Groundwater

What you need to learn

o   How large amounts of water are stored underground

o   How groundwater dissolves limestone and forms caves and other natural features

o   How groundwater is removed from the ground by humans and what problems endanger our groundwater supply

Movement and Storage

o   Groundwater is present everywhere beneath the surface of land, but is only a small fraction of all water on Earth

o   Hydrosphere: all the water on or in Earth

n     97% oceans             3% by landmasses

n     90% of freshwater is found in ice

o   Ultimate source of water is in the oceans

How is groundwater stored?

o    Water that doesn’t runoff the land is absorbed into the ground by infiltration

o    The porosity of a material determines how much water it can hold

n      Well sorted material contains around 30%

o    Zone of Saturation: depth below the surface that all the pores fill up with water

n      The upper portion is called the water table

 

The Water Table

o  Depth depends on local conditions

n    It is shallow if there is a lot of surface water

o  Changes with the topography

o  Changes with the precipitation

Groundwater Movement

o   Flows downhill in the direction of the slope

o   The speed is extremely slow, but depends on the materials permeability

o   Most ground water moves through permeable layers called aquifers

o   Aquicludes: are impermeable layers

 

 

Erosion and Deposition

o    Groundwater is slightly acidic and can corrode carbonate rocks (such as limestone)

o    Caves are produced when groundwater dissolves limestone

o    Sinkholes are produced when caves or bedrock collapse and sink the surface of the ground sinks

n      Regions of sinking landscape are called karst topography

 

Groundwater Deposits

o    Hard water: contains high concentrations of calcium

o    Natural deposits: dripstone formations found in caves

n      Stalactites: hang for cave ceiling

n      Stalagmites: form on the cave floor

n      Columns: form when they grow together

n      Travertine: the type of limestone that makes them

 

Groundwater Systems

o    Groundwater eventually reaches the surface after hundreds of years

o    Springs: natural discharges of groundwater

o    The temperature of the water usually matches the area and is colder in the summer and warmer in the winter

n      Hot springs have temperatures above 98°

n      Geysers are explosive hot springs

Wells

o    Wells are holes dug or drilled deep into the ground to an aquifer

n      Overpumping of a well can cause drawdown where the water table lowers

n      Watertables can recharge with increased precipitation

n      Aquifers that are under pressure are called Artesian wells

Threats to our water supply

o    Overuse

o    Subsidence – the sinking of land

o    Pollution – sewage, industrial waste, landfills, and agricultural chemicals

o    Chemicals

o    Salt

o    Radon – causes cancer