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5 results for “suspended sediment transport”

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zenodo40/100

Longitudinal transport of suspended sediment in the Modaomen Estuary of the Pearl River: effects of river, tide, and mouth bar: Datasets

<p><strong>This&nbsp;dataset supplements the article: Longitudinal transport&nbsp;of suspended sediment in the Modaomen </strong><strong>E</strong><strong>stuary of the Pearl River: effects of river, tide, and mouth bar, submitted to Marine Geology</strong></p> <p>Contact information: Dr. Liu, F., School of Ocean Engineering and Technology, Sun Yat-sen University, Guangzhou, 510275, China.</p> <p>Email: <a href="mailto:liuf53@mail.sysu.edu.cn">liuf53@mail.sysu.edu.cn</a> (Liu, Feng)</p> <p><strong><em>Brief view of the dataset</em></strong></p> <p>Hydrodynamics, suspended sediment concentration and salinity distribution were measured&nbsp;at three fixed stations along the longitudinal direction of the estuary.&nbsp;The stations were located at Guadingjiao (M1), inside the bar (M2), and outside the bar (M3), and sampling was simultaneously conducted at neap tide (NT) from July 31 to August 1 and spring tide (ST) from August 8 to August 9 in 2017. All observation data has been compiled to include data from the surface to the bottom six layers within 26 hours. This directory contains the following datasets.</p> <p><strong>M10731.xlsx: </strong>Current velocity, current direction, salinity and SSC during neap tide at Station M1&nbsp;</p> <p><strong>M10808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M1&nbsp;</p> <p><strong>M20731.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during neap tide at Station M2</p> <p><strong>M20808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M2</p> <p><strong>M30731.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during neap tide at Station M3</p> <p><strong>M30808.xlsx:&nbsp;</strong>Current velocity, current direction, salinity and SSC during spring&nbsp;tide at Station M3</p>

opencc-by-4.0Jun 2023View details →
dryad40/100

UNO experimental dataset for: Multiscale bedform reorganization at the onset of substantial suspended sediment transport

Open the record for dataset details and reuse information.

publicOct 2025View details →
dryad40/100

Data for: Multiscale bedform reorganization at the onset of substantial suspended sediment transport

Open the record for dataset details and reuse information.

publicOct 2025View details →
dryad36/100

Data from: A study on the Influence of submergence ratio on the transportation of suspended sediment in a partially vegetated channel flow

<p><span>Riparian or aquatic vegetation thrives with seasons. The understanding of canopies' Submergence-Ratio SR (stems' height to water depth) influence on suspended sediments' transportation is still limited. Thus, Large Eddy Simulations (LES) coupled with the Discrete Phase Method (DPM) are used to investigate the particles' 3-dimensional distribution in a partially vegetated straight channel. The spanwise distribution of particles is quantified by the Probability Density Function (PDF), showing a non-uniformity of particles in time as quantified by the PDF variance. The findings and conclusions: (Ⅰ) With SR rising, the particles' depletion effects exerted by the vegetation-side mixing layer are improved along the interface between vegetated and vegetation-side bare channel region. However, the SR has little effect on the variance of the particles' PDF in the spanwise direction when the mixing layer is fully developed. (Ⅱ) During the developing stage of the over-canopy mixing layer, submerged vegetation with higher SR gain a stronger upwards (vertical) entrainment capability. </span><span>The case (SR=60%) has a higher sediment concentration than other cases in the fully developed vertical mixing layer region above canopy.</span><span> (III) </span><span>The vertical suspension of particles in the vegetation-side bare channel region is analysed. Particles migrating from the vegetated region are entrained into the vegetation-side bare channel region by turbulent structures. Nevertheless, the vertical concentration profile is more uniform in the vegetated region than in the vegetation-side bare channel at the same streamwise location. The cases SR=40% and 60% still have higher sediment concentrations than other cases in the vegetation-side bare channel's upper region.</span></p>

opencc-zeroJan 2023View details →
dryad36/100

Data from: A study on the Influence of submergence ratio on the transportation of suspended sediment in a partially vegetated channel flow

Open the record for dataset details and reuse information.

publicJan 2023View details →

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