1 / 23

Groundwater

Groundwater. What is it?. Subterranean water that saturates the Earth’s crust just below the surface. How does water get underground?. Cracks, crevices in rock Spaces between grains in the soil

aoife
Download Presentation

Groundwater

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Groundwater

  2. What is it? Subterranean water that saturates the Earth’s crust just below the surface

  3. How does water get underground? • Cracks, crevices in rock • Spaces between grains in the soil • Rocks/beds that store and transmit groundwater in sufficient quantity to supply wells are called aquifers • 22% of all fresh water flows as groundwater

  4. How does rock flow through soil? • The only open spaces for water to flow are between individual grains, called pore spaces • Porosity: percentage of the total volume that is taken up by pores

  5. Porosity • How loosely packed are the grains? • Higher in sedimentary rocks

  6. Permeability • Are the pores connected? • How big are they? • How torturous is the path to be traveled? • Some cave systems are so permeable that people can move through them

  7. The (Ground) Water Table

  8. Zone of aeration “coke” table (aka water table) Zone of saturation

  9. The Effect of the Water Table • If you drill a well below the water table, it will fill to the level of the water table • Straw in pop • It forms a surface roughly parallel to the ground surface • And it moves downhill under gravity and is exposed at rivers and lakes

  10. Aquifers • Rocks/beds that store and transmit groundwater in sufficient quantity to supply wells are called aquifers • Confined • Unconfined

  11. Balancing Recharge and Discharge • Normal “Problem”

  12. Balancing Recharge and Discharge • Extreme Problems • saltwater intrusion

  13. Land Subsidence • Groundwater commonly flows through spaces in sediment (sand and gravel) • Pumping groundwater can cause grains to rearrange and “compact” • Irreversible • Permanent damage to reservoirs

  14. San Joaquin Valley • CA 1st in agriculture • Central Valley = 25% of nation’s food, 1% of land • “Groundwater mining” • Valley is filled with river sediments and clays

  15. Land Subsidence • First noted here in 1935 • >1/2 of San Joaquin Valley (5,200 mi2) irrigable land has sunk by 1’ Darn Kids…

  16. Groundwater and Erosion • Recall how water is a great dissolver • Rainwater contains carbon dioxide which therefore is present in groundwater • Carbon dioxide acts to dissolve limestone • Carbonic acid (COKE) causes faster reactions • Therefore the passage of groundwater through limestone can make HUGE caves

  17. Just Below Water Table • Water coming down from above can evaporate when it reaches opening • Stalactite • Water that drips down to base can form • Stalagmite

More Related