Groundwater resources Flashcards
What is the zone of aeration?
Rock or sediment that allows water to pass through it and has pore space that could store water.
What is the zone of saturation?
Rock or sediment that can store water in its pore space and allow water to move through it.
What is the water table?
The upper surface of the zone of saturation; the boundary between the zone of aeration and zone of saturation.
What is an impermeable layer?
A layer of rock that does not allow fluids to flow through it; impermeable layers around porous and permeable rock can form good aquifers
What is the recharge area of an aquifer?
Area on Earth’s surface that allows water to infiltrate into an aquifer.
Why do urban aquifers recharge slower than rural aquifers?
Buildings and roads form an impermeable layer in the recharge area. Urban areas experience more surface runoff and evaporation.
What type of rock is necessary for Karst to form?
Carbonate rocks and other soluble minerals
How do caverns form?
Fractures and joints in carbonate rock allows water to dissolve the rock and enlarge the passages.
How can water naturally form an acid that can dissolve rock?
Carbon dioxide in the air and soil reacts with water to form a weak carbonic acid.
How does cavern formation change locations?
Surface stream erosion or changes in the recharge area can lower the water table and empty caverns. New cavern formation occurs at a lower level.
How do sinkholes form?
Surface fractures widen to form bowl-shaped depressions, or pressure on unsupported caverns can cause surface land to fall into the cavern.
Why is Karst topography an economic concern?
Millions of dollars are spend annually repairing buildings and roads that are damaged due to unstable ground conditions.
What is a stalactite?
A growth of evaporate minerals that formed from flowing or dripping water and that hangs down from the ceiling of a cavern
What is a stalagmite?
A growth of evaporate minerals that formed from flowing or dripping water and that rises from the floor of a cavern.
Why is Karst Topography vulnerable to groundwater contamination?
Fractures and joints allow contaminants to easily enter groundwater systems without natural filtration.