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- W4238936229 abstract "Abstract The detachment and transportation of soil is termed soil erosion. Every stream carries some sediment in suspension and moves larger particles along its bed. The deposition of sediment in channels or reservoirs creates a variety of problems, such as raising stream beds, meandering and overflow along the banks, and, of course, depletion of storage capacity in reservoirs. The sediment content in river waters varies with flow conditions. It is small in lean flow months, but it attains a maximum value during floods. The total quantity of sediment transported annually to the sea by rivers of the world is about 2 × 10 10 tons or about 13.5 km 3 in volume. Worldwide, reservoirs are annually losing about 1% of their storage capacity or about 65 km 3 /year. The rate of loss of reservoir storage in the United States is about 0.22%/year which is equivalent to 2020 million m 3 /year. Based on weighted average data from 144 reservoirs in India, the annual loss of gross storage was estimated at 0.44%. Sediment source and reservoir locations are not uniformly distributed; the problem is really severe in some countries. China has more than 80,000 reservoirs that are annually losing, on average, 2.3% of their storage capacity due to sedimentation." @default.
- W4238936229 created "2022-05-12" @default.
- W4238936229 creator A5017131679 @default.
- W4238936229 date "2004-10-15" @default.
- W4238936229 modified "2023-10-10" @default.
- W4238936229 title "Reservoir Sedimentation" @default.
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- W4238936229 doi "https://doi.org/10.1002/047147844x.sw786" @default.
- W4238936229 hasPublicationYear "2004" @default.
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