 400 nm approximately) and well observed deposited on the mineral layers (indicated by an arrow). These minerals of small size, considered as non-clay minerals, are closely associated to clay and not easily eliminated during purification. Also, SEM examination revealed natural clay morphology of very fine-grained aggregates of clay platelets, irregular curved flakes and mats of coalesced flakes. In any case and because of particle coalescence, it is difficult to determine their exact texture. A sharp decrease in particle size caused by acid activation is visible in the modified clay (Figure 3b). It consists mainly of small aggregates of nanoparticles and exhibits a distinct porous structure.

Determination of the Phyllitic Phases by X-ray Diffraction
The XRD patterns of oriented specimens, natural state (air dried), saturated with ethylene glycol and heated at 500 • C of raw clay sample, S 0 , are illustrated in Figure 4.
A non-symmetrical peak at 15.05 Å is observed by X-ray diffraction patterns of (001) reflection for the air-dried sample. This peak is characteristic of divalent cations occupying the interlayer sites. Once the sample is saturated by ethylene glycol, the peak expands to 17.39 Å, indicating the presence of smectite. This phase of expandable layers remain predominant. The asymmetrical form of the latter reflection is characteristic of a partly interstratified phase illite/smectite. It is frequently observed that illite is interstratified with the smectite by small particles included in the smectite [34,35]. It is not ambiguous that the reflections at 7.18 Å and 3.58 Å unaffected by the treatment with ethylene glycol and disappeared following the heat treatment, correspond to the reflection of the phyllitic phase 1:1 kaolinite. As previously mentioned, the examination of oriented clay specimens by X-ray diffraction shows peaks at 3.34 Å and 3.03 Å corresponding to quartz and calcite, respectively. The infrared spectrum (IR) of natural clay (S 0 ) is presented in Figure 5.  The results of IR spectrum ( Figure 5) confirmed the data obtained by X-ray diffraction, that is, smectite was the dominant mineral phase. The two bands between 3500 cm −1 and 3700 cm −1 and near 3430 cm −1 indicate the presence of smectite [35]. The peak at 3620 cm −1 is assigned to stretching vibrations of the OH group of water molecules. The broad band at 3430 cm −1 and the band at 1640 cm −1 belong to the OH stretching and bending vibration of sorbed water molecules present in the clay, respectively. Furthermore, the strong absorption band at 1040 cm −1 and the band at 795 cm

Effect of Acid-Activation
Changes in crystallinity resulting from acid activation of raw material were investigated by the X-ray powder diffraction patterns of some typical samples. Figure 6 presents the XRD patterns together of raw material S 0 and acid-activated clays (S 1 , S 2 , S 3 ). The pattern of raw material is shown here for sake of comparison. It is observed that acid-activation causes a clear decrease in the crystallinity as indicated by decreasing intensity of the smectite peaks. Some of them are gradually deteriorated and completely disappeared. As it can be seen, XRD analysis has shown that clay acid-activation leads to total dissolution of calcite (reflections at 3.858; 3.04; 1.915 and 1.878 Å) and gypsum (reflections at 2.09 Å).
Under strong conditions of H 2 SO 4 , some of the quartz peaks are still present in the activated samples indicating that quartz is more resistant to acid attack than smectite. This result was similar to that found by Komadel and Madejova [13], hence quartz which appeared as the most abundant non-clay mineral in the natural clay (see reflections at d = 3.34; 2.28; 2.13; 1.819 Å and d = 4.26 Å) cannot be completely eliminated from clay by acid-activation. Temuujin et al. [36] have reported similar results for montmorillonite activated by hydrochloric acid. For a greater extent of acid treatment (sample S 3 ), it is observed that layered structure of clay mineral is indicated by the loss of crystallinity and the appearance of amorphous silica remaining from leached smectite phase. These results are in agreement with those obtained by Shinoda et al. [37]; indicating that the acid-activated product of smectite is generally amorphous silica.  X-ray diffraction patterns of oriented activated clay specimens ( Figure 7S 1 -S 3 ) prove a complete disappearance of the interstratified phase illite/smectite for the severity conditions but no effect on the kaolinite phase was observed (reflection at d = 7.18 Å and d = 3.58 Å).
From these results, it can be concluded that acid treatment mainly affected the smectite phase and led to a partial decrystallization of the clay structure.
The IR spectra presented in Figure 8 showed that the acid-activation led to a partial dissolution of the octahedral sheets especially with the sample S 3 prepared at high conditions of acid treatment. This is confirmed by the decrease in intensity of the band at 914 cm −1 corresponding to −OH bending vibration (AlAlOH), bands at 530 cm −1 assigned to (Si-O-Al), 1030 cm −1 attributed to (Si-O) and band at 3430 cm −1 related to adsorbed H 2 O.The broadening of the IR bands between 1100 and 900 cm −1 is indicative of the formation of amorphous opal.
In addition, a significant decrease or almost disappearance of the band at 3620 cm −1 was observed, this is due to the important leaching of cations after the acid activation. The comparison between raw material and acid-activated clay IR spectra showed that for more severe conditions (S 3 ), acid-activation destroys the smectite mineral phase as proved by the disappearance of the bands located between 3500 cm −1 and 3700 cm −1 [35]. The complete disappearance of bands at 1430 cm −1 and 872 cm −1 pointed out to the dissolution of calcite CaCO 3 and dolomite CaMg(CO 3 ) for the three samples (S 1 , S 2 , S 3 ) as previously reported by Khalil et al. [38]. Chemical analysis was performed on both raw material (S 0 ) and acidified clays (S 1 , S 2 and S 3 ). The results are illustrated in Table 1. The chemical analysis of raw clay (S 0 ) proved the presence of silica, alumina, iron and calcium as major constituents, along with traces of sodium, potassium, phosphate and titanium oxides. The higher mass percentage of silica and alumina reveals that clay mineral is an alumino-silicate matter.
The N 2 adsorption/desorption isotherms of raw material and activated clays presented in Figure 9 showed that isotherms are reversible for lower equilibrium pressure but at higher relative pressure, they exhibited a hysteresis loop of H 3 type [39]. Such hysteresis loops exist in the slit-shaped pores or in the ink-bottle pores (pores with narrow necks and wide bodies). The textural properties of raw clay (S 0 ) and acid-activated clays (S 1 , S 2 , S 3 ) are presented in Table 2. Table 2. Textural properties of raw material (S 0 ) and acid-activated clay samples (S 1 , S 2 , S 3 ). It can be noted that surface area, total pore volume and average pore diameter were changed as the severity of acid treatment was increased. Data presented in Table 2 shows that surface area depends on acid attack but the relation between surface area and acid treatment is non-linear. Taylor et al. have reported that surface area increases with acid concentration [25]. As it can be seen from Table 2, acid activation improves the volume of pores. The pore volume was only 0.1374 cm 3 /g for natural clay (S 0 ) but after acid treatment it becomes much higher and reaches 0.4558 cm 3 /g for more severe treatment (sample S 3 ). Assuming that the pores are cylindrical, the mean pore diameter was calculated from the formula d = 4V p /S p . where, V P is the pore volume and S p is the specific surface area of the pores. The average pore diameter for starting material (S 0 ) is 79.56 Å. It decreases for low acid treatment and average condition and then increases at higher conditions for sample S 3 , to reach the value of 98.9 Å. This can be explained by the fact that acid-activated samples had a greater increase in percentage of pore volume of micro pores than meso pores. As a consequence the lower values of the average pore diameter for samples S 1 and S 2 were obtained compared to that of natural clay. However, the strong acid treatment that produced S 3 , caused large increase of pore volume in the range of micro pore and meso pore diameter and consequently an increase in average pore diameter. This suggests a considerable structural changes and decomposition occurred in this sample. A similar result was observed by Jovanovic and Janackovic [40].

Samples Total
The change in mean pore diameter with the acid treatment is also confirmed by the mesopore size distribution curve calculated by BJH equation [41]. The pore size distribution for both raw material and acid-activated clays (S 1 , S 2 and S 3 ) is presented in Figure 10. From pore size analysis, it was found that the most frequent pore size of the raw material (S 0 ) is 3.7 nm, the same result is found for samples S 1 and S 2 . However, in higher conditions, the activated clay mineral (S 3 ) has mesopores with the most frequent size of 6 nm. The increase of peak amplitude and width of the sample S 3 confirm that the pore volume increases with acid-activation. The large increase in pore volume and the enlargement of the pore size distribution, observed during the strong acid treatment, suggest that significant structural changes and partial destruction may occur in this sample. Similar tendency was reported by Tatjana [9]. These changes in pore structure may result from the removal of exchangeable cations and impurities from the clay lattice following the H 2 SO 4 attack.

Adsorption Equilibrium Studies of Methylene Blue (MB)
In order to evaluate the equilibrium characteristics of adsorption, three models were used to analyze the adsorption data; Langmuir; Freundlich and Frumkin models. The non-linearized forms of Langmuir, Freundlich and Frumkin models can be described by Equations (1)-(3), respectively.
where K L (L/mg) is the Langmuir adsorption constant related to the energy of adsorption, q max and q e (mg/g) are the maximum and equilibrium adsorption capacity, respectively. K f and n are the Freundlich constants corresponding to adsorption capacity and intensity, respectively. For Frumkin model, the constant K Fr is related to equilibrium adsorption and "a" is the interaction parameter. A positive value of "a" corresponds to repulsive interactions among adsorbed molecules, whereas a negative value means attraction between the adsorbed molecules. When a = 0 the adsorbed molecules do not interact each other and the Frumkin isotherm reduces to Langmuir isotherm. The adsorbed quantity of MB dye at the equilibrium (q e ), versus residual concentration (C e ) is presented in Figure 11. The adsorption isotherms exhibited the classical type-I behaviors of adsorbents. The Langmuir model provided the best fit to the experimental data in all range of concentrations ( Figure 11). The Feundlich and Frumkin isotherms failed to correlate the results and showed large deviation (not presented). The linearization of Feundlich model (ln q e vs. ln C e ) shows a correlation factor (R 2 ) of 0.87, 0.89, 0.84 and 0.97 for sample isotherms S 0 , S 1 , S 2 and S 3 , respectively. However the plot of equation ln 1 C e versus θ for Frumkin isotherm shows linear relationship with correlation factor, R 2 which did not reach 0.8 in all sample isotherms; S 0 , S 1 , S 2 and S 3 (θ = q e q max represent the degree of surface coverage by the adsorbent).
The adsorption data were compared with the adsorption isotherm model of Langmuir and the parameters were estimated with regression by minimizing the sum of squared residuals. The fitting function δq to be minimized is established in the following equation: q exp and q cal are the experimental and the calculated adsorbed quantities at concentration C e , respectively. δq is an objective function and has a relative value that depends on the fitting model and the experimental data. The deviations between the fitting model and the experimental data were determined by Equation (4), N is the number of experimental points.
For Langmuir model, the overall mean deviation calculated by Equation (4) was <2%. The results of this analysis are illustrated in Table 3. Much research has reported that MB adsorption on montmorillonite, phosphorous rock and palygorskite correlate well with the Langmuir isotherm and provided a good fit with the experimental data than other isotherms [42][43][44][45]. As expected, the result suggests that the MB adsorption process by clay minerals was a single layer adsorption and that the maximum monolayer adsorption capacities were found to be 241.96, 198.36, 168.59 and 93.42 mg/g, for S 0 , S 1 , S 2 and S 3 , respectively. It is observed that the maximum quantity of MB adsorbed on raw material (S 0 ) was reduced by about 60% for sample activated by strong conditions (S 3 ).
The uptake of methylene blue by clays is strongly related to cationic exchange. As reported by Li et al. [46] a complete balance between MB adsorbed and desorbed exchanged cations is needed to account for the mechanism of cationic exchange. Therefore the uptake of MB is accompanied by dual mechanism of ion exchange as well as adsorption. Overall, the quantities of desorbed exchangeable cations are linearly proportional to those of adsorbed MB [45]. Moreover, the decrease in adsorption ability of MB for activated samples (S 1 , S 2 and S 3 ) could be a consequence of the collapse of the clay lattice to some extent of acid activation. A similar result was found by Zhansheng et al. [18]; when more concentrated acids were used, the crystallinity of the clay minerals deteriorated. The decrease in MB uptake could also be attributed to the electrostatic repulsion between the positively charged surface of acid activated clays and the positively charged dye molecule in the acidic medium, in addition to the competitive adsorption between the H + ions and dye cations to reach the surface.

Conclusions
This paper deals with the acid activation of clay minerals. It is concluded that a deep interlayer modification occurs even at low percentage of H 2 SO 4 . Spectroscopy analysis by infra-red (IR), X-ray diffraction (XRD) and chemical analysis have shown that chemical structure of clay changes from a partially crystallized state to amorphous silica state at a great extent of acid-activation. This result was confirmed by the disappearance of the interstratified phase illite/smectite, which leads almost to a total destruction of natural clay structure. During acid-activation, a part of octahedral cations (magnesium, iron, aluminum) was dissolved, creating new acid sites and the interlayer exchangeable cations are replaced by protons. The content of three oxides Al 2 O 3 , Fe 2 O 3 and MgO of the raw material decreased from 14.27; 6.07; 1.46 to 9.4%; 1.89%; 0.43% for severe acid-treatment (S 3 ), respectively. Acid attack process mainly affected the smectite phase of clay and caused a broad pore distribution of material, created mesopores and increased external surface area of clay. Acid-activation of clay minerals reduces the adsorption capacity of methylene blue used as cationic dye; this is attributed to the competition between the H + ions and dye cations to reach the surface. Also, this clear decrease could be a consequence of the partial collapse of the clay lattice to some extent of acid activation.