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Water Resources and Water
Pollution
Chapter 11
Freshwater is an irreplaceable resource that we
are managing poorly
- Freshwater is relatively pure and contains few
dissolved salts.
- Earth has a precious layer of water—most of it
saltwater—covering about 71% of the earth’s
surface.
- Water is an irreplaceable chemical with unique
properties that keep us and other forms of life
alive. A person could survive for several weeks
without food, but for only a few days without
water.
Freshwater is an irreplaceable resource that we
are managing poorly
- Concerns regarding water include:
- Access to freshwater is a global health issue. Every day an average of 3,900 children younger than age 5 die from waterborne infectious diseases.
- An economic issue – vital for reducing poverty and producing food and energy.
- A women’s and children’s issue in developing countries because poor women and girls often are responsible for finding and carrying daily supplies of water.
Freshwater is an irreplaceable resource that we
are managing poorly
- A national and global security issue because of increasing tensions within and between nations over access to limited water resources that they share.
- An environmental issue because excessive withdrawal of water from rivers and aquifers results in dropping water tables, lower river flows, shrinking lakes, and losses of wetlands.
Most of the earth’s freshwater is not available to us
- The world’s freshwater supply is continually
collected, purified, recycled, and distributed in
the earth’s hydrologic cycle, except when:
- Overloaded with pollutants.
- We withdraw water from underground and surface water supplies faster than it is replenished.
- We alter long-term precipitation rates and distribution patterns of freshwater through our influence on projected climate change.
Most of the earth’s freshwater is not available to us
- Freshwater is not distributed evenly.
- Differences in average annual precipitation and economic resources divide the world’s continents, countries, and people into water haves and have- nots.
- Canada, with only 0.5% of the world’s population, has 20% of the world’s liquid freshwater, while China, with 19% of the world’s people, has only 7% of the supply.
Groundwater and surface water are
critical resources
- Aquifers: underground caverns and porous layers of sand, gravel, or bedrock through which groundwater flows—typically moving only a meter or so (about 3 feet) per year and rarely more than 0.3 meter (1 foot) per day.
- Watertight layers of rock or clay below such aquifers keep the water from escaping deeper into the earth.
Groundwater and surface water are critical resources
- Surface water is the freshwater from precipitation
and snowmelt that flows across the earth’s land
surface and into lakes, wetlands, streams, rivers,
estuaries, and ultimately to the oceans.
- Precipitation that does not infiltrate the ground or return to the atmosphere by evaporation is called surface runoff.
- The land from which surface water drains into a particular river, lake, wetland, or other body of water is called its watershed, or drainage basin.
We use a large and growing portion of the world’s reliable runoff
- Worldwide, about 70% of the water we
withdraw each year comes from rivers, lakes,
and aquifers to irrigate cropland, industry uses
another 20%, and residences 10%.
- Affluent lifestyles require large amounts of
water.
Freshwater shortages will grow
- The main factors that cause water scarcity in any
particular area are a dry climate, drought, too
many people using a water supply more quickly
than it can be replenished, and wasteful use of
water.
- More than 30 countries—mainly in the Middle
East and Africa—now face water scarcity.
- By 2050, 60 countries, many of them in Asia, with
three-fourths of the world’s population, are likely
to be suffering from water stress.
Groundwater is being withdrawn faster than it is
replenished in some areas
- Aquifers provide drinking water for nearly half of
the world’s people.
- Most aquifers are renewable resources unless their
water becomes contaminated or is removed faster
than it is replenished by rainfall.
- Water tables are falling in many areas of the world
because the rate of pumping water from aquifers
(mostly to irrigate crops) exceeds the rate of natural
recharge from rainfall and snowmelt.
Groundwater is being withdrawn faster than it is
replenished in some areas
- The world’s three largest grain producers—China, India, and the United States—as well as Mexico, Saudi Arabia, Iran, Yemen, Israel, and Pakistan are overpumping many of their aquifers.
Overpumping of aquifers has several harmful effects
- Groundwater overdrafts near coastal areas can
pull saltwater into freshwater aquifers. The
resulting contaminated groundwater is
undrinkable and unusable for irrigation.
- Deep water aquifers hold enough freshwater to
support billions of people for centuries.
- Concerns about tapping these ancient deposits of
freshwater:
- They are nonrenewable and cannot be replenished on a human timescale.
Overpumping of aquifers has several
harmful effects
- Little is known about the geological and ecological impacts of pumping large amounts of freshwater from deep aquifers.
- Some deep aquifers flow beneath more than one country and there are no international treaties that govern rights to them. Without such treaties, water wars could break out.
- The costs of tapping deep aquifers are unknown and could be high.