Measurements of aeolian mass flux distributions on a fine-grained beach: Implications for grain-bed collision mechanics
Document Type
Conference Proceeding
Publication Date
12-1-2009
Abstract
Saltation is the primary mechanism of sediment transport responsible for supplying sand to coastal dunes. Of the several sub-processes involved in saltation, the collision-rebound process is generally considered the most poorly understood. This study presents measurements of the vertical and horizontal distributions of sand mass flux collected on a fine-grained beach at Mustang Island, Texas, USA, immediately downwind of five test beds containing narrow ranges of pre-sieved sand. Measured mass flux distributions were increasingly stretched in the vertical and horizontal dimensions with increasingly large grain-sizes in the test beds. It is inferred that the effective inertia of the target bed grains imposes a limit on the rebound/launch velocity of saltating grains, such that impact energies in excess of the effective inertia are transferred to the target grains (and possibly adjacent grains) thereby setting them in motion. The characteristic scales of particle trajectories are thus substantively controlled by bed texture.
Publication Source (Journal or Book title)
Journal of Coastal Research
Number
623
First Page
337
Last Page
341
Recommended Citation
Namikas, S., Bauer, B., Edwards, B., Hesp, P., & Zhu, Y. (2009). Measurements of aeolian mass flux distributions on a fine-grained beach: Implications for grain-bed collision mechanics. Journal of Coastal Research (SPEC. ISSUE 56), 337-341. Retrieved from https://repository.lsu.edu/geoanth_pubs/623