Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Over the past several decades, hydrologic models have advanced from independent models
of the surface and subsurface to integrated models that can capture the terrestrial hydrologic …

Abstract Concentration‐discharge (C‐Q) relationships are frequently used to understand the
controls on material export from watersheds. These analyses often use a log‐log power‐law …

Riverine discharge (Q) and dissolved concentrations (C) dictate solute mass export from
watersheds. Commonly Q is tracked at a much higher frequency than C for most major …

Long-term relationships between stream chemistry and discharge are regulated by
watershed subsurface structure and biogeochemical functioning. The extent to which these …

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 …

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 …

We provide a new generalized framework accounting for the effects of water and nutrient
uptake by roots in the weathering zone on broad patterns of solute concentration-discharge …

Abstract Concentration-isotope Ratio-Discharge (CRQ) relationships offer a promising
means of disentangling the underlying hydrologic, geochemical, and ecological factors that …

Land use changes are known to alter terrestrial silicon cycling and the export of dissolved
silicon from soil to fluvial systems, but the impact of such changes on groundwater systems …