Articles | Volume 7, issue 3
https://doi.org/10.5194/esurf-7-723-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-7-723-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Aug 2019
Research article |
| 09 Aug 2019
| 09 Aug 2019
Seeking enlightenment of fluvial sediment pathways by optically stimulated luminescence signal bleaching of river sediments and deltaic deposits
Elizabeth L. Chamberlain
CORRESPONDING AUTHOR
Department of Earth and Environmental Sciences, Tulane University, New
Orleans, LA, USA
Department of Earth and Environmental Sciences, Vanderbilt University,
Nashville, TN, USA
Netherlands Centre for Luminescence Dating & Soil Geography and
Landscape group, Wageningen University, Wageningen, the Netherlands
Jakob Wallinga
Netherlands Centre for Luminescence Dating & Soil Geography and
Landscape group, Wageningen University, Wageningen, the Netherlands
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- Determining the Age of Terrace Formation Using Luminescence Dating—A Case of the Yellow River Terraces in the Baode Area, China J. Zhang et al. 10.3390/mps3010017
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- Holocene sedimentary evolution of the Mekong River floodplain, Cambodia Y. Ishii et al. 10.1016/j.quascirev.2020.106767
- Luminescence dating of tsunami deposits from the algarve shelf, Portugal D. Brill et al. 10.1016/j.quageo.2024.101513
- Luminescence dating of Holocene sediment cores from a wave-dominated and mountainous river delta in central Vietnam S. Qiaola et al. 10.1016/j.quageo.2022.101277
- Cross-comparison of last glacial radiocarbon and OSL ages using periglacial fan deposits S. Palstra et al. 10.1016/j.quageo.2020.101128
- Illuminating past river incision, sediment source and pathways using luminescence signals of individual feldspar grains (Rangitikei River, New Zealand) A. Guyez et al. 10.1002/esp.5357
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Latest update: 19 Nov 2024
Short summary
Sand and mud may take many different pathways within a river as they travel from inland to the coast. During the trip, grains may be exposed to daylight, resetting a signal trapped within certain minerals. The signal can be measured in a laboratory to estimate the time since last light exposure. Here, we measure the trapped signal of sand and mud grains from the Mississippi River and its banks. We use this information to infer sediment pathways. Such knowledge is useful for delta management.
Sand and mud may take many different pathways within a river as they travel from inland to the...
