Removal of Cadmium ( II ) and Lead ( II ) Ions from Aqueous Phase on Sodic Bentonite

This paper describes the adsorption of Cd and Pb ions using sodic bentonite clay type Fluidgel modified. The Fluidgel before and after chemical modification and thermal activation was characterized by different techniques including X-ray diffraction, thermal analysis, Fourier transform infrared, surface area, helium pycnometry, cation exchange capacity and scanning electron microscopy. Pseudo-first order, pseudo-second order and intra-particle diffusion models were used to analyze the kinetic curves. Equilibrium data were analyzed using Langmuir and Freundlich models. The thermodynamic study indicated that lead adsorption process is endothermic and interactions between clays and solutions of lead occurred spontaneously, while cadmium adsorption revealed an exothermic and spontaneous nature. The maximum removal efficiencies were 97.62% for Cd(II) using Fluidgel modified chemically and 91.08% for lead by Fluidgel modified chemical and thermally.


Introduction
The increment of human wastes mainly caused by industries, due to the constant discharge of pollutants, contributes to declining water quality.Metal species from industrial waste are the most problematic pollutants that affect the biological function of many organisms, reducing the self-purification capacity of water, interfering with the metabolic cycle and causing an increase in the concentration of metals along the food chain.
Heavy metals are a great concern in the environmental area and also in the area of public health.Cadmium is bio-persistent and once absorbed, it remains resident for long time in the kidneys and liver, causing severe damage to these organs.Lead is one of the most dangerous pollutants; even at low concentrations is extremely toxic, causing brain damage in children 1 .
Traditional processes have been used for treating effluents that contain heavy metals, they include: ion exchange 2 , reverse osmosis 3 , chemical coagulation and precipitation 4 , ultrafiltration 5 , and adsorption 6 .The latter is one of the most effective and economical techniques used to remove heavy metals 7 .Different adsorbents have been employed in the process of adsorption: activated charcoal 8 , kaolinite 9 , natural and synthetic zeolites 10 , rice husks 11 , clays 12 , among others.Clays have properties such as high cation exchange capacity, they are easily available and low cost adsorbents, which can be recycled and reused for subsequent cycles.Bentonites are highly efficient in adsorption of heavy metals 13 .
The atomic structure of bentonite clay is composed of montmorillonite, which is a 2:1 type aluminosilicate.The inner layer is composed by an octahedral sheet located between two tetrahedral sheets.The octahedral sheet is composed of oxygen atoms, which are present in a compact form and aluminum, iron and magnesium atoms arranged.The second structural unit is the layer of tetrahedral silica in which the silicon atom is equidistant from four oxygen atoms 14 .Substitutions inside the lattice structure of trivalent aluminium for quadrivalent silicon in the tetrahedral sheet and of ions of lower valence, particularly magnesium, for trivalent aluminium in the octahedral sheet are responsible for the appearance of an electric charge, which is usually negative on the clay surfaces.The negative charges on the surface of the crystals attract cations and this process is known as ion exchange and confers important properties to clays in industrial applications 15 .
Several studies have been developed using bentonite clay as adsorbent of heavy metals: Almeida et al. 16 evaluated the removal of copper using bentonite clay, achieving around 81% of efficiency using raw clays and 42% by calcined bentonite clays.Bertagnolli et al. 17 used Brazilian bentonite clay for adsorption of copper in porous beds, obtaining 50% of the removal percentage.Karapinar and Bonatb 18 studied the adsorption process of copper and cadmium, the results showed that the maximum removal efficiencies for Cu 2+ and Cd 2+ onto natural bentonite were 84.49 and 87.02%, respectively and Inglezakisa 19 reached 100% of efficiency in the removal of Pb(II) form aqueous solutions using clinoptilolite and bentonite as adsorvents.
The reserves of smectite clays such as Fluidgel clay in the city of Boa Vista -PB (Brazil) represent a major national source of clays that are used for perforating fluid.In this context, the aim of this research was to evaluate an additional use of this clay such as alternative adsorbent for removing metal ions in aqueous solution.
The suitable design of adsorption processes determines the efficiency of the treatment techniques.Batch experiments are commonly used in laboratory to evaluate the treatment of small volumes of effluents, providing preliminaries information based on the kinetics and the thermodynamics studies, which are helpful for selecting optimum operating conditions for the full-scale batch and fixed bed process.Previous researchers have reported the kinetics and thermodynamics studies of the adsorption of Cd 2+ and Pb 2+ on clays; Cd 2+ on HACC-benonite 20 ; Pb 2+ onto Turkish kaolinite clay 21 ; Cd 2+ and Pb 2+ ions on tripolyphosphate-modified kaolinite clay 22 and removal of Pb 2+ ions by phosphatic clay 23 .
In this study, Fluidgel clay was treated with acid with the purpose to remove its carbonates and additionally a heat treatment was performed in order to improve their physical stability.The aim of this paper was to analyze the removal of cadmium and lead onto acid-treated Fluidgel bentonite clay and Fluidgel modified chemical and thermally bentonite clay.Kinetic parameters were calculated to determine the sorption mechanisms and potential rate-controlling steps, such as external and intra-particle mass transfer involved in the adsorption processes of cadmium and lead ions.Adsorption isotherms, including Langmuir and Freundlich isotherms were applied to the equilibrium data with the objective to describe the principal interactive mechanisms involved in the removal processes.

Sodic bentonite clay: Fluidgel
The sodic bentonite clay was obtained from Boa Vista, Paraíba, located in the northeastern region of Brazil.Fluidgel is composed of natural clay with sodium carbonate addition.The material was subjected to acid treatment, with the purpose to remove carbonates, because the pH of the Fluidgel occasioned chemical precipitation.In order to improve the physical stability, it was also carried out a thermal treatment; the calcination temperature was defined from thermogravimetric analysis.

Preparation and methods of analysis of materials
Fluidgel clay was ground and classified to obtain a size range of (0.855 mm) suitable for the sorption tests.
Chemically treated clay: The preparation of the Fluidgel TA-bentonite was done for the removal of carbonates, then 100 g of Fluidgel clay was treated using 1000 mL of acetic acid solution (4%), and the suspension was stirred at 1300 rpm for 4 hours.After this, the suspension was filtered and the residue was washed thoroughly with 4 L of deionized water.The residue was dried at 60 °C for 24 hours.This clay was named Fluidgel TA-bentonite.
Thermally treated clay: The Fluidgel TA-bentonite clay additionally was thermally activated at 750 °C for 24 hours after the chemical treatment to improve their physical stability and this clay was named as Fluidgel TACal-bentonite.

Adsorbate solutions
The adsorption study was performed using synthetic effluents containing Cd 2+ and Pb 2+ separately.Aqueous solutions were prepared by dissolving Cd(ND 3 ) 2 .4H 2 D and Pb(ND 3 ) 2 , respectively, in deionizer water to desired concentrations.The pH study was performed through Hydra Medusa Chemical Diagrams software to determine the predominant chemical species of Cd(II) and Pb(II) and by the isoelectric point or pH of zero of charge (pH ZPC ).The pH was adjusted by using 0.1 M HND 3 .Cadmium and lead concentrations were determined using a PerkinElmer ANALYST-100 atomic absorption spectrophotometer.

Clay characterization
The adsorbents, named as Fluidgel, Fluidgel TA-bentonite and Fluidgel TACal-bentonite composite, were characterized using the following techniques such as: X-ray diffraction: The XRD patterns of the samples were obtained using a Philips X`PERT X-ray diffractometer instrument with filtered Cu Kα radiation, voltage 40 kV, 40 mA, step size of 0.02 and time per step of 1.0 seconds.
Thermal analysis: The thermogravimetric and the differential scanning calorimetric analysis were performed using Shimadzu thermal analyzer in the following conditions: flow rate of 50 mL/min of N 2 , heating rate 10 °C/min and temperature range from room temperature to 1000 °C and 500 °C for TG and DSC analysis, respectively.
Scanning Electron Microscopy (SEM) coupled with the energy dispersive system (EDX): Samples were previously covered with gold.Scanning electron microscopy (SEM) was performed using a LED 4410.The acceleration voltage of the instrument ranged from 300 V to 30 kV, with an image point resolution of 10 nm, with the magnification ranging between 30× to 300.000×.
FTIR spectroscopy analysis: Spectra were obtained on the (Spectrum Dne -FT-IR, Perkin Elmer).The FT-IR spectra of the samples pressed into KBr pellets were collected in the wave number range of 4000-400 cm −1 .
Helium pycnometry: experiments were developed using a Micromeritics, model AccuPyc 1330 gas pycnometer using helium.The analyses were carried out at 28 °C and 0.0010 psig/min equilibrium rates.
Surface area: The surface area was performed in a Micromeritics Gemini III 2375 Surface Area Analyzer device using the BET method with an average particle diameter of 0.855 mm.
Cation exchange capacity (CEC): The CEC was determined by using ammonium acetate and was expressed in mEq.(100 g) -1 of clay 24 , according to Equation 1: Where C Na + is the Na + concentration measured by atomic adsorption (mg.L -1 ), V (mL) is the volume of 3M ammonium acetate, m is the sample mass (g) and f is the conversion factor of sodium to equivalents = 23 g of sodium by equivalents.
In the estimative of CEC method only was considered the cation Na + , in view of the fact that this clay was chemically modified with sodium carbonate, being the Na + the main exchangeable cation.This method is widely used in the scientific literature 24 .Indeed, other cations such as K + , Ca 2+ or Mg 2+ present in the clay may also act as exchangeable cations, consequently the CEC estimated by this method may have been underestimated.The cation exchange capacity can be also estimated by using methylene blue adsorption; however, this colorimetric method may also present inaccurate results.

Adsorption study
The kinetic tests for the two metallic ions utilizing Fluidgel TA-bentonite and Fluidgel TACal-bentonite were performed at room temperature (20 °C) under constant agitation (250 rpm).
Adsorption experiments were carried out by mixing known amounts of clay adsorbents (20 g) with 2000 mL at 0.394 mmol.L -1 concentration of each aqueous solution containing Cd 2+ and Pb 2+ ions, respectively.Samples were withdrawn from the shaker at different time intervals; and were centrifuged for 10 minutes.The amount of metal ion adsorbed on the adsorbent (q) was calculated by Equation 2.
where q is adsorbed amount (mmol metal/g clay), V is the solution volume (mL), C 0 is the initial concentration metal ion (mmol.L -1 ), C(t) (mmol.L -1 ) is the concentration of metal ion in solution at time t (minutes) and m the mass of clay adsorbent (g).

Adsorption kinetic models
The well-known pseudo-first order, pseudo-second order and intra-particle diffusion kinetic models were applied to experimental data with the purpose of evaluating the adsorption process.In cases where the resistance to mass transfer in the solid is dominant, the removal rate is represented by the following Equation 3: ( ) where q e , is the amount of metal sorbed at equilibrium (mmol.g - ) and k 1 is the adsorption rate constant (min -1 ).
After integration and applying boundary condition t = 0 to t = t and q = 0 to q = qt, is obtained the Equation 4: In q q In q k t − = − The pseudo-second-order model is expressed by Equation 5: where 2 2 e k q that can be defined as the initial sorption rate when t → 0. The plot t/q e versus t graph gives a linear relationship that allows computation of q e and k 2 .
When there is possibility for diffusing the adsorbate species into the adsorbent pores, the intraparticle diffusion rate constant (k i ) can be obtained from Equation 6: In this case, the intraparticle diffusion has a significant effect on the control of the adsorption process kinetics.The q t versus t 1/2 graph provides a straight line passing by the y axis with an inclination equal to the value of k i .The values for c provide an approximation of the boundary layer thickness, the greater the c value, the greater the boundary layer effect is the deviation of the straight line from the origin may be attributed to a difference in mass transfer between the initial and final adsorption stages.
The coefficient of determination, R 2 , was determined using additionally others statistical parameters such as reduced chi-square (X 2 ) and root mean square error (E RMS ) values, according to Equations 7 and 8.

Adsorption isotherm
Adsorption isotherms were obtained at temperatures of 273, 293, 313 and 333 K. 0.5 g of clay Fluidgel TA-bentonite and Fluidgel TACal-bentonite, respectively, were put into Erlenmeyer flasks, each of them filled with 50 mL heavy metal solution at different concentrations (2 to 500 ppm).The time of the experiments was determined from the kinetic test and the pH of the solutions of Cd 2+ and Pb 2+ was adjusted at around 8 for Cd 2+ and 5.2 for Pb 2+ using nitric acid 0.1 M.

Isotherm models
With the purpose to establish the relationship between the amount of adsorbed metal onto Fluidgel TA-bentonite and Fluidgel TACal-bentonite and its equilibrium concentration in aqueous system, Langmuir and Freundlich isotherm models were used to fit the experimental data.

Langmuir isotherm
The model of Langmuir (1918) was originally developed assuming monolayer adsorption on a surface of the adsorbent with a finite number of adsorption sites.
The Langmuir equation is expressed by Equation 9: where C e is the concentration of the adsorbate at equilibrium in the liquid phase (mmol.L -1 ) and q is the concentration of the adsorbate in the solid phase (mmol.g - ), b (L.g -1 ) and q max (mmol.g - ) are Langmuir constant related of the adsorbateadsorbent equilibrium and the maximum adsorbed amount on the monolayer, respectively.The essential characteristics of Langmuir isotherm model is explained in terms of a dimensionless constant separation factor or equilibrium parameter R L , which is defined in Equation 10: where K L is the Langmuir constant (L.mmol -1 ) and C o is the initial Cd(II) and Pb(II) ions concentration (mmol.L -1 ).
The parameter R L indicates the curvature of the sorption isotherm: if 0 < R L < 1, the adsorption is favorable.

Freundlich isotherm
The Freundlich model assumes that adsorption takes place on heterogeneous surfaces of an adsorbent.Equation 11 represents this model.
where K and n are Freundlich coefficients.
where ∆H is the enthalpy, ∆S is the entropy and ∆G Gibbs free energy.R is the gas constant.The plots of lnK versus 1/T provide the values of ∆H and ∆S.The variation in Gibbs free energy (∆G) is the fundamental criterion of process spontaneity.

The XRD study
Fluidgel, Fluidgel TA-bentonite and Fluidgel TACalbentonite are presented in Figure 1.The acid treatment caused structural changes in the samples; similar results were reported by other works 25,26 .The diffractograms show the presence of the characteristic peaks of montmorillonite and quartz.The result of the XRD analysis for basal spacing characteristic peaks (d 001 ) for Fluidgel was 1.483 nm, which is a characteristic of the presence of divalent cations 27 .
The peak (d 001 ) expanded to 1.821 nm after the sample was treated with acid, indicating that the expandable layers of smectite type continue being predominant, this increase can be related to the presence of the acetic acid dissociated between the structural sheets.The decrease in the basal spacing to 1.130 nm indicates alterations in the interlayer of the clay layers after calcination at 750 °C28 .X-ray diffraction results showed the presence of other peaks in the ranges: 0.45 nm (corresponding to the smectite clay mineral) and the additional peaks of quartz prevailing at 0.32 and 0.25 nm.
The basal spacing characteristic peaks (d 060 ) is an important feature used for identifying the type of smectites and is located at 0.15 nm, indicating that the smectite clay mineral is dioctahedral 29 .The samples showed the presence of sodium bicarbonate in the region of 0.34 nm corresponding to basal distance (2Θ = 29.58),which was not detected neither for Fluidgel TA-bentonite nor Fluidgel TACal-bentonite.

Thermogravimetric analysis
The thermal analysis diagrams for Fluidgel and Fluidgel TA-bentonite clay are shown in Figure 2. The corresponding weight loss for Fluidgel and Fluidgel TA-bentonite were 19.64 and 16.3% respectively.
Results showed an endothermic peak in the DTA curve of Fluidgel (Figure 2a) in the range of 25 °C to 130 °C due to the dehydration of clay minerals.The second endothermic phenomenon took place between 350 and 600 °C, this peak is referring to the loss of hydroxyl in the structure 30 .The corresponding loss of bicarbonates and carbonates are related to the endothermic peak around 283 °C and 702 °C, respectively.
The thermogravimetric results for Fluidgel TA-bentonite clay (Figure 2b) revealed a weight loss corresponding to free and absorbed water on the outer surface of bentonite and organic materials originating from acetate, due to acid treatment in the range of 34 to 133 °C.The second peak occurring between 397 to 536 °C refers to the loss of hydroxyl in the structure.

Physical properties of the Fluidgel clays
The results obtained for the specific surface areas according to the BET method besides other physical properties are shown in Table 1.Considering BET adsorption isotherms, the micropores (V mi ) and the mesopores (V mes ) volumes are obtained through the reading of adsorbed volume (V ads ) in P/P 0 = 0.10 and 0.95 expressed by Equations 14 and 15.
The specific area of Fluidgel was found to be 57.60 m 2 .g - , this value is in agreement with those reported in the literature 31 , i.e. 53.6 m 2 .g - .

Scanning electron micrograph (SEM)
The morphologic analysis of three types of clay particles by scanning electron microscopy provided the micrograph shown in Figure 3.The SEM micrographs indicated macropores in the Fluidgel clay (Figure 3a) that were not evident in the modified clays (Figure 3b) whereas the Fluidgel TACal (Figure 3c) showed breaks in their particles.
The semi-quantitative chemical composition of the compounds for the Fluidgel clay and treated clays are shown in Table 2.The increase in silicon content for the modified clay is due to remobilization of octahedral cations 32 , which are removed into the solution while the silicon remained and increased its content due to it insolubility in acid solution 33 .
The results show that exchangeable cations (Na + , Ca 2+ , K + ) were reduced, which was caused by cation exchange of H + ions 34 .The structural formula for natural clay was calculated according to the method described by Souza Santos 35 .The structural formula obtained for Fluidgel bentonite clay was (Al 1.02 Fe 0.69 Mg 0.47 ) IV (Si 3.72 Al 0.27 ) IV D 10 (DH) 2 (Ca,Na,K) 1.404 , presenting chemical compositions reported for clays originating from northeast of Brazil 35 .
The levels of Mg, Fe and others elements presented little changes, which can be attributed to the type of analysis, given that the technique of EDX detects the semi-quantitative chemical composition of the compounds point to point on the surface of the adsorbent.

Fourier transform infrared spectroscopy
Figure 4 shows the FTIR spectra of the Fluidgel samples as well as their respective treated samples.The presence of asymmetric stretching vibration of Si-D were found at 1000 to 1042 cm -1 , the stretching vibrations of Al-DH and deformation of the water H-D-H occurring at 916 and 1645 cm -1 .The other vibration at 796 and 524 cm -1 are attributable to vibration Si-D-Al.The stretching bands near 3650 cm -1 are characteristics of DH group and the presence of octahedral layers in the range of (920 cm -1 , 800 and 525 cm -1 ) 36 .

Estimation of cation exchange capacity (CEC)
The Fluidgel commercial clay was treated with sodium carbonate, presenting a large excess of this salt.Thus,  the CEC was estimated by assuming the displacement of sodium ions by ammonium ions, knowing that the industrial treatment with sodium ions did not replace calcium or potassium.
The cation exchange capacity values obtained for Fluidgel clay was of 171.74 mEq.(100 g) -1 , being for Fluidgel TA-bentonite 60.98 mEq.(100 g) -1 and finally to Fluidgel TACal-bentonite 32.914 mEq.(100 g) -1 .The results showed that the cation exchange capacity decreased dramatically with acid and heat treatment, accordingly to the results reported by other works [37][38][39][40] .These results did not prevent adsorption process of lead and cadmium onto bentonite, since the ion exchange is not the only mechanism here involved.

Adsorption of Lead and Cadmium
The adsorption of Cd(II) and Pb(II) has been thoroughly studied in batch system onto Fluidgel TA-bentonite as well as Fluidgel TACal-bentonite.The Fluidgel was not used because its pH occasioned chemical precipitation.
Fluidgel TA-bentonite: The kinetic tests were performed using monocomponent solutions containing Cd 2+ and Pb 2+ ions at 0.394 mmol.L -1 .The adsorption kinetics curves are shown in Figure 5a, b.Adsorption process of cadmium and lead ions into pores of clays occurred rapidly at the first moments.Equilibrium was reached in 150 minutes for Cd 2+  and 250 minutes Pb 2+ .The maximum amount removed for cadmium was of 0.038 and for lead 0.035 mmol.g -1 .The ion exchange can be an additional process for removal of cadmium and lead onto Fluidgel TA-bentonite, being verified by results of chemical composition presented in Table 2, where the percentage of exchangeable sodium in the clay after adsorption drastically decreased.The mechanism of ion exchange can be written as follows: 2Na + -Clay + Pb 2+ → Pb 2+ -Clay + 2Na + 2Na + -Clay + Cd 2+ → Cd 2+ -Clay + 2Na + The linear correlation coefficients and pseudo-first-order constants (k 1 ) and second-order constants (k 2 ) as well as the equilibrium capacity obtained in Figure 5 are shown in Table 4.In order to determine the equation that best describes the adsorption of Cd and Pb, other statistical parameters such as reduced chi-square (x 2 ) and root mean square error (E RMS ) values were calculated (Table 4).The intraparticle diffusion constants (k i ) obtained in Figure 6 are reported in Table 4.
The pseudo-first-order and pseudo-second-order models presented good fits for all adsorption kinetic curves as shown by the coefficients of determination in Table 3. However it can be observed that pseudo second order model presented the highest R 2 , the lowest X 2 and E RMS values approach to zero, which indicated a better fit to adsorption kinetic.Figure 6a, b show amount of heavy metals adsorbed per unit mass of adsorbent, q versus t 1/2 for Cd(II) and Pb(II) adsorption.The value of k i obtained varied from 0.45 to 20 minutes for diffusion kinetics of cadmium onto Fluidgel TA-bentonite clay.The coefficient of determination R 2 was (R 2 > 0.95), indicating that the intra-particle diffusion in the second phase is a limiting step.According to the results for Pb 2+ (Figure 6b), it can be seen that intra-particle diffusion is not the rate-limiting step in the adsorption process, being observed only two phases: the instantaneous diffusion and equilibrium stage.Therefore, it was not possible to obtain the parameter of gradual intra-particle diffusion for the sorption of Pb 2+ .
Fluidgel TACal-bentonite: The kinetic tests were performed using monocomponent solutions containing Cd 2+ and Pb 2+ ions at a concentration of 0.394 mmol.L -1 (44.3 ppm) and of 0.178 (36.93 ppm), respectively.The kinetic curve of lead removal is shown on Figure 5c.Adsorption process of cadmium and lead ions into pores of clays also occurred rapidly at the first moments; however the removal capacity reduced due to thermal treatment, which was verified by other work 16 .The maximum amount removed for lead was of 0.033 mmol metal.g - clay while for cadmium was not significant (0.005 mmol.g -1 ), for this reason its kinetic curve was not shown.
In the Table 3 are reported coefficients of determination.The pseudo-first order and pseudo-second order models cannot be fitted to experimental data onto Fluidgel TACal-bentonite, resulting in lower values of coefficients R 2 compared with those obtained for the clay Fluidgel TA-bentonite.
The kinetics of intra-particle diffusion (Pb 2+ ) in the clay Fluidgel TACal-bentonite (Figure 6c), presents two stages of diffusion, an instantaneous adsorption stage and a second sloping linear portion, which indicates the gradual  adsorption stage.The equilibrium point was not reached.The coefficients of determination R 2 was 0.95, indicating that the intra-particle diffusion in the second phase is a limiting step.

Adsorption equilibrium
Fluidgel TA-bentonite: To identify the mechanism of the adsorption process, the adsorption of Cd 2+ and Pb 2+ on Fluidgel TA-bentonite is determined as a function of equilibrium concentrations and the corresponding adsorption isotherms are plotted in Figure 7a, b.The isotherm constants calculated using Langmuir and Freundlich models are summarized in Table 5.
In Table 5 are reported coefficients of determination for the adsorption of Cd 2+ and Pb 2+ .The process was well represented by Langmuir and Freundlich models.The maximum adsorption capacity of Pb 2+ (q max ) and constant b obtained by Langmuir fit increased with the increase of the temperature (293-333 K).In contrast, the adsorption capacity of Cd 2+ did not significantly change with increasing the temperature, which means that, the removal of cadmium by clay Fluidgel TA-bentonite is exothermic.The R L values obtained in this work (data not shown) varied in the range of 0 < R L < 1, indication of favorable adsorption.
Fluidgel TACal-bentonite: Figure 7c shows isotherm plots obtained on the adsorption process of Pb 2+ on Fluidgel TACal-bentonite.The isotherm constants are also summarized in Table 5.The maximum adsorption capacity was obtained to 333 K.However, above this value, an increase in the temperature has no effect on the adsorption capacity of the lead.From the results for adsorption of lead we can be established that the affinity of Pb 2+ onto Fluidgel TA-bentonite is greater than Pb 2+ onto Fluidgel TACal-bentonite.The cadmium removal by Fluidgel TACal clay did not occurred.

Adsorption thermodynamics
The thermodynamic parameters such as change in enthalpy (∆H), change in entropy, (∆S) and change in Gibbs free energy (∆G) obtained for the adsorption of Cd 2+ and Pb 2+ at different temperatures onto Fluidgel TA and Fluidgel TACal clay adsorbent are given in Table 6.
The negative values of both ∆H and ∆S indicate an exothermic reaction during the adsorption of Cd 2+ onto Fluidgel TA, whereas negatives values of ∆G values for cadmium and lead by Fluidgel TA-bentonite and Fluidgel TACal-bentonite indicate a spontaneous adsorption process.The value of ∆H was found < 40 kJ.mol -1 for all cases onto the two clays, suggesting that the adsorption is physical with electrostatic interaction between sorption sites and the metal ion 41 .
Dn the other hand for Pb 2+ ions, the change in enthalpy values (∆H) is positive, showing that the sorption of Pb 2+ on Fluidgel TA-bentonite and Fluidgel TACal-bentonite is endothermic in nature.It can be observed that ∆G values obtained for Cd 2+ and Pb 2+ were found to be negative indicating that the adsorption of both metal ions onto Fluidgel TA-bentonite and also Fluidgel TACal-bentonite clays were spontaneous.Thus, the positive ∆S (Pb 2+ ) value represents the rise of randomness in the interface between the solid and the solution during the fixation of Pb 2+ on the active sites of the adsorbent 20 .It can be seen that adsorption of Cd 2+ has a negative ∆S suggesting some structural changes in the clay and adsorbate 42 .

Conclusions
The basal spacing characteristic peaks (d 001 ) presented structural change due to thermal and chemical treatments.Pseudo-second order model presented the highest R 2 and the lowest x 2 and E RMS values approach to zero, indicating a better fit to adsorption kinetic for cadmium and lead ions onto Fluidgel TA-bentonite.The mechanism of ion exchange was considered part of the adsorption process onto Fluidgel TA-bentonite, considering the decrease of sodium percentage in the chemical composition of clay after process.The maximum removal efficiencies were 97.62% for Cd(II) using Fluidgel TA-bentonite and 91.08% for lead by Fluidgel TACal-bentonite modified chemical and thermally.The results also showed that Fluidgel TA and Fluidgel TACal clays can be used as alternative adsorbents for the removal of Pb 2+ ions, due to its adsorptive properties.Cd 2+ and Pb 2+ ions by Fluidgel TA-bentonite and Fluidgel TACAl-bentonite clay were found to be negative, which suggests that adsorption of cadmium and lead onto these clays is spontaneous in nature.

Figure 6 .
Figure 6.Sorption of Cd 2+ (a) and Pb 2+ (b) onto Fluidgel TA-bentonite and sorption of Pb 2+ onto Fluidgel TACal-bentonite (c) as a function of square root of time for intra-particle diffusion rate constant determination.

Table 1 .
Samples surface area calculated by the BET method and real density of Fluidgel, Fluidgel TA-bentonite and Fluidgel TACal-bentonite.

Table 2 .
Chemical analysis of the clays.

Table 3 .
Pseudo-first and second order kinetic parameters for the sorption of Cd(II) and Pb(II) onto Fluidgel TA-bentonite clay and Cd(II) and Pb(II) onto Fluidgel TACal-bentonite clay.

Table 4 .
Parameters of intra-particle diffusion for the sorption of Cd(II) and Pb(II) onto Fluidgel TA-bentonite clay and Cd(II) and Pb(II) onto Fluidgel TACal-bentonite clay.

Table 6 .
Thermodynamic parameters for the sorption processes of Cd(II) and Pb(II) onto Fluidgel TA-bentonite and Fluidgel TACalbentonite clays.

Table 5 .
Langmuir and Freundlich isotherm constants and correlation coefficients.