20
Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches the water table Groundwater flow from recharge area to stream Water table rises Evaporation removes intercepted water Evapotranspiration (ET) from plants removes water from soil Baseflow to streams depletes water in aquifer Hydrologic Cycle Baseflow and ET continue until next rainfall Rainfall Aquifer Vadose zone Soil B horizon Stream water table Rain stops Overland + Interflow = Stormflow. Stream level rises

Interception on trees, impermeable surfaces Infiltration into soil Interflow downslope along B horizon Overland flow during heavy rain Recharge reaches

Embed Size (px)

Citation preview

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

Fractured crystalline rock

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

Hydrogeologic Conceptual Model

R: 0.2 m/yr

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

Atlantic Coastal Plain

Coastal Plain

Santee River Delta

Sand and clay

clay

Sand

Columbia Myrtle Beach

Atlantic Coastal Plain

Flowing wells

Edwards Aquifer, San Antonio, Texas Roswell Basin, NM, 3600 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

Floridan Limestone Aquifer

Dissolution

Cave stream

Limestone aquifer

Floridan Aquifer

• T: 1000-100,000 m2/day

• Recharge: 0.03-0.5 m/yr

• Well Yield: 1000-20,000 gpm

Comparison of SE Regions

Region T (m2/day) Recharge (m/yr) Qwell (gpm)

Piedmont 1-100 0.03-0.3 10-100

Coastal Plain Clastic 500-10,000 0.05-0.5 100-5000

Floridan Limestone 1,000-100,000 0.03-0.5 1000-20,000