
Environmental Encyclopedia 3
Water conservation
of the oceans and seas of the world. Only 3% of the earth’s
entire water is freshwater. This includes Arctic and Antarctic
ice,
groundwater
, and all the rivers and freshwater lakes.
The amount of usable freshwater is only about 0.003% of
the total. To put this small percentage in perspective, if the
total water supply is equal to one gallon, the volume of the
usable freshwater supply would be less than one drop. This
relatively small amount of freshwater is recycled and purified
by the
hydrologic cycle
, which includes evaporation, con-
densation, precipitation,
runoff
, and
percolation
. Since
most of life on earth depends on the availability of freshwater,
one can say “water is life.”
Worldwide, agricultural
irrigation
uses about 80% of
all freshwater. Cooling water for electrical
power plants
,
domestic consumption, and other industry use the remaining
20%. This figure varies widely from place to place. For
example, China uses 87% of its available water for agricul-
ture. The United States uses 40% for agriculture, 40% for
electrical cooling, 10% for domestic consumption, and 10%
for industrial use.
Water
conservation
may be accomplished by improv-
ing crop water utilization efficiency and by decreasing the
use of high-water-demanding crops and industrial products.
The table shows the amount of water, in pounds, required
to produce one pound of selected crops and industrial prod-
ucts (one gal = 7.8 lb).
Freshwater sources are either surface water (rivers and
lakes) or groundwater. Water that flows on the surface of
the land is called surface runoff. The relationship between
surface runoff, precipitation, evaporation, and percolation is
shown in the following equation: Surface runoff = precipita-
tion - (evaporation + percolation): When surface runoff re-
sulting from rainfall or snowmelt is confined to a well-
defined channel it is called a river or stream runoff
Groundwater is surface water that has permeated
through the
soil
particles and is trapped among porous soils
and rock particles such as sandstone or shale. The upper
zone of saturation
, where all pores are filled with water,
is the
water table
. It is estimated that the groundwater is
equal to 40 times the volume of all earth’s freshwater includ-
ing all the rivers and freshwater lakes of the world.
The movement of groundwater depends on the poros-
ity of the material that holds the water. Most groundwater is
held within sedimentary aquifers. Aquifers are underground
layers of rock and soil that hold and produce an appreciable
amount of water and can be pumped economically.
Water utilization efficiency is measured by water with-
drawal and water consumption. Water withdrawal is water
that is pumped from rivers, reservoirs, or groundwater
wells
,
and is transported elsewhere for use. Water consumption is
water that is withdrawn and returned to its source due to
evaporation or
transpiration
.
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Water consumption varies greatly throughout the
world. A conservative figure for municipal use in the United
States is around 150 gal (568 L) per person per day. This
includes home use for bathing, waste disposal, and landscape
in addition to commercial and industrial use. The total water
demand per person is around 4,500 gal (17,000 L) per person
per day when one accounts for the production of food, fiber,
and fuel. The consumptive use world wide is considerably
less than that for the United States.
According to the United Nations World Health Orga-
nization (WHO), 5 gal (18 L) per person per day is consid-
ered a minimum water requirement. The majority of the
people in the undeveloped world are unable to obtain the
five gallon per day minimum requirement. The WHO esti-
mates that nearly two billion people in the world risk con-
suming contaminated water. Waterborne diseases such as
polio, typhoid, dysentery, and
cholera
kill nearly 25 million
people per year. In order to meet this demand for freshwater,
conservation is an obvious necessity.
Since irrigation consumes 80% of the world’s usable
water, improvements in agricultural use is the logical first
step in water conservation. This can be accomplished by
lining water delivery systems with concrete or other impervi-
ous materials to minimize deep percolation or by using
drip
irrigation
systems to minimize evaporation losses. Drip irri-
gation systems have been successfully used on fruit trees,
shrubs, and landscape plants.
Subsurface irrigation is an emerging technology with
extremely high water utilization efficiency. Subsurface irriga-
tion uses a special drip irrigation tubing that is buried 6–8 in
(15–20 cm) underground with 12–24 in (26–50 cm) between
lines. The tubing contains emitters, or drip outlets, that
deliver water and dissolved nutrients at the plant’s root zone
at a desired rate. In addition to water conservation, subsur-
face irrigation has several advantages that overhead sprinklers
do not: no overwatering, no disease or
aeration
problems,
no runoff or
erosion
, no weeds, and no vandalism. Subsur-
face irrigation in California has been used on trees, field
crops, and lawns with up to 50% water savings.
Xeriscape, the use of low water consuming plants, is
a most suitable landscape to conserve water, especially in
dry, hot urban regions such as the Southwestern United
States, where approximately 50% of the domestic water con-
sumption is used by lawns and non-drought tolerant land-
scape. Plants such as cacti and succulents, ceanothus, arctos-
taphylos, which is related to foothill manzanita, trailing
rosemary (Rosemarinus officinale), and white rock rose (Cistus
cobariensis) adapt well to hot, dry climates and help conserve
water.
In addition to improving irrigation techniques, water
conservation can be accomplished by improving domestic
use of water. Such a conservation practice is the installation