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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 4
Earth Surf. Dynam., 6, 1011-1021, 2018
https://doi.org/10.5194/esurf-6-1011-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Surf. Dynam., 6, 1011-1021, 2018
https://doi.org/10.5194/esurf-6-1011-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 07 Nov 2018

Research article | 07 Nov 2018

Uniform grain-size distribution in the active layer of a shallow, gravel-bedded, braided river (the Urumqi River, China) and implications for paleo-hydrology

Laure Guerit1, Laurie Barrier2, Youcun Liu3, Clément Narteau2, Eric Lajeunesse2, Eric Gayer2, and François Métivier2 Laure Guerit et al.
  • 1GET, Université de Toulouse, CNRS, IRD, UPS, Toulouse, France
  • 2Institut de Physique du Globe de Paris – Sorbonne Paris Cité, Université Paris Diderot, CNRS, UMR 7154, Paris, France
  • 3School of Resources and Environmental Engineering, Jiangxi University of Science and Technology, Ganzhou 341000, China

Abstract. The grain-size distribution of ancient alluvial systems is commonly determined from surface samples of vertically exposed sections of gravel deposits. This method relies on the hypothesis that the grain-size distribution obtained from a vertical cross section is equivalent to that of the riverbed. Such an hypothesis implies first that the sediments are uniform in size in the river bed, and second that the sampling method implemented on a vertical section leads to a grain-size distribution equivalent to the bulk one. Here, we report a field test of this hypothesis on granulometric samples collected in an active, gravel-bedded, braided stream: the Urumqi River in China. We compare data from volumetric samples of a trench excavated in an active thread and from surface counts performed on the trench vertical faces. Based on this data set, we show that the grain-size distributions obtained from all the samples are similar and that the deposit is uniform at the scale of the river active layer, a layer extending from the surface to a depth of approximately 10 times the size of the largest clasts. As a consequence, the grid-by-number method implemented vertically leads to a grain-size distribution equivalent to the one obtained by a bulk volumetric sampling. This study thus brings support to the hypothesis that vertical surface counts provide an accurate characterization of the grain-size distribution of paleo-braided rivers.

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The grain-size distribution of ancient alluvial systems is commonly determined from sections of gravel deposits exposed vertically to reconstruct paleo-environments or changes in tectonics and/or climate. To test whether such a grain-size distribution is equivalent to one of the sediments that was in direct contact with the flow at the time of deposition, we dug a large trench in an active gravel-bedded, braided river. We show that the granulometry is uniform at the scale of the active layer.
The grain-size distribution of ancient alluvial systems is commonly determined from sections of...
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