Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers

Mountain rivers and lowland rivers differ in many ways. Some of the many elements that distinguish both river systems apart are the rivers’ geomorphological appearances, hydraulic geometry, pollution transport, sediment transport, and its own roughness and coarseness. In this particular study, the e...

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Published in:Environmental Earth Sciences
Main Author: Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
Format: Article
Language:English
Published: Springer Verlag 2017
Online Access:https://www.scopus.com/inward/record.uri?eid=2-s2.0-85032072378&doi=10.1007%2fs12665-017-6620-y&partnerID=40&md5=02cb1411c872d9e7a8f77fd5feafcb3c
id 2-s2.0-85032072378
spelling 2-s2.0-85032072378
Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
2017
Environmental Earth Sciences
76
7
10.1007/s12665-017-6620-y
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85032072378&doi=10.1007%2fs12665-017-6620-y&partnerID=40&md5=02cb1411c872d9e7a8f77fd5feafcb3c
Mountain rivers and lowland rivers differ in many ways. Some of the many elements that distinguish both river systems apart are the rivers’ geomorphological appearances, hydraulic geometry, pollution transport, sediment transport, and its own roughness and coarseness. In this particular study, the element of sediment transport is given distinctive attention too. This study employs the deterministic approach for bed load prediction entailing the use of the parameterization concept where particle size and flow variation is taken into full consideration. Apart from that, the classical approach of Shields number is also used to determine the transport rates at the fluvial system. However, due to some limitation and range of applicability, the Shields number approach was re-modified to suit the range of applicability. Changes were made to the alleviating critical stress term and formulating exponential approach. For this research, it was important to deduce the underlying principles which are universal and common to all river systems, due to obvious and distinct differences between the mountain and lowland rivers. A special attribute was given to the Malaysian natural rivers because of the limited recorded data available. All datasets were compiled and tested with the bed load predictors to observe the commonality pattern between the lowland and mountain river systems. Most of the bed load transport equations limit the range of applicability by isolating the flow regime or bed roughness individually. Thus, it was vital for researchers to find the commonality pattern between these two river systems which needed to be statistically sound in its form. It was postulated that the particle densimetric Froude number is graphically and statistically fit for both river systems. Hence, this predictor is used as it has a high potential to be included in the sediment transport parameterization for Malaysian natural rivers. © 2017, Springer-Verlag Berlin Heidelberg.
Springer Verlag
18666280
English
Article

author Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
spellingShingle Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
author_facet Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
author_sort Sulaiman M.S.; Sinnakaudan S.K.; Azhari N.N.; Abidin R.Z.
title Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
title_short Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
title_full Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
title_fullStr Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
title_full_unstemmed Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
title_sort Behavioral of sediment transport at lowland and mountainous rivers: a special reference to selected Malaysian rivers
publishDate 2017
container_title Environmental Earth Sciences
container_volume 76
container_issue 7
doi_str_mv 10.1007/s12665-017-6620-y
url https://www.scopus.com/inward/record.uri?eid=2-s2.0-85032072378&doi=10.1007%2fs12665-017-6620-y&partnerID=40&md5=02cb1411c872d9e7a8f77fd5feafcb3c
description Mountain rivers and lowland rivers differ in many ways. Some of the many elements that distinguish both river systems apart are the rivers’ geomorphological appearances, hydraulic geometry, pollution transport, sediment transport, and its own roughness and coarseness. In this particular study, the element of sediment transport is given distinctive attention too. This study employs the deterministic approach for bed load prediction entailing the use of the parameterization concept where particle size and flow variation is taken into full consideration. Apart from that, the classical approach of Shields number is also used to determine the transport rates at the fluvial system. However, due to some limitation and range of applicability, the Shields number approach was re-modified to suit the range of applicability. Changes were made to the alleviating critical stress term and formulating exponential approach. For this research, it was important to deduce the underlying principles which are universal and common to all river systems, due to obvious and distinct differences between the mountain and lowland rivers. A special attribute was given to the Malaysian natural rivers because of the limited recorded data available. All datasets were compiled and tested with the bed load predictors to observe the commonality pattern between the lowland and mountain river systems. Most of the bed load transport equations limit the range of applicability by isolating the flow regime or bed roughness individually. Thus, it was vital for researchers to find the commonality pattern between these two river systems which needed to be statistically sound in its form. It was postulated that the particle densimetric Froude number is graphically and statistically fit for both river systems. Hence, this predictor is used as it has a high potential to be included in the sediment transport parameterization for Malaysian natural rivers. © 2017, Springer-Verlag Berlin Heidelberg.
publisher Springer Verlag
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