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Coral Limestone Modified by Magnetite and Maghemite Nanocomposites for Sequestration of Lead(II) and Chromium(VI) Ions from Aqueous Solution
Author(s) -
Cynthia Sibongile Nkutha,
Ntaote David Shooto,
Eliazer Bobby Naidoo
Publication year - 2021
Publication title -
asian journal of chemistry/asian journal of chemistry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.145
H-Index - 34
eISSN - 0975-427X
pISSN - 0970-7077
DOI - 10.14233/ajchem.2021.23027
Subject(s) - maghemite , chemistry , adsorption , magnetite , nanocomposite , physisorption , iron oxide , chemical engineering , specific surface area , inorganic chemistry , mineralogy , materials science , metallurgy , hematite , organic chemistry , engineering , catalysis
In present work, a one pot synthesis of magnetic nanocomposites was synthesized by using co-precipitation method in air atmosphere.The synthesis of magnetite and maghemite supported on biogenic coral limestone was done by varying the ratio of Fe(II)/Fe(III) insolution to obtain the two phases of iron oxide and capping with sucrose in air atmosphere. The nanocomposites were characterized byFTIR, where the results showed a distinct peak for Fe-O, while UV/vis showed an absorption in the visible region which is typical of ironoxide. Photoluminescence results showed that the nanocomposites were both red shifted for magnetite-PCLS (PCLS = pristine corallimestone) and magnetite-CCLS (CCLS = calcined coral limestone); while a blue shift and red shift was observed for the maghemite-PCLS and maghemite-CCLS. From the SEM a deviation of sphericity of the nanocomposites, with maghemite having an uneven distributionwas observed. Equilibrium was reached within 60 min, of which maghemite showed higher metal uptake. The kinetic data fit PSOMbetter as compared to PFOM, this means that adsorption was due to the charge density on the surface of the nanocomposites. The good fitfor intraparticle diffusion (IPD) also suggested that adsorption was also observed due to mass transfer, it was observed that the rate limitingstep was due to surface adsorption. This was in good correlation with the better fit of PSOM. The mechanism of adsorption was found tobe better explained by physisorption and the surface was heterogeneous whereby multilayer adsorption was possible. The data was alsosubjected to Dubinin-Radushkevich isotherm, which suggests that the uptake of the pollutants was due to physisorption. The adsorptionprocess was spontaneous and favourable which is supported by the negative values of Gibb’s free energy for the system.

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