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Pools or Reservoirs
The places where you can find water
Fluxes
Flows from one reservoir to another, in units of mass per time or volume per time
Consumptive Water Uses
Water is removed from water source and used
Non-consumptive Water Uses
Water is not taken from the reservoir, or is returned to the reservoir soon after being used
Overexploitation
Extracting too much water
Subsidence
The vertical sinking of the Earth’s surface in a region
Salinization
The accumulation of salt in water, making it largely useless
Groundwater
Water that resides under the surface of the Earth, mostly in pores or cracks of rock or sediment
Vadose (Unsaturated) Zone
The region of the subsurface above the water table, the pore space is mostly air
Phreatic (Saturated) Zone
The region below the water table where pore space is filled with water.
Water table
The boundary between the Vadose and Phreatic Zones
Aquifers
Rocks or sediments in the saturated zone, from which water can be reasonably removed using a well
Unconfined Aquifers
Aquifers whose upper boundary is the water table
Confined Aquifers
An aquifer isolated from the surface by an aquitard
Perched Aquifer
A local aquitard causes water to "perch" atop it, above the regional water table
Aquitard
Sediment or rock that does not transmit water easily and therefore retards the motion of the water.
Porosity
The fraction of the rock's volume that consists of pore space
Permeability
The ease with which water can move through pore space in a rock or other material
Potentiometric Surface
The level groundwater naturally rises to in a well because of its pressure.
Recharge
When new water from the surface infiltrates downward and adds to the groundwater in an aquifer
Discharge
Discharge is when groundwater leaves an aquifer and flows back to the surface into streams, springs, wetlands, or wells.
Gaining Streams
A stream that receives water from the groundwater
Losing Streams
A stream that loses water to the groundwater