A Unified Approach to Bed Load Transport Description Over a Wide Range of Flow Conditions via the Use of Conditional Data Treatment

Bed load transport is a highly nonlinear phenomenon. Numerous stress‐transport power relations, with exponents varying between 1.5 and 16, have been proposed to capture the entire range of solid discharge trends exhibited by experimental data. A physics‐based explanation of the variation in exponent...

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description Bed load transport is a highly nonlinear phenomenon. Numerous stress‐transport power relations, with exponents varying between 1.5 and 16, have been proposed to capture the entire range of solid discharge trends exhibited by experimental data. A physics‐based explanation of the variation in exponent values is provided here. The concept of time‐resolved local stream power is used to determine the above‐threshold energy available for mobilizing bed materials, giving rise to solid discharge estimates. The generated transport capacity records, analyzed by a long‐term averaging process, allow for the construction of bed load curves that resemble the trends frequently reported in prior experimental studies. Under such conditions, use of long‐term averaged bed shear stress and bed load transport rates provide practical, yet oversimplified accounts of the transport phenomenon. The limitation of this methodology is particularly evident in low‐to‐moderate transport rates, where the calculated bed shear stress and consequent bed load transport rates are underestimated compared to values based on active periods of sediment movement. As the degree of intermittency in bed load transport increases, so does the exponent to compensate for the inactive periods of bed mobility. Conditionally averaged stress‐transport data, based on the active periods of bed load transport alone, however, exhibit a constant trend, reasonably well represented by a 1.5 power formula across the entire transport range. This approach better reflects the prevailing cause and effect relation by properly accounting for varied transport timescales. Furthermore, the resulting transport trend signifies a nearly constant efficiency in entraining and transporting sediment particles. Plain Language Summary Bed load transport is a complex phenomenon involving nonlinear interactions between the fluid and solid particle dynamics. The conventional quantitative methods, based on a long‐term averaging framework, lead to various power regression equations that link the bed load transport rates to the bed shear stress values, with exponents varying from 1.5 to 16, or even higher exponents, over a wide range of transport scenarios. The highly varied exponent values represent uncertainties that will compromise the utility of such empirical regression formulas in assessing bed load transport rates at different flow conditions. The unique contribution of this work is to elaborate on the underlying mechanism responsibl
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Numerous stress‐transport power relations, with exponents varying between 1.5 and 16, have been proposed to capture the entire range of solid discharge trends exhibited by experimental data. A physics‐based explanation of the variation in exponent values is provided here. The concept of time‐resolved local stream power is used to determine the above‐threshold energy available for mobilizing bed materials, giving rise to solid discharge estimates. The generated transport capacity records, analyzed by a long‐term averaging process, allow for the construction of bed load curves that resemble the trends frequently reported in prior experimental studies. Under such conditions, use of long‐term averaged bed shear stress and bed load transport rates provide practical, yet oversimplified accounts of the transport phenomenon. The limitation of this methodology is particularly evident in low‐to‐moderate transport rates, where the calculated bed shear stress and consequent bed load transport rates are underestimated compared to values based on active periods of sediment movement. As the degree of intermittency in bed load transport increases, so does the exponent to compensate for the inactive periods of bed mobility. Conditionally averaged stress‐transport data, based on the active periods of bed load transport alone, however, exhibit a constant trend, reasonably well represented by a 1.5 power formula across the entire transport range. This approach better reflects the prevailing cause and effect relation by properly accounting for varied transport timescales. Furthermore, the resulting transport trend signifies a nearly constant efficiency in entraining and transporting sediment particles. Plain Language Summary Bed load transport is a complex phenomenon involving nonlinear interactions between the fluid and solid particle dynamics. The conventional quantitative methods, based on a long‐term averaging framework, lead to various power regression equations that link the bed load transport rates to the bed shear stress values, with exponents varying from 1.5 to 16, or even higher exponents, over a wide range of transport scenarios. The highly varied exponent values represent uncertainties that will compromise the utility of such empirical regression formulas in assessing bed load transport rates at different flow conditions. The unique contribution of this work is to elaborate on the underlying mechanism responsible for the variation in exponent values. Furthermore, a conditional data treatment is applied to the entire range of solid discharge trends, which appropriately accounts for the varied transport timescales shown at different levels of bed mobilization. This approach gives rise to a reasonably consistent power regression with exponents of 1.5. This 1.5th power relation signifies a nearly constant energy transfer efficiency by which the flow can entrain and transport sediment materials. These findings provide a better understanding of the transport mechanism(s) and facilitate the development of a consistent and physically meaningful bed load transport expression. Key Points Conditionally averaged stress‐transport data exhibit a consistent 1.5th power relation over the entire bed load transport range Long‐term averaged flow strength descriptors properly account for high levels of solid discharge conditions Impulse‐based considerations are important in reflecting the timescale effect imposed by bed load intermittency at low transport cases</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/2017WR022373</identifier><language>eng</language><publisher>Washington: John Wiley &amp; Sons, Inc</publisher><subject>Bed load ; bed load intermittency ; bed load transport ; Bottom stress ; Capacity ; conditional data treatment ; Data ; Discharge ; Dynamics ; Empirical analysis ; Energy transfer ; Entrainment ; Exponents ; Formulas (mathematics) ; Frameworks ; Interactions ; Load distribution ; Mathematical models ; Nonlinear phenomena ; Particle dynamics ; Physics ; Regression analysis ; Sediment ; Sediment load ; Sediment movement ; Sediment transport ; Sediments ; Shear stress ; stream power ; Transport ; Transport phenomena ; Trends ; turbulence</subject><ispartof>Water resources research, 2018-05, Vol.54 (5), p.3490-3509</ispartof><rights>2018. 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All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3684-c1a0c2c5cfa683f7ecf3c2a25b013f50a61cb4af56cc8ffae98be5acd4ca87573</citedby><cites>FETCH-LOGICAL-a3684-c1a0c2c5cfa683f7ecf3c2a25b013f50a61cb4af56cc8ffae98be5acd4ca87573</cites><orcidid>0000-0002-5860-4179</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2017WR022373$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2017WR022373$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,11494,27903,27904,45553,45554,46446,46870</link.rule.ids></links><search><creatorcontrib>Shih, WuRong</creatorcontrib><creatorcontrib>Diplas, Panayiotis</creatorcontrib><title>A Unified Approach to Bed Load Transport Description Over a Wide Range of Flow Conditions via the Use of Conditional Data Treatment</title><title>Water resources research</title><description>Bed load transport is a highly nonlinear phenomenon. Numerous stress‐transport power relations, with exponents varying between 1.5 and 16, have been proposed to capture the entire range of solid discharge trends exhibited by experimental data. A physics‐based explanation of the variation in exponent values is provided here. The concept of time‐resolved local stream power is used to determine the above‐threshold energy available for mobilizing bed materials, giving rise to solid discharge estimates. The generated transport capacity records, analyzed by a long‐term averaging process, allow for the construction of bed load curves that resemble the trends frequently reported in prior experimental studies. Under such conditions, use of long‐term averaged bed shear stress and bed load transport rates provide practical, yet oversimplified accounts of the transport phenomenon. The limitation of this methodology is particularly evident in low‐to‐moderate transport rates, where the calculated bed shear stress and consequent bed load transport rates are underestimated compared to values based on active periods of sediment movement. As the degree of intermittency in bed load transport increases, so does the exponent to compensate for the inactive periods of bed mobility. Conditionally averaged stress‐transport data, based on the active periods of bed load transport alone, however, exhibit a constant trend, reasonably well represented by a 1.5 power formula across the entire transport range. This approach better reflects the prevailing cause and effect relation by properly accounting for varied transport timescales. Furthermore, the resulting transport trend signifies a nearly constant efficiency in entraining and transporting sediment particles. Plain Language Summary Bed load transport is a complex phenomenon involving nonlinear interactions between the fluid and solid particle dynamics. The conventional quantitative methods, based on a long‐term averaging framework, lead to various power regression equations that link the bed load transport rates to the bed shear stress values, with exponents varying from 1.5 to 16, or even higher exponents, over a wide range of transport scenarios. The highly varied exponent values represent uncertainties that will compromise the utility of such empirical regression formulas in assessing bed load transport rates at different flow conditions. The unique contribution of this work is to elaborate on the underlying mechanism responsible for the variation in exponent values. Furthermore, a conditional data treatment is applied to the entire range of solid discharge trends, which appropriately accounts for the varied transport timescales shown at different levels of bed mobilization. This approach gives rise to a reasonably consistent power regression with exponents of 1.5. This 1.5th power relation signifies a nearly constant energy transfer efficiency by which the flow can entrain and transport sediment materials. These findings provide a better understanding of the transport mechanism(s) and facilitate the development of a consistent and physically meaningful bed load transport expression. Key Points Conditionally averaged stress‐transport data exhibit a consistent 1.5th power relation over the entire bed load transport range Long‐term averaged flow strength descriptors properly account for high levels of solid discharge conditions Impulse‐based considerations are important in reflecting the timescale effect imposed by bed load intermittency at low transport cases</description><subject>Bed load</subject><subject>bed load intermittency</subject><subject>bed load transport</subject><subject>Bottom stress</subject><subject>Capacity</subject><subject>conditional data treatment</subject><subject>Data</subject><subject>Discharge</subject><subject>Dynamics</subject><subject>Empirical analysis</subject><subject>Energy transfer</subject><subject>Entrainment</subject><subject>Exponents</subject><subject>Formulas (mathematics)</subject><subject>Frameworks</subject><subject>Interactions</subject><subject>Load distribution</subject><subject>Mathematical models</subject><subject>Nonlinear phenomena</subject><subject>Particle dynamics</subject><subject>Physics</subject><subject>Regression analysis</subject><subject>Sediment</subject><subject>Sediment load</subject><subject>Sediment movement</subject><subject>Sediment transport</subject><subject>Sediments</subject><subject>Shear stress</subject><subject>stream power</subject><subject>Transport</subject><subject>Transport phenomena</subject><subject>Trends</subject><subject>turbulence</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2018</creationdate><recordtype>article</recordtype><recordid>eNp9kEtLw0AUhQdRsFZ3_oALbo3OK5lkWesTCoXQ0mW4nczoSMzEmWhx7R83tSKuXB0u5-NwzyHklNELRnlxySlTq5JyLpTYIyNWSJmoQol9MqJUioSJQh2SoxifKWUyzdSIfE5g2TrrTA2Trgse9RP0Hq6Ge-axhkXANnY-9HBtog6u651vYf5uAiCsXG2gxPbRgLdw2_gNTH1buy0T4d0h9E8GlvHb_nWwgWvscYg22L-Ytj8mBxabaE5-dEyWtzeL6X0ym989TCezBEWWy0QzpJrrVFvMcmGV0VZojjxdUyZsSjFjei3RppnWubVoinxtUtS11JirVIkxOdvlDj1f30zsq2f_FoZ_YsVpxrhUskgH6nxH6eBjDMZWXXAvGD4qRqvtzNXfmQdc7PCNa8zHv2y1KqclF0JI8QUQhn-b</recordid><startdate>201805</startdate><enddate>201805</enddate><creator>Shih, WuRong</creator><creator>Diplas, Panayiotis</creator><general>John Wiley &amp; Sons, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7QL</scope><scope>7T7</scope><scope>7TG</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H94</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>M7N</scope><scope>P64</scope><orcidid>https://orcid.org/0000-0002-5860-4179</orcidid></search><sort><creationdate>201805</creationdate><title>A Unified Approach to Bed Load Transport Description Over a Wide Range of Flow Conditions via the Use of Conditional Data Treatment</title><author>Shih, WuRong ; Diplas, Panayiotis</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3684-c1a0c2c5cfa683f7ecf3c2a25b013f50a61cb4af56cc8ffae98be5acd4ca87573</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2018</creationdate><topic>Bed load</topic><topic>bed load intermittency</topic><topic>bed load transport</topic><topic>Bottom stress</topic><topic>Capacity</topic><topic>conditional data treatment</topic><topic>Data</topic><topic>Discharge</topic><topic>Dynamics</topic><topic>Empirical analysis</topic><topic>Energy transfer</topic><topic>Entrainment</topic><topic>Exponents</topic><topic>Formulas (mathematics)</topic><topic>Frameworks</topic><topic>Interactions</topic><topic>Load distribution</topic><topic>Mathematical models</topic><topic>Nonlinear phenomena</topic><topic>Particle dynamics</topic><topic>Physics</topic><topic>Regression analysis</topic><topic>Sediment</topic><topic>Sediment load</topic><topic>Sediment movement</topic><topic>Sediment transport</topic><topic>Sediments</topic><topic>Shear stress</topic><topic>stream power</topic><topic>Transport</topic><topic>Transport phenomena</topic><topic>Trends</topic><topic>turbulence</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shih, WuRong</creatorcontrib><creatorcontrib>Diplas, Panayiotis</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Meteorological &amp; 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Numerous stress‐transport power relations, with exponents varying between 1.5 and 16, have been proposed to capture the entire range of solid discharge trends exhibited by experimental data. A physics‐based explanation of the variation in exponent values is provided here. The concept of time‐resolved local stream power is used to determine the above‐threshold energy available for mobilizing bed materials, giving rise to solid discharge estimates. The generated transport capacity records, analyzed by a long‐term averaging process, allow for the construction of bed load curves that resemble the trends frequently reported in prior experimental studies. Under such conditions, use of long‐term averaged bed shear stress and bed load transport rates provide practical, yet oversimplified accounts of the transport phenomenon. The limitation of this methodology is particularly evident in low‐to‐moderate transport rates, where the calculated bed shear stress and consequent bed load transport rates are underestimated compared to values based on active periods of sediment movement. As the degree of intermittency in bed load transport increases, so does the exponent to compensate for the inactive periods of bed mobility. Conditionally averaged stress‐transport data, based on the active periods of bed load transport alone, however, exhibit a constant trend, reasonably well represented by a 1.5 power formula across the entire transport range. This approach better reflects the prevailing cause and effect relation by properly accounting for varied transport timescales. Furthermore, the resulting transport trend signifies a nearly constant efficiency in entraining and transporting sediment particles. Plain Language Summary Bed load transport is a complex phenomenon involving nonlinear interactions between the fluid and solid particle dynamics. The conventional quantitative methods, based on a long‐term averaging framework, lead to various power regression equations that link the bed load transport rates to the bed shear stress values, with exponents varying from 1.5 to 16, or even higher exponents, over a wide range of transport scenarios. The highly varied exponent values represent uncertainties that will compromise the utility of such empirical regression formulas in assessing bed load transport rates at different flow conditions. The unique contribution of this work is to elaborate on the underlying mechanism responsible for the variation in exponent values. Furthermore, a conditional data treatment is applied to the entire range of solid discharge trends, which appropriately accounts for the varied transport timescales shown at different levels of bed mobilization. This approach gives rise to a reasonably consistent power regression with exponents of 1.5. This 1.5th power relation signifies a nearly constant energy transfer efficiency by which the flow can entrain and transport sediment materials. These findings provide a better understanding of the transport mechanism(s) and facilitate the development of a consistent and physically meaningful bed load transport expression. Key Points Conditionally averaged stress‐transport data exhibit a consistent 1.5th power relation over the entire bed load transport range Long‐term averaged flow strength descriptors properly account for high levels of solid discharge conditions Impulse‐based considerations are important in reflecting the timescale effect imposed by bed load intermittency at low transport cases</abstract><cop>Washington</cop><pub>John Wiley &amp; Sons, Inc</pub><doi>10.1029/2017WR022373</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-5860-4179</orcidid><oa>free_for_read</oa></addata></record>
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subjects Bed load
bed load intermittency
bed load transport
Bottom stress
Capacity
conditional data treatment
Data
Discharge
Dynamics
Empirical analysis
Energy transfer
Entrainment
Exponents
Formulas (mathematics)
Frameworks
Interactions
Load distribution
Mathematical models
Nonlinear phenomena
Particle dynamics
Physics
Regression analysis
Sediment
Sediment load
Sediment movement
Sediment transport
Sediments
Shear stress
stream power
Transport
Transport phenomena
Trends
turbulence
title A Unified Approach to Bed Load Transport Description Over a Wide Range of Flow Conditions via the Use of Conditional Data Treatment
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