- Ray Kenny
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The hydrologic cycle describes the complex and dynamic distribution, transfer and temporary storage of water over and under the Earth's surface. As the term cycle suggests, there is a recurring succession of events (evaporation, condensation, precipitation, surface runoff, subsurface infiltration, and evapotranspiration) that keep nearly all near-surface water in an endless circulation pattern (Figure H5). Figure H5
All of Earth's surface and near-surface water has accumulated through a gradual release of water from volcanic activity (juvenilewater). The primary reservoir of water is the ocean, which contains greater than 97% of all surface water on Earth. Solar energy evaporates water from the ocean; approximately 13 million metric tons of water per year per average square kilometer are converted to atmospheric vapor. The amount of water evaporated varies conside ...
- Bouwer, H. (1978) Groundwater Hydrology. New York: McGraw-Hill, 480 pp.
- Drever, J.I. (1988) The Geochemistry of Natural Waters. New Jersey: Prentice Hall, 437 pp.
- Driscoll, F.G. (1986) Groundwater and Wells. Minnesota: Johnson Filtration Systems, 1089 pp.
- Freeze, R.A. and Cherry, J.A. (1979) Groundwater. New Jersey: Prentice Hall, 604 pp.
- Manning, J.C. (1992) Applied Principles of Hydrology. New York: MacMillan, 294 pp.
- Biogeochemistry; Carbon cycle; Earth's atmosphere; Earth's ocean geochemistry; Geochemistry: low temperature; Hydrogen isotopes; \ Nitrogen cycle; Oxygen isotopes; Paleoenvironments; Sulfate reduction; Sulfur cycle; Water
- Hydrologic cycle
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- pp 330-331
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- Encyclopedia of Earth Science
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- Springer Netherlands
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- Kluwer Academic Publishers
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