Chapter 10-Water: Hydrologic Cycle and Human Use Flashcards
The degree to which water is pure enough to fulfill the requirements of various uses
Water quality
The amount of water available to meet demands
Water quantity
Water having a salt concentration below 0.1%; as a result of purification by evaporation, all forms of precipitation are freshwater, as are lakes, rivers, groundwater, and other bodies of water that have a throughflow of water from precipitation
Freshwater
Water that contains at least 3% salt (30 parts salt per 1,000 parts water), typical of oceans and seas
Saltwater
A mixture of freshwater and saltwater, typically found where rivers enter the ocean
Brackish water
Water that contains minerals, especially calcium or magnesium, that cause soap to precipitate, producing a scum, curd, or scale in boilers
Hard water
Water that is relatively free of minerals
Soft water
Water that contains one or more impurities, making it unsuitable for a desired use
Polluted water
Water that has pollutants removed or is rendered harmless
Purified water
Water from precipitation that runs off of land surfaces in surges
Storm water
Water in vapor form originating from water bodies, the soil, and organisms-the source of water for precipitation. Water vapor
Green water
Precipitation, renewable surface water runoff and groundwater recharge-the focus of management and the main source of water for human withdrawals and natural ecosystems. Liquid water
Blue water
Also called the hydrologic cycle; the movement of water from points of evaporation, through the atmosphere, through precipitation, and through or over the ground, returning to points of evaporation
Water cycle
Water rising to the atmosphere
Evaporation
The loss of water vapor as it moves from the soil through green plants and exits through leaf pores, or stomata
Transpiration
Formation of liquid water from a gas state
Condensation
Release of water from clouds in form of rain, sleet, snow, or hail
Precipitation
The amount of water vapor in the air
Humidity
The amount of water vapor as a percentage of what the air can hold at a particular temperature. Humidity is usually measures using this
Relative humidity
Droplets that form in the atmosphere
Fog and clouds
Droplets that form on the cool surfaces of vegetation
Dew
Microscopic liquid or solids particles originating from land and water surfaces
Aerosols
Occurs when warm air rises, expands and cools (lower pressure)
Adiabatic cooling
Occurs when the air descends and is compressed by the higher air pressure in the lower atmosphere
Adiabatic warming