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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Main Authors: Vito Ferro, Alessio Nicosia
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/15/2091
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spelling 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
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