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water is the
basis for all life
Water defines the
physical landscape, limits human activity (population size and location, economic growth), and makes patterns in nature (vegetation and wildlife)
there is only how much freshwater in the world
2.5%
the demand of water is increasing—which means there is rising consumption—meanwhile the supply is remaining somewhat stable, this results in
an increasing gap between supply and demand of water
has water consumption and water withdrawals risen, dropped, or stayed the same compared to the human population?
water consumption and water withdrawals have risen
Water geopolitics are
Trade-offs between consumption and instream values, producing conflict (like Syria)
the basic water needs of many people
are not being met
as of 2025,
2 billion people lack access to clean water and 4.4 billion people lack clean water at home
the result of people lacking access to clean water is
250 million (2019 estimate) cases of water-related diseases, 3.5 million deaths each year, and > 1,000 children under 5 die every day on average
2.5 billion people rely on
groundwater supplies; in US - 38%
21 of 37 largest aquifers are being depleted worldwide, or in other words have
exceeded sustainability tipping points
some areas of Mexico City are
sinking at 1 inch per month
in Beijing, the water table has
dropped 1,000 feet since the 1970’s
Houston is the
fastest sinking major city in the US
What is subsidence?
the downward vertical movement of the Earth’s surface
Subsidence is due primarily to
ground water (GW) pumping, also oil extraction
subsidence causes major
damage to infrastructure (roads, buildings, underground pipelines; changes in drainage patterns; making some infrastructure obsolete)
Aquifer pores are the interconnected spaces within
the rock or sediment that allow groundwater to flow
Aquifer pores are drying up, which results in
compaction within the aquifer which is permanent damage (can’t hold as much water as before)
the inflow of water and the outflow of water are
not balanced
Aquifer water turns over much more
slowly than most other water pools
rates of turnover for aquifer water can be
100s to 1,000’s of years (the range in turnover rate is large)
what is Fossil Water?
an aquifer not actively being recharged, they are nonrenewable
more than 75% of groundwater
is nonrenewable
it is critical for water management and policy to have a clear distinction
and identification between renewable and non-renewable water tables
renewable aquifers depend on
current rainfall for recharge
in Edward’s Aquifer, pumping has increased
4x since the 1930s, and at times now exceeds annual recharge rates
increased water withdrawal makes aquifers more susceptible to
climatic changes and contamination - like saltwater intrusion
links between surface and ground waters are most important in regions
with low rainfall (like arid and semi-arid regions) (33% of earth’s surface, 20% of global population-primary source of water for drinking and irrigation)
in areas of low rainfall, results are
limited in opportunities for aquifer recharge, and are highly susceptible to depletion
the water footprint of a product contains the sum of
the volume of freshwater used for production (water consumed + water polluted throughout the supply chain)
does it cost more to pump groundwater or use rain to irrigate cropland?
cost more to pump groundwater, rain = free
what are the order of categories that use land in the US from least to greatest?
Miscellaneous — cemeteries, golf courses, areas of “low economic value like marshes or deserts” — (3.6%)
Urban (3.7%)
Special Use—national parks, wildlife areas, highways, railroads, military bases (8.9%)
Cropland (20.7%)
Forest (28.5%)
Pasture/Range (34.6%)
what is the current rate of change?
an increase in urban area of 1,000,000 acres per year (area of Los Angeles, Houston, and Phoenix combined)
why do we care about the California drought?
$35 billion in agricultural revenue – most productive in US
70% of US-produced fruits and nuts
55% of vegetables
22% of milk and cream
Nation’s sole producer of a dozen crops
State employs 27% of all farm workers in the US
what are the different variable resources for water
variable in space, variable in time, variable in quality
what are the different variables in space?
variations over large or small distances, globally, regionally, locally
what are different variables in time
duration, frequency, amounts, hourly, daily, monthly, seasonally, annually, cycles
what are different variables in quality
sediments, contaminants, natural state
Precipitation: Local Spatial Variability - Goliad, Texas example
Goliad, Texas
Two stations located about one mile apart
One in Goliad
The other about 1 mile SE of town
37 years between 1950 and 2004
Average annual rainfall in Goliad is 35.80 inches
Average at the station 1 mile SE of Goliad is 32.19 inches
Mean annual rainfall at the Goliad 1SE location is more similar to mean annual rainfall at Beeville (31.13 inches) 31 miles southwest of the Goliad 1SE location than it is to the Goliad station 1 mile north.
List the three water resource problems
Problems of absolute supply (quantity)
Problems of regimen (timing)
Problems of quality
Solutions for Absolute Supply Problems (Quantity)
1) Importation of water from an area in which a surplus occurs naturally.
2) Weather modifications - rain-making or cloud seeding
3) Desalinization of Brackish Water
4) Reduction of evapotranspiration losses
Explain the importation of water from an area in which a surplus occurs naturally
One of the oldest solutions used by man (Roman Aqueducts).
Many present-day examples:
Texas Water Import Plan- 1970’s
Lake Alan Henry
Owens Valley, CA
Provide drinking water to Los Angeles
Year Completed 1913
Construction Duration 5 years
Aqueduct Capacity 485 cfs (cubic feet per second)
Construction Cost < $23million ($1.5 billion in today’s money)
Total Length of Aqueduct ~233 miles
Drained Owens Lake dry
Left a salt flat
Now have a problem with dust storms
Pumping ground water
Mojave Desert – 4” of rainfall average in some places
Ample groundwater from runoff off Sierra Nevada Mountains
Led to significant legal issues with residents
Lubbock, Texas
Prior to 2011
Majority of water from Lake Meredith
In 2011
Voters approved 16% rate increase on water bills
50-mile pipeline and water treatment system
Drawing water from Lake Alan Henry in 2013
Today
Most water comes from Lake Alan Henry
GW from Bailey and Roberts Counties
...a bit from Lake Meredith
Weather modifications - rain-making or cloud seeding
Spread chemicals
Silver iodide, potassium iodide, dry ice, table salt
Done by aircraft or dispersion devices on the ground
Studies have produced mixed results
Concern about the chemicals
Do occur in low concentrations
Concern regarding sensitive wildlife species
2008 Summer Olympics in Beijing
Tried to prevent rain clouds from reaching Beijing during the opening and closing ceremonies
**NOT currently a viable solution
Desalinization of Brackish Water
Not practical
Expensive
$1.32 to $4.27 per 1000 gallons just for desalinization
Lower cost – treatment of brackish water
Higher cost – treatment of seawater
Additional costs for piping of water
Translates to $429-$1390 per acre-foot
Too expensive for irrigation
Saudi Arabia
30 facilities
Produce 11.5 million cubic meters / day
1.5 million barrels of oil / day
Solar power instead
Currently at 120 megawatts
Slated to grow to 770 megawatts
Costs?
Riyadh – capital city
Currently requires 1.6 million cubic meters / day
Expected - 6 million cubic meters / day by 2030
Cost – do or die…
Australia
All energy produced by solar
Produce grown hydroponically in one location
Shipped across the continent
Reduction of evapotranspiration losses
Reduce the amount of energy available for vaporization of water
Examples
Lining canals – increase velocity, reduce evaporation losses
Shading channels with vegetation - cooling
Wind breaks
Use of black “shade balls”
Millions of black balls floating on surface
Reduce solar radiation reaching the water
Lower temperature
Black vs. white – reduce UV absorption causing formation of carcinogenic bromate
Solar panels over canals
Reduce losses due to evaporation
Cooling of panels, so operate more efficiently
what are the problems of regimen (timing)
1) Solutions to High Flows
2) Solutions to Low Flows
what are the solutions to high flows?
Otherwise known as “Flooding”
Increase channel capacity to handle excess flows
Decrease volume of flow so it does not exceed channel capacity
Remember: both high and low flows are natural!
Benefits to high flows?
Some desert riparian vegetation requires flooding to clear away debris and allow for germination and optimal production
describe the 2019 floods in the midwest
Over $3 billion in damages
$1.6 billion in Iowa
$1.3 billion in Nebraska
3 deaths
describe the 2013 floods in colorado
100-year storm in mountainous terrain
Over $2 billion in damages
2000 homes destroyed, 17,500 homes damaged
200 miles of roads and 50 bridges damaged
what are some solutions to low flows?
Need storage and regulation to give even flow
Dams and reservoirs
Evaporation is chief cause of losses
list the problems of water quality:
No simple solution exists!
Options
When water is naturally unsuitable for use
Develop a different source
Treat to make usable
With anthropogenic unsuitability
Careful use of lands and potential polluting agents
Treatment of wastes prior to discharge into streams
Modification of waste disposal to take advantage of natural conditions
definition of a watershed:
an area of land drained by (or which sheds its water into) a stream or river system
Synonymous with “catchment” or “drainage basin”
management refers to what?
the act, art or manner of managing, controlling, directing, etc.
Watershed Management Defined
The management of land for the “optimum” production of high-quality water, the regulation of water yields and for maximum soil stability, along with other products of the land.
list the three principal aspects, or ingredients, of watershed management
water, land (or landscape), manipulation (or management)
objectives of watershed management
Maintain and / or increase water yields
Maintain and / or improve water quality
Regulate timing of stream flow
Control excessive soil erosion and excessive runoff
Excessive implies man-induced
historical development of watershed management
1342
First known governmental action for watershed protection
Establishment of a “forest preserve” in Switzerland
1833
First action in the US
New York – created the Adirondack Forest Preserve
“to protect the headwaters of the chief rivers of the state”
1890
Congressional appropriations for rain making experiments
1908
Arizona – first forest experiment station
Many additional “simplistic” attempts
Only in last 30 years have studies become more extensive and scientifically rigorous
Decision to do nothing is still a decision
1910
Wagon Wheel Gap, Colorado
Classic watershed experiment
Paired watersheds in Rio Grande Basin
Installed gauges for precipitation and stream flow
Clearcut one of the watersheds in 1919
Saw increases
Runoff – max daily, high-flow volumes, average annual yield
Erosion