Evaluating the Effects of Sediment Transport on Pipe Flow Resistance
In this paper, the applicability of a theoretical flow resistance law to sediment-laden flow in pipes is tested. At first, the incomplete self-similarity (ISS) theory is applied to deduce the velocity profile and the corresponding flow resistance law. Then the available database of measurements carr...
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doaj-2ff4e88126684963ab78a11b4b8a29fc2021-08-06T15:34:01ZengMDPI AGWater2073-44412021-07-01132091209110.3390/w13152091Evaluating the Effects of Sediment Transport on Pipe Flow ResistanceVito Ferro0Alessio Nicosia1Department of Agricultural, Food and Forest Sciences, University of Palermo, Viale delle Scienze, Building 4, 90128 Palermo, ItalyDepartment of Agricultural, Food and Forest Sciences, University of Palermo, Viale delle Scienze, Building 4, 90128 Palermo, ItalyIn this paper, the applicability of a theoretical flow resistance law to sediment-laden flow in pipes is tested. At first, the incomplete self-similarity (ISS) theory is applied to deduce the velocity profile and the corresponding flow resistance law. Then the available database of measurements carried out by clear water and sediment-laden flows with sediments having a quasi-uniform sediment size and three different values of the mean particle diameter <i>D<sub>m</sub></i> (0.88 mm, 0.41 mm and 0.30 mm) are used to calibrate the Γ parameter of the power-velocity profile. The fitting of the measured local velocity to the power distribution demonstrates that (i) for clear flow the exponent δ can be estimated by the equation of Castaing et al. and (ii) for the sediment-laden flows δ is related to the diameter <i>D<sub>m</sub></i>. A relationship for estimating the parameter Г<sub>v</sub> obtained by the power-velocity profile and that Г<sub>f</sub> of the flow resistance law is theoretically deduced. The relationship between the parameter Г<sub>v</sub>, the head loss per unit length and the pipe flow Froude number is also obtained by the available sediment-laden pipe flow data. Finally, the procedure to estimate the Darcy-Weisbach friction factor is tested by the available measurements.https://www.mdpi.com/2073-4441/13/15/2091pipe flowvelocity profileflow resistancedimensional analysisself-similaritysediment transport |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Vito Ferro Alessio Nicosia |
spellingShingle |
Vito Ferro Alessio Nicosia Evaluating the Effects of Sediment Transport on Pipe Flow Resistance Water pipe flow velocity profile flow resistance dimensional analysis self-similarity sediment transport |
author_facet |
Vito Ferro Alessio Nicosia |
author_sort |
Vito Ferro |
title |
Evaluating the Effects of Sediment Transport on Pipe Flow Resistance |
title_short |
Evaluating the Effects of Sediment Transport on Pipe Flow Resistance |
title_full |
Evaluating the Effects of Sediment Transport on Pipe Flow Resistance |
title_fullStr |
Evaluating the Effects of Sediment Transport on Pipe Flow Resistance |
title_full_unstemmed |
Evaluating the Effects of Sediment Transport on Pipe Flow Resistance |
title_sort |
evaluating the effects of sediment transport on pipe flow resistance |
publisher |
MDPI AG |
series |
Water |
issn |
2073-4441 |
publishDate |
2021-07-01 |
description |
In this paper, the applicability of a theoretical flow resistance law to sediment-laden flow in pipes is tested. At first, the incomplete self-similarity (ISS) theory is applied to deduce the velocity profile and the corresponding flow resistance law. Then the available database of measurements carried out by clear water and sediment-laden flows with sediments having a quasi-uniform sediment size and three different values of the mean particle diameter <i>D<sub>m</sub></i> (0.88 mm, 0.41 mm and 0.30 mm) are used to calibrate the Γ parameter of the power-velocity profile. The fitting of the measured local velocity to the power distribution demonstrates that (i) for clear flow the exponent δ can be estimated by the equation of Castaing et al. and (ii) for the sediment-laden flows δ is related to the diameter <i>D<sub>m</sub></i>. A relationship for estimating the parameter Г<sub>v</sub> obtained by the power-velocity profile and that Г<sub>f</sub> of the flow resistance law is theoretically deduced. The relationship between the parameter Г<sub>v</sub>, the head loss per unit length and the pipe flow Froude number is also obtained by the available sediment-laden pipe flow data. Finally, the procedure to estimate the Darcy-Weisbach friction factor is tested by the available measurements. |
topic |
pipe flow velocity profile flow resistance dimensional analysis self-similarity sediment transport |
url |
https://www.mdpi.com/2073-4441/13/15/2091 |
work_keys_str_mv |
AT vitoferro evaluatingtheeffectsofsedimenttransportonpipeflowresistance AT alessionicosia evaluatingtheeffectsofsedimenttransportonpipeflowresistance |
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