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Books on the topic 'Sediment salinity'

Author: Grafiati
Published: 25 January 2025

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1

D, Boon John, Virginia. Dept. of Transportation., and Virginia Institute of Marine Science., eds. Three dimensional hydrodynamic-sedimentation modeling study: Hampton Roads Crossing, Lower James River, Virginia : a report to the Virginia Department of Transportation. Gloucester Point, Va: Virginia Institute of Marine Science, Dept. of Physical Science, 1999.

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2

T, Yost Brian, Geological Survey (U.S.), California. Dept. of Water Resources., and California. State Water Resources Control Board., eds. Description of salinity, temperature, chlorophyll, suspended-sediment, and velocity data, south San Francisco Bay, California, February-April 1987. Sacramento, Calif: U.S. Geological Survey, 1990.

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3

T, Yost Brian, Geological Survey (U.S.), California. Dept. of Water Resources, and California. State Water Resources Control Board, eds. Description of salinity, temperature, chlorophyll, suspended-sediment, and velocity data, south San Francisco Bay, California, February-April 1987. Sacramento, Calif: U.S. Geological Survey, 1990.

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4

Rogowski, David. Saltwater intrusion in Salmon Bay and Lake Union sediments. [Olympia, Wash.]: Washington State Dept. of Ecology, 2000.

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5

Riedel-Lorjé, Jeannette Cornelie. Salzgehalts- und Trübstoffverhältnisse in dem oberen Brackwassergebiet der Elbe. [Hamburg]: Wassergütestelle Elbe, 1992.

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6

Baldys, S. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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7

Baldys, S. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Geological Survey, 1996.

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8

S, Baldys. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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9

Baldys, S. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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10

S, Baldys. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Geological Survey, 1996.

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11

S, Baldys. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Geological Survey, 1996.

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12

S, Baldys. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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13

Baldys, S. Effects of low-flow diversions from the South Wichita River on downstream salinity of the South Wichita River, Lake Kemp, and the Wichita River, north Texas, October 1982-September 1992. Austin, Tex: U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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14

Brazil/U.S. Workshop on Physical Oceanography (1987 Ocean Process Analysis Laboratory). Brazil/U.S. Workshop on Physical Oceanography Held on 3-6 August 1987. Durham, NH: Ocean Process Analysis Laboratory, Institute for the Study of Earth, Oceans and Space, University of New Hampshire, 1987.

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15

Monabbati, Mehran. Effect of salinity and organic matter content of sediments on the sediment-water exchange of arsenic. 1999.

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16

Sheppard, Charles R. C., Simon K. Davy, Graham M. Pilling, and Nicholas A. J. Graham. Coral reefs. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198787341.003.0001.

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Abstract:
Coral reefs are the ocean’s richest ecosystem in terms of biodiversity and productivity. They are restricted to tropical waters, where conditions of salinity, temperature and sedimentation are suitable. Where they grow, their main benthic organisms deposit substantial limestone skeletons, such that they effectively make their own habitat which sustains their dynamic nature and supports the wide range of species which inhabit them. Reefs grow to the low tide level, thus providing a breakwater, but the richest parts lie 5–20 metres below the surface, an area where light is still sufficient but where sediment and turbulence are not severe. Reefs may occur as narrow fringing reefs bordering a continental coast, as huge offshore barrier reefs or as series of atolls that support entire nations; the biogenic nature of corals is enormously important to mankind.
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