Characteristics of breaking and abrasion mechanisms acting on fluvial sediments during production and transport processes: relationships between rock type, grain size, and roundness of gravel and sand
Author:
Affiliation:
1. Department of Geography, Rissho University
2. Department of Geography, Tokyo Metropolitan University
Publisher
The Sedimentological Society of Japan
Link
https://www.jstage.jst.go.jp/article/jssj/78/1/78_15/_pdf
Reference55 articles.
1. Blom, A., Viparelli, E. and Chavarrías, V., 2016, The graded alluvial river: Profile concavity and downstream fining. American Geophysical Union Publications, 6285-6293, doi: 10.1002/2016GL068898.
2. Boggs, S.Jr., 2013, Principles of Sedimentology and Stratigraphy, fifth edition. Pearson New International Edition, Harlow, Pearson Education Limited, Essex, 564 p.
3. Brewer, P. A. and Lewin, J., 1993, In-transport modification of alluvial sediment: Field evidence and laboratory experiments. Special Publications of the International Association of Sedimentologists, 17, 23-35.
4. Domokos, G., Jerolmack, D.J., Sipos. A.A. and Török, Á., 2014, How river rocks round: resolving the shape-size paradox. PLoS ONE 9 (2), e88657, doi:10.1371/journal.pone.0088657.
5. Dumitriu, D., Niculiţă, M., and Condorachi, D., 2011, Downstream variation in the pebble morphometry of the Trotuş River, Eastern Carpathians (Romania). Forum geografic, 10, 78-90, doi:10.5775/fg.2067-4635.2011.00008.i.
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