Groundwater recharge (GWR) is a strategic hydrologic variable, and its estimate is
necessary to implement sustainable groundwater management. This is especially true in a …

Interactions between headwater aquifers and peatlands have received limited scientific
attention. Hydrological stresses, including those related to climate change, may adversely …

The interactions between precipitation, streamflow and groundwater are very complex. In
cold temperate regions characterized by harsh winters, winter streamflow is mainly derived …

Le bassin versant de la rivière Châteauguay couvre une partie du nord-ouest de l'état de
New York (USA) et du sud-ouest de la province de Québec. L'aquifère régional est présent …

The Lorraine Triassic Sandstone Aquifer (LTSA), which has already been the subject of a
chemical and radioisotopic study (1979), is used to investigate the impacts of 20a of large …

Groundwater discharge areas, including low-flow bedrock aquifer springs, are ecologically
important and can be impacted by climate change. The development of and results from a …

Groundwater contribution to river flows, generally called base flows, often accounts for a
significant proportion of total flow rate, especially during the dry season. The objective of this …

Pump tests and geophysical logs acquired in a fluvial sandstone aquifer within the resource-
rich Moncton Subbasin of New Brunswick, Canada, have been used to characterize fracture …

The problem of flow through heterogeneous confined aquifers of variable thickness is
analyzed from a stochastic point of view. The analysis is carried out on the basis of the …

Fracture lengths govern permeability and are unknowns in geothermal assessment. Along
their lengths, fracture widths vary due to growth by linkage. Under the influence of …