Acid solutions of the herbicide 2-(2,
4-
dichlorophenoxy)propionic
acid (2,
4-DP) of pH 3.0 at 25.0°C have been treated with ozone and ozonation catalyzed with Fe
2+, Cu
2+ and/or UVA light. This herbicide is slowly degraded by ozonation alone, while its destruction is enhanced under UVA irradiation. In the presence of Fe
2+, the initial mineralization rate is accelerated due to the generation of oxidizing hydroxyl radical (OH
), but a large proportion of stable products are formed. These species are partially removed when Fe
2+ and UVA light are combined, since greater amounts of OH
are produced and Fe
3+ complexes are photodecomposed. Addition of Cu
2+ to this system does not significantly improve its oxidizing ability, since the Cu
2+/Cu
+ pair gives a low additional OH
concentration. The herbicide decay always follows a pseudo first-order reaction. 2,
4-Dichlorophenol, chlorohydroquinone and chloro-
p-benzoquinone are detected as aromatic intermediates by reversed-phase chromatography. The initial chlorine is always transformed into chloride ion. Ion-exclusion chromatography allows the quantification of generated carboxylic
acids such as lactic, pyruvic, maleic, fumaric, oxalic and
acetic. These
acids are completely removed, except the two latter ones. Acetic
acid remains stable in all cases. Oxalic
acid is stable in the O
3 system, being partially mineralized to CO
2 by the O
3/UVA one. It also yields stable Fe
3+-oxalato complexes in the O
3/Fe
2+ system, which are rapidly photodecarboxylated in the O
3/Fe
2+/UVA and O
3/Fe
2+ + Cu
2+/UVA methods. Cu
2+-oxalato complexes also formed in the latter procedure are slowly mineralized with OH
. A possible reaction sequence for 2,
4-DP degradation involving all intermediates detected is proposed.