Agricultural and urban development alters nitrogen and other biogeochemical cycles in
rivers worldwide. Because such biogeochemical processes cannot be measured empirically …

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 …

Accurate modelling of constructed wetlands is vital for furthering the use of these systems.
Constructed wetlands can treat various types of wastewater, including domestic wastewater …

Determination of longitudinal dispersion coefficient (LDC) using artificial intelligence (AI)
techniques can improve environmental management strategies for river systems. However …

Hydrologic exchange fluxes (HEFs) vary significantly along river corridors due to
spatiotemporal changes in discharge and geomorphology. This variability results in the …

Space‐fractional advection‐dispersion models provide attractive alternatives to the classical
advection‐dispersion equation for model applications that exhibit early arrivals and plume …

Hyporheic and parafluvial flows between streams and the underlying streambed, or adjacent
alluvium, are important drivers of biogeochemical cycling in streams. Here we present a new …

Because pollutant dispersion in rivers is strongly influenced by the longitudinal dispersion
coefficient (K x), its accurate estimation is critical in the field of environmentally sound …

Large rivers are major conduits for sediment and nutrient transport and play an important
role in global biogeochemical cycles. While smaller rivers received attention in recent …

Dispersion model is an important tool for decision makers to accurately assess risks and
effectively plan countermeasures during river pollution accidents, but their applications …