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 …

This work reviews the use of heat as a tracer of shallow groundwater movement and
describes current temperature‐based approaches for estimating streambed water …

Understanding groundwater recharge is essential for successful management of water
resources and modeling fluid and contaminant transport within the subsurface. This book …

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 dynamic distribution of thermal conditions present in saturated near-surface sediments
have been widely utilised to quantify the flow of water. A rapidly increasing number of …

Heat is a useful tracer for quantifying groundwater–surface water interaction, but analyzing
large amounts of raw thermal data has many challenges. We present a computer program …

Over the past few decades, groundwater has become an essential commodity owing to
increased demand as a result of growing population, industrialization, urbanization and so …

Vertical temperature profiling in the river beds of losing streams has been shown to be
useful in obtaining seepage rates. We present a method for high-resolution vertical …

Chlorinated ethenes (CEs) are legacy contaminants whose chemical footprint is expected to
persist in aquifers around the world for many decades to come. These organohalides have …

Denitrification is the main process removing nitrate in river drainage basins and buffer input
from agricultural land and limits aquatic ecosystem pollution. However, the identification of …