Chapter 9 Review

chapter 9Review

Page 317

In this chapter, we have learned that fresh water is a critical, scarce resource. The major sources of fresh water are groundwater, surface water, and atmospheric water. When groundwater is extracted faster than it is replaced, we can experience dry water wells and saltwater intrusion. Humans alter the availability of water by constructing levees, dikes, and dams to constrain water movement. We transport water from one place to another using aqueducts and we are able to convert salt water into fresh water through distillation or reverse osmosis. The use of water among countries can be determined by calculating the water footprint of a country; developed countries typically have a larger water footprint than developing countries. Most water is used for agriculture, followed by industrial and household use. Recent changes in each of these sectors have improved water use and reuse efficiency and conservation.

Key Terms

Question

Aquifer
Unconfined aquifer
Confined aquifer
Water table
Groundwater recharge
Spring
Artesian well
Cone of depression
Saltwater intrusion
Floodplain
Impermeable surface
Levee
Dike
Dam
Reservoir
Fish ladder
Aqueduct
Desalination
Desalinization
Distillation
Reverse osmosis
Water footprint
Hydroponic agriculture
Gray water
Contaminated water
A stair-like structure that allows migrating fish to get around a dam.
The uppermost level at which the water in a given area fully saturates rock or soil.
Wastewater from toilets, kitchen sinks, and dishwashers.
A barrier that runs across a river or stream to control the flow of water.
An infiltration of salt water in an area where groundwater pressure has been reduced from extensive drilling of wells.
An area lacking groundwater due to rapid withdrawal by a well.
The process of removing the salt from salt water. Also known as Desalination.
The cultivation of plants in greenhouse conditions by immersing roots in a nutrient-rich solution.
An aquifer surrounded by a layer of impermeable rock or clay that impedes water flow.
A process by which water percolates through the soil and works its way into an aquifer.
A process of desalination in which water is boiled and the resulting steam is captured and condensed to yield pure water.
The water body created by a damming a river or stream.
A structure built to prevent ocean waters from flooding adjacent land.
The total daily per capita use of fresh water.
A canal or ditch used to carry water from one location to another.
A process of desalination in which water is forced through a thin semipermeable membrane at high pressure.
Wastewater from baths, showers, bathrooms, and washing machines.
The land adjacent to a river.
The process of removing the salt from salt water. Also known as Desalinization.
An aquifer made of porous rock covered by soil out of which water can easily flow.
A natural source of water formed when water from an aquifer percolates up to the ground surface.
A permeable layer of rock and sediment that contains groundwater.
Pavement or buildings that do not allow water penetration.
An enlarged bank built up on each side of a river.
A well created by drilling a hole into a confined aquifer.

Learning Objectives Revisited

Module 26 The Availability of water

Module 27 Human Alteration of Water Availability

Module 28 Water Use by Humans Now and in the Future

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