Fifty years of hyporheic zone research have shown the important role played by the
hyporheic zone as an interface between groundwater and surface waters. However, it is only …

Fine sediment represents an important part of the solid flux of rivers. Due to the size of these
particles, they are often transported as suspended load. They gradually fill the pores of the …

In this chapter, the authors provide a comprehensive analysis and synthesis of the
interactions between important drivers and controls of hyporheic exchange and …

The interface between groundwater and surface water within riverine/riparian ecosystems—
the hyporheic zone (HZ)—is experiencing a rapid growth of research interest from a range of …

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 hyporheic zone is an ecotone connecting the stream and groundwater ecosystem that
plays a significant role for stream biogeochemistry. Water exchange across the stream …

The irregular planform morphology of rivers leads to formation of hyporheic zones along its
banks. This study investigates how hyporheic exchange in stream banks, whose planform is …

The dynamics of chemicals within a catchment are strongly affected by the exchange
between surface water and groundwater. The activity of hyporheic microorganisms plays a …

To understand how redox processes influence carbon, nitrogen, and iron cycling within the
intrameander hyporheic zone, we developed a biotic and abiotic reaction network and …

The parallel physically-based surface–subsurface model PARFLOW was used to investigate
the spatial patterns and temporal dynamics of river–aquifer exchange in a heterogeneous …