Vanadium (V) is a highly toxic multivalent, redox-sensitive element. It is widely distributed in
the environment and employed in various industrial applications. Interactions between V …

Terrestrial enhanced rock weathering (ERW) is a carbon dioxide removal technology that
aims at accelerating one of the most powerful negative feedbacks on Earth's climate, the …

Recent studies have shown that the rare earth elements and yttrium (REY)-rich deep-sea
sediments often contain abundant phillipsite, which is considered as an indicator mineral for …

The transition from mafic to felsic upper continental crust (UCC) is crucial to habitability of
Earth, and may be related to the onset of plate tectonics. Thus, defining when this crustal …

Early animals experienced multiple-phase radiations and extinctions from the late Ediacaran
to early Cambrian. Oxygen likely played an important role in these evolutionary events, but …

Sorption of oxyanions, such as pentavalent vanadium (V (V)), by reactive, poorly crystallized
clay minerals and Fe-(hydr) oxides surfaces significantly contributes to the nutrient and …

Soil is one of the largest reservoirs and re-emission sources of mercury (Hg) on Earth's
surface. The accumulation and remobilization of Hg during pedogenesis affect how Hg is …

Stable Nd isotope ratio is a potentially useful tool to provide new constraints on the
geological reservoir formation processes, complementing information from the radiogenic …

This study explored the mechanism of antimony (Sb) isotopic fractionation during chemical
weathering and soil biogeochemical processes, which have important implications for Sb …

Nickel isotope fractionation during continental weathering is not well constrained due to the
limited research on Ni isotopes during weathering of mafic rocks such as basalt. This study …