GW-SW interactions Flashcards
Hydrogeological unit
comprises one or more geological units with almost similar hydrogeological properties (ex hydraulic conductivity)
Aquifer
permeable hydrogeological unit that stores large amount of water and permits large amount of water move throguh it under field conditions
ex. sands, gravels from aluvial, glacial or deltaic origins
sandstone, karst limestone, fractured basalt
Aquitard
less permeable hydrogeological unit that stores water but is incapable of transmitting significant quantities of water
ex. silt and clay
shales and crystaline rocks
unconfined vs confined aquifer
unconfined = an aquifer in which the water table forms the upper boundary
confined = aquifer confined between aquitard layers (ex clay), or aquifer that is overlain by relatively impermeable unit such that the aquifer could be under pressure and the water level rises above the confined unit
Groundwater Table/Phreatic Surface
surface along which pressure head =0
Baseflow
the portion of the stream(or river) that is sustained between precipitation events, fed to stream from groundwater storage
Describe ground-water stream interactions
gaining streams
-water table level with stream; ground-water flows into stream
-contour lines point upstream
losing stream
-water table below river level; surface water leaches into ground-water
-contour lines point in downstream direction
Describe disconnected streams
streams are separated from groundwater by an unsaturated zone
describe bank storage
if stream levels rise higher than adjacent ground-water levels, stream moves into the streambanks as bank storage
Describe ground-water stream water withdrawal interactions
If you draw water near stream, it will pull water groundwater away from stream
if you increase the discharge of the withdrawal it will pull surface water into the ground and through your withdrawal(dry up lakes/rivers)
Describe ground-water spring interactions
when perched aquifer intersects with land surface it causes springs
-occurs when water table intersects with earths surface
Describe ground-water lake interactions
lakes can have ground-water inflow or outflow throughout their entire bed, or have both inflow and outflow at different localitites
Describe ground-water wetland interactions
can occur at slopes (unlike lakes/rivers)
-at seepage face or break in slope