Chapter 13 Flashcards
Zone of saturation
The spaces in soil and rock close to the earth’s surface
hold little moisture. However, below a certain depth, in
the zone of saturation, these spaces are completely
filled with water.
Water table
The top of this groundwater zone
Aquifers
underground caverns and porous layers of sand, gravel, or rock through which groundwater flows
Surface water
the freshwater from precipitation and melted snow that flows across the earth’s land surface and into lakes, wetlands, streams, rivers, estuaries, and ultimately into the oceans.
Surface runoff
Precipitation that does not infiltrate the ground or return to the atmosphere by evaporation is called
Watershed or drainage basin
The land from which surface water drains into a particular river, lake, wetland, or other body of water is called its
Reliable runoff
According to water scientists (hydrologists), two-thirds of the annual surface runoff into rivers and streams is lost in seasonal floods and is not available for human use. The remaining one-third is
Drought
a prolonged period in which precipitation is at least 70% lower than average and evaporation is higher than normal in a particular area.
Groundwater
one of our most important sources of freshwater and a key component of the earth’s natural capital.
Desalinization
involves removing dissolved salts from
ocean water or from brackish (slightly salty) water in
aquifers or lakes. It is another way to increase supplies
of freshwater
Floodplain
A flood happens when water in a stream overflows its normal channel and spills into an adjacent area, called a