3.1 Changes in organic matter
Ozone reacts with organic and inorganic matter because of its high reproduction potential and reactivity (Hoigne & Bader 1983a; Hoigne & Bader 1983b, Hoigne & Bader 1985). As a result of the experiment under ozone injection conditions, the changes in the organic matter were as follows (Fig. 1). CODMn dropped significantly from 167.6 mg/L to 86.7 mg/L at 40 min, then decreased gently to 46.9 mg/L at 180 min. The final removal rate was 72.0%. CODCr decreased by 69.1% from 230.0 mg/L to 71.0 mg/L at 180 minutes. TOC showed a similar trend to CODMn, which fell sharply from 148.5 mg/L to 76.8 mg/L in 5 minutes, then decreased gently, and finally decreased by 68.7% to 46.5 mg/L. Although there was a difference for each indicator, the organic matter decreased significantly between 5 and 20 minutes and decreased at a relatively small rate after that. Ozone utilization is more effective at lower ozone concentrations, but longer retention times are required for optimal efficiency (Shin & Lim, 1996). Only a slight nitrogen reduction was observed at the highest oxidant doses over time, indicating that only minor mineralization occurred.
On the other hand, organic nitrogen decreased following a linear trend, and reductions varied between 20 and 30% after 120 min of treatment. Due to the constraint characteristics of ammonia nitrogen, during 20 min of reaction, the NH3-N concentration was increasing steadily, and after 20 min, it decreased by around 28%. However, the ozone had a nominal effect on T-N, and the results show a variation in the removal of Total Nitrogen. The summary of these results showed that the ozone treatment mainly had a crucial changing effect on organic nitrogen.
3.2 UV-vis spectrum change
The curve change of the UV-vis spectrum after ozone treatment of the anaerobic digestion wastewater is shown in Fig. 2. The anaerobic digestion wastewater subjected to ozonation had a high curve and fell gently from 230 nm to 667 nm. After that, the curves were sequentially stabilized until 20 minutes, and after that, almost similar results were shown. As a result of tracking the treatment results after 20 minutes, there was no significant difference, but rather a shoulder between 270 nm and 340 nm appeared. (Noethe et al. 2009) stated that highly concentrated organic compounds absorb at higher wavelengths (e.g., 436 nm), and possible to change compounds that still have absorption at lower wavelengths (e.g., 254 nm) after ozonation. Most important is that during UV/H2O2 treatment, some of the change compounds formed and absorbed in the higher UV region, that is, as opposed to ozonation. Presumably, these changes in organic compounds were also formed during ozone treatment, but the rate of decomposition exceeded the rate of formation due to their high reactivity to ozone. The distinction of ozone is also exemplified by the fact that the shape of the normalized DAS changes appreciably as a function of time. In comparison with the results of (Nanaboina & Korshin, 2010), at higher wavelengths, the normalized DAS values were initially higher and gradually decreased with ozone dose. This appears to be a result of the strong reactivity of organic intermediates produced as by-products after the ozone reaction. (Audenaert et al., 2013)
The graph of DAS showing the differential value of UV-vis spectrum in Fig. 3a. DAS increased by 20 minutes and there was no significant difference thereafter. Rather, Fig. 3b, showed it decreased little by little. According to (Audenaert et al., 2013), comparably DAS decreased in ozone treatment and increased in UV-AOP process.
Changes in the above spectrum are visible, but it isn't easy to compare them by representing them with a single numerical value. Therefore, the representative values of the spectral changes were taken as the sum at each wavelength and the absorbance at 254 nm and are shown in the following graph. As a result, there was no significant difference after the sum of the wavelengths decreased sharply up to 20 min, and after 20 min, it increased slightly at the 254 nm wavelength. However, the curves during ozone treatment almost coincide, and this phenomenon means that during the ozonation process, DAS curves changed uniformly. Hence, the absorbance removal efficiency at a particular wavelength was almost independent of oxidant exposure. Therefore, it was hypothesized that the change of organic compounds that were initially absorbed in 30 min contributed to the formation of products absorbing until 180 min. After 30 minutes of ozone treatment, the normalized DAS overlapped further as the areas preferentially charged by ozone were almost completely oxidized. The decreasing trend of the sum of these wavelengths is shown in Fig. 4. It appeared similar to CODMn and TOC curve of Fig. 1.
3.3 Comparison of UV-Vis representative extraction and water quality index
Spectral analysis is used to find the periodicity contained in a time series. For this, DFT was selected to go from time domain to frequency domain. This approach converts a finite number of equally spaced samples into multiple coefficients of a finite combination of frequency-ordered complex sinusoids (components) with values of the same number of samples (Proakis &Manolakis, 2007). DFT coefficients were extracted from each UV-Vis spectrum. For the spectrum shown in Fig. 5, the coefficient values from a1 to a10 are shown in the graph. The most representative curves were a1 and a3, which decreased sequentially with time.
To compare the correlation between the actual organic matter water quality index and the DFT coefficients a1 to a10, Pearson's product-moment correlation (Correlation) and Root Mean Square Slope (RSQ) index were used in Fig. 6 and Fig. 7. Among organic material indicators, the correlation was highest in the order to express CODMn, TOC, and CODCr values. In particular, the correlation between CODMn and a3 was the highest (correlation function = 0.694, RSQ = 0.482).
CODMn and coefficients correlation shows that there are a3, a6, a8, a10 specifically higher values. Summary of UV 254-Abs absorbance values (UV254-Abs) of UV-VIS indicators and the smallest values from 186.232 to 667.856 nm. Moreover, the sum of UV254-Abs and UV-Abs for CODCr and TOC, 0.694 more than the sum of UV254-Abs and UV-Abs, and a8 values are showing 0.688, 0.652, and 0.572 accordingly.
The effects of different practices on the UV–Vis absorption spectrum of CODMn in different regression Curve are presented in Fig. 8. Linear regression analysis was performed for the data with the absolute value (UV254-Abs, Fig. 8a) and, sum of all data (Sum of UV-Abs, Fig. 8b) was used to normalize the data before performing linear regression analysis. According to the results of UV-DFT correlation analysis (Fig. 8), it was found that the correlations between UV254-Abs, CODMn and UV-FT, CODMn spectral parameters were used to determine the organic contents in wastewater. Due to the large variation in organic content in anaerobic digestion tank effluent different field experimental treatments, both the individual correlations of each treatment and the overall correlations were investigated. Due to the large variation in organic content in anaerobic digestion tank effluent different field experimental treatments, both the individual correlations of different 4 samples and the overall correlations were investigated. From the overall regressions, the determination coefficient (R2) was determined and the value of 3rd coefficients was most fitted to the CODMn among the other cases.