INTERTIDAL BEDFORMS AND BEDLOAD TRANSPORT ON SPRATT SAND, TEIGNMOUTH (UK)

摘要

Bedload transport on Spratt Sand is a result of migrating bedforms and a lack of sediment clearly limits the growth and development of these bedforms. Maximum bedload transport based on dune-tracking is observed for a combination of waves and currents, probably due to an increase in migration rates rather than an increase in ripple dimensions.