The increased use of hydropower is currently driving the greatest surge in global dam
construction since the mid-20th century, meaning that most major rivers on Earth are now …

The hyporheic zone is the subsurface area below and adjacent to a stream where
groundwater mixes with stream water, through vertical, lateral, and longitudinal flows. The …

Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic
zone is a ubiquitous, reactive interface between the main channel and its surrounding …

Increased loading of nitrogen (N) and phosphorus (P) from agricultural and urban
intensification has led to severe degradation of inland and coastal waters. Lakes, reservoirs …

The hyporheic zone, defined by shallow subsurface pathways through river beds and banks
beginning and ending at the river, is an integral and unique component of fluvial systems. It …

The use of smart tracers to study hydrologic systems is becoming more widespread. Smart
tracers are compounds that irreversibly react in the presence of a process or condition under …

Streams and rivers play a major role in the global carbon cycle as they collect, transform and
deliver terrestrial organic carbon to the ocean. The rate of dissolved organic carbon (DOC) …

Rivers display essential role in nitrogen (N) cycling in terrestrial and aquatic ecosystems, but
now they are suffering from damming worldwide, especially from cascade damming. Despite …

Decades of agricultural intensification have led to elevated stream nitrogen (N)
concentrations and eutrophication of inland and coastal waters. Despite widespread …

Transient storage (TS) zones are important areas of dissolved inorganic nitrogen (DIN)
processing in rivers. We assessed sensitivities regarding the relative impact that the main …