Production of hydroxyl radicals (•OH) upon the oxidation of solid Fe(II) by O2 or H2O2 in soils and sediments has been confirmed, which benefits in situ remediation of contaminants. However, Fe(III) reduction by H2O2 is rate-limiting. Accelerating the Fe(III)/Fe(II) cycle could improve the efficiency of remediation. This study intended to use hydroxylamine to promote Fe(III)/Fe(II) cycle during 100g/L soil oxidation by H2O2 for phenol degradation. The removal of phenol was 76% in 3h during soil oxidation with 1mM H2O2 in the presence of 1mM hydroxylamine but was negligible in the absence of hydroxylamine. Fe(III) in the soil was reduced to 0.21mM Fe(II) by 1mM hydroxylamine in 30min. The accelerated cycle of Fe(III)/Fe(II) in the soil by hydroxylamine could effectively decompose H2O2 to produced •OH, which was responsible for the effective enhancement of phenol degradation during soil oxidation. Under the conditions of 1mM H2O2 and 100g/L soil, the pseudo-first-order kinetic constant of phenol degradation increased proportionally from 0.0453 to 0.0844min-1 with the increase of hydroxylamine concentrations from 0.5 to 1mM. The kinetic constant also increased from 0.0041 to 0.0111min-1 with H2O2 concentration increased from 0.5 to 2mM, while it decreased from 0.0100 to 0.0051min-1 with soil dosage increased from 20 to 200g/L. In addition, column experiments showed that phenol (10mg/L) degradation ratio kept at about 48.7% with feeding 2mM hydroxylamine and 2mM H2O2 at 0.025 PV/min. Column experiments suggested an optional application of hydroxylamine and H2O2 for in situ remediation. The output of this study provides guidance and optional strategies to enhance contaminant degradation during soil oxidation.