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 …

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 as a tracer has received increasing attention in recent decades and has become a
popular and widely used tool for quantifying streambed fluxes, among many other …

Coupled groundwater flow and heat transport within hyporheic zones extensively affect
water, energy, and solute exchange with surrounding sediments. The local and cumulative …

Analytical modelling of heat transport was used to address effects of uncertainty in thermal
conductivity on groundwater–surface water exchange. In situ thermal conductivities and …

Soil moisture and temperature are some of the most important controls for a wide variety of
geochemical and ecological processes in the vadose zone (VZ). Soil moisture is highly …

We introduce LPMLE3, a new 1‐D approach to quantify vertical water flow components at
streambeds using temperature data collected in different depths. LPMLE3 solves the partial …

Amplitude decay and phase delay of oscillating temperature records measured at two
vertical locations in near‐surface sediments can be used to infer water fluxes, thermal …

The application of heat as a hydrological tracer has become a standard method for
quantifying water fluxes between groundwater and surface water. The typical application is …

Interaction between surface water and groundwater plays a fundamental role in influencing
aquatic chemistry, where hyporheic exchange processes, distribution of flow paths and …