Studies of the oxidative degradation of picric acid (2,4,6trinitrophenol) by H 2 O 2 catalyzed by a fluorine-tailed tetraamido macrocyclic ligand (TAML) activator of peroxides [Fe III {4,5-Cl 2 C 6 H 2 -1,2-(NCOCMe 2 NCO) 2 CF 2 }(OH 2 )] − (2) in neutral and mildly basic solutions revealed that oxidative degradation of this explosive demands components of phosphate or carbonate buffers and is not oxidized in their absence. The TAML-and buffer-catalyzed oxidation is subject to severe substrate inhibition, which results in at least 1000-fold retardation of the interaction between the iron(III) resting state of 2 and H 2 O 2 . The inhibition accounts for a unique pH profile for the TAML catalysis with the highest activity at pH 7. Less aggressive TAMLs such as [Fe III {C 6 H 4 -1,2-(NCOCMe 2 NCO) 2 CMe 2 }(OH 2 )] − are catalytically inactive. The roles of buffer components in modulating catalysis have been clarified through detailed kinetic investigations of the degradation process, which is first order in the concentration of 2 and shows ascending hyperbolic dependencies in the concentrations of all three participants, i.e., H 2 O 2 , picrate, and phosphate/carbonate. The reactivity trends are consistent with a mechanism involving the formation of double ([LFe III −Q] 2− ) and triple ([LFe III −{Q−H 2 PO 4 }] 3− ) associates, which are unreactive and reactive toward H 2 O 2 , respectively. The binding of phosphate converts [LFe III −Q] 2− to the reactive triple associate. Density functional theory suggests that the stability of the double associate is achieved via both Fe−O phenol binding and π−π stacking. The triple associate is an outer-sphere complex where phosphate binding occurs noncovalently through hydrogen bonds. A linear free energy relationship analysis of the reactivity of the mono-, di-, and trinitro phenols suggests that the rate-limiting step involves an electron transfer from phenolate to an oxidized ironoxo intermediate, giving phenoxy radicals that undergo further rapid oxidation that lead to eventual mineralization.