Iron (Fe) is the fourth most abundant element in the earth's crust and plays important roles in
both biological and chemical processes. The redox reactivity of various Fe (II) forms has …

Interfacial reactions drive all elemental cycling on Earth and play pivotal roles in human
activities such as agriculture, water purification, energy production and storage …

Sulfate radical-based advanced oxidation processes (AOPs) have drawn increasing
attention during the past two decades, and Mn-based materials have been proven to be …

The utilization of persulfate-based advanced oxidation processes (PS-AOPs) in the
presence of nanomaterials has gained increased attention for the degradation of organic …

Fe (II) redox chemistry is a pivotal process of biogeochemical Fe cycle and the
transformation of organic pollutants in subsurface aquifers, while its interfacial reactivity on …

Interactions between aqueous Fe (II) and solid Fe (III) oxy (hydr) oxide surfaces play
determining roles in the fate of organic contaminants in nature. In this study, the adsorption …

Goethite is a commonly found iron (hydr) oxide in soils and sediments that has been proven
to possess abundant defects in structures. However, the underlying impact of these defects …

Abstract Conspectus: Redox reactions of Fe-and Mn-oxides play important roles in the fate
and transformation of many contaminants in natural environments. Due to experimental and …

The interfacial electron transfer on iron (Fe) minerals with electron shuttles may play a great
significance to the fate of pollutants in soils, while the exact surface chemistry is barely …

Predicting the redox behavior of organic contaminants and heavy metals in soils is
challenging because there are few soil redox potential (E h) models. In particular, current …