aquifer recharge, lakes, and springs
DESCRIPTION
Aquifer Recharge, Lakes, and Springs. The Florida Platform was dominated by marine carbonate deposition between 150 and 24 mya. The most recently deposited carbonates from the Oligocene and the Eocene between 55 and 24 Mya comprise the principal water bearing - PowerPoint PPT PresentationTRANSCRIPT
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Aquifer Recharge, Lakes, and Springs
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The Florida Platform was dominated by marinecarbonate deposition between 150 and 24 mya
The most recently deposited carbonates fromthe Oligocene and the Eocene between 55 and24 Mya comprise the principal water bearingunit of the Floridan aquifer.
Silicon-based (siliciclastic) Miocene sediments fromthe continent, principally the Appalachians, settledover the carbonates beginning 24 million yearsago forming the upper confining unit for the aquifer
Sandier sediments subsequently covered the Miocene deposits
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55 – 24 million years ago
Miocene Clays(low permeability)
Surface Siliciclastics (sandy)(highly permeable)
The Floridan aquifer is a confined aquifer.The water-bearing unitis permeable limestone.
Low PermeabilityConfining Unit(poor water movement)
Unconfined aquifer isextensive throughoutthe state of Florida
Low permeability rock (confining)
Rudimentary Picture
Low permeability rock
Source of permeability
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CaCO3 + H+ = HCO3- + Ca2+
Acidity from rainfall reacts with CaCO3
and dissolves the carbonate rock.
(solid) (solution)(acid) (solution)
CO2 + H2O = H2CO3
H2CO3 => H+ + HCO3-
Dissolution Cave
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Caves andSolution Cavities
Acid dissolves calcium carbonate
CaCO3 + H+ = HCO3- + Ca2+
Hold and deliverbillions of gallonsof fresh water
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Florida is Dominated by Karst Topography.
Characterized by sinkholes, springs, depressions, lakes
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Sinkhole Types
Dissolution Cover Subsidence Cover Collapse
Gradual Abrupt
Gradual
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Sinkhole formation depends on the material overlying the carbonate water-bearing unit
Thin, sandy covering
Dissolution Sinkholes
Thick sands up to 200 ft thick and some clays
Subsidence Sinkholes
Cohesive clays up to 200ft thick
Collapse Sinkholes
Miocene clays have been eroded and shaped throughout their historyresulting in extreme variability in thickness across the state.
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Sinkholes, Lakes, Aquifer Recharge
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Sinkholes and Lakes
The most common origin of lake formation in Florida
Limestone bedrock is dissolved by acids
Land subsidence into dissolvedlimestone cavities createsdepressions filled with water
Subsidence and collapsesinkholes both can form lakes. Subsidence lakesare the most common.
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Initially the limestone contains fractures, but no subsidence has occurred
Small cavities and cracks grow larger as time progresses, and water moving through the rock erodes the rock matrix. Sediments carried by the water fill the voids in the rock.
Sediments from the upper layers continue to fill in the openings in the limestone, causing a depression at the land surface. If water collects in the depression, a new lake is formed.
Subsidence Lakes(most common)
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The Importance of Sinkholes and Sinkhole Lakes
Hydrologic connections between the surfaceand the underlying limestone are often maintained.
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As water levels belowground decline, thepressure beneath the land surface drops,causing an increase in water seeping fromlakes into the ground
Rainfall and shallow groundwater arethe greatest factors affecting waterlevels in Florida’s lakes.
Lakes and Water Levels
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Keystone Heights
Blue Pond Lake LowryMagnolia LakeLake Brooklyn Lake Geneva
Interconnected cluster of lakes
Supplied by rainwater
Sandy bottoms contact the Floridan Aquifer below
Lake levels are controlled by water in the aquifer.
Groundwater withdrawals continue to increase.
Thriving Lake Community
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Plug the Bottom?
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Thicker sands and some clays(subsidence sinkholes)
Cohesive clays up to 200ft(Cover Collapse sinkholes)
Sinkholes and Lakes Statewide
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35% of Florida’s lakes
Lake, Polk, Osceola, Orange
Thick sands and some clays(subsidence sinkholes)
Subsidence Sinkhole Lakes
*
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Maintenance of hydrologic connection with the underlyinglimestone is a primary source of recharge to the Floridan
Lakes and Aquifer Recharge
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Elevation, Recharge, andGroundwater Movement
Subsidence lakes and sinks area primary source of recharge
to the Floridan Aquifer
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Elevation (m)
Recharge Areas
Much of the Recharge Occurs at Higher Elevations
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Groundwater flows from topographichighs toward lower elevations
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Recharge
Generalized Groundwater Movement and Artesian Conditions
confining
confining
Artesian Aquifer
Water under pressure
Central partOf state
CoastThin sandy overburden
Groundwater
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Artesian Aquifers Produce Springs
Water under pressure breaks through upperconfining layers producing water at the surface
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Thin confining layer
Thick confining layer
Groundwater
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Springs Form Best Where the Confining Layer is Thin
Thin sandy overburden
Groundwater
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Florida’s Springs
Form at low elevationswhere the upper confining unit is thin or absent
(64.6 million gallons per day)Thin or absent
30 – 200 ft sandy
30 – 200 ft clayey
> 200 ft thick
Hawthorne Thickness
27 of 78 First Magnitude Springs Nationally
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Ginnie
Poe Spring
http://www.underwaterflorida.homestead.com/springs.html
Manatee
Juniper
Homosassa
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Summary
The Floridan Aquifer is under confined conditions
The water-bearing unit is marked by dissolution cavities
Dissolved limestone caves and cavities create karst conditions
Karst is characterized by depressions, sinkholes, lakes, springs
Subsidence and collapse sinkholes produce numerous lakes
Lakes often maintain hydrologic connection with the underlyinglimestone and can function in recharge for the aquifer
Much of the recharge occurs at higher elevations leading to a generalized movement of groundwater to lower elevations
Water under pressure at lower elevations can discharge at the surface as springs, particularly when confinement is thin
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Florida Lakes: Features and Types
Florida has more natural lakes than any other state in the southeast
Next
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