interception on trees, impermeable surfaces infiltration into soil interflow downslope along b...
TRANSCRIPT
Interception on trees, impermeable surfacesInfiltration into soilInterflow downslope along B horizonOverland flow during heavy rainRecharge reaches the water tableGroundwater flow from recharge area to streamWater table rises Evaporation removes intercepted waterEvapotranspiration (ET) from plants removes water from soilBaseflow to streams depletes water in aquifer
Hydrologic Cycle
Baseflow and ET continue until next rainfallRainfall
Aquifer
Vadose zoneSoil B horizon
Streamwater table
Rain stopsOverland + Interflow = Stormflow. Stream level rises
Hydrogeologic Regions
Geologic controls on – Porosity and hydraulic conductivity
– Layering, structure, and aquifer type
– Water chemistry
– Well yield
Hydro-geology of
the Southeast
Floridan
Floridan
Lim
estone
Lim
estone
Appal
achi
an
Sed
imen
tary
Rock
Lim
esto
nePied
mont C
rysta
lline
rock
Coasta
l Plai
n
San
d + cl
ay
Ground Water Atlas
http://capp.water.usgs.gov/gwa/gwa.html
Transition
Fractured metamorphic and igneous rock
K: 10-11-10-3 m/s
T: 1-100 m2/day
S: 10-3 -10-4
Saprolite: K: 10-6-10-5 m/s
S: 0.1-0.4
Fractured Rock Aquifers in Piedmont
• K: 10-5-10-6 m/s bulk fractured rockCompare to 10-10 to 10-11 m/s for intact samples
• T: 10-100 m2/day
• Recharge: 0.03-0.3 m/yr
• Well Yield: 30-300 gpm
Coastal Plain Clastic Aquifers
• T: 500-10,000 m2/day
• Recharge: 0.05-0.5 m/yr
• Well Yield: 100-5000 gpm
Floridan Aquifer
Floridan
Floridan
Lim
estone
Lim
estone
Appal
achi
an
Sed
imen
tary
Rock
Lim
esto
nePied
mont C
rysta
lline
rock
Coasta
l Plai
n
San
d + cl
ay
Ground Water Atlas
http://capp.water.usgs.gov/gwa/gwa.html