Water
resources
Most
abundant, but also most essential of resources. Needed to drink (potable), washing (hygene), energy
(hydroelectric), industry.
Distribution
very different matter as either
too little - drought
too much - floods
Either
causes problems
Water
Use
Domestic - each person uses minimum 190gals/year just to survive.
washing
etc extras
Agriculture
- irrigation
Industrial
Use in
each sector depends on country's economy
Domestic Agric Industry
US 10 40 50
Japan 10 70 20
Ger/UK 20-30 10 60-70
India 5 85-90 5-10
Global
distribution of Water
1.36 x
1021 km3 97.2
% in oceans, 2.15% ice caps - but inaccessible
Our
requirements met by 0.65% remaining
.001%
atmosphere
.0001
rivers streams
.009
% freshwater lakes
.008%
saline lakes and inland seas
.005%
soil water (vadose)
.31%
shallow ground water (less than 1km)
.31%
deep ground water
Global
precipation
Cycling
of water in the Earth : the
hydrologic cycle
Water
one of the few earth resources that is renewable
Evaporation
Precipitation - rain, snow, hail. Factors effecting precipitation
collection
of precipitation
Runnoff
rivers streams and lakes -
Factors
effecting ratio between runnoff and infiltration
Infiltration - vadose and groundwater zones
Evapotranspiration
- roots take up
soil moisture and is exhaled through leaves. A large tree may transpire 2 - 300 gals/day!!
Groundwater
Major
source of potable water.
Porosity and permeability of rocks.
Aquifers and aquitards
Water
table
Phreatic
zone, vadose zone
Slope
of water table (head) and flow of groundwater (in S florida not
much slope natural flow rates about
1-2m/day)
Springs where water table meets the ground surface - discharge - and lowering of water table
Head
and discharge (also permeability)
Lakes
and water table level
also
rivers
Recharge
of water table and seasonal fluctuations
Aquitards(aquicludes)
and perched water tables
Wells
and water table
Cone of
depression of water table around regularly pumped well
Drawdown
(in S Florida domestic well few inches; well fields 7-8ft)
Artesian
Wells
Florida
situation- Floridan aquifer and
wells at John Pennekamp and Chekika
park
Oases
Contamination
of groundwater
Sources
of contamination:
human/animal
wastes (bacteria); industrial wastes , gas stations, factories
etc (toxic wastes)
Flow of
groundwater - filtering action, time of flow to discharge point
Limestone
(Karst) Aquifers
Solution
of limestone; developement of caves
Surface
drainage in karst areas - swallow holes and sink holes
Groundwater
flow in karst areas - conduit flow
in caves
Surface
Water
Drainage
patterns and drainage basins
divides
Flow
in streams and rivers
Stream
gauging
Hydrographs
Importance
in design of dams etc
Dams
Primary
purpose: control of water for domestic/agricultural purposes
Secondary: benefit in some cases - capacity to
generate electricity if discharge and head sufficiently great.
Design
of dams
Use
of water
Usage
(withdrawal) and consumption
usage
(withdrawal)
- quantity physically extracted
consumption – that portioj of
withdrawal removed from system – withheld from returning to source
US usage
6130 liters(1620 gallons) per person per day. Household 400 liters (105 gallons). Total usage needed to maintain
lifestyle often overlooked.
Drinking
water
Treatment:
filtration,
"scrubbing",
addition of chlorine for disinfectant purposes, fluoridation
Irrigation
To grow
crops in areas of low rainfall.
Now 42% of US usage - more
in west than east due to rainfall patterns (80-90% in India and Mexico). Consumes vast amount of water (due to
evaporation)
Industry
and mining
85%
returned (therefore less consumption than for irrigation). Problem is quality of that water
– pollution
Hydroelectric
power
Dominates
US water usage, but consumes little.
In US most of potential developed. Rest of world could develop 7 times
present capacity. Problem is often
that power isn’t generated where most needed
Desalinization
of water
In
island and coastal communities desalinization of seawater may make sense,
although expensive.
Distillation
Electrodialysis
Reverse
Osmosis
Freezing
Disposal
of brine an issue as is a contaminant
Saudi
Arabia, Curaçao, Catalina Islance (California)
Ownership
of water - water law
Eastern US: rule is Riperian Law - right of every landowner to make reasonable use
of water. Abundance and scarcities shared equally (nobody upstream can legally
take all water for example) Exception municipalities get preferred treatment in
time of scarcity (eminent domain)
Western US: rule is Prior appropriation whoever got permission to use water
first has first rights to it - ie oldest appropriation honored first. Grew out of 1849 gold rush.
(Los Angeles bought rights to Owen's Valley water in
1900's environmentalists and OV residents say LA is "stealing" their
water, but LA sauyst by "prior appropriation" their use is legal)
Groundwater
rights
Legal
decisions on groundwater more difficult than surface because less obvious. Many early descisions made on
assumption of unlimited quantities
Environmental
water rights
Increasingly
damage to environment of misuse of water recognized. Human needs do not now automatically prevail over natural
needs. Endangered Species Act,
Wetlands Act have been used to
restore
Water
supply problems
Drought
Groundwater
depletion
Sustained
extraction that exceeds recharge will cause a problem. Ogallala aquifer (Miocene gravel) of
High Plains depleted by 150,000 wells.
Not just
US but a global problem
Ground
subsidence
Extraction
of water can lower not just water table, but land. New Orleans, Ganges delta (Bangla Desh), Santa Clara
Valley(California), Houston-Galveston.
Soil
deterioration
salinization
and alkalinazation in irrigated arid regions, desertification.
Salt
Water Intrusion
Contamination
in coastal aquifers. Effect of urbanization - increased drawdown because of
use; reduced recharge
(infiltration) because of roads, buildings, storm sewers intrusions, etc. Result in "salt water
intrusions"
some
Florida Water issues
Surface
water system in South Florida
Okeechobee
and Everglades system; pollution problem
in Everglades; Everglades restoration.
Kissimmee
River project
Biscayne
and Floridan aquifers
Geology
of Biscayne aquifer, karstification increases porosity
Hawthorn
aquitard
Flow
patterns in Biscayne aquifer
Contamination
problems
High
level of water table; gas
stations, dry cleaners, industry all
polluters
Municipal
land fills west of urban area
Salt
water intrusions
Ground
subsidence and sinkholes
Central
Florida region