Fifty years of hyporheic zone research have shown the important role played by the
hyporheic zone as an interface between groundwater and surface waters. However, it is only …

Karst aquifers, capable of storing and transmitting large amount of water, are the main
source of drinking water in many regions worldwide. Their excessive permeability leads to …

Groundwater is important for energy and food security, human health and ecosystems. The
time since groundwater was recharged—or groundwater age—can be important for diverse …

Interaction between groundwater and surface water in watersheds has significant impacts
on water management and water rights, nutrient loading from aquifers to streams, and in …

Groundwater level fluctuations are one of the main components of the hydrogeological cycle
and one of the required variables for many water resources operation models. The …

Develo** an understanding of how groundwater (GW) and surface water (SW) systems
function and interact to impact water quantity, water quality, and ecosystem health provides …

The interaction between surface water and groundwater is crucial for the management of
water resources and the preservation of ecosystems within arid basins, but knowledge on …

The hyporheic zone, defined by shallow subsurface pathways through river beds and banks
beginning and ending at the river, is an integral and unique component of fluvial systems. It …

The analysis of the impact of climate change on water resources in plains requires integral
simulation tools that quantify topographic complexity and the strong interaction of …

Lake eutrophication is a large and growing problem in many parts of the world, commonly
due to anthropogenic sources of nutrients. Improved quantification of nutrient inputs is …