Experimental determination of the flood wave transformation and the sediment resuspension in a small regulated stream in an agricultural catchment

Zumr, David; Dostál, Tomáš; Devátý, Jan; Valenta, Petr; Rosendorf, Pavel; Eder, Alexander; Strauss, Peter

doi:https://doi.org/10.5194/hess-21-5681-2017

Articles | Volume 21, issue 11

https://doi.org/10.5194/hess-21-5681-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/hess-21-5681-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 21, issue 11

Research article

|

16 Nov 2017

Research article |

| 16 Nov 2017

Experimental determination of the flood wave transformation and the sediment resuspension in a small regulated stream in an agricultural catchment

David Zumr, Tomáš Dostál, Jan Devátý, Petr Valenta, Pavel Rosendorf, Alexander Eder, and Peter Strauss

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Final revised paper (published on 16 Nov 2017)
Preprint (discussion started on 06 Jun 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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RC1: 'Paper review on Zumr et al.', Anonymous Referee #1, 05 Jul 2017
RC2: 'Fine Sediment Transport in Agricultural Drainage, in the Czech Republic', Anonymous Referee #2, 07 Jul 2017
AC1: 'Authors replies to the reviewers comments', David Zumr, 10 Aug 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (further review by Editor) (26 Aug 2017) by Patricia Saco

AR by David Zumr on behalf of the Authors (05 Sep 2017) Author's response Manuscript

ED: Publish as is (25 Sep 2017) by Patricia Saco

AR by David Zumr on behalf of the Authors (03 Oct 2017)

Short summary

Intensively cultivated landscape is the main non-point source of eroded sediment. The soil particles, carrying bounded nutrients and pollutants, cause both environmental and economic problems downstream. We did several flooding experiments in a typical rural drainage channel to show how the eroded sediment behaves in the headwater streams during spring and summer. We conclude that the channel behaves as a sediment trap during summer. In spring the sediment moves quickly.