X-ray photoelectron spectroscopy (XPS)is utilised to investigate the valence state of pure LCO and Te in-cooperated LCO with a Te content of 5 wt.%. The XPS survey spectra in
Figure 5(a) and (d) demonstrate the presence of Co, O, La, and Te (5 wt.% Te in-cooperated LCO). Core-level XPS spectra verify the real valence states of the individual components. Co 2p core level spectra, both pure and Te in-cooperated, are shown in Figures 5 c and f, respectively. LCO's two asymmetric peaks are located at 780.18 and 795.45 eV and are most similar to those of Co 2p
3/2 and Co 2p
1/2. Paramagnetic Co
2+ is formed at the surface, accounting for the visible satellite peaks above the primary photo peaks [
34]. Because of the presence of numerous excitations and the coexistence of Co
3+ and Co
2+ states, the Co 2p peak expanded and shifted toward higher energy when Te was present in conjunction with LCO. The existence of both high-spin Co
2+ and low-spin Co
3+ ions were further validated by the appearance of the Co2p
3/2 peaks at 781.23 eV with decreased satellite peaks [
35,
36]. The Co 2p photoelectron spectra of Te-LCO are chemically shifted sufficiently to permit chemical identification. The Co 2p
3/2 and Co 2p
1/2 lines for Te-LCO were chemically shifted to 1.05 eV and 1.14 eV, respectively, to higher binding energies than for LCO. The Co 2p
3/2 has diminished satellite peak may be due to well exposure of LCO when we mechanically ball mill with Te, which leads to further oxidation of the samples towards the surface. According to research by Frost and colleagues [
34,
37], photoelectron spectra of high-spin Co
2+ compounds show robust satellites, while those of low-spin Co
2+ compounds either show weak satellites or none at all. Te-LCO has a core photoemission peak separation of 15.36 eV, while LCO's is 15.27 eV. These values are fairly close to the CoO and Co
3O
4 values that have previously been published [
34,
38] as depicted in
Figure 5. As anticipated, the La 3d line shows the four component peaks (b and e). According to our prior research [
19], the La 3d
5/2 and La 3d
3/2 are associated to the double peaks of LCO, which emerge at 834.7 and 838.34 eV, respectively. These peaks can be attributed to the La
3+ state and represent charge transfer between the La
2O
3, O2p and La 4f orbits [
36,
37,
38] or substantial electronic configuration final state mixing [
42]. Te in-corporation causes a shift toward greater binding energies, indicating that the lattice structure is being destroyed. Because of Te's multivalence state, the additive peak with the highest intensity at 837.34 eV could be attributable to the synthesis of La sub-oxide (La-O
x). The observed core-level Te3d spectra have been deconvoluted into single 3d
3/2 and 3d
5/2 spin-state peaks at about 587 and 576 eV, respectively, to help explain it better.The chemical shift seen at Te 3d
5/2 of approximately 3 eV towards higher binding energy from Te
2- is characteristics of NaBH
4 reduced TeO
2, which may form some surface oxidation layers (Te
0).
Figure 5 (i) shows the two asymmetric peaks of high-resolution Te 3d XPS spectroscopy, which reveals the Te
4+/Te
2-/Te
0 oxidation state for the NaBH
4 reduced TeO
2.The binding energy difference between 3d
3/2 and 3d
5/2 is 10.4 eV, which agrees with the literature [
43,
44,
45]. As was previously mentioned, the presence of Te at high oxidation states reconstructs the crystal structure and produces more Co
2+ and Co
3+ at various spin states, which leads to additional defects. The perovskite's A and B sites are both affected by the equally distributed Te
4+, which results in an increase in the amount of La
2+ in the A site and an anisotropic Co
2+ in the B site to balance the charge. As a result, the magnetic state of the perovskite LCO was affected by the discrete La 3d and Co 2p photoemission peaks that the 5% Te in-coordinated LCO displayed at various spin states [
46,
47]. The same O1s peaks associated with the LCO and 5% Te-LCO provide evidence that Te played a part in the incorrect perovskite oxide's formation. As demonstrated in
Figure 5, both the pristine and Te-LCO O1s peaks had three unique peaks (h & g). O1s peaks observed at 528.8, 530.9, and 532.6 eV on the LCO surface. This major signal at 528.8 eV can be attributable to either bulk oxide or to lattice oxygen (O
2-), which is in line with the findings from earlier studies [
41]. When looking at the oxide system, the broad peaks that have greater binding energies are the ones that are the most challenging to interpret. The value of 530.9 eV can be explained by the presence of chemisorbed oxygen (O
-) or adsorbed H
2O/OH
- species, both of which create a vacancy at the surface for oxygen to occupy [
48].O 1s XPS spectra of the Te impregnated LCO surface show that superoxide (O
2-) formation occurs at a peak energy of 532.6 eV, while the other two peaks can be attributed to lattice oxygen, chemically adsorbed oxygen species on the oxygen vacancies, and physically adsorbed oxygen species on the surface. Three peaks with centres at BE = 529.5, 531.6, and 532.7 eV were revealed by deconvolution of the Te-impregnated LCO asymmetric O 1s spectra (
Figure 5 g) [
49]. These peaks correspond to lattice oxygen (such as O
2), chemically adsorbed oxygen (such as O
-), and physically adsorbed oxygen (H
2O, O
2), respectively. This encourages the conception of more peroxide/superoxide ions, which results in the acquisition of stronger peaks at 532.7 eV. Te
4+ is in higher oxidation states in the Te in-cooperated LCO as a result of the exchange of oxygen species that occurs as oxygen vacancies form between bulk and surface oxides [
40].