Springs sustain groundwater-dependent ecosystems and provide freshwater for human use.
Springs often occur because faults modify groundwater flow pathways leading to discharge …

Groundwater flow depends on the heterogeneity of hydraulic properties whose field
characterization is challenging. Recently developed active‐Distributed Temperature …

Thermodynamic coupling between atmosphere and ground yields increasing aquifer
temperatures as a consequence of global warming. While this is expected to manifest as a …

Aquifers contain the largest store of unfrozen freshwater, making groundwater critical for life
on Earth. Surprisingly little is known about how groundwater responds to surface warming …

Active distributed temperature sensing (ADTS) experiments are very useful to provide in‐situ
and distributed estimates of thermal conductivities of the subsurface and of groundwater …

When modelling heat transport in hydrogeological systems, a standard assumption is local
thermal equilibrium (LTE), which implies that the porous medium temperature at the …

Heat as a tracer in fractured porous aquifers is more sensitive to fracture‐matrix processes
than a solute tracer. Temperature evolution as a function of time can be used to differentiate …

Accurate SGD (submarine groundwater discharge) mass export calculations require
detailed knowledge of the spatial and temporal variability in SGD rates. In coastal aquifers …

This study introduces a novel heat tracing method for estimating lateral groundwater flow
velocity induced and sustained by heavy rainfall events in lowland areas, leveraging the …

Heat as a groundwater tracer has potential application in identifying earthquake-induced
changes in fluid flow. Since convective heat transport modifies the phase and amplitude of …