We recently synthesized prospective new materials composed
of alternating
quasi-atomic sheets of brucite-type hydroxide (Mg, Fe)(OH)2 and CuFe1–x
S2 sulfide
(valleriites). Herein, their thermal behavior important for many potential
applications has been studied in inert (Ar) and oxidative (20% O2) atmospheres using thermogravimetry (TG) and differential
scanning calorimetry (DSC) analyses and characterization with X-ray
diffraction (XRD), X-ray photoelectron spectroscopy (XPS), scanning
electron microscopy (SEM), and energy-dispersive X-ray (EDX). In the
Ar media, the processes are determined by the dehydroxylation of the
hydroxide layers forming MgO, with the temperature of the major endothermic
maximum of the mass loss at 413 °C. Sulfide sheets start to degrade
below 500 °C and melt at nearly 800 °C, with bornite, chalcopyrite,
and troilite specified as the final products. In the oxidative atmosphere,
the exothermic reactions with the mass increase peaked at 345 and
495 °C, corresponding to the partial and major oxidations of
Cu–Fe sulfide layers. Sulfur oxides captured in magnesium hydroxide
layers to form MgSO4 compromised the layer integrity and
promoted the oxidation of the sulfide entities. The final products
also contained minor MgO, Cu2MgO3, Fe3O4, and MgFe2O4 phases. Samples
doped with Al, which decreases the content of Fe in hydroxide layers,
show notably impeded decay of valleriite in argon but facilitated
the oxidation of Cu–Fe sulfides, while the impact of Li (it
slightly increases the number of the Fe–OH sites) was less
expressed. The mutual stabilization of the two-dimensional (2D) hydroxide
and sulfide layers upon heating in an inert atmosphere but not in
oxygen as compared with bulk brucite and chalcopyrite was suggested
to explain high thermal resistance across the stacked incommensurate
sheets, which slows down the endothermic reactions and accelerates
the exothermic oxidation; the high number of Fe atoms in the hydroxide
sheets are expected to promote the phonon exchange and heat transfer
between the layers.