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- W1991055868 abstract "During the past few years a series of measurements has been made of flow conditions and associated sediment motion occurring in several high-velocity tidal channels in Puget Sound, Washington. Measurements consist of the velocity distribution occurring within 2 m of the bed, visual observation of the occurrence of incipient grain movement, and time-lapse photography of the seabed. From these data estimates have been made of the mean bottom velocity (Ū100), shear velocity (U∗) and Shield's friction coefficient (θt) associated with the sediment movement. Results indicate that for mean grain sizes ranging from 0.30 mm to 1.10 mm and a variety of bed configurations the critical values of Ū100, U∗, and θt required to initiate general sediment motion agree with experimentally derived competency curves. The bed-load transport of sediment corresponding to the occurrence of general sediment motion for grain sizes approximately 0.40 mm in diameter is estimated to be 8.4·10−3 g cm−1sec−1. This movement is associated with mean velocity (Ū100) and shear velocity (U∗) of 38.5 and 2.30 cm/sec, respectively." @default.
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- W1991055868 date "1971-02-01" @default.
- W1991055868 modified "2023-09-26" @default.
- W1991055868 title "Measurements of incipient motion of sediment particles in the marine environment" @default.
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- W1991055868 doi "https://doi.org/10.1016/0025-3227(71)90049-1" @default.
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