Recent studies have shown that the
addition of Ca as host ion in
the layered compounds RBaCo2O5+δ (with R a rare earth or yttrium) produces a dramatic
effect on their magnetic properties, as well as on their Seebeck coefficient
and resistivity. Studies performed so far have opened up the possibility
that the substitution site for Ca atoms might not be obvious, having
been reported at the Y site, at the Ba site, or regarded as not decisive
to the ferromagnetism enhancement. In this work, we present a comparative
study of Ca-doped cobaltite samples synthesized with two different
nominal substitution sites, namely, Ca replacing Ba, and Ca replacing
Y. X-ray absorption spectroscopy performed at the Ca, Ba, and Co edges
to study the local environment around these elements allowed to unequivocally
determine that the substitutional site of Ca is the Y site. This important
result helps to clarify the mixed valence state of cobalt as Co3+ and Co4+, which would be responsible for the
ferromagnetic interactions, and explains the antiferromagnetic to
ferrimagnetic switch occurring already at 10% Ca doping level.