In few research reports, the sound velocity anomaly in manganite has been taken as a proof of the observation of charge ordering and the temperature where anomaly has been observed (called charge ordering transition temperature (TCO)).
My question: Is it really so, or is the anomaly just an indication of diverging lattice degrees of freedom at that temperature?
As I understand, the diverging of the lattice degrees of freedom can occur due to many reasons like any type of structural/magnetic/electronic phase transition which can modify the lattice structure in a strongly correlated material at that temperature and thus can lead to an anomaly in sound velocity.