In the case of Ag=0 sample, observed vibration peaks around 209 cm
-1, 441 cm
-1, 535 cm
-1, and 693 cm
-1 were ascribed to recorded, but with different intensities. According to
Figure 3, the CuAlO
2 and Ag doped CuAlO
2 samples' room temperature Raman scattering spectra exhibit many photonic bands of the delafossite structure. From Raman spectrum of Ag
0 sample, Raman modes present around 209 cm
-1, 441 cm
-1, 535 cm
-1, and 693 cm
-1, in agreement with earlier results on CuAlO
2 [
21,
22]. Observed modes identified as A
1g at 693 cm
-1, E
g at 441 cm
-1, and A
g at 209 cm
-1, in addition to band at 535 cm
-1 are the bands that make up this pattern. Moreover, the mode at 535 cm
-1 is attributed to relaxation of selection rules by defects such as Cu vacancies, interstitial oxygen’s or tetrahedrally coordinated Al on the Cu site [
23]. It implies that these vibrations could be linked to the spectrum characteristics of the edge-sharing AlO
6 octahedra and perhaps the O-Cu-O linear bond. It suggests that these vibrations may be associated with the spectral features of the edge-sharing AlO
6 octahedra and possibly the O-Cu-O linear bond. The substitution of Cu by Ag induces a change in frequency and inline width of A
1g and E
g modes. Moreover, the A
1g depicts the vibrations of the Cu-O bonds along the c-axis while the E
g mode is describes the atomic vibrations perpendicular to c-axis [
24,
25]. In other words, Cu is replaced with Ag, which results in a change in the frequency and inline width of the A
1g and E
g modes. The observed lattice expansion along various axes and the difference in ionic radii between Cu and Ag are both compatible with the two frequencies' shift to shorter wavenumbers, which denotes a weak (Cu, Ag)-O bonding. Particularly, the A
1g mode is displaced up 33, and the A
1g mode frequency is highly dependent on the oxygen bonding properties of the (Cu, Ag)-site atoms. We also observe a sharp decline in the intensity of the initially prominent band at 535 cm
-1 for these Ag-doped materials, as well as a reversal in the A
1g-E
g mode magnitude ratio. The peak at 535 cm
-1 is thought to result from the presence of a prohibited non-zero wavevector phonon, which shows a breakdown in the translational symmetry of the crystal and relaxes the Raman selection rules, indicating the presence of crystal structure defects. Several delafossites have also shown comparable forbidden modes, which may have similar causes, such as interstitials, vacancies, and substitutional defects [
26]. We contend that the decline in disorder and intensity are connected. Consequently, it can be deduced that the Raman spectrum are affected by the existence of number of defects (oxygen vacancies, stacking faults, antisite disorder, structural inhomogeneities, etc.) that are introduced into the CuAlO
2 lattice structure during the simultaneous Ag-doping. All the observed changes in the Raman spectra of the samples are consistent with the results of XRD analysis, which further confirm the successful Cu-site substitution with Ag and the structural distortion. The Raman modes show that increasing the concentration of x from 0.00 to 0.04 results in the emergence of peak shifting and broadening along with the change in intensity and the disappearance of mode at 535 cm
-1. This variation might be due to the lattice distortion induced by Ag ions into the host lattice of copper aluminate.
Our results demonstrate that the substitution of Cu by Ag in the studied concentration range of Cu1-xAgxAlO2 compound can be made without changing the delafossite structure. However, local changes do occur, and they are much more relevant in Raman spectroscopy, that is a local probe, more than X-ray diffraction, where the impacts of cationic composition changes are averaged and mostly seen as peak variation.
FT-IR spectra in the wavenumber range of 400 – 4000 cm
-1 for Cu
1-xAg
xAlO
2 nanoparticles with x=0, 0.01, 0.02, 0.03, and 0.04 are presented in
Figure 4. A small amount of water vapour, CO
2 and N
2 are absorbed on CuAlO
2 powder from atmosphere. In the case of Ag=0 sample, broad band at 3467 cm
-1 is due to the stretching vibration of hydroxyl groups attached on the surface of nanocrystalline powders, indicating the existence of water absorbed on the surfaces of grains [
27], the ranging band from 2356 cm
-1 is assigned to C-H stretching, and a peak near 1560 cm
-1 appears due to CO
2 adsorbed on the surface, which might have been incorporated from the atmosphere [
28]. The peak around 1400 cm
-1 is associated to nitrate groups [
29], and 1016 cm
-1 attributed to C-O stretching [
30]. The bands originated at the region below 1000 cm
-1 demonstrate the mixed vibrations of metal and oxygen molecules due to the formation of Cu-O, Al-O, and Ag-O stretching bonds [
22,
31]. FTIR spectra of Cu
1-xAg
xAlO
2 close agree with those previously reported for this material [
32].