Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir

In reservoir of dams, especially near the dam body, the cohesive fine sediments are deposited mainly. The mechanical behavior of these sediments is largely controlled by the interparticle attraction caused by electrostatic and physiochemical forces. these properties cause the stickiness and accumula...

Full description

Bibliographic Details
Main Authors: Mahnaz Shadorvan, Babak Lashkar-Ara, Hesam Seyed kaboli
Format: Article
Language:fas
Published: Shahid Chamran University of Ahvaz 2018-06-01
Series:علوم و مهندسی آبیاری
Subjects:
Online Access:http://jise.scu.ac.ir/article_13671_5edf5d1920ed773f6487f0fc6d204f20.pdf
_version_ 1818446751502172160
author Mahnaz Shadorvan
Babak Lashkar-Ara
Hesam Seyed kaboli
author_facet Mahnaz Shadorvan
Babak Lashkar-Ara
Hesam Seyed kaboli
author_sort Mahnaz Shadorvan
collection DOAJ
description In reservoir of dams, especially near the dam body, the cohesive fine sediments are deposited mainly. The mechanical behavior of these sediments is largely controlled by the interparticle attraction caused by electrostatic and physiochemical forces. these properties cause the stickiness and accumulation of clay particles and formation of dense masses called flocs, which is sometimes referred to as flocculation. flocculation is influenced by several factors including salinity, flow regime, sediment concentration and organic matter. Flocculation is the most important factor that makes the settling, fall velocity and transfer of cohesive sediment considerably more complex and dynamic than non-cohesive sediments. In order to determine the relations governing cohesive sediments, the physical characteristics and behavior of these sediments should be identified. The terminal settling velocity of sedimentary particles in liquids, called particle fall velocity, is one of the most important properties in determining the physical properties of sediments caused transfer, deposition and consolidation. The fall velocity of cohesive sediments is influenced by many factors, including salinity, initial particle size, turbulence, temperature of water, and suspended sediment concentration. <br />McLaughlin (1959) provided a method for measuring the fall velocity of particle (ω) in stillwater, using a settling cylinder with 10 cm diameter and less than 1 meter height and established a differential formula based on its research as follows: <br /><br />d(wC)/dz+dC/dt=0                                                                                                                                       (1) <br /><br />Fathi Moghadam et al (2011) studied the settling properties of the cohesive sediments in the Dez Dam reservoir. They concluded that particles for all concentrated samples and in all depths reached to their maximum fall velocity approximately at the same time (15 minutes after starting the test). The lower concentration samples appeared to have higher maximum fall velocities than the higher concentration samples, but for a shorter duration.
first_indexed 2024-12-14T19:52:42Z
format Article
id doaj.art-7738363762e54d0db6ed60d0f7dc61b6
institution Directory Open Access Journal
issn 2588-5952
2588-5960
language fas
last_indexed 2024-12-14T19:52:42Z
publishDate 2018-06-01
publisher Shahid Chamran University of Ahvaz
record_format Article
series علوم و مهندسی آبیاری
spelling doaj.art-7738363762e54d0db6ed60d0f7dc61b62022-12-21T22:49:22ZfasShahid Chamran University of Ahvazعلوم و مهندسی آبیاری2588-59522588-59602018-06-0141221122410.22055/jise.2018.22358.160113671Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam ReservoirMahnaz Shadorvan0Babak Lashkar-Ara1Hesam Seyed kaboli2M.Sc. Student, Department of Civil Engineering, Jundi-Shapur University of Technology, Dezful, Iran.Assistant Professor, Department of Civil Engineering, Jundi-Shapur University of Technology, Dezful, IranAssistant Professor, Department of Civil Engineering, Jundi-Shapur University of Technology, Dezful, IranIn reservoir of dams, especially near the dam body, the cohesive fine sediments are deposited mainly. The mechanical behavior of these sediments is largely controlled by the interparticle attraction caused by electrostatic and physiochemical forces. these properties cause the stickiness and accumulation of clay particles and formation of dense masses called flocs, which is sometimes referred to as flocculation. flocculation is influenced by several factors including salinity, flow regime, sediment concentration and organic matter. Flocculation is the most important factor that makes the settling, fall velocity and transfer of cohesive sediment considerably more complex and dynamic than non-cohesive sediments. In order to determine the relations governing cohesive sediments, the physical characteristics and behavior of these sediments should be identified. The terminal settling velocity of sedimentary particles in liquids, called particle fall velocity, is one of the most important properties in determining the physical properties of sediments caused transfer, deposition and consolidation. The fall velocity of cohesive sediments is influenced by many factors, including salinity, initial particle size, turbulence, temperature of water, and suspended sediment concentration. <br />McLaughlin (1959) provided a method for measuring the fall velocity of particle (ω) in stillwater, using a settling cylinder with 10 cm diameter and less than 1 meter height and established a differential formula based on its research as follows: <br /><br />d(wC)/dz+dC/dt=0                                                                                                                                       (1) <br /><br />Fathi Moghadam et al (2011) studied the settling properties of the cohesive sediments in the Dez Dam reservoir. They concluded that particles for all concentrated samples and in all depths reached to their maximum fall velocity approximately at the same time (15 minutes after starting the test). The lower concentration samples appeared to have higher maximum fall velocities than the higher concentration samples, but for a shorter duration.http://jise.scu.ac.ir/article_13671_5edf5d1920ed773f6487f0fc6d204f20.pdfsettling columnflocculation reactionfall velocitycohesive sediment
spellingShingle Mahnaz Shadorvan
Babak Lashkar-Ara
Hesam Seyed kaboli
Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
علوم و مهندسی آبیاری
settling column
flocculation reaction
fall velocity
cohesive sediment
title Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
title_full Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
title_fullStr Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
title_full_unstemmed Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
title_short Assessment of the Cohesive Sediments Fall Velocity in Karkheh Dam Reservoir
title_sort assessment of the cohesive sediments fall velocity in karkheh dam reservoir
topic settling column
flocculation reaction
fall velocity
cohesive sediment
url http://jise.scu.ac.ir/article_13671_5edf5d1920ed773f6487f0fc6d204f20.pdf
work_keys_str_mv AT mahnazshadorvan assessmentofthecohesivesedimentsfallvelocityinkarkhehdamreservoir
AT babaklashkarara assessmentofthecohesivesedimentsfallvelocityinkarkhehdamreservoir
AT hesamseyedkaboli assessmentofthecohesivesedimentsfallvelocityinkarkhehdamreservoir