pH below optimum

Reference

pH above optimum

Reference

Scavenging of ŸOH by excess H+

[88]

Deficiency of H+, which hampers ŸOH formation

[59]

Formation of [Fe(H2O)]2+ which has low oxidative power

[89]

Decomposition of H2O2

[90]

Prevent the interaction between Fe3+ and H2O2

[91]

Decline in the oxidative power of ŸOH

[92]

H2O2 may be unstable to formed H 3 O 2 + which impedes production of ŸOH

[93]

Precipitation of Fe3+ as iron hydroxide

[60] [61]