Iron (Fe) oxides can rapidly recrystallize in the presence of aqueous Fe (II)(Fe (II) aq) under
anoxic conditions. Since different Fe oxides have diverse affinities and redox reactivities for …

The incorporation of secondary metal atoms into iron oxyhydroxides may regulate the
surface chemistry of mediating electron transfer (ET) and, therefore, the biogeochemical …

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 …

Iron (Fe)(oxyhydr) oxides, which are among the most reactive iron-bearing minerals
commonly found in nature, are enriched in various dopants, such as aluminum (Al). This …

Ferrihydrite (Fhy) is the initial Fe-oxyhydroxide in supergene soils, and its structural
instability is affected by many environmental factors. However, little attention has been paid …

The presence of ferrous minerals has been demonstrated to have a significant impact on the
destiny, migration, and availability of uranyl (U (VI)) in natural surroundings. The iron …

Interfacial reactions between iron (Fe)(hydr) oxide surfaces and the activity of bacteria
during dissimilatory Fe reduction affect extracellular electron transfer. The presence of …

Cadmium sulfide nanoparticles (CdS-NPs) can be formed prevalently in the environment via
microbial transformation of anthropogenic Cd (II). The behavior of CdS-NPs in various …

Coexistence of crystals with multiple facets on an individual particle or different crystals is
prevalent in real environments. However, the reduction efficiency of individual crystal facets …

摘要赤铁矿(α-Fe2O3) 是热力学最稳定的氧化铁矿物, 广泛存在于土壤和沉积物中,
并在元素的生物地球化学循环中发挥重要作用. 天然赤铁矿颗粒由于形成条件的差异而具有不同 …