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APESCH17

TermDefinition
Aquifers porous, water-bearing layers of sand, gravel, and rock below the earth's surface; reservoirs for groundwater
Artesian well the result of a pressurized aquifer intersecting the surface or being penetrated by a pipe or conduit, from which water gushes without being pumped; also called a spring
Condensation the aggregation of water molecules from vapor to liquid or solid when the saturation concentration is exceeded
Condensation Nuclei
Consumption the fraction of withdrawn water that is lost in transmission or that is evaporated, absorbed, chemically transformed, or otherwise made unavailable for other purposes as a result of human use
Degraded deteriration in water quality due to contamination or pollution; makes water nsuitable for other desirable purposes
Desalination removal of salt from water by distillation, freezing, or ultrafiltration
Dew point the temp at which condensation occurs for a given concentration of water vapor in the air
Discharge the amount of water that passes a fixed point in a given amount of time; usually expressed as liters or cubic feet of water per second
Evaporation when st turns to vapor from liquid because of heat
Groundwater water held in gravel deposits or posrous rock below the earth's surface; does not include water or crystallization held by chemical bonds in rocks or moisture in upper soil layers
Infiltration the process of water percolation into the soil and pores and hollows of permeable rocks
Rain Shadow dry area on the downwind side of a mountain
Recharge Zones area where water infiltrates into an aquifer
Relative Humidity
Renewable Water Supplies wannual freshwater surface runoff plus annual infiltration into underground freshwater aquifers that are accessible for human use
Residence Time the length of time a component, such as an individual water molecule, spends in a particular compartment or location before it moves on through a particular process or cycle
Saltwater Intrusion movement of saltwater into freshwater aquifers in coastal areas where groundwater is withdrawn faster than it is replenished
Saturation Point
Sinkholes a large surface crater caused by the collapse of an underground channel or cavern; often triggered by groundwater withdrawal
Sublimation
Subsidence a settling of the ground surface caused by the collapse of porous formations that reslt from withdrawal of large amounts of groundwater, oil, or other undergound materials
Transpiration
Water Scarcity annual available freshwater supplies less than 1000 m^3 per person
Water Stress a situation when residents of a country don't have enough accessible, high-quality water to meet their everyday needs
Water Table the top layer of the zone of saturation; undulates according to the surface topography and subsurface structure
Withdrawal a description of the total amount of water taken from a lake, river, or aquifer
Zone of Aeration upper soil layers that hold both air and water
Zone of Saturation lower soil layers where all spaces are filled with water
Created by: AlanaR
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