The confined type lies completely within the vadose zone, and their yield per unit decline in hydraulic head is known as "storativity."
In certain situations, the Ergun and Forchheimer expressions effectively model these entities, and the Richards equation can model transport within them. The confined type lies completely within the vadose zone, and their yield per unit decline in hydraulic head is known as "storativity." Sodium intrusion is a common problem in these entities if they are located in coastal areas. Massive examples in the U.S. include the Mahomet and the Ogallala ones, and when these entities meet the surface, artesian wells form. For 10 points, name these porous rocks that contain underground water reservoirs.
In certain situations, the Ergun and Forchheimer expressions effectively model these entities, and the Richards equation can model transport within them.
aquifers