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groundwater
freshwater that is stored underground
aquifer
storage system for groundwater
porous
has a lot of pore space and ability to hold water
permeable
water can move through easily
hydraulic conductivity
measures porosity, permeability, and properties of fluid to determine if a source is good for water storage/transport
potable water
water that is safe to drink
vadose/unsaturated zone
zone where pore space is filled with mostly air and some water
saturated zone
zone where pore space is completely filled with water
water table
line that divides the saturated and unsaturated zones
confining layer
layer that prevents water from moving in/out of aquifers
aquiclude
type of confined aquifer, water cannot get in/out
aquitard
type of confined aquifer, water can get in slowly
potentiometric surface
area where water rises when a well is drilled in due to high pressure, don’t have to pump water
springs
areas where groundwater intersects the surface
artesian/flowing wells
a well where water rises to the surface without pumping
gaining stream
streams where the water table intersects with the stream bed
losing stream
streams where the water table is below the stream bed
hydrograph
charts that show changes in the water table over time
darcy’s law
equation that describes the flow of liquid through a porous medium
drawdown
water table lowering from groundwater extraction
cone of depression
area where water table lowers surrounding a groundwater extraction site
recharge
rate at which groundwater is replenished
discharge
rate at which groundwater is extracted
groundwater mining
over-extraction of groundwater
pore pressure
pressure that comes from the weight of overlying water, keeps aquifers stable
subsidence
land surface down-warping due to rapid groundwater removal
point source pollution
pollution that has one defined source
non-point source pollution
pollution that doesn’t have a defined source or has multiple sources
superfund site
water area that has federal support to clean up
remediation
making polluted groundwater suitable for human use again
karst
system of above and below ground features that are produced by bedrock being dissolved by water/acid
limestone
type of rock that makes up karst systems due to high solubility
disappearing streams
streams that “disappear” under a wall of rock and turn into an underground karst system
calcite
mineral that makes up limestone, easily dissolved
tufa
calcite/water deposit that forms in lakes/streams
travertine
calcite/water deposit that forms in hot springs/caves
cave
a natural cavity, recess, or chamber formed beneath the surface by dissolved bedrock
speleothem
structure in caves made of mineral deposits from water reacting with calcite
stalacties
speleothems that hang on the celing
stalagmites
speleothems that grow up from the floor
sinkhole
funnel/bowl shaped depression that comes from the dissolution of underlying bedrock/sediment
soda straw
the thin starting of speleothems
column
speleothems that connect from floor to ceiling
dissolution
the dissolving of something
underground streams
streams that flow underground through karst systems
cave spring
area where underground streams emerge