Driven by the need for integrated management of groundwater (GW) and surface water
(SW), quantification of GW–SW interactions and associated contaminant transport has …

Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

This text combines the science and engineering of hydrogeology in an accessible,
innovative style. As well as providing physical descriptions and characterisations of …

The conversion from conventional tillage (CT) to no-tillage (NT) of the soil is often suggested
for positive long-term effects on several physical and hydraulic soil properties. In fact …

River water temperature measurement networks suffer from an inadequate spatial coverage
and a lack of data. No methods exist for the regional estimation of river water temperature at …

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

Groundwater seepage influences the temperature of streams and rivers by providing a
relatively cool input in summer and warm input in winter. Because of this, groundwater …

Using heat as a tracer to estimate the vertical streambed fluxes (VSFs) and sediment thermal
properties, the choice of mathematical models of heat transport is critical for the accuracy of …

This article reviews scientific studies in which heat was used as a natural tracer to
investigate stream–aquifer interactions in the Silala River in Chile and provide evidence that …

As a natural tracer, heat has some remarkable advantages over competing test methods and
has become a popular and widely used tool for quantifying streambed fluxes. In recent …