Version 1
: Received: 3 April 2019 / Approved: 4 April 2019 / Online: 4 April 2019 (12:22:36 CEST)
Version 2
: Received: 4 April 2019 / Approved: 5 April 2019 / Online: 5 April 2019 (15:26:21 CEST)
Version 3
: Received: 8 April 2019 / Approved: 9 April 2019 / Online: 9 April 2019 (12:31:43 CEST)
How to cite:
Kuriqi, A.; Koçileri, G.; Ardıçlıoğlu, M. Recalling Meyer-Peter and Müller Approach for Assessment of Bed-Load Sediment Transport. Preprints2019, 2019040050. https://doi.org/10.20944/preprints201904.0050.v3
Kuriqi, A.; Koçileri, G.; Ardıçlıoğlu, M. Recalling Meyer-Peter and Müller Approach for Assessment of Bed-Load Sediment Transport. Preprints 2019, 2019040050. https://doi.org/10.20944/preprints201904.0050.v3
Kuriqi, A.; Koçileri, G.; Ardıçlıoğlu, M. Recalling Meyer-Peter and Müller Approach for Assessment of Bed-Load Sediment Transport. Preprints2019, 2019040050. https://doi.org/10.20944/preprints201904.0050.v3
APA Style
Kuriqi, A., Koçileri, G., & Ardıçlıoğlu, M. (2019). Recalling Meyer-Peter and Müller Approach for Assessment of Bed-Load Sediment Transport. Preprints. https://doi.org/10.20944/preprints201904.0050.v3
Chicago/Turabian Style
Kuriqi, A., Gerti Koçileri and Mehmet Ardıçlıoğlu. 2019 "Recalling Meyer-Peter and Müller Approach for Assessment of Bed-Load Sediment Transport" Preprints. https://doi.org/10.20944/preprints201904.0050.v3
Abstract
In this paper is discussed sediment transport as a mechanical process that characterises a natural stream or channel flow regime. The objective of experimental work presented in this paper is to recall and to give another prospect of well-known Meyer-Peter and Müller approach for estimation of Shield’s number (θ_c,θ) in laboratory conditions, and calibration of dimensionless MPM number (A). For this purpose two different experiments are conducted, during the first experiment water amount flushed on the flume and bed slope was changed simultaneously until equilibrium state is achieved, meanwhile is estimated the critical Shield’s number (θ_c). While, during the second experiment, water amount was kept constant, only bed slope of flume was continuously tilted, meanwhile sediment, discharge and Shield’s number (θ) was determined for given hydraulic conditions. In addition calibration of dimensionless MPM number (A) was performed, where several iteration were considered until for (A=3.42), sediment discharge measured become almost equal with sediment discharge computed by using MPM formula. After these experiments, is concluded that MPM formula can be used also for other certain initial condition and similar procedure may be adopted to calibrate the dimensionless MPM number (A) .
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.