4.7 Article

Experimental Observations of Bedload Tracer Movement: Effects of Mixed Particle Sizes and Bedforms

Journal

WATER RESOURCES RESEARCH
Volume 59, Issue 5, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022WR033114

Keywords

bedforms; tracers; bedform trap efficiency

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This study investigates the influence of bedforms on the transport of bedload tracer particles in rivers. The results demonstrate that bedforms act as primary controls on tracer travel distances and there is a linear relationship between bedform trapping and the ratio of bedform height to tracer grain size. The findings provide important theoretical insights for understanding particle transport.
Predicting the transport of bedload tracer particles is a problem of significant theoretical and practical interest. Yet, little understanding exists for transport in rivers in the presence of bedforms, which may trap grains and thereby influence travel distance. In a series of flume experiments with a sandy gravel bed in a large experimental flume, bed elevation and tracer travel distances were measured at high resolution for a range of discharges. As discharge increased, bedform height increased and bedform length decreased, increasing bedform steepness. For all tracer sizes and flow conditions, bedforms act as primary controls on the tracer travel distances. Bedform trapping increases linearly with the ratio of bedform height to tracer grain size, with 50% trapping efficiency for a ratio of two and 90% trapping efficiency for a ratio of four. A theoretical model based on the extended active layer formulation for sediment transport is able to capture much of the distribution of measured travel distances for all tracer sizes and discharges, providing a first connection between tracer transport theory and bedform trapping and indicating normal diffusion of tracers at relatively small timescales. Variable bedform geometry can influence trap efficiency for individual bedforms and the theoretical model can help identify preferential trapping conditions. The distribution of tracer travel distances for a mixture of grain sizes and variable discharge, as expected in natural rivers, displays heavy tail characteristics.

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