Groundwater recharge is difficult to estimate, especially in fractured aquifers, because of the
spatial variability of the soil properties and because of the lack of data at basin scale. A …

To supplement the use of hydraulic tests and assess catchment-scale hydraulic conductivity
(K), we propose a methodology for shallow aquifers only based on the Digital Elevation …

Streamwater transit time distributions display a variable proportion of old waters (≥ 1 year).
We hypothesize that the corresponding long transit times result from groundwater …

Nitrate contamination affects many of the Earth's aquifers and surface waters. Large-scale
predictions of groundwater nitrate trends normally require the characterization of multiple …

Groundwater flow at the hillslope scale is controlled by hydraulic properties and topography.
Geological media are inherently heterogeneous, with properties depending on both …

This study investigates the influence of topography on the desaturation rates of groundwater-
dependent wetlands in response to changes in recharge. We examined sixty catchments …

Groundwater recharge is difficult to estimate, especially in fractured aquifers, because of the
spatial variability of the soil properties and because of the lack of data at basin scale. A …

Abstract Strack's (1984, 2017) analysis of infiltration from a pond into a shallow aquifer, with
a generated groundwater mound, is modified for steady phreatic groundwater flows in …

Mountains, often referred to as the world's water towers, play a vital role in global water
distribution. They receive significant precipitations and redistribute these waters to lower …

The transit time distribution (TTD) of groundwater is the flow-weighted spectrum of
groundwater ages from recharge to discharge. Though society relies on water from large …