Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream

Direct bedload samples were taken with a large metal basket at the steep Erlenbach stream in Switzerland. These measurements were compared with the signal of the Swiss impact plate geophone system to derive information about bedload transport. The so-called amplitude histogram (AH) method was develo...

Full description

Bibliographic Details
Main Authors: Rickenmann Dieter, Steeb Nicolas, Badoux Alexandre
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:E3S Web of Conferences
Online Access:https://doi.org/10.1051/e3sconf/20184002009
id doaj-d55ca5208b6e4b2ebcfbae6b7219d1fb
record_format Article
spelling doaj-d55ca5208b6e4b2ebcfbae6b7219d1fb2021-03-02T09:52:13ZengEDP SciencesE3S Web of Conferences2267-12422018-01-01400200910.1051/e3sconf/20184002009e3sconf_riverflow2018_02009Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach streamRickenmann DieterSteeb NicolasBadoux AlexandreDirect bedload samples were taken with a large metal basket at the steep Erlenbach stream in Switzerland. These measurements were compared with the signal of the Swiss impact plate geophone system to derive information about bedload transport. The so-called amplitude histogram (AH) method was developed in an earlier study to estimate the bedload flux for different grain-size classes at the Erlenbach. A new analysis of a larger set of measurements was made here to improve the performance of the AH method. The approach relies on an identification of the transported grain sizes through their dependency on the signal amplitude. As a new element we introduce here the impulse rate, which is found to affect the number of impulses recorded for each amplitude class. As compared to the original method, the new version of the AH method shows a slightly improved performance for total calculated bedload mass, and results in a clearly better agreement between calculated and measured characteristic grain sizes.https://doi.org/10.1051/e3sconf/20184002009
collection DOAJ
language English
format Article
sources DOAJ
author Rickenmann Dieter
Steeb Nicolas
Badoux Alexandre
spellingShingle Rickenmann Dieter
Steeb Nicolas
Badoux Alexandre
Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
E3S Web of Conferences
author_facet Rickenmann Dieter
Steeb Nicolas
Badoux Alexandre
author_sort Rickenmann Dieter
title Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
title_short Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
title_full Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
title_fullStr Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
title_full_unstemmed Improving bedload transport determination by grain-size fraction using the Swiss plate geophone recordings at the Erlenbach stream
title_sort improving bedload transport determination by grain-size fraction using the swiss plate geophone recordings at the erlenbach stream
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2018-01-01
description Direct bedload samples were taken with a large metal basket at the steep Erlenbach stream in Switzerland. These measurements were compared with the signal of the Swiss impact plate geophone system to derive information about bedload transport. The so-called amplitude histogram (AH) method was developed in an earlier study to estimate the bedload flux for different grain-size classes at the Erlenbach. A new analysis of a larger set of measurements was made here to improve the performance of the AH method. The approach relies on an identification of the transported grain sizes through their dependency on the signal amplitude. As a new element we introduce here the impulse rate, which is found to affect the number of impulses recorded for each amplitude class. As compared to the original method, the new version of the AH method shows a slightly improved performance for total calculated bedload mass, and results in a clearly better agreement between calculated and measured characteristic grain sizes.
url https://doi.org/10.1051/e3sconf/20184002009
work_keys_str_mv AT rickenmanndieter improvingbedloadtransportdeterminationbygrainsizefractionusingtheswissplategeophonerecordingsattheerlenbachstream
AT steebnicolas improvingbedloadtransportdeterminationbygrainsizefractionusingtheswissplategeophonerecordingsattheerlenbachstream
AT badouxalexandre improvingbedloadtransportdeterminationbygrainsizefractionusingtheswissplategeophonerecordingsattheerlenbachstream
_version_ 1724238394898251776