The use of assemblage models to describe trace element partitioning, speciation, and fate: a review
The fate of trace elements in soils, sediments, and surface waters is largely determined by
their binding to reactive components, of which organic matter, metal oxides, and clays are …
their binding to reactive components, of which organic matter, metal oxides, and clays are …
Transformation of two-line ferrihydrite to goethite and hematite as a function of pH and temperature
S Das, MJ Hendry… - Environmental science & …, 2011 - ACS Publications
Under oxic aqueous conditions, two-line ferrihydrite gradually transforms to more
thermodynamically stable and more crystalline phases, such as goethite and hematite. This …
thermodynamically stable and more crystalline phases, such as goethite and hematite. This …
Quantitative contribution of oxygen vacancy defects to arsenate immobilization on hematite
J Liu, Y ** various simple adsorption isotherm models. However, though …
Immobilization of phosphorus in sediments by nano zero-valent iron (nZVI) from the view of mineral composition
Immobilization of phosphorus (P) in sediments is essential for controlling eutrophication in
natural waters. As sediment is a complex assemblages of minerals, it is necessary to explore …
natural waters. As sediment is a complex assemblages of minerals, it is necessary to explore …
The impact of aggregation between clay and phytoplanktonic cyanobacteria on trace elemental cycling in coastal environments
Clay minerals and cyanobacteria occur ubiquitously in nature, and both independently
influence trace metal cycling due to their high specific surface areas and reactivity. Although …
influence trace metal cycling due to their high specific surface areas and reactivity. Although …