“…The peaks at 26°, 26.7°, and 31.4° mainly originate from the ZnP2 phase and are matched well to the (1 0 4), (1 1 2), and (1 1 4) planes, respectively (JCPDF 24-1464) [39]. The peaks at 40.2° and 44.1° mainly originate from Fe2P and matched well with the (1 1 1) and (2 0 1) planes, respectively (JCPDF 51-0943) [40,41]. All the other peaks are characteristic of Co2P (JCPDF 32-0306) and also matched well with the (1 2 1) and (2 0 1) planes [42,43].…”