Topic #6 - Water
Geol 357: Urban Geology
I. Hydrologic Cycle
| II. Principles Of Groundwater
| III. Groundwater In Southern California
| IV. Sea Water Intrusion
| V. Methods Of Augmenting Local Water Supplies
| VI. History Of Aqueducts In California |
VII. Who Does What With Water | VIII.
The Use Of Water | IX. Water Quality - Nation
Wide | Links | top | Geol
357 Lecture Home
II. Principles Of Groundwater
- A. Introduction
- 1. Water found in the pores and fractures of soil
and bedrock
- 2. Largest reservoir of fresh water
- 3. Tends to be less polluted than surface water
- B. An important erosional agent
- 1. Groundwater is often mildly acidic
- 2. Contains weak carbonic acid
- 3. Forms caverns at or just below the zone of saturation
- 4. Karst topography on the surface
- C. Equalizer of streamflow
- 1. Most water percolates down into the Earth
- 2. Forms underground "streams"
- D. Terms
- 1. Porosity - Percentage of void space in a rock/soil
- 2. Permeability - The ability of a material to transmit
a fluid
- 3. Specific retention - The portion whish is retained
as a film on particles, rock surfaces, and pore spaces
- 4. Specific yield - The portion which will drain under
gravity
- a. In general, Porosity = Specific retention +
Specific yield
- 5. Aquifer
- a. A zone of Earth material capable of supplying
groundwater at a useful rate from a well
- b. Mostly sands and gravels deposited in stream
channels in California
- 6. Aquitard
- a. A zone of Earth material that holds water but
cannot transmit it fast enough to pump from a well
- b. Usually forms a confining layer
- E. Groundwater basins (http://www.waterplan.water.ca.gov/groundwater/gwdefinition.htm)
- 1. "an area underlain by permeable materials
capable of furnishing a significant supply of groundwater
to wells or storing a significant amount of water"
- 2. Groundwater basin boundaries (http://www.waterplan.water.ca.gov/groundwater/gwdefinition.htm)
- a. Impermeable Bedrock - Impermeable bedrock consist
of rocks of low water yielding capacity. These include
rocks of marine origin and crystalline/or metamorphic
rock.
- b. Constrictions in Permeable Materials - A narrow
gap in impermeable material, even though filled
with permeable stream channel materials, generally
forms a basin boundary due to groundwater flow constriction
in these areas.
- c. Fault - A fault that crosses permeable materials
generally forms a barrier to groundwater movement.
This is usually indicated by noticeable difference
in water levels and/or flow patterns on either side
of the fault.
- d. Low Permeability Zone - Areas of clay or other
fine-grained material that have significant aerial
or vertical extent generally forms a barrier to
groundwater movement.
- e. Groundwater Divide - A groundwater divide generally
forms a barrier to groundwater movement. Groundwater
divides have noticeably divergent groundwater flow
directions on either side of the divide with the
water table sloping away from the divide.
- f. Adjudicated Basin Boundaries - The basin boundaries
established by court order were used for all adjudicated
basins.
- F. Movement of Groundwater
- 1. Very slow - centimeters/day
- 2. Measuring groundwater flow
- a. Primarily done with dyes & Carbon-14
- 3. Pollution implications
- G. Getting Groundwater Out of the Ground
- 1. Extraction Methods
- a. "Natural" Methods
- (1) Springs
- (a) Occur where the water table intersects
Earth's surface
- (2) Hot Springs
- (a) The water for most hot springs is
heated by cooling of igneous rock
- (3) Geysers
- (a) Intermittent hot springs
- b. Man-made Methods
- H. Artesian well/spring
- 1. A situation in which groundwater under pressure
rises above the level of the aquifer
- 2. Types of artesian wells
- a. Nonflowing - pressure surface is below ground
level
- b. Flowing - pressure surface is above the ground
- I. Problems with groundwater removal
- 1. Non-renewable resource
- 2. Subsidence
- 3. Contamination
I. Hydrologic Cycle
| II. Principles Of Groundwater
| III. Groundwater In Southern California
| IV. Sea Water Intrusion
| V. Methods Of Augmenting Local Water
Supplies | VI.
History Of Aqueducts In California | VII.
Who Does What With Water | VIII. The
Use Of Water | IX. Water Quality -
Nation Wide | Links | top
| Geol 357 Lecture Home
|
III. Groundwater In Southern California
- A. Geological Setting
- 1. S. California is broken into fault blocks of different
elevation
- 2. Sediment deposited on the lower blocks forms the
aquifers
- B. Coastal Plain
- 1. These areas are formed by alluvial deposits of
the LA, San Gabriel, and Santa Ana Rivers
- a. These rivers start in the mountains, flow across
the inland valleys, through the narrows and onto
the coastal plain
- 2. Unconfined aquifers lie just beyond the narrows
- a. Confined aquifers along the coast
- C. Inland Valleys
- 1. Water here drains in the subsurface through the
narrows to the coastal plain
- 2. San Fernando Valley
- a. Has extensively used groundwater for agriculture
and domestic needs
- (1) Now polluted with TCE - a Superfund site
- b. Has also used Owens Valley water since 1915
- 3. San Gabriel Valley
- a. Groundwater is heavily used
- b. Basin has the storage capacity of 10 million
acre feet
- (1) Entire State Water Project stores 6.84
million acre feet
- c. The San Gabriel Basin is polluted with cancer
causing chemicals
- (1) trichloroethylene (TCE) - first found
in Irwindale in 1979
- (2) perchloroethylene (PCE)
- (3) carbon tetrachloride (CTC)
- d. San Gabriel Valley became a Superfund site
in 1985
- (1) Clean up progress has been slow
- (2) Cost is estimated at $800 million (1990)
- e. More than 1 million people rely on the San
Gabriel aquifer for drinking water.
- (1) As pollution spreads, pressure on other
water sources will intensify.
- (2) Economic impact could be staggering
I. Hydrologic Cycle
| II. Principles Of Groundwater
| III. Groundwater In Southern California
| IV. Sea Water Intrusion
| V. Methods Of Augmenting Local Water
Supplies | VI.
History Of Aqueducts In California | VII.
Who Does What With Water | VIII. The
Use Of Water | IX. Water Quality -
Nation Wide | Links | top
| Geol 357 Lecture Home
|
VI. History Of Aqueducts In California
- A. Owens Valley Aqueduct
- 1. Concept resulted from the drought of 1892-1904
which threatened the growth of LA
- 2. Aqueduct was conceived by Mayor Fred Eaton and
William Mulholland
- a. Mulholland - engineer and superintendent of
L.A. Water Department
- b. Eaton - Former
- 3. US Reclamation Service interested in area for irrigation
purposes
- a. J.B. Lippincott, supervising engineer for the
Reclamation Service, made sure that only public
land was set aside for future development
- 4. 1904 - LA agents secretly buy options on land with
water rights
- a. Residents thought the land Eaton was purchasing
was for the irrigation project
- b. Result = they got no water for development
/ irrigation
- 5. 1905 - Preliminary bond measure approved
- a. 100,000 people of LA approved a bond issue
for $1.5 million in 1905
- 6. 1906 - Congress grants aqueduct right of way over
federal land with strong backing from President Theodore
Roosevelt
- 7. 1907 - Full bond measure for $25M approved
- 8. 1913 - Construction of aqueduct completed
- a. Initially 233 miles long
- (1) System was extended to the Mono Basin
by 1940 - 338 miles long
- b. Supplies 450,000 acre-feet/yr average over
20 years
- (1) Equals 60 to 80% of LA's needs
- (2) A future environmental reduction to 380,000
acre-ft is planned
- (3) Supplies San Fernando Valley and the western
part of the city
- 9. 1915 - San Fernando Valley annexed into LA
- 10. 1924 - Owens Lake and ~50 miles of the Owens River
are dry
- 11. 1930 - 95% of Owens Valley farmland owned by Los
Angeles; $40M bond issue approved to expand aqueduct
into Mono Basin
- 12. 1940 - Extension completed, diversions begun
- 13. 1963 - plans for a second aqueduct approved
- 14. 1970 - DWP plans to fill new aqueduct by:
- a. Reducing irrigation water
- b. Diverting surface water from Inyo and Mono
counties
- c. Pumping groundwater
- 15. 1972
- a. Inyo county successfully sued to stop groundwater
pumping increase
- b. Wetland meadows, seeps, springs, and marshes
dried and disappeared, well water levels dropped,
and vegetation in the valley began to change.
- 16. Opposition to the aqueduct
- a. Began in Owens Valley with the first land acquisitions
in 1905
- b. Still controversial today
- B. Colorado River Aqueduct
- 1. Droughts from the mid-1920's to early 1930's resulted
in 500,000 people of LA approving a $220 million bond
issue in 1931 for a new aqueduct
- 2. The MWD (128 cities, 12 million people) built the
Colorado River Aqueduct
- a. Extends 242 miles from Lake Havasu behind Parker
Dam
- b. Supplied 1.2 million acre-ft/year to S. California
for many years
- (1) Now reduced to 550,000 acre-ft/year
- c. Supplies 6% of LA's needs
- d. Supplies East LA, the Harbor & part of
the central city
- C. California Aqueduct
- 1. 2.5 million people of LA approved a $1.75 billion
water project
- a. Supplies the Great Valley and large parts of
Southern California
- 2. Aqueduct stretches 444 miles from Oroville Dam
- a. 257' wide and 36' deep in its northern parts
- b. Pumps in the Tehachapi Mtns use 650MW
- 3. Deliveries began in 1971
- a. Supplies a small amount to northern parts of
the city
- D. Future Aqueducts are unlikely
- 1. Belief that more water means more people and more
pollution
- a. Opposition arose to all new water sources -
Columbia River, desalination, cloud seeding, water
reclamation, etc
- 2. Water rationing first occurred in LA on July 1,
1977
I. Hydrologic Cycle
| II. Principles Of Groundwater
| III. Groundwater In Southern California
| IV. Sea Water Intrusion
| V. Methods Of Augmenting Local Water
Supplies | VI.
History Of Aqueducts In California | VII.
Who Does What With Water | VIII. The
Use Of Water | IX. Water Quality -
Nation Wide | Links | top
| Geol 357 Lecture Home
|
IX. Water Quality - Nation Wide
- A. Legislation and Enforcement
- 1. Major Legislation - Federal
- a. Federal Water Pollution Control Act (Clean
Water Act) of 1948
- (1) "
comprehensive programs for
eliminating or reducing the pollution of interstate
waters and tributaries and improving the sanitary
condition of surface and underground waters
conserve
waters for public water supplies, propagation
of fish and aquatic life, recreational purposes,
and agricultural and industrial uses" (http://laws.fws.gov/lawsdigest/fwatrpo.html)
- b. Water Quality Improvement Act of 1970
- (1) "
amended the prohibitions on
discharges of oil to allow such discharges only
when consistent with regulations to be issued
by the President and where permitted by Article
IV of the 1954 International Convention for
the Prevention of Pollution of the Sea by Oil
(33 U.S.C. 1321). In issuing regulations, the
President was authorized to determine quantities
of oil which would be harmful to the public
health or welfare of the U.S., including, but
not limited to, fish, shellfish, and wildlife,
as well as public and private property, shorelines
and beaches." (http://laws.fws.gov/lawsdigest/fwatrpo.html)
- c. Water Pollution Control Act 1972
- (1) "
stipulated broad national
objectives to restore and maintain the chemical,
physical, and biological integrity of the Nation's
waters." (http://laws.fws.gov/lawsdigest/fwatrpo.html)
- d. Toxic Substance Control Act 1976
- e. Clean Water Act 1977 (http://laws.fws.gov/lawsdigest/fwatrpo.html)
- f. Clean Air Act of 1990
- (1) This will greatly help reduce acid rain
- (2) "The primary objective of the Clean
Air Act is to establish Federal standards for
various pollutants from both stationary and
mobile sources and to provide for the regulation
of polluting emissions via state implementation
plans. In addition, the amendments are designed
to prevent significant deterioration in certain
areas where air quality exceeds national standards,
and to provide for improved air quality in areas
which do not meet Federal standards ("nonattainment"
areas)." (http://laws.fws.gov/lawsdigest/clenair.html)
- 2. EPA requires that states establish and enforce
water quality standards
- a. Standards in California are established by
the State Dept of Water Resources
- B. Acid Rain
- 1. Acid rain has become an international problem
- a. US - Canada
- b. England - Norway
- 2. Acid rain appears to be killing lakes, streams,
forests, and people
- a. Acid rain may kill 50,000 people per year in
the US (LA Times - 1/1982)
- 3. Acid rain is caused by:
- a. CO2 from cars and power plants
- b. NOx from cars
- c. SO2 from power plants
I. Hydrologic Cycle
| II. Principles Of Groundwater
| III. Groundwater In Southern California
| IV. Sea Water Intrusion
| V. Methods Of Augmenting Local Water
Supplies | VI.
History Of Aqueducts In California | VII.
Who Does What With Water | VIII. The
Use Of Water | IX. Water Quality -
Nation Wide | Links | top
| Geol 357 Lecture Home
|
- Hydrologic Cycle / Climate / Precipitation
- Groundwater
- Aqueducts
|