On the basis of the active species capture experiments and some previous studies [
9,
13,
21], a possible mechanism for radicals transfer routes according to the simultaneous effect of photocatalysis and PMS activation in BTA degradation was evaluated (
Scheme 1). The adsorbed light caused the excitation in the valence band (VB) of the catalyst, which could produce photo-induced electron and hole groups (e
‒/h
+) as Eq. (25) showed, with strong redox reaction ability. Conduction band electrons (e
CB‒) of CuFe
2O
4 could quickly reduce dissolved O
2 to O
2•‒ radicals (Eq. (26)) based on the standard redox potential difference (
E0eCB‒ = ˗0.48 eV vs. NHE compared to
E0O2/O2•‒ = ˗0.46 eV vs. NHE) [
21]. At the same time, h
+ directly entered in the catalytic degradation when adsorbed H
2O or OH
‒ were thermodynamically able to be converted to
•OH (Eq. 27), thereby establishing the photo-induced charges separation in CuFe
2O
4 [
41]. O
2•‒ could also trigger a series of redox reactions to produce
•OH (Eq. (28) and (29)) [
9].
Additionally, it was observed that PMS further enhanced the catalytic reaction that can be attributed to the chemical stability arising from redox cycles of surface active centers. It was concluded from evidences that the process of CuFe
2O
4 catalyzed PMS for generating reactive species was initially related to the binding of hydroxyl groups (−OH) obtained from the dissociation of water on the surface metal (Fe or Cu) sites in CuFe
2O
4 catalyst [
26]. In this regards, HSO
5‒ could form bond with the surface Cu(II) of the catalyst via surface −OH displacement and generate Cu(II)-(OH)OSO
3‒ intermediate by the inner-sphere complexation (Eq. (30)). Therefore, the favorability of the electron transfer from Cu(II), with the obtained high electron density, to OH of HSO
5‒ could lead to the production of SO
4•‒ radical directly and new surface −OH group which would bond to higher valence Cu(III) ion (Eq. (31)). Supposing that ≡Cu(III) −OH oxidized HSO
5‒ to SO
5•‒ bonded to copper initial valence (i.e., Cu(II)) (Eq. (32)), then the combination of surface SO
5•‒ moieties would again generate SO
4•‒ via Eq. (33). The efficient participation in redox process could result in the reductant character for Fe(II), reducing ≡Cu(III) to ≡Cu(II) (Eq. (34)), since
E0≡Cu(III)/≡Cu(II) = 2.3 V is much higher than
E0≡Fe(III)/≡Fe(II) = 0.77 V. The resulting ≡Fe(III) would be possibly turned to ≡Fe(II) during the process of HSO
5‒ reduction (Eq. (35)), which would be afterward oxidized to ≡Fe(III) by the production of SO
4•‒ radicals (Eq. (36)). Thus, redox mediators i.e., Cu(II-III-II) and Fe(III-II-III) by maintaining the reaction cycles not only enhance the activity of CuFe
2O
4 via Eq. (34), but also contribute to the further decomposition of PMS through Eqs. (35) and (36). From the hydrolization of SO
4•‒ •OH can be released, which further yielded following the interaction of OH
‒ (Eqs. (37) and (38)) [
42]. Photocatalytic activation of PMS, under the action of photoinduced electrons, opened another route for direct generation of
•OH and SO
4•‒ radicals (Eq. (39)). In this way, the photoinduced holes could be captured by PMS to produce SO
4•‒ via subsequent self-reaction of SO
5•‒ radicals (Eqs. (40) and (41)). On the other hand, photo-induced electrons under the different valence states of Cu-Fe during the reaction, could provide a new equilibrium to get the cyclic Cu(III)/Cu(II) and Fe(III)/Fe(II) (Eq. (42)), leading to the fast photo charge transfer in the presence of PMS and it would be the reason for higher reactivity than the binary systems i.e., CuFe
2O
4/UV and CuFe
2O
4/PMS (
Figure 3). Thus, PMS oxidation when combined with photocatalysis was synergistic with the production of more free active species. Negligible amount of SO
4•‒,
•OH, O
2•‒, and h
+ radicals, which might be leached from the surface bound layer to the solution bulk in the CuFe
2O
4/UV/PMS system, had key role in mineralization of BTA (Eq. (43)).