What is groundwater?
Groundwater is water stored beneath Earth’s surface in soil and sediment pores and in rock fractures.
Study 5 Groundwater with 12 free online flashcards. Review key terms, definitions, and concepts with this interactive flashcard deck.
What is groundwater?
Groundwater is water stored beneath Earth’s surface in soil and sediment pores and in rock fractures.
What makes a rock or sediment layer an aquifer?
An aquifer is saturated rock or sediment that can store and transmit enough water to supply wells or springs.
What does porosity describe?
Porosity is the proportion of a material’s volume made up of openings; it indicates how much space is available to hold water.
What is a confining layer?
A confining layer transmits water poorly and may restrict groundwater flow between aquifers.
What does water level in a well tapping a confined aquifer indicate?
In a well tapping a confined aquifer, water rises to the aquifer’s potentiometric surface, which reflects pressure rather than the aquifer’s depth.
When is a well called a flowing artesian well?
A flowing artesian well occurs when pressure in a confined aquifer raises water above the land surface.
In which direction does groundwater generally move?
Groundwater generally moves from higher hydraulic head to lower hydraulic head; gravity and pressure drive the movement.
What is groundwater recharge?
Recharge is water that reaches the saturated zone and adds to groundwater storage.
What is a cone of depression?
Pumping lowers water level or pressure near a well, forming a roughly cone-shaped zone of drawdown called a cone of depression.
How do gaining and losing rivers differ?
Groundwater flowing into a river makes it gaining; this contribution is called baseflow. A losing river seeps water into the ground and recharges an aquifer.
What does permeability describe?
Permeability describes how readily water can move through a material, especially how well its openings connect.
What is the water table in an unconfined aquifer?
In an unconfined aquifer, the water table is the upper boundary of the saturated zone. It can rise or fall as recharge and discharge change.
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