By measuring the infrared spectra and laser Raman spectra for various hopeite films and phosphophyllite films, the influence of metal component composition in these films on those spectra can be investigated. In infrared spectra, peaks corresponding to (ν
1 +
3) andν
4, the fundamental vibrational modes of PO
43-, were seen, but the peak patterns ofν
4, were d ifferent for hopeite films containing manganese component from that not containing it (Figs.2, 3, 5 and 6). Raman s pectra for these films were shown in Figs.7-11. Four clear peaks due to PO
43-were found in the region of 800-1300 cm
-1. Tetrahedral orthophosphate (PO
43-) has four fundamental vibrational modes ofν
1, ν
2, ν
3, and
ν, (Fig.4) ;
ν1, andvν
3are observed in 800-1300 cm
-1. Essentially, ν
3 degenerates triply. But in the crystalline state of zinc phosphate films, the tetrahedral structure of PO
43- will be deformed, and the degeneracy of ν
3 is untied and the band is split to three peaks. Accordingly, it was considered that the spectra with four peaks containing ν
1 were generated. Here, main peak corresponds to ν
1 and other th ree peaks correspond toν
3. This consideration was supported by the Raman data for 85%-H
3PO
4solution (Fig.12). The peak fr equencies of Raman bands for various zinc phosphate films were compared (Table 2). For both hopeite films and phosphophyllite films, the Raman peaks shifted to lower wavenumbers with the increase of nickel or manganese component (Fig.13). In particular, the Raman peaks of hopeite C and D was similar to that of phosphophyllite E. The composition of modified hopeite films by the doping of nickel or manganese comp onent has been analyzed as Zn
3-x Me
x(PO
4)
2-4 H
20 (Me: Ni and/or Mn). This composition is different from neat hopeite films of Zn
3(PO
4)
24 H
20 and is modified to the composition as phosphophyllite films. Thus, it was possible to correlate the modification level of zinc phosphate films, for instance, the crystal morphologies of these films or chemical stability like anti-alkaline property with the observation of PO
43- peak shift in Raman spectra.
View full abstract