“…Thus, the Al/Fe + Co + Al mole ratio increased from 8% for the G CoAl sample to 33% for sample Fe CoAl (figure 5), indicating a further and more important enrichment of Al cations in the particle outer layers during its reduction process, which explains its role in avoiding interparticle sintering. In addition, it was observed that the proportion of cobalt in the particle outer layers decreased from goethite to iron for both Fe Co and Fe CoAl samples, respectively (figure 5), which suggested the diffusion of this cation to the inner part of the iron particles and, thereby, the formation of Fe-Co alloy, as previously observed by other authors [14,15]. Finally, the position observed for the Fe 2p 3/2 (710.3 eV) and Co 2p 3/2 (780.3 eV) XPS peaks (data not shown) was consistent with the presence of oxidized iron and cobalt in the particle outer layers, which could consist of a ferrimagnetic spinel phase similar to that suggested for Al-doped iron from Mössbauer studies [18].…”