Definitions Flashcards
Subsurface Water
all water occurring beneath the Earth’s surface
Groundwater
the subsurface water that occurs beneath the water table in soils and geological formations that are fully saturated
Unsaturated Zone/Vadose Zone
the zone above the water table where pore water pressure is less than atmospheric (due to capillary forces)
Capillary Fringe
saturated zone that sits above the water table in the vadose zone. Water is held in the capillary fringe due to surface tension forces, cohesion and adhesion.
Saturated Zone/Phreatic Zone
The zone below the water table where water pressure is greater than atmospheric pressure and pores are saturated with water
Interflow
Water that flow laterally through the unsaturated zone
Aquifer
A GW reservoir composed of geological units that are saturated with water and are sufficiently permeable to yield water in a useable quantity to wells and/or springs
Aquitard
A unit of low but not negligible permeability. Can be saturated or saturated to some degree
Aquiclude
A unit of negligible permeability
Piezometeric surface
The surface representing the level to which water would rise in boreholes puncturing the aquifer, where the groundwater pressure is equal to the atmospheric pressure
Unconfined aquifer
An aquifer in which the water table forms the upper boundary. (water table = piezometeric level)
Confined aquifer
An aquifer that is confined between two aquitards.
How do you distinguish the potentiometeric surface and the piezometeric surface?
The potentiometeric surface is the level to which water will rise in any borehole. For unconfined aquifers, this is the water table. In unconfined aquifers, this is called the piezometeric surface
Leaky aquifer
A leaky aquifer is a semi-confined aquifer. A water bearing formation with an underlying for overlying confining layer of low permeability that stored GW and also transmits it slowly from the aquifer
Potentiometer surface
The potentiometer surface is a general term best used to mean either the water table (unconfined aquifers) or piezometeric surface (confined aquifer). It is the level to which water will rise in any borehole