Lithium isotope ratios (δ7Li) of rivers are increasingly serving as a diagnostic of the balance
between chemical and physical weathering contributions to overall landscape denudation …

The stable isotopes of lithium (Li) serve as a robust proxy of silicate weathering. The fate and
transport of these isotopes in the dissolved load of major rivers have been characterized to …

To investigate the impact of riverine discharge and weathering intensity on lithium isotopes
(δ 7 Li) in a mono-lithological terrain, this study examines the dissolved load and leached …

Antecedent hydrological conditions are recorded through the evolution of dissolved lithium
isotope signatures (δ 7 δ^7 Li) by juxtaposing two storm events in an upland watershed …

Increasing global temperatures are causing widespread changes in the Arctic, including
permafrost thawing and altered freshwater inputs and trace metal and carbon fluxes into the …

Abstract To trace Critical Zone processes and to quantify Li fluxes from one Critical Zone
compartment into another, we investigated the Li concentration and isotopic composition (δ …

Lithium isotopes are used to trace weathering intensity, but little is known about the
processes that fractionate them in highly weathered settings, where secondary minerals play …

The Ganges river system is responsible for the transportation of a large flux of dissolved
materials derived from Himalayan weathering to the oceans. Silicate weathering-driven …

We illustrate two different, but complementary, applications of lithium (Li) isotope tracers for
river-basin characterization at two different scales within the Loire River basin (LRB) in …

Lithium (Li) isotopes are a promising tracer of chemical weathering processes for both
modern and ancient times. In order to improve the use of Li isotopes in the sedimentary …