Ground Water Write everything in PURPLE!.

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Presentation transcript:

Ground Water Write everything in PURPLE!

Groundwater Vocabulary Aquifer Water table Wells & springs Write everything in PURPLE

What is Groundwater? Rain and snowmelt that infiltrate the ground. What is this called? Soil and rock act as giant sponges, full of tiny pores and cracks which allows water to infiltrate and collect underground.

Groundwater Feeds the River Systems Groundwater and surface water are one connected water system. Water wells intercept groundwater that may be on its way to springs that feed streams and rivers.

The Water Table Draw this in your notebook!!

The Water Table Unsaturated zone: through which water moves downward and whose pore space is not completely filled. Saturated zone: in which water collects and whose pore space is completely filled. The plane of separation between these two zones is the water table.

Groundwater Basics Beds of rock, and sediment, with high porosity (% of pore space) are better suited to holding groundwater. Aquifers: Beds that hold large amounts of groundwater. Pores – spaces between grains of rock and soil

Permeability: Just because pore space exists doesn't mean that water can flow through it. Pores may be isolated. Permeability: the ability of a solid to allow fluids to pass through.

Aquifers are permeable layers of rock and sediment that have groundwater in enough quantity to supply wells.

Which picture shows a drought? Plenty of rain?

Aquifers: Aquifers are any underground layer of rock or sediment that holds water The Ogallala aquifer reaches from South Dakota to Texas

Groundwater: aquifers What would be the properties (porosity/permeabil ity) of conglomerate? High porosity, high permeability

Groundwater: aquifers What would be the properties (porosity/permeabil ity) of un-fractured granite? Low porosity, low permeability

Water flowing downhill beneath an aquiclude may be under pressure Water flowing downhill beneath an aquiclude may be under pressure. This is artesian flow. Drilling into it will create an artesian well, through which water will flow spontaneously.

Water Table Topography slope = hydraulic gradient

The Water Table

The Water Table

Groundwater and Geology Groundwater containing carbonic acid dissolves limestone, forming caverns and features of karst topography. 1. Rainwater containing carbonic acid seeps into the ground. 2. Limestone dissolves, forming underground caves. Limestone Cave Formation 3. Below the water table, the cave is filled with water.

A aerial photograph of a classic karst terrain north of Lewisburg, WV.

Underground spring comes to the surface.

Wells What happens when this well is heavily pumped?