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- W2023462661 abstract "Approximately 40 min of boundary-layer data were collected while sediment was in motion over the floor of a tidal channel in Puget Sound, Washington. Measurements consisted of bottom photographs using stereo cameras and underwater television, velocity measurements throughout the water column, and the collection and analysis of bottom sediment. Results suggest that processes of marine erosion are similar to those observed in laboratory experiments. The threshold of grain motion measured in the field compares favorably with existing competency curves for mean sizes ranging from 0.3 mm to 1.10 mm. Within the framework of the observations the rate of ripple migration roughly corresponds to the fifth power of the mean velocity 10 cm from the bed. It appears that the existing sediment erosion relationships, although derived from conditions greatly different from the marine environment (shallow flumes using uniform sand), are applicable to the conditions measured in the study area and may have application in the marine environment in general." @default.
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- W2023462661 date "1967-06-01" @default.
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- W2023462661 title "Measurements of sediment movement and ripple migration in a shallow marine environment" @default.
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- W2023462661 doi "https://doi.org/10.1016/0025-3227(67)90081-3" @default.
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