UNDERGROUND WATER
This
is the water found below the earth surface in pores of permeable rocks and
above an impermeable rock layer.
Also
called groundwater
INFILTRATION
The
movement of water vertically into the soil/rocks through pores, cracks or
joints
PERCOLATION
The
movement of water downwards and horizontally in the rocks/soil
EFFLUENT STREAMS
Underground
streams supplied with water from the water table above them
INFLUENT STREAMS
They
are underground streams supplied with water from the water table below their
level
SOURCES OF UNDERGROUND
WATER
There
are four sources of underground water:
- Rainwater;
- Melt water
- Lakes, seas, oceans, rivers and swamps
- Magmatic water/ plutonic water; this is the water that gets trapped in the rocks beneath the surface during volcanism
Factors Influencing
Existence of Underground Water
Precipitation/ rainfall:
Little
rainfall has little or no infiltration as most of the water evaporates
Little
rainfall over a long duration, gives time for infiltration, increasing
underground water
Heavy
rainfall in a short period has more surface run-off, and has little time for
infiltration
Heavy
rainfall over a long has more infiltration as it saturates the ground,
increasing the underground water.
Slope gradient
Flat
gentle slopes gives water more time to infiltrate into the ground, as it
remains in the same place for long duration
Steep
slopes have more run-off, and therefore water has little time to infiltrate
into the ground.
Vegetation cover
Vegetation
hold water on the ground by reducing surface run-off, giving water more time to
sink.
Bare
ground has more surface run-off and has little surface run-off
Plants
also break the speed of rain drops, giving the water time to infiltrate into the
ground
Level of saturation
Dry
ground/soil has more open spaces which allows for more infiltration of water
Saturated
and wet soils have minimal spaces to hold water reducing infiltration
Evapotranspiration
High
rate of evaporation caused by low moisture content in the atmosphere reduce the
amount of water that infiltrates into the ground
Evapotranspiration
reduces the amount of water in the soil/ground. This makes the soil dry,
increases the spaces in the soil, and in turn increases infiltration.
Nature of the rocks
Permeable
rocks allow water to penetrate through.
Highly
permeable rocks allow for a lot of infiltration.
Impermeable
rocks do not allow water to penetrate through, reducing the level of
infiltration
Some
rocks such as clay allow water to enter them but does not allow it to pass
through. This is because when clay particles absorb water, they expand reducing
the air spaces, preventing percolation of water
Note
An aquifuge; is
an rock that does not allow water to pass through/ infiltrate e.g. gabbro,
shale and slate
A porous rock;
is permeable rock that has air spaces/pores between the rock grains
A Pervious rock; is a rock that has
cracks, fractures and joints through which water enters