Groundwater Flashcards
what is ground water
the water in the ground occupying the pore spaces within bedrock and regolith
where must water be to be considered groundwater
within bedrock and regolith
compare the volume of groundwater to volume of fresh water in lakes/streams
40 times larger
what is larger the volume of ground water or freshwater lakes/streams
volume of groundwater
what is the largest ACCESSIBLE fresh water reservoir
groundwater
how much of the water on earth is ground water
less than 1 percent
how does most groundwater originate
rainfall and the rest as surface water
where does more than half of all ground water occur
above a depth of 750 meters
why does water below 750 meters diminish in volume
- groundwater comes from precipitation
- the likelihood of water coming in contact with impermeable material increases as it gets deeper
what is the zone of aeration
layer of moist soil followed by a zone where open spaces in regolith/bedrock are filled with air
what zone is below the zone of aeration
saturated zone
saturated zone
all the openings in regolith/bedrock are filled with water
what is the upper surface of the saturated zone called
water table
water table
surface zone of saturation BELOW zone of aeration
does water table and groundwater mean the same thing
NO
1
zone of aeration
2
water table
3
zone of saturation
4
cone of depression
what layer will have pores filled with air and water
zone of aeration
what zone is considered unsaturated
zone of aeration
what zone will have pores completely filled with water
saturated zone
does the water table change seasonally
YES
does the water table follow topography
yes - higher under hills and lower under lakes
where does the water table slope toward
the nearest stream or lake
what is capillary attraction
the adhesive force between a liquid and a solid that causes water to be drawn into small openings
where does capillary fringe pull water from
zone of saturation
does the capillary fringe have air in pores
NO - fully fill of water
is the capillary fringe apart of the water table
NO
can water be pumped from a capillary fringe
NO
where is the capillary fringe located compared to water table
ABOVE it
describe the water table in humid regions
subdued to imitate the land surface above it (high beneath hills and low beneath valleys)
why does the water table in humid regions follow topography above it
because water tends to move towards low points in topography under influence of gravity
what cycle is ground water a part of
hydrologic cycle
what is the slowest part of the hydrologic cycle
groundwater cycle
how does water enter a groundwater reservoir
when rain seeps into the ground
when does groundwater enter back into the hydrologic cycle
when it reaches streams/lakes
is groundwater in motion
yes
is movement of groundwater fast or slow
very slow
when is movement of water faster
in regions with more permeable materials
how does water travel in materials
through small, constricted passages
does deeper surface water reach the surface faster
NO - will take longer than shallower groundwater to reach surface
porosity
percentage of total volume of body of regolith or bedrock consisting of open spaces (pores)
what determines the amount of water a volume of regolith or bedrock can contain
porosity
what material has highest porosity
material with largest grains that have largest space between them
how does shape and size of particles affect porosity in sedimentary rocks
bigger particles = more porosity
smaller particles = less porosity
how compaction of particles affect porosity in sedimentary rocks
less compact = more space between particles = more porosity
how weight of overlying rock affect porosity in sedimentary rocks
more weight overlying = more compaction of underlying rocks = less porosity
how pores filled with cement affect porosity in sedimentary rocks
less cement holding rocks together = more porosity
what is the porosity of igneous and metamorphic rock
low because can only hold liquid when very fracture
permeability
measure of how easily a solid allows fluid to pass through
does high porosity mean high permeability
NO
example of high porosity but low permeability
clay
is this poor or good permeability
poor
is this poor or good permeability
good
how does diameter affect permeability
as diameter of pores increase = permeability increases
what is a good permeable material
gravel
recharge
the process by which groundwater is replenished
what surface above oceans can be part of groundwater recharge
all surfaces above oceans
discharge
process where groundwater reaches and flows from surface into streams or lakes
where are the common discharge areas
streams and lakes
recharge area
area of landscape where precipitation seeps downward beneath surface and reaches saturated zone
is the discharge or recharge area larger for groundwater
recharge area
does water move fast or slow to discharge areas
slow
describe recharge areas in humid regions
nearly encompass all landscape beyond streams and their flood plains
describe recharge zones in arid regions
only occurs in certain areas
1. mountains
2. alluvial fans
3. along channels of major streams underlain by permeable alluvium
do arid regions have discharge or recharge zones by streams and rivers
recharge zones
what determines the rate groundwater takes to travel from recharge zone to discharge zone
depends where the discharge area is (how far from recharge zone) and how fast the water can move (how permeable material is)
how does water move in zone of aeration
- water initially soaks into soil containing clay after precipitation
- low permeability of the zone and fine clay particles cause part of water to be retained in soil
- some of moisture evaporates directly into air or absorbed by plant roots
- pull of gravity means water cannot be held in soil and seeps downward until reaches zone of saturation
what initially hold water in the zone of aeration
retained in soil by forces of molecular attraction
movement of water in saturated zone
- water reaches saturated zone and moves by percolation
- percolating water moves through small pores along parallel, thread like paths
- respond to gravity and percolates from areas of high water content to low water content
- percolates toward surface steams or lakes
does percolating water in saturated zone move slow or fast
very slow
describe the route percolating water takes in saturated zone
goes from areas of high water content to areas of low water content
how does water move in saturated zone
percolation
what increases the velocity of groundwater flow in saturated zone
increases as slope of water table increases
why is percolating water moving so slowly
because groundwater encounters large amount of frictional resistance
why is Henri Darcy important for groundwater
came up with the hydraulic gradient equation
what is the hydraulic gradient
the slope of the water table
what is the velocity of groundwater related to according to Darcy
- hydraulic gradient
- permeability of rock
- coefficient of permeability (K)
what is a spring
a flow of groundwater emerging NATURALLY at the ground surface