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Download fileAdsorption Behaviors and Mechanisms of Methyl Orange on Heat-Treated Palygorskite Clays
journal contribution
posted on 2012-10-31, 00:00 authored by Hao Chen, Aiguo Zhong, Junyong Wu, Jie Zhao, Hua YanUnderstanding completely the interaction of clay mineral
and anionic
dye is very important for the applications of clay minerals. In this
paper, the adsorption behaviors of heat-treated palygorskite clays
for methyl orange (MO) from an aqueous medium were studied using equilibrium
batch and theoretic calculation techniques. The crystal structure
and surface appearance of the heat-treated samples were studied using
Fourier transform infrared (FTIR) and scanning electron microscopy
(SEM). The adsorption results reveal that a higher calcining temperature
helps in improving removal performance of palygorskite clay for methyl
orange. The isothermal adsorption experiments show that there is almost
no adsorption at low dye concentrations but a sudden linear increase
occurs when the dye concentration exceeds to a certain value. A lower
change point is observed for 700 °C treated sample compared with
that of the natural sample. The leaching of exchangeable Mg2+ ions located in palygorskite should be a key factor affecting the
adsorption capacity. Both the experimental and theoretical studies
suggest that the adsorption of MO onto heat-treated palygorskite clay
is controlled by the two mechanisms: for samples treated at lower
temperatures (<300 °C), the hydrogen bonding between oxygen
groups of −SO3– (anionic head
groups of MO) and H+ of both the bound zeolitic water and
coordinated water should be important. While for samples calcined
at higher temperature (>400 °C), electrostatic interaction
between
the dye–Mg2+ complexes and negatively charged surface
of heat-treated palygorskite clay becomes dominant. In addition, the
latter becomes stronger with the increasing the calcination temperature,
which can be ascribed to the formation of a higher ratio of complexes
and stronger negatively charged surface of the adsorbent caused by
leaching of more metal ions. This work provides a deep insight into
the interaction of heat-treated palygorskite clay and anionic dye,
which paves the way for their practical applications in anionic dye
adsorption.
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calcining temperaturehead groupsremoval performanceadsorption capacitysamples calcinedoxygen groupspalygorskite claymetal ionsFTIRclay mineralsMOzeolitic waterdye adsorptioninteractionclay mineraladsorption resultscalcination temperaturetheoretic calculation techniquesadsorption experiments showSEMscanning electron microscopydye concentrationsAdsorption Behaviorssurface appearancecrystal structureequilibrium batchadsorption behaviorsdye concentrationMethyl Orangechange point