Hydrogen peroxide decomposition into oxygen in different soils: Kinetic analysis, mechanism and implication in catalyzed hydrogen peroxide propagations

Rapid hydrogen peroxide (H2O2) decomposition in soils is one of the most important barriers standing in front of catalyzed H2O2 propagations (CHP) for soil and groundwater remediation, and the rates depend greatly on soil components. However, there are lack of indicators to quantitatively evaluate the processes in various soils. Different from previous studies focusing on H2O2 decomposition, O-2 production kinetics are more valuable due to the direct relationship with H2O2 utilization. In this contribution, O-2 production during H2O2 decomposition in the soil slurry was in situ detected using a fiber-optic oxygen transmitter. A kinetic model of O-2 production was developed, which can be fitted well by the measured data of 18 soil samples. A kinetic constant on O-2 production (k(O2)) ranging from 0.001 min(-1) to 0.057 min(-1) was obtained from the model, which represents the diverse catalytic activity of the soils. The constant k(O2) is correlated with the contents of manganese, iron as well as inorganic carbon in the soils, and Mn mineral is the dominant factor. Three types of soils were selected to investigate the effect of acid-washing and stabilizer phosphate addition on phenol oxidation in CHP. Acid-washing can greatly suppress O-2 production, while phosphate addition is not desirable for the highly active soils. Phenol slightly inhibits O-2 production in the soils with higher k(O2) values, which are inverse with those of phenol degradation. Acid washing can remove Mn minerals but retain most of Fe components, and accordingly increase phenol degradation. Both hydroxyl radicals and superoxide radicals contribute to phenol degradation, and the latter ones display a more significant role. This work increases the understanding of the mechanism of H2O2 decomposition in the soils and provides a parameter (k(O2)) to guide CHP technologies in soil remediation. (C) 2021 Elsevier Ltd. All rights reserved.

Automated summary

Rapid hydrogen peroxide decomposition in soils poses a major obstacle to catalyzed H2O2 propagation for soil and groundwater remediation, and O-2 production kinetics are more valuable for evaluating H2O2 utilization. The kinetic constant of O-2 production (k(O2)) in soils is correlated with the contents of manganese, iron, and inorganic carbon, with manganese mineral being the dominant factor. Acid-washing can suppress O-2 production, while phosphate addition is not ideal for highly active soils.