This study deals with the process of zeolite formation in
an agricultural soil artificially polluted by high amounts of
Cu (15 mg of Cu/g of soil dry weight) and treated with
fused coal fly ash at 30 and 60 °C and how this process
affects the mobility and availability of the metal. As a
consequence of the treatment, the amount of dissolved
Cu, and thus its mobility, was strongly reduced, and the
percentage of the metal stabilized in the solid phase increased
over time, reaching values of 30% at 30 °C and 40% at
60 °C. The physicochemical phenomena responsible for Cu
stabilization in the solid phase have been evaluated by
EDTA sequential extractions and synchrotron radiation based
X-ray microanalytical techniques. These techniques
were used for the visualization of the spatial distribution
and the speciation of Cu in and/or on the neo-formed zeolite
particles. In particular, micro XRF (X-ray fluorescence)
tomography showed direct evidence that Cu can be entrapped
as clusters inside the porous zeolitic structures while
μ-XANES (X-ray absorption near edge structure) spectroscopy
determinations revealed Cu to be present mainly as
Cu(II) hydroxide and Cu(II) oxide. The reported results
could be useful as a basic knowledge for planning new
technologies for the on site physicochemical stabilization
of heavy metals in heavily polluted soils.