The magnesium isotopic composition (δ 26 Mg) of river water could provide evidence for
continental weathering and the global Mg cycle. However, constraining the lithological and …

Magnesium isotope behavior in dissolution and precipitation reactions during chemical
weathering have been well documented. However, mechanisms of mineral dissolution and …

Magnesium isotopic composition (δ 26 Mg) could constrain sources and processes of
riverine Mg, thus providing new perspectives on budgeting the global Mg cycle. Carbonate …

Mg isotopic composition of river water is dominantly controlled by the dissolution of both
silicate and carbonate sources and a series of biogeochemical processes. However, the …

The magnesium isotopic composition (δ 26 Mg) of river water is a promising indicator of
continental chemical weathering. While many studies have investigated the factors that …

The magnesium (Mg) isotopic composition of river waters is mainly controlled by riverine Mg
sources and geochemical processes. It is meaningful to characterize Mg isotope behavior …

In recent years, a series of important progresses have been made in the aspect of
magnesium isotopes behavior in weathering processes. These progresses are not only …

Carbonate weathering plays a significant role in regulating global carbon budget at short
time scales, and thus needs to be better constrained in the context of global warming …

In order to better understand how stable metal isotope signals in large rivers can be used to
constrain present and past weathering, the seasonal riverine Mgsingle bond Sr isotopic …

Carbonate weathering regulates the short-term carbon (C) cycle and global climate due to
its fast response to hydrological processes. The carbonate weathering flux needs to be well …