Groundwater extraction is increasing rapidly in many areas of the world, causing serious
impacts such as falling water tables, ground surface subsidence, water quality degradation …

Quantitative evaluation of earthquake‐induced permeability changes is important for
understanding key geological processes, such as advective transport of heat and solute and …

Non-perennial rivers and streams make up over half the global river network and are
becoming more widespread. Transitions from perennial to non-perennial flow are a …

The major driver of water-level changes in many heavily stressed aquifers is irrigation
pumping, which is primarily a function of meteorological conditions (precipitation and …

Hydraulic head and gradient measurements underpin practically all investigations in
hydrogeology. There is sufficient information in the literature to suggest that head …

Effective management of groundwater resources requires accurate estimates of aquifer
hydraulic parameters. One approach for estimating these parameters is to use aquifer water …

Water level changes in wells provide a direct measure of the impact of groundwater
development at a scale of relevance for management activities. Important information about …

Laboratory tests are commonly used to determine properties (vertical compressibility, α;
specific storage, SS; and vertical hydraulic conductivity, Kv) of claystone aquitards; however …

Aquifers supporting irrigated agriculture are under stress worldwide as a result of large
pumping‐induced water deficits. To aid in the formulation of more sustainable management …

Groundwater responses to barometric pressure fluctuations are characterized using the
concept of barometric efficiency (BE). For semiconfined and confined aquifers, BE values …