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Water
Terms


        http://commons.wikimedia.org/wiki/File:Michael_Melgar_LiquidArt_resize_droplet.jpg
Porosity vs. Permeability

The terms porosity and permeability are related.
Porosity is a measure of the amount and size of pore
space within an earth material, such as soil, clay, gravel,
silt, rock, etc.
Some rocks and soils are very porous, while others have
very little space between the particles.
Porosity is how much water a material can hold. It is
usually stated as a percentage of the material’s total
volume.
Porosity vs. Permeability

Permeability is a measure of the ability of an earth
material to let water pass through it.
Permeability is affected by the size of the particles and
shape of the spaces between the particles.
Some materials have many spaces between particles,
while others have virtually no space between particles
and are called impermeable.
Porosity vs. Permeability


Water flows between the spaces in the material.

If the spaces are close together, such as in clay based soils,
the water will tend to cling to the material and not pass
through it easily or quickly.

If the spaces are large, such as in the gravel, the water
passes through quickly.
Percolation and Infiltration

There are two other terms that are used with water:
percolation and infiltration.

Infiltration is when the water enters the soil surface
after falling from the atmosphere.

Percolation is the downward movement of water from
the land surface into soil or porous rock, caused mainly
by gravity.
Particle Sizes And Pore Space:
Groundwater vs. Surface Water

Groundwater is water that flows through the pores in the
rocks and soil beneath the surface of the ground.
The groundwater trickles downward until it reaches an
impermeable layer of soil or rock.
We use wells and springs to pull groundwater back to the
surface to drink.
Ninety-eight percent of Earth’s available freshwater is
groundwater.
Groundwater vs. Surface Water

Surface water includes
rivers, streams, lakes, ponds, oceans, and even the water
that runs down streets during thunderstorms.
Surface water will, unless interfered with, flow downhill
until it reaches a creek or stream. The creek or stream will
eventually feed a river that will flow into the ocean. Along
the way, some water will evaporate back into the
atmosphere and will fall back to the Earth as rain.
Surface water supplies 80% of the water used on a daily
basis.
Groundwater vs. Surface Water


Surface water which has not yet
flowed into a creek is called
runoff. Bare ground allows a
great deal of runoff to occur.
Plants and dug ponds (a
small, shallow pond created
artificially by digging a
depression in the land) reduce
the amount of runoff.
Watershed Diagram
Watershed vs. Aquifer

A watershed is an area of land where all of the surface
water within a specified area drains downward and
flows to the same place.

Each drainage basin, or watershed, is separated
topographically from adjacent basins.
Aquifer

An aquifer is a natural, underground area where large
quantities of ground water fill the spaces between rocks
and sediment and accumulates.

This water is available for use by using wells to pump out
the water.
Texas Aquifers

The state of Texas has 23 aquifers that cover
approximately ¾ of the state.

The Ogallala Aquifer accounts for about 90%
of the water in all of Texas aquifers.

Groundwater from Texas aquifers is used
for irrigation, city use, manufacturing, and
livestock production.

Pumping water from many aquifers in Texas
has resulted in a significant lowering of the
water table.                                    A map showing watersheds in Texas
More about Aquifers

Less permeable rock below an aquifer that keeps
groundwater from draining away is called a confining layer
or aquitard.

The water table in an aquifer is at the very top of the zone
of saturation.

The zone of saturation is where water completely fills all
the interconnected pore spaces.
Water Table
The water table is the upper
surface of ground water below
                                  The water table fluctuates
which the soil or rocks are
                                  both with the seasons and
permanently saturated with
                                  from year to year because it is
water and where the pressure of
                                  affected by climatic variations
water in the soil equals the
                                  and the amount of
pressure of the atmosphere.
                                  precipitation used by
                                  vegetation. It also is affected
                                  by withdrawing excessive
                                  amounts of water from wells.
Pollution

Pollution is the introduction of a contaminant into the
environment.
It is created mostly by human actions, but can also be a
result of natural disasters, such as flooding.
Pollution has a harmful effect on any living organism in
an environment, often making it impossible to sustain
life.
Pollution to drinking water can cause diseases.

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12 s070403 c_water terms

  • 1. Water Terms http://commons.wikimedia.org/wiki/File:Michael_Melgar_LiquidArt_resize_droplet.jpg
  • 2. Porosity vs. Permeability The terms porosity and permeability are related. Porosity is a measure of the amount and size of pore space within an earth material, such as soil, clay, gravel, silt, rock, etc. Some rocks and soils are very porous, while others have very little space between the particles. Porosity is how much water a material can hold. It is usually stated as a percentage of the material’s total volume.
  • 3. Porosity vs. Permeability Permeability is a measure of the ability of an earth material to let water pass through it. Permeability is affected by the size of the particles and shape of the spaces between the particles. Some materials have many spaces between particles, while others have virtually no space between particles and are called impermeable.
  • 4. Porosity vs. Permeability Water flows between the spaces in the material. If the spaces are close together, such as in clay based soils, the water will tend to cling to the material and not pass through it easily or quickly. If the spaces are large, such as in the gravel, the water passes through quickly.
  • 5. Percolation and Infiltration There are two other terms that are used with water: percolation and infiltration. Infiltration is when the water enters the soil surface after falling from the atmosphere. Percolation is the downward movement of water from the land surface into soil or porous rock, caused mainly by gravity.
  • 6. Particle Sizes And Pore Space:
  • 7. Groundwater vs. Surface Water Groundwater is water that flows through the pores in the rocks and soil beneath the surface of the ground. The groundwater trickles downward until it reaches an impermeable layer of soil or rock. We use wells and springs to pull groundwater back to the surface to drink. Ninety-eight percent of Earth’s available freshwater is groundwater.
  • 8. Groundwater vs. Surface Water Surface water includes rivers, streams, lakes, ponds, oceans, and even the water that runs down streets during thunderstorms. Surface water will, unless interfered with, flow downhill until it reaches a creek or stream. The creek or stream will eventually feed a river that will flow into the ocean. Along the way, some water will evaporate back into the atmosphere and will fall back to the Earth as rain. Surface water supplies 80% of the water used on a daily basis.
  • 9. Groundwater vs. Surface Water Surface water which has not yet flowed into a creek is called runoff. Bare ground allows a great deal of runoff to occur. Plants and dug ponds (a small, shallow pond created artificially by digging a depression in the land) reduce the amount of runoff.
  • 11. Watershed vs. Aquifer A watershed is an area of land where all of the surface water within a specified area drains downward and flows to the same place. Each drainage basin, or watershed, is separated topographically from adjacent basins.
  • 12. Aquifer An aquifer is a natural, underground area where large quantities of ground water fill the spaces between rocks and sediment and accumulates. This water is available for use by using wells to pump out the water.
  • 13. Texas Aquifers The state of Texas has 23 aquifers that cover approximately ¾ of the state. The Ogallala Aquifer accounts for about 90% of the water in all of Texas aquifers. Groundwater from Texas aquifers is used for irrigation, city use, manufacturing, and livestock production. Pumping water from many aquifers in Texas has resulted in a significant lowering of the water table. A map showing watersheds in Texas
  • 14. More about Aquifers Less permeable rock below an aquifer that keeps groundwater from draining away is called a confining layer or aquitard. The water table in an aquifer is at the very top of the zone of saturation. The zone of saturation is where water completely fills all the interconnected pore spaces.
  • 15. Water Table The water table is the upper surface of ground water below The water table fluctuates which the soil or rocks are both with the seasons and permanently saturated with from year to year because it is water and where the pressure of affected by climatic variations water in the soil equals the and the amount of pressure of the atmosphere. precipitation used by vegetation. It also is affected by withdrawing excessive amounts of water from wells.
  • 16. Pollution Pollution is the introduction of a contaminant into the environment. It is created mostly by human actions, but can also be a result of natural disasters, such as flooding. Pollution has a harmful effect on any living organism in an environment, often making it impossible to sustain life. Pollution to drinking water can cause diseases.