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Groundwater is water that…
is beneath Earth’s surface
Groundwater flows with
the surface topography
The hydrosphere is water
on and in the earth's crust
97% of water is in the
ocean
Precipitation enters into the ground through
infiltration
Runoff - returned directly to the
oceans (does not infiltrate)
Porosity is the percentage of the total volume of a
rock or sediment that consists of open spaces
Factors of porosity:
Sorting, well-sorted, and poorly-sorted
Sorting is the amount of uniformity in the
size of rock/particle size
Well sorted =
Same size: High porosity
Poorly sorted:
Many sizes: low porosity
Permeability is the ability of a rock or sediment to let fluids pass through
its open spaces/pores that are connected
Impermeable(Aquiclude):
Water cannot flow through
Permeable (Aquifer):
Water can flow through
Zones of Groundwater
Zone of Aeration, Water Table, and Zone of Saturation
Zone of Aeration:
Moist, but pore space mostly filled with air
Water Table: The upper boundary of the zone of saturation
Depth depends on local conditions
Fluctuates with seasonal & other weather conditions
Zone of Saturation:
Pore space is completely filled with water
Wells are hole that is dug below the level of the water table and through
which groundwater is brought to Earth’s surface
Artesian Well:
well through which water flows freely without being pumped
Cone of Depression
pumping too much water out
Spring is the natural flow of groundwater to Earth’s surface in places where
the ground surface dips below the water table
Hot Spring: hot groundwater that is at least 37 o C and
rises to the surface before cooling
Geyser is a hot spring that periodically erupt from
surface pools or through small vents
Examples of Geysers:
Old Faithful, Yellowstone National Park
Groundwater problems:
Groundwater depletion, pollution, and saltwater intrusion
Groundwater depletion:
Using faster than it can recharge
Saltwater intrusion:
Saltwater can enter if near the ocean