First-principles calculations done
via density functional theory
were used to study the structural and electronic properties of sodium
montmorillonite clay (Mt-Na+) of general formula MxAl3Si8O24H4Na·nH2O (Mx: Mg or Fe). The final position of the interlamellar sodium
atom is found to be close to the oxygen atoms located on the upper
surface of silica. Following Fe-Mt-Na+ system relaxation,
with subsequent analysis of magnetic moment and magnetic states, the
electroneutrality of the system established that both Fe2+ and Fe3+ oxidation states are possible to occur. The
Mg2+-Mt-Na+ material shows a band gap energy
greater than that of Fe2+-Mt-Na+ when iron is
in the octahedral site. It is found that the valence-band maximum
and the conduction-band minimum of iron-doped montmorillonite are
both at the Γ-point, while it is at V →
Γ for magnesium-doped montmorillonite. The calculated band gap
from hybrid functional (HSE06) of Fe2+-Mt-Na+ is equal to 4.3 eV, exhibiting good agreement with experimental
results obtained from ultraviolet–visible spectroscopy of the
natural Mt-Na+ (Cloisite-Na+).