XRD pattern for Fe3O4-Pd nanoparticles

These peaks are assigned to specific crystallographic planes of Fe₃O₄ and Pd. For Fe₃O₄, the characteristic diffraction peaks typically correspond to a face-centered cubic (fcc) spinel structure.

The presence of peaks at 17.84°, 30.05°, 35.43°, 46.20°, 53.28°, 56.95°, and 62.52° can be indexed to the (111), (220), (311), (400), (422), (511), and (440) planes of Fe₃O₄, respectively, confirming the crystalline nature of magnetite [27]. The peaks at 40.06° and 68.49° are assigned to Pd (111) and Pd (220) planes, respectively, indicating the presence of crystalline palladium [28].