EP23E-08
Traveling at the Speed of Light: Using Luminescence to Estimate Sediment Transport Rates

Tuesday, 15 December 2015: 15:25
2005 (Moscone West)
Harrison J Gray, University of Colorado at Boulder, Earth Sciences, Boulder, CO, United States, Gregory E Tucker, University of Colorado at Boulder, Boulder, CO, United States and Shannon Mahan, United States Geological Survey, Denver, CO, United States
Abstract:
Most people live near a river which is actively transporting sediment, and for many, a change in sediment
dynamics can greatly a ffect livelihoods. A better understanding of sediment transport mechanics is critical
for improving our coexistence with river systems, especially in the face of a changing climate. However,
there are currently few ways in which to measure and quantify sediment transport rates in rivers. Tracer
experiments are laborious and time consuming, sediment traps are diffcult to construct without altering
flow dynamics, and reservoir in fill methods require long observation timescales. The difficulty in obtaining
these data has precluded its collection on a large scale and is limiting progress within the fi eld. A method
that circumvents these issues would be invaluable.
We present a new means to estimate the sediment transport rates of rivers using luminescence, a property
of minerals used by the geoscience community for geochronology. Luminescence is a concentration of energy
stored within the crystal lattice of minerals that can be removed by sunlight and restored by natural radiation.
We use a continuity equation to describe the change in luminescence equivalent doses as a function of
downstream distance and compare against eld data. Our model can reproduce fi eld measurements from
two rivers with varying sediment transport styles for fi ne sand (180-200 µm). The fi eld data and modeling
results reveal two patterns of interest for both rivers: an upstream region showing a gradual decline in
luminescence followed by a region where the luminescence is approximately constant. When the observed
luminescence is spatially constant, this represents a balance between bleaching and in flux of unbleached
sediment. The information obtained from applying the model to these regions can be used to estimate
sediment velocity and erosion and deposition of unbleached and bleached grains. Potential exists to extend
the model to bedload transport.