Processes that drive variability in catchment solute sourcing, transformation, and transport
can be investigated using concentration–discharge (C–Q) relationships. These relationships …

How does climate control river chemistry? Existing literature has examined extensively the
response of river chemistry to short‐term weather conditions from event to seasonal scales …

Watersheds have served as one of our most basic units of organization in hydrology for over
300 years (Dooge, 1988, https://doi. org/10.1080/02626668809491223; McDonnell, 2017 …

Solutes in rivers often come from multiple sources, notably precipitation (above) and
generation from the subsurface (below). The question of which source is more influential in …

The negative feedback between chemical weathering and climate is hypothesized to act as
an important control on modulating atmospheric CO2 over geologic timescales, affecting the …

Critical zone influences on hydrologic partitioning, subsurface flow paths and reactions
along these flow paths dictate the timing and magnitude of groundwater and solute flux to …

Dissolved organic carbon (DOC) and nitrogen (DON) are important energy and nutrient
sources for aquatic ecosystems. In many northern temperate, freshwater systems DOC has …

High‐frequency in situ sensors have enabled researchers to measure solute concentrations
at a time scale that captures the variability in stream discharge. We analyzed discrete …

It has long been recognized that the advent of vascular plants in the Paleozoic must have
changed silicate weathering and fundamentally altered the long-term carbon cycle. Carbon …

How does hillslope structure (eg, hillslope shape and permeability variation) regulate its
hydro‐geochemical functioning (flow paths, solute export, chemical weathering)? Numerical …