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Environmental Science: A Global Concern 5/e Cunningham/Saigo | |||||
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Chapter Key Terms |
Chapter 19: Water Use and Management |
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aquifers |
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Porous, water-bearing layers of sand, gravel, and rock below the earth's surface; reservoirs for groundwater. |
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artesian |
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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. |
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condensation |
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The aggregation of water molecules from vapor to liquid or solid when the saturation concentration is exceeded. |
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condensation nuclei |
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Tiny particles that float in the air and facilitate the condensation process. |
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consumption |
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The fraction of withdrawn water that is lost in transmission or that is evaporated, absorbed, chemically transformed, or otherwise made unavailable for other purposes as a result of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. |
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degradation (of water resource) |
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Deterioration in water quality due to contamination or pollution; makes water unsuitable for other desirable purposes. |
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desalination |
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Removal of salt from water by distillation, freezing, or ultrafiltration. |
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dew point |
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The temperature at which condensation occurs for a given concentration of water vapor in the air. |
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discharge |
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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. |
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evaporation |
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The process in which a liquid is changed to vapor (gas phase). |
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groundwater |
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Water held in gravel deposits or porous rock below the earth's surface; does not include water or crystallization held by chemical bonds in rocks or moisture in upper soil layers. |
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infiltration |
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The process of water percolation into the soil and pores and hollows of permeable rocks. |
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rain shadow |
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Dry area on the downwind side of a mountain. |
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recharge zone |
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Area where water infiltrates into an aquifer. |
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relative humidity |
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At any given temperature, a comparison of the actual water content of the air with the amount of water that could be held at saturation. |
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residence time |
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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. |
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runoff |
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The excess of precipitation over evaporation; the main source of surface water and, in broad terms, the water available for human use. |
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saltwater intrusion |
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Movement of saltwater into freshwater aquifers in coastal areas where groundwater is withdrawn faster than it is replenished. |
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saturation point |
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The maximum concentration of water vapor the air can hold at a given temperature. |
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sinkholes |
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A large surface crater caused by the collapse of an underground channel or cavern; often triggered by groundwater withdrawal. |
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stable runoff |
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The fraction of water available year round; usually more important than total runoff when determining human uses. |
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sublimation |
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The process by which water can move between solid and gaseous states without ever becoming liquid. |
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subsidence |
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A settling of the ground surface caused by the collapse of porous formations that result from withdrawal of large amounts of groundwater, oil, or other underground materials. |
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water table |
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The top layer of the zone of saturation; undulates according to the surface topography and subsurface structure. |
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withdrawal |
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A description of the total amount of water taken from a lake, river, or aquifer. |
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zone of aeration |
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Upper soil layers that hold both air and water. |
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zone of saturation |
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Lower soil layers where all spaces are filled with water. |
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