3.3. Effect of Inorganic Anion Content on Herbicide Photodegradation Using Na2S2O8/UV
The composition of the water on the photodegradation process is critical to the assessment of its suitability for real wastewater treatment, and its impact can be complex in some cases. In addition to dissolved organic matter, the unfavorable effects of some inorganic ions (mainly anions) such as Cl
-, HCO
3-/CO
32-, NO
3-/NO
2-, PO
4H
3- and/or SO
42-, among others can be explained by the fact that they reduce the oxidising power of the solution. The scavenging of HO
• and SO
4•- by various anions generates the corresponding radicals such as ClOH
•−, Cl
•, Cl
2•−, CO
3•−, HCO
3•, Br
•, Br
2•−, NO
•, and/or H
2PO
4•, which have a lower
E0 than HO
• and SO
4•- or by promoting the formation of ROS, as in the case of NO
3−, which is capable of generating HO
• and NO
2• radical species, which promote the photodegradation of pesticides, especially those for which indirect photolysis is the main reaction pathway [
28,
38,
44]. Some anions and cations present in water are transparent to solar radiation, while nitrate (λ = 303 nm) and nitrite (λ = 355 nm) show some adsorption. Both absorb light and undergo homolysis to form HO
• and nitrogen reactive species such as NO
•, NO
2•, N
2O
3, and/or N
2O
4 such as leading to the herbicide degradation, although HO
•can be further scavenged by NO
2- to form NO
2• [
45]. However, the concentrations of NO
3-/NO
2 in real wastewater is usually low (< 5 mg L
-1). For this reason, we have assessed the influence of SO
42-, Cl
- and HCO
3-, which are present at much higher concentrations.
As shown in
Figure 3, the removal efficiency of the herbicides was not affected by the presence of sulphate at the concentration studied. Even, the presence of SO
42- in the solution (test 7) has a positive effect on the photodegradation of both herbicides, especially for ISP, because higher values of
k were obtained according to the results shown in
Table 4. SO
4= is not a strong scavenger of HO
• such as Cl
-, HCO
3- and CO
32-. On the contrary, it has been shown to promote the oxidative degradation of the antibiotics chloramphenicol [
46] and ciprofloxacin [
47] or polyvinyl alcohol [
42], as occurs in our case. According to Cabrera-Reina et al. [
48], the removal efficiency of acetamiprid, carbamazepine and caffeine was also unaffected by sulphate concentration in the range 0-550 mg L
-1. Therefore, sulphate impact on activated PS processes, summarized in Equation 13-14, is very low.
Chloride ion (Cl
−) is one of major inorganic anions in natural water. The adverse effect of Cl
−, especially at high concentration on the degradation of many organic micropollutants has been reported by some authors [
28]. In the case of ISP, a minimal influence was observed when chloride ions (150 mg L
-1) are present in the solution because k
PS/K
PS/Cl is 0.98 (
Table 4). However, a significant influence was observed for TBZ where the ratio k
PS/K
PS/Cl was 4.1 as can be seen in
Figure 3. The adverse effects of high Cl
− concentrations could favour the scavenging of HO
• and SO
4•− according to the following reactions (Equation 15-18):
Compared to HO
•-based AOPs, radical scavenging by Cl
- in SO
4•--based AOPs is a major challenge. The reaction between Cl
- and HO
• gives ClOH
•- (Equation 16), but this is a reversible reaction that mostly returns to HO
• [
49]. In contrast, SO
4•- produces Cl
• (
E0 = 2.4 V) by one-electron abstraction from Cl
- (Equation 15), which is often reflected in lower efficiencies in organic pollutant removal as well as higher generation of reactive chlorine species such as Cl
2•- (
E0 = 2.1 V), ClO
2• (
E0 = 0.9 V), (ClO
• E0 = 1.4 V) and ClOH
•- (
E0 = 1.9) V, all of them with lower
E0 than HO
• and SO
4•- [
50].
An overall negative effect of HCO
3- and CO
32- anions on the SO
4•--based AOPs has traditionally been assumed [
51]. The alkalinity of a water body is mainly contributed by CO
32-and HCO
3- ions, which are generally present in natural waters ranging from 50-250 mg L
-1. Both CO
32-and HCO
3- are known to be radical scavengers in AOPs [
28]. Among them, the radical scavenging ability of CO
32- is stronger than that of HCO
3- due to its higher reaction rate constant with OH
• (3.9 × 10
8 M
-1 s
-1 vs 8.5 × 10
6 M
-1 s
-1) [
52].
However, depending on the chemical structure of the pesticides, the HCO
3-/CO
32 effect will be neutral, positive or negative for their degradation rate, which makes it very difficult to predict due to the complex mixtures of pollutants always present in wastewater [
53,
54]. Although CO
3•- have low redox potential than HO
•, it could exhibit better removal performing in degrading organic micropollutants, which could be due to its high selectivity and longer survival time in solution [
55].
When HCO
3- was added, the initial pH of the aqueous solution changed to about 8.3, rather than pH 6.7 without the addition of any anions, and the basic conditions reduced the efficiency of degradation of both herbicides, as discussed by some authors [
56]. CO
2, CO
32- and HCO
3- are present in aqueous media at pH > 4. CO
32- and HCO
3-, responsible of water alkalinity, can compete with herbicides for HO
• and SO
4•- to generate other weaker radicals, such as CO
3•- and/or HCO
3•. Above pH = 10.3, CO
32- is the prevalent specie, but at pH below 8.3 all CO
32- has been converted to HCO
3- [
57]. As pH decreases, HCO
3- also decreases and dissolved CO
2 increases (
Figure 4). The relationship between CO
32-/HCO
3- and solution pH is represented as follows (Equation 19):
The high concentration (125 mg L
-1) of HCO
3- strongly scavenges HO
• and SO
4•-, generating electrophilic CO
3•-, a more selective and less reactive reaction radical with a lower electrode potential (
E0 = 1.6 V) than HO
• and SO
4 [
58]. Detailed reaction mechanisms between CO
3•- and micropollutants are still largely unclear. In previous studies, the single electron transfer was determined to be the dominant pathway [
52]. The nature of CO
3•- makes it more selective towards electron-rich moieties such as such as -NH
2, -OH and aromatic rings. HCO
3• has lower reaction rate with organic pollutants than HO
•. For SO
4•-, it has lower reaction rate with CO
32- (6.1 × 10
6 M
-1 s
-1) and similar reaction rate with CO
32- (9.1 × 10
6 M
-1 s
-1) compared to HO
• [
59]. Nevertheless, the presence of CO
32-/HCO
3- can cause the transformation of HO
• and SO
4•-, which can further affect the performance of AOPs. In radical-based treatment processes, CO
3•- and HCO
3• can be formed by oxidation of CO
32- and HCO
3- with highly reactive radical species, such as HO
• and SO
4•- (Equation 20-23) [
60]:
In addition, the carbonate precipitation can result in fouling on the membrane surface, which further affects the removal efficiency of micropollutants [
61].
After studying the individual effects of SO
4=, Cl
- and HCO
3- on the UV/PS process, their combined effect was then assessed (test 10). The
Rr of both herbicides is presented in
Figure 3. As can be seen, Cl
- (150 mg L
-1) and HCO
3- (125 mg L
-1) generally had a negative effect on herbicide
Rr, although the magnitude depended on the chemical structure of each herbicide. As can be observed in
Table 4 the R values ranged from 0.976 to 0.996 for TBZ and 0.988 to 0.998 for ISP, with standard errors of estimation less than 0.08 and 0.05, respectively, indicating good fit. The time to 50% disappearance (DT
50) for ISP was slightly higher in the presence of anions (8.2 min) than in the corresponding experiment carried out in the absence of anions (5.5 min). However, a substantial effect was observed for TBZ, as the DT
50 was approximately 23 times higher than in the absence of anions, mainly due to the impact of HCO
3-.
The initial pH of the aqueous solution of herbicides in absence/presence of inorganic anions decreased in all cases during the photoperiod (
Table 5). The acidification may be caused by the formation of acidic products as consequence of the herbicide degradation, and acidic photoproducts derived from S
2O
8=, such as HSO
4−, with release of H
+ (Equation 24, 25) as reported by Yang et al. [
28]:
In addition, the concentration of SO
42- increased significantly throughout the process (Equation 25), as can be seen from the EC values shown in
Table 6, due to the transformation of the initially added S
2O
82- into SO
42. Various methods have been proposed to remove SO
4= from water over the past decades, such as adsorption on activated carbon, neutralisation with calcium carbonate, biological treatment, reverse osmosis and dialysis, and ion exchange. The choice of wastewater treatment method is usually based on the type of wastewater, the removal rate, the waste concentration and the cost of treatment. Of these, adsorption on an ion exchange resin is the most popular method for removing SO
4= from water and wastewater and shows good potential for industrial wastewater treatment [
62].
Figure 5 shows the evolution of DOC during the different tests carried out. It is important to monitor the process using this tool because only DOC values close to zero guarantee that recalcitrant pollutants or intermediates with greater persistence and toxicity than the initial ones do not persist. In the absence of any ions (test 5) and in the presence of SO
4= (test 7) a high mineralisation rate was observed because the remaining DOC after 120 min was less than 5%. However, in the presence of HCO
3- (test 8) and Cl
- (test 9), the residual DOC concentration after 120 min was 20% and 10% respectively, while in the presence of all anions in the reaction solution (test 10), the residual DOC concentration at the end of the experiment was significantly increased (37%). These residual DOC fraction may be due to the partial removal of herbicides in aqueous solution and the formation of non-degradable organic intermediates produced during the irradiation time.