Spatiotemporal bedload transport patterns over two-dimensional bedforms
<p>Despite a rich history of studies investigating fluid dynamics over bedforms and dunes in rivers, the spatiotemporal patterns of sub-bedform bedload transport remain poorly understood. Previous experiments assessing the effects of flow separation on downstream fluid turbulent structures and...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2023-09-01
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| Series: | Earth Surface Dynamics |
| Online Access: | https://esurf.copernicus.org/articles/11/835/2023/esurf-11-835-2023.pdf |
| _version_ | 1797692386378252288 |
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| author | K. C. P. Leary L. Tevis M. Schmeeckle |
| author_facet | K. C. P. Leary L. Tevis M. Schmeeckle |
| author_sort | K. C. P. Leary |
| collection | DOAJ |
| description | <p>Despite a rich history of studies investigating fluid dynamics over bedforms and dunes in rivers, the spatiotemporal patterns of sub-bedform bedload transport remain poorly understood. Previous experiments assessing the effects of flow separation on downstream fluid turbulent structures and bedload transport suggest that localized, intermittent, high-magnitude transport events (i.e., permeable splat events) play an important role in both downstream and cross-stream bedload transport near flow reattachment. Here, we report results from flume experiments that assess the combined effects of flow separation–reattachment and flow re-acceleration over fixed two-dimensional bedforms (1.7 cm high; 30 cm long). A high-speed camera observed bedload transport along the entirety of the bedform at 250 frames per second. Grain trajectories, grain velocities, and grain transport directions were acquired from bedload images using semiautomated particle-tracking techniques. Downstream and vertical fluid velocities were measured 3 mm above the bed using laser Doppler velocimetry (LDV) at 15 distances along the bedform profile. Mean downstream fluid velocity increases nonlinearly with increasing distance along the bedform. However, observed bedload transport increases linearly with increasing distance along the bedform, except at the crest of the bedform, where both mean downstream fluid velocity and bedload transport decrease substantially. Bedload transport time series and manual particle-tracking data show a zone of high-magnitude, cross-stream transport near flow reattachment, suggesting that permeable splat events play an essential role in the region downstream of flow reattachment.</p> |
| first_indexed | 2024-03-12T02:26:52Z |
| format | Article |
| id | doaj.art-3fbb747e083d4058a5d9e229fded37b7 |
| institution | Directory Open Access Journal |
| issn | 2196-6311 2196-632X |
| language | English |
| last_indexed | 2024-03-12T02:26:52Z |
| publishDate | 2023-09-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Earth Surface Dynamics |
| spelling | doaj.art-3fbb747e083d4058a5d9e229fded37b72023-09-05T11:44:07ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2023-09-011183584710.5194/esurf-11-835-2023Spatiotemporal bedload transport patterns over two-dimensional bedformsK. C. P. Leary0L. Tevis1M. Schmeeckle2New Mexico Bureau of Geology and Mineral Resources, Socorro, NM, USADepartment of Earth and Environmental Sciences, New Mexico Tech, Socorro, NM, USASchool of Geographical Sciences and Urban Planning, Arizona State University, Tempe, AZ, USA<p>Despite a rich history of studies investigating fluid dynamics over bedforms and dunes in rivers, the spatiotemporal patterns of sub-bedform bedload transport remain poorly understood. Previous experiments assessing the effects of flow separation on downstream fluid turbulent structures and bedload transport suggest that localized, intermittent, high-magnitude transport events (i.e., permeable splat events) play an important role in both downstream and cross-stream bedload transport near flow reattachment. Here, we report results from flume experiments that assess the combined effects of flow separation–reattachment and flow re-acceleration over fixed two-dimensional bedforms (1.7 cm high; 30 cm long). A high-speed camera observed bedload transport along the entirety of the bedform at 250 frames per second. Grain trajectories, grain velocities, and grain transport directions were acquired from bedload images using semiautomated particle-tracking techniques. Downstream and vertical fluid velocities were measured 3 mm above the bed using laser Doppler velocimetry (LDV) at 15 distances along the bedform profile. Mean downstream fluid velocity increases nonlinearly with increasing distance along the bedform. However, observed bedload transport increases linearly with increasing distance along the bedform, except at the crest of the bedform, where both mean downstream fluid velocity and bedload transport decrease substantially. Bedload transport time series and manual particle-tracking data show a zone of high-magnitude, cross-stream transport near flow reattachment, suggesting that permeable splat events play an essential role in the region downstream of flow reattachment.</p>https://esurf.copernicus.org/articles/11/835/2023/esurf-11-835-2023.pdf |
| spellingShingle | K. C. P. Leary L. Tevis M. Schmeeckle Spatiotemporal bedload transport patterns over two-dimensional bedforms Earth Surface Dynamics |
| title | Spatiotemporal bedload transport patterns over two-dimensional bedforms |
| title_full | Spatiotemporal bedload transport patterns over two-dimensional bedforms |
| title_fullStr | Spatiotemporal bedload transport patterns over two-dimensional bedforms |
| title_full_unstemmed | Spatiotemporal bedload transport patterns over two-dimensional bedforms |
| title_short | Spatiotemporal bedload transport patterns over two-dimensional bedforms |
| title_sort | spatiotemporal bedload transport patterns over two dimensional bedforms |
| url | https://esurf.copernicus.org/articles/11/835/2023/esurf-11-835-2023.pdf |
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