ground water - suffolk public schools blog
TRANSCRIPT
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Ground Water
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VA SOL
SOL 9 The student will investigate and understand how freshwater resources are influenced by geological processes and the activities of humans. Key concepts include
b. development of karst topography
c. identification of groundwater zones including the water table, zone of saturation, and zone of aeration;
e. dependence on freshwater resources and the effects of human usage on water quality;
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Objective
1. Interpret a simple groundwater diagram showing the zone of aeration, the zone of saturation, the water table, and an aquifer.
2. Describe underground water sources (such as aquifers and springs).
3. Explain the development of karst topography to include key terminology: joint, cavern, sinkhole, carbonation, stalactite, and stalagmite.
4. Locate the region of karst topography in Virginia as the Valley & Ridge Province where limestone/dolomite is common.
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Enduring Understanding
Weathering, erosion, and deposition are interrelated processes that form a cycle of forces that wear down and build up the Earth’s surface.
Water is continuously passed through the hydrologic cycle.
Fresh water is necessary for survival and most human activities.
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Ground Water
If you drill a hole deep enough anywhere on Earth you will find water. Even in the desert! Groundwater is present everywhere, but is only a small fraction of the Earth’s water supply.
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The Hydrosphere
Hydrosphere is the water on and in Earth’s crust.
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The Hydrosphere
97% of the hydrosphere in contained in the oceans
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The Hydrosphere
The 3% contained by landmasses is mostly fresh water
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The Hydrosphere
2.15% of that fresh water is locked in ice caps and glaciers
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The Hydrosphere
Most of the remaining fresh water is stored underground
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Groundwater Movement and
Storage
As the Water Cycle runs much of the precipitation that falls on land becomes groundwater. From there it will begin a journey back to the ocean again.
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Groundwater Movement and
Storage
Infiltration is the process by which precipitation enters the ground and becomes groundwater
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Groundwater Movement and
Storage
Porosity is the percentage of pore space in a material
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Groundwater Movement and
Storage
Well-sorted sand has a porosity of about 30%
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Groundwater Movement and
Storage
Permeability is the ability of a material to let water pass through it and depends on how well connected the pores are
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Groundwater Movement and
Storage
Sandstone, limestone and well-fractured bedrock is very permeable
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Groundwater Movement and
Storage
Silt, clay and shale are impermeable
http://techalive.mtu.edu/meec/module06/Permeability.htm
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Groundwater Movement and
Storage
Zone of Saturation is the depth at which groundwater completely fillsall the pores of a material
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Groundwater Movement and
Storage
Water Table is the upper boundary of the zone of saturation
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Groundwater Movement and
Storage
Aquifer is a permeable layerthrough which groundwater flows
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Groundwater Movement and
Storage
Aquiclude is an impermeable barrier to groundwater flow
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Groundwater Erosion
Most groundwater contains carbonic acid that forms when carbon dioxide dissolves in water and combines in water molecules. The slightly acidic groundwaterattacks certain rocks
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Groundwater Erosion
Carbonate rocks such as limestone that consist mostly of CaCO3 are susceptible to acid dissolution
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Groundwater Erosion
Caves are natural underground openings that connect to the surface and are formed when groundwater dissolves limestone
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Groundwater Erosion
Stalactites are dripstone formations that form slowly on the top of cavesas water drips slowly leaving a tiny deposit of CaCO3 that accumulates over time
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Groundwater Erosion
Stalagmites are mound-shaped dripstone deposits that form underneath the stalactites.
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Groundwater Erosion
Dripstone columns are formed when stalactites and stalagmites grow together
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Karst Topography Limestone regions
that have sinkholes, sinks, and sinking streams are said to have karsttopography named after a limestone region in Croatia where these features are especially well-developed.
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Karst Topography
About 10% of the Earths surface and 15% of the United States is this type
Click on link
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Karst Topography
Sinkhole is a depression in the ground caused by the collapse of a cave
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Karst Topography
Sinkholes are common in Florida, and Texas
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Karst Topography
Virginia has an extensive cave system that extends through the valley and Ridge that can be visited and explored quite easily
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Ground Water Systems