Minerals and organic matter (OM) may form intricate associations via myriad interactions. In
soils, the associations of OM with mineral surfaces are mainly investigated because of their …

In the 1830s, iron bacteria were among the first groups of microbes to be recognized for
carrying out a fundamental geological process, namely the oxidation of iron. Due to lingering …

The association of organic matter (OM) with minerals is recognized as the most important
stabilization mechanism for soil organic matter. This study compared the properties of Fe …

Poorly crystalline Fe (III)(oxyhydr) oxides like ferrihydrite are abundant in soils and
sediments and are often associated with organic matter (OM) in the form of mineral-organic …

The Most Detailed Resource Available on Points of Zero ChargeWith their work growing in
complexity, chemists involved with surface phenomena-related projects have outgrown the …

Aqueous Fe (II) is known to catalyze the abiotic transformation of ferrihydrite to more stable
Fe minerals. However, little is known about the impacts of coprecipitated OM on Fe (II) …

Coprecipitation of Fe/Cr hydroxides with natural organic matter (NOM) is an important
pathway for Cr immobilization. However, the role of NOM in coprecipitation is still …

In soil and water, ferrihydrite frequently forms in the presence of dissolved organic matter.
This disturbs crystal growth and gives rise to coprecipitation of ferrihydrite and organic …

In soils and sediments ferrihydrite often precipitates from solutions containing dissolved
organic matter, which affects its crystallinity. To simulate this process we prepared a series of …

Ferric oxyhydroxides play an important role in controlling the bioavailability of oxyanions
such as arsenate and phosphate in soil. Despite this, little is known about the properties and …