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| 1 . |
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The hydrologic cycle operates across the entire surface of the planet, from several kilometers below ground level to several kilometers above it.
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| 2 . |
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As water evaporates from a lake surface, there is a release of latent heat to the lake, and a resulting increase in water temperature.
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| 3 . |
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Potential evapotranspiration is the amount of water that would evaporate and transpire under optimum conditions.
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| 4 . |
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Compared to an evaporation pan, a lysimeter is a simpler, but less accurate, device for determining potential evapotranspiration.
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| 5 . |
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The wilting point is the point at which soil particles contain only hygroscopic water, which is unavailable to plants.
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| 6 . |
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As soil-moisture recharge removes soil water, plants must exert greater effort to extract the same amount of moisture.
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Permeability is the amount of pore space in soil.
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| 8 . |
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The zone of aeration is the part of the subsurface in which pores are not completely filled with water.
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| 9 . |
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The height to which water can rise without the aid of pumps is refered to as the aquiclude.
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| 10 . |
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A confined aquifer is less susceptible to surface pollution than is an unconfined aquifer.
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| 11 . |
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Aquifers can collapse as a result of overpumping, causing the ground above them to subside.
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| 12 . |
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Earth's largest known aquifer, the High Plains Aquifer, would require about 1000 years to recover from historic pumping if all groundwater mining stopped today.
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