Identifying sediment transport mechanisms from grain size–shape distributions, applied to aeolian sediments
Johannes Albert van Hateren et al.
Related subject area
Cross-cutting themes: Quantitative and statistical methods in Earth surface dynamicsA photogrammetry-based approach for soil bulk density measurements with an emphasis on applications to cosmogenic nuclide analysisDominant process zones in a mixed fluvial–tidal delta are morphologically distinctComputing water flow through complex landscapes, Part 3: Fill-Spill-Merge: Flow routing in depression hierarchiesDetermining the optimal grid resolution for topographic analysis on an airborne lidar datasetSystematic identification of external influences in multi-year microseismic recordings using convolutional neural networks
Earth Surf. Dynam., 8, 995–1020,2020
Earth Surf. Dynam., 8, 809–824,2020
Earth Surf. Dynam. Discuss.,2020
Revised manuscript accepted for ESurf
Earth Surf. Dynam., 7, 475–489,2019
Earth Surf. Dynam., 7, 171–190,2019
Arens, S. M., Van Boxel, J. H., and Abuodha, J. O. Z.: Changes in grain size of sand in transport over a foredune, Earth Surf. Proc. Land., 27, 1163–1175, https://doi.org/10.1002/esp.418, 2002.
Arens, S. M., Mulder, J. P., Slings, Q. L., Geelen, L. H., and Damsma, P.: Dynamic dune management, integrating objectives of nature development and coastal safety: examples from the Netherlands, Geomorphology, 199, 205–213, https://doi.org/10.1016/j.geomorph.2012.10.034, 2013.
Beal, M. A. and Shepard, F. P.: A use of roundness to determine depositional environments, J. Sediment. Res., 26, 49–60, https://doi.org/10.1306/74D704B6-2B21-11D7-8648000102C1865D, 1956.
Cox, E. P.: A method of assigning numerical and percentage values to the degree of roundness of sand grains, J. Paleontol., 1, 179–183, 1927.
Dietrich, W. E.: Settling velocity of natural particles, Water Resour. Res., 18, 1615–1626, https://doi.org/10.1029/WR018i006p01615, 1982.