Rare earth elements (REE), essential metals for the transition to a zero-emission economy,
are mostly extracted from REE-fluorcarbonate minerals in deposits associated with …

The structure of the uranyl aqua ion (UO 2 2+) and a number of its inorganic complexes
(specifically, UO 2 C l+, UO 2 C l 2 0, UO 2 SO 4 0, UO 2 SO 4 2 2−, UO 2 CO 3 3 4− and UO …

Abstract Knowledge of Sn (II) speciation in aqueous and gaseous phases and the
corresponding isotope effects are critical for understanding the transport and deposition of …

Molybdenum (Mo) is extracted predominantly from magmatic-hydrothermal ore deposits,
and knowledge of the thermodynamic properties of aqueous Mo complexes over a wide …

Rare earth element (REE) phosphates such as xenotime (YPO 4) are important hosts to the
heavy (H) REE in natural systems. Xenotime is commonly associated with hydrothermal …

Understanding the speciation and thermodynamic properties of aqueous tungsten (W)
complexes under various conditions is essential for predicting W transport in hydrothermal …

Abstract Knowledge of the chemical speciation of platinum and the solubility of Pt-bearing
minerals in hydrothermal fluids is required to assess Pt transport, remobilization and …

Surficial deposits in Namibia's Erongo district contain substantial but low-grade resources of
uranium and vanadium (nearly 500 Mlb U3O8), hosted in palaeochannels. This review …

We investigated the effective interaction potential (EIP) between charged surfaces in solvent
comprised of dipole dimer molecules added with a certain amount of ionic liquid. Using …

Chlorine is the most common ligand in geofluids, and one of the most important complexing
agents for rare earth elements. The geometry and thermodynamic properties of La (III)-Cl …