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

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 …

Performance measures (PMs) and corresponding performance evaluation criteria (PEC) are
important aspects of calibrating and validating hydrologic and water quality models and …

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

Environmental sensor networks offer a powerful combination of distributed sensing capacity,
real‐time data visualization and analysis, and integration with adjacent networks and remote …

Two methods applying natural heat as a tracer to quantify surface water–groundwater
exchange were evaluated using field data. Arrays capable of monitoring and recording the …

More than 75 years after its introduction, the seepage meter remains the only device for
directly quantifying exchange across the sediment-water interface between 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 …

Concentrations of dissolved orthophosphate (ortho P) in the unsaturated zone, groundwater,
tile drains, and groundwater/stream water interfaces were assessed in five agricultural …

Understanding nutrient pathways to streams will improve nutrient management strategies
and estimates of the time lag between when changes in land use practices occur and when …