Lecture 6 Flashcards
What is Groundwater
Water that exists underground in saturated zones beneath the land surface. Including all subsurface sources including those in soil solution
Void Spaces
(pores/fractures) in the bedrock
What are void spaces important for maintaining
- streamflows
- drinking water
- irrigation
Groundwater Distribution (Aeration/Unsaturated/Vadose zone)
Land surface to top of the phreatic zone
Groundwater Distribution (Capillary Fringe)
Region in which water seeps/wicks up from vadose zone
Groundwater Distribution (water table)
Top of saturated zone
Groundwater Distribution (saturated zone)
- Region in which space is filled with water
- Coincides with most rivers and lakes at surface to swamps, ponds
Groundwater Distribution (Aquifer)
Layer of water bearing material (permeable; supports springs)
Groundwater Distribution (Aquitard)
Layer that retards water flow (ex. clay)
Relatively impermeable
Groundwater Distribution (Aquiclude)
Layer absorbs, holds but does not transmit water
Impermeable
What is a Perched Water Table
Aquifer that occurs above the regional water table
What is a Spring
Exit point at which groundwater emerges from the aquifer and flows onto the top of the Earth’s crust to become surface water
What is a Well
Is a hole made into the ground to access water contained in an aquifer
What is a Watershed (Surface Water)
An area of land in which percipitation drains to a common point on a stream, river, pond, lake or other body of water (drainage basin)
What is the Groundwater Divide
A curve representing the water table ridge (described with contours of the groundwater level) that seperates the flow domain into subdomains
Where does Groundwater Divide Flow
Flows from upland recharge areas to valley discharge areas
What is an Aquifer?
Geological formations:
1. stores
2. transmits
3. yields water
What does the Aquifer Depend on:
The geology: recharge, aquitards, aquicludes, etc.
What are Unconfined (water table) Aquifers Influenced By:
Atmosphere (need pump)
What is an Artesian Well:
A well that brings groundwater to the surface without pumping because it is under pressure within a body of rock and/or sediment in a confined aquifer
Wells: Cone of Depression/Ascension
Active withdrawal of groundwater can have consequences by changing the slope or shape of the water table
- Continental and Costal wells
What is Hydrodynamic Equilibrium
When discharge = recharge