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Bedform alignment in directionally varying flows.

D M Rubin, R E Hunter

    Science (New York, N.Y.)
    |July 17, 1987
    PubMed
    Summary
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    Sediment bedform orientation is often used to infer sediment transport direction. However, experiments show bedforms can trend in various directions, challenging this assumption for accurate transport analysis.

    Area of Science:

    • Geomorphology
    • Sediment Transport Dynamics
    • Fluid Mechanics

    Background:

    • Sediment bedforms are commonly assumed to align perpendicular or parallel to sediment transport direction.
    • This assumption underpins the use of observed bedform trends from remote sensing and field studies to determine transport pathways.

    Purpose of the Study:

    • To experimentally investigate the relationship between bedform orientation and sediment transport direction under bidirectional flow conditions.
    • To test the validity of presumptions regarding bedform trend as a sole indicator of sediment transport direction.

    Main Methods:

    • Controlled laboratory experiments using a rotating sand-covered board in steady winds to simulate bidirectional flows.
    • Systematic variation of the angle between two wind components and the proportion of sand transport in each direction.

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  • Observation and analysis of resultant bedform types (transverse, oblique, longitudinal) and their orientation relative to transport.
  • Main Results:

    • Experimental bedforms, regardless of their classification (transverse, oblique, longitudinal), consistently oriented to maximize gross sediment transport across them.
    • A significant proportion of generated bedforms exhibited trends that were neither perpendicular nor parallel to the resultant sediment transport direction.
    • Bedform orientation was found to be dependent on the interplay between flow direction components and sediment transport proportions.

    Conclusions:

    • The study demonstrates that the orientation of sediment bedforms is not a reliable sole indicator of sediment transport direction.
    • Presuming bedform alignment (transverse or parallel) can lead to inaccurate estimations of sediment transport pathways.
    • Understanding the complex dynamics of bidirectional flows is crucial for accurately interpreting geomorphological evidence of sediment movement.