Abstract
AbstractA reversible topotactic oxidizing–reducing process has been clearly evidenced in the annealing treatment followed to stabilize rhombohedral and orthorhombic La1–tMn1–tO3 (0.016 ≤ t ≤ 0.038) samples. The study of the surface evolution followed by characterization by scanning electron microscopy (SEM) and atomic force microscopy (AFM) gives evidence for a diffusion mechanism of La and Mn cations through the grain boundaries which provides a fast pathway in the perovskite related compound; however, contrary to theoretical predictions, the overall cationic ratio (La:Mn 1:1) is kept.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
