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Adsorption of As (III) on Iron Coated Quartz Sand: Influence of Temperature on the Equilibrium Isotherm, Thermodynamics and Isosteric Heat of Adsorption Analysis

  • Shashi Bala Gautam EMAIL logo , Siraj Alam and Suantak Kamsonlian
Published/Copyright: November 21, 2015

Abstract

The influence of temperature on the sorption of As(III) onto iron oxide coated quartz sand (IOCQS) was studied in the temperature range of 298–318 K. An increase in temperature was found to have positive influence on the adsorption of As(III) ions onto IOCQS surfaces because of increased diffusion of As(III) ions into the pores of IOCQS at higher temperature. The enhanced sorption at higher temperature indicated endothermic adsorption process. Equilibrium isotherms for the adsorption of As(III) on IOCQS were analyzed at different temperatures. Among the conventional isotherms, Freundlich isotherm best predicted specific uptake at different temperatures, followed by Redlich–Peterson, Langmuir and Temkin isotherm models. Various thermodynamic parameters namely heat of adsorption (∆H0), change in entropy (∆S0), and Gibbs free energy change (∆G0) were computed from the equilibrium constant (KD) values. The results indicated positive value for heat of adsorption ∆H0, a positive ∆S0 and a negative ∆G0. Finally, the isosteric heat of adsorption (ΔHst,a) values were calculated and quantitatively correlated with the fractional loading of As(III) onto IOCQS. The surface heterogeneity of adsorbents could be quantitatively described with an isosteric enthalpy function of fractional loading based on Do and Do model. The results show that the IOCQS possesses heterogeneous surface with sorption sites having different activities.

Nomenclature

1/n

heterogeneity factor, dimensionless

aR

constant of Redlich –Peterson isotherm (l/mg).

B1

related to the heat of adsorption (mg/g)

C

constant that gives idea about the thickness of boundary layer (mg/g)

Ce

equilibrium concentration liquid phase concentration (mg/l).

ΔG0

free energy change (kJ/mol),

ΔH0

change in enthalpy (kJ/mol),

IOCQS

iron oxide coated quartz sand

KD (=qe/Ce)

single point or linear sorption distribution coefficient.

kf

rate constant of pseudo- first order adsorption model (min–1)

ks

rate constant of pseudo- second order adsorption model (g/mg/s)

kid

inter particles diffusion rate of constant (mg/g/min1/2)

KF

constant of Freundlich isotherm ((mg/g)/(l/mg)1/n)

KL

constant of Langmuir isotherm (l/g)

KT

equilibrium binding constant corresponding to maximum binding energy (l/g)

kR

constant of Redlich –Peterson isotherm (l/g)

qe

equilibrium solid phase concentration (mg/g)

qe,cal

calculated value of solid phase concentration of adsorbate at equilibrium (mg/g)

qe.exp

experimental value of solid phase concentration of adsorbate at equilibrium (mg/g)

qm

maximum adsorption capacity of adsorbent (mg/g)

qt

amount of adsorbate adsorbed by adsorbent at time t

R

universal gas constant (8.314 J/K mol)

SSE

sum of square error function

t

time (min)

R

universal gas constant (8.314×10–3 kJ/mol K)

ΔS0

entropy change (kJ/mol K),

T

absolute temperature (K)

Greek symbol

α

initial adsorption rate constant (mg/g/s)

β

desorption constant (g/mg)

β1

constant of Redlich–Peterson isotherm (0 <β1 <1)

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Published Online: 2015-11-21
Published in Print: 2016-2-1

©2016 by De Gruyter

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