A study on erosion of soft sediment deposits

Erosional pattern of fine cohesive sediment must be defined to predict the transport model in estuarial water Resistance to erosion is largely dependent on physicochemical properties of sediment and fluid, as well as the interparticle bond which is characterized by shear strength. Successively in...

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Main Authors: Zawawi Samba Mohamed,, Mahbubur Rahman,, Jamal Mohd Amin,
Format: Article
Published: 1997
Online Access:http://journalarticle.ukm.my/1329/
http://www.ukm.my/jkukm/index.php/jkukm
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spelling my-ukm.journal.13292011-10-11T03:45:19Z http://journalarticle.ukm.my/1329/ A study on erosion of soft sediment deposits Zawawi Samba Mohamed, Mahbubur Rahman, Jamal Mohd Amin, Erosional pattern of fine cohesive sediment must be defined to predict the transport model in estuarial water Resistance to erosion is largely dependent on physicochemical properties of sediment and fluid, as well as the interparticle bond which is characterized by shear strength. Successively incremental flow-induced bed shear stress is applied to initiate layer by layer erosion of soft cohesive sediment deposit to determine the rate of erosion. A decrease in erosion rate is observed at the end of each time step. This behavior is due to the increasing shear strength with depth. The rate of erosion was found to vary exponentially with cubic root of excess bed shear stress 1997 Article PeerReviewed Zawawi Samba Mohamed, and Mahbubur Rahman, and Jamal Mohd Amin, (1997) A study on erosion of soft sediment deposits. Jurnal Kejuruteraan, 9 . http://www.ukm.my/jkukm/index.php/jkukm
institution Universiti Kebangsaan Malaysia
building Perpustakaan Tun Sri Lanang Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Kebangsaan Malaysia
content_source UKM Journal Article Repository
url_provider http://journalarticle.ukm.my/
description Erosional pattern of fine cohesive sediment must be defined to predict the transport model in estuarial water Resistance to erosion is largely dependent on physicochemical properties of sediment and fluid, as well as the interparticle bond which is characterized by shear strength. Successively incremental flow-induced bed shear stress is applied to initiate layer by layer erosion of soft cohesive sediment deposit to determine the rate of erosion. A decrease in erosion rate is observed at the end of each time step. This behavior is due to the increasing shear strength with depth. The rate of erosion was found to vary exponentially with cubic root of excess bed shear stress
format Article
author Zawawi Samba Mohamed,
Mahbubur Rahman,
Jamal Mohd Amin,
spellingShingle Zawawi Samba Mohamed,
Mahbubur Rahman,
Jamal Mohd Amin,
A study on erosion of soft sediment deposits
author_facet Zawawi Samba Mohamed,
Mahbubur Rahman,
Jamal Mohd Amin,
author_sort Zawawi Samba Mohamed,
title A study on erosion of soft sediment deposits
title_short A study on erosion of soft sediment deposits
title_full A study on erosion of soft sediment deposits
title_fullStr A study on erosion of soft sediment deposits
title_full_unstemmed A study on erosion of soft sediment deposits
title_sort study on erosion of soft sediment deposits
publishDate 1997
url http://journalarticle.ukm.my/1329/
http://www.ukm.my/jkukm/index.php/jkukm
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score 13.211869