Environmental Geology Spring 2010 – Text Notes

Water Supply and Use

Groundwater supplies over 50% of our drinking water needs in the U.S., greater than 40% of irrigation water and about 25% of industrial water.

World Water Sources:
Ocean                       97.2%
Glaciers                     2.15%
Groundwater             0.61%
Lakes
    Fresh                 0.009%
    Saline                0.008%
Soil Moisture         0.005%
Atmosphere           0.001%
Rivers                    0.0001%

World Fresh Water:
Ice and Glaciers                  85%
Groundwater                      14%
Lakes and Reservoirs         0.6%
Soil Moisture                     0.29%
Water Vapor                     0.05%
Rivers                                0.004%

Residence Time:
Oceans                    Thousands of years (average if there is such a thing is about 5000 years)
Atmosphere             about 9 days
Rivers                      about 2 weeks
Groundwater           hundreds to many thousand years
Lakes                     tens of years
Ice and Glaciers      may be tens of thousand of years

Look over components of hydrologic cycle in your text:

Confined and Unconfined Aquifers:
Unconfined: water table is open to receive recharge (pressure at water table is equal to atmospheric pressure).  Unsaturated zone overlies the water table.  Below the water table is the zone of saturation (saturated zone).

Confined: by definition pressure is greater than atmospheric pressure therefore water will rise above the top of the aquifer unit.  The primary water bearing unit is confined (sandwiched) between lower permeability units (confining units).  If pressure is sufficient to cause the water to flow at the ground surface then it is known as a flowing artersian system.
Effluent (gaining) and Influent (losing) streams

Effluent streams gain flow from the adjacent groundwater reservoir.  Often this is sufficient to maintain flow in these streams throughout the year (even when no recent precipitation has occurred).

Influent streams lose water through infiltration and feed the underlying groundwater reservoir.  We see examples of this in many of the streams throughout the karst region of northwest Arkansas.

Water Budget:  Just like your checkbook (It’s supposed to balance!!).  Inputs = outputs

Main input is atmospheric moisture

Part of this falls as precipitation.

Of this, some infiltrates, some runs off, and some evaporates, and some is transpired by plants and animals.

In the U.S. the consumptive use is about 106 billion gallons per day (this is an early 90’s number but is still relavent today).

If we divide this by the mid-1990’s U.S. population of about 275,000.000 we find a per capita water use in the U.S. of about 385 gallons per person per day.

We went over the exercise in class to show that each of us uses about 120 gallons per day for our personal household needs not including car washing and lawn watering. The remainder of the 385 gallons/day consists of water used for the products we consume such as milk, steak, paper, etc.

A recent article by the U.S. Geological Survey indicates that when water used for power generation is included the per capita use in the U.S. rises to over 1,400 gallons per person per day.

Instream Use:
•    Navigation
•    Power generation (pass through the turbines)
•    Fish and wildlife maintenance
•    Recreation
•    Water quality maintenance

Offstream Use:
Irrigation
•    Municipal and domestic supply
•    Industrial supply
•    Power generation (cooling water that evaporates)
•    Livestock water

Consumptive vs. non-consumptive Use:

Consumptive use moves water from one reservoir to another  while non-consumptive use puts the water to use without changing the physical, or chemical characteristics of the water.  Off stream uses tend to be consumptive uses while instream uses tend to be non-consumptive uses.

Groundwater depletion:

Looked at a map of U.S. showing areas of significant groundwater depletion and pointed out that some areas are impacted due to agriculture (example: Ogallala Aquifer) while other areas are impacted by withdrawals for municipal (eastern seaboard, Houston) or industrial (Baton Rouge) withdrawals.

Agriculture is the largest water user, public supply is second, and self supplied industrial is third.

The Ogallala Aquifer has over 168,000 irrigation wells that irrigate over 16 million acres of land.  Over 23 million acre-feet of groundwater is withdrawn from this aquifer annually which accounts for about 30% of the groundwater used for irrigation in the U.S. each year and 20% of the U.S. irrigated land.  All with water that was put in place primarily during the last major glacial period.

Dams and Reservoirs:

Purpose:
•    Flood Control
•    Navigation
•    Recreation
•    Water supply (both irrigation and municipal use)
•    Power generation

Looked at cross section of a reservoir illustrating various pools within the reservoir including the sediment pool, upper and lower conservation pools, and the area designated for flood control.

Water Conservation:

Estimated that we can save about 20% to 30 % of current use through conservation.

Home:
Low water use landscaping (xeriscaping)
•    Rock
•    Cactus
•    Painted

Graywater Use
•    House plants
•    Lawns

Low flow toilets (they really are getting better!!)

Low flow shower heads

Shower with a friend

Drive a dirty car

Price structure to force conservation

Agricultural:
More efficient irrigation
•    Drip irrigation (not economically realistic on large scale row crop production)
•    Computer driven sprinkler systems tied to soil moisture monitors
•    Recycle waste water for irrigation use

Change to less water hungry crops

Industry:
•    Fix leaks
•    Recycle and reuse water in other plant processes

Colorado River:

Make the desert bloom

Supplies 7 states plus Mexico

First formal management 1922 with signed Colorado River Compact

Separated into Upper Basin and Lower Basin

Upper Basin allocated 7.5 million acre-feet/yr; Lower Basin allocated 8.5 million acre-feet/yr; Mexico allocated 1.5 million acre-feet/yr

Original flow estimates based on short period of record during relatively high period of flow

Actually long term average is about 13 million acre-feet/yr so the result is the river has been over-allocated by at least 4.5 million acre-feet/yr.

Tribal governments including the Navajo Nation and the Hope Nation made claims to the water under treaties with the Federal government and have been awarded substantial water rights in addition to that already allocated to the 7 states and Mexico.

Evaporation from large lakes causes increases in salinity that must be dealt with prior to releasing the flows to Mexico.  The U.S. must provide water of no greater than 900 mg/L salinity to Mexico as part of the compact agreement.  This is accomplished by desalinization of the river water near Yuma, Arizona just before it flows into Mexico (Wow!!  What an environmental mess in an area of the U.S. with the fastest growing population).

Review slides for alternate water supply options