Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang

In general, sediment comprises many shapes and sizes. The sediment size can be small, such as sand,small pebbles and silt, or large such as boulders, which are normally found upriver. Sediments found in estuaries are mostly fingrained, such as sand and silt. The speed at which water flows in rivers...

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Main Authors: Nadiatul Adilah, Ahmad Abdul Ghani, Fatin Adnin, Mohamad Prim Nasir
Format: Conference or Workshop Item
Language:English
Published: 2013
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Online Access:http://umpir.ump.edu.my/id/eprint/5719/1/CV-007.pdf
http://umpir.ump.edu.my/id/eprint/5719/
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spelling my.ump.umpir.57192018-02-05T02:02:12Z http://umpir.ump.edu.my/id/eprint/5719/ Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang Nadiatul Adilah, Ahmad Abdul Ghani Fatin Adnin, Mohamad Prim Nasir TA Engineering (General). Civil engineering (General) In general, sediment comprises many shapes and sizes. The sediment size can be small, such as sand,small pebbles and silt, or large such as boulders, which are normally found upriver. Sediments found in estuaries are mostly fingrained, such as sand and silt. The speed at which water flows in rivers plays an important part in determining its capacity to carry away sediments. Slower moving rivers will have a lower rate of sediment movement. According to Allison, J (1995), the process of sediment deposition is also dependent on river discharge and speed of river flow. As such, a higher discharge values and water velocity would result in higher amounts of sediment. In addition, time is a factor whereby the longer the sediment deposition process, the higher the sediment loads.Over a period of time, the high amount of sediment will settle down and the accumulated sediment will eat up the river bed thus causing the river to overflow or flooding. Thus, knowledge of the quantity, quality and dynamics of sediments is essential for managing our water resources systems and to against negative effects from happen.A study on sediment load was conducted at the Galing River in three different days which are 28/02/13, 13/03/13 and 27/03/13. Three sampling point representing the length of Galing River which is about 7.7km has been selected: Station 1 (S1) upstream Galing River, Station 2 (S2) mid-streams Galing River and Station 3 (S3) downstream Galing River (Figure 1). Sediment samples were collected using grab sampler. Three sample replications were collected from each station and the finding was presented by the average of the replicated samples. The samples collected were analysed in the laboratory. 2013 Conference or Workshop Item PeerReviewed application/pdf en http://umpir.ump.edu.my/id/eprint/5719/1/CV-007.pdf Nadiatul Adilah, Ahmad Abdul Ghani and Fatin Adnin, Mohamad Prim Nasir (2013) Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang. In: Malaysian Technical Universities Conference on Engineering & Technology (MUCET 2013), 3-4 December 2013 , Kuantan, Pahang. pp. 1-2..
institution Universiti Malaysia Pahang
building UMP Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Malaysia Pahang
content_source UMP Institutional Repository
url_provider http://umpir.ump.edu.my/
language English
topic TA Engineering (General). Civil engineering (General)
spellingShingle TA Engineering (General). Civil engineering (General)
Nadiatul Adilah, Ahmad Abdul Ghani
Fatin Adnin, Mohamad Prim Nasir
Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
description In general, sediment comprises many shapes and sizes. The sediment size can be small, such as sand,small pebbles and silt, or large such as boulders, which are normally found upriver. Sediments found in estuaries are mostly fingrained, such as sand and silt. The speed at which water flows in rivers plays an important part in determining its capacity to carry away sediments. Slower moving rivers will have a lower rate of sediment movement. According to Allison, J (1995), the process of sediment deposition is also dependent on river discharge and speed of river flow. As such, a higher discharge values and water velocity would result in higher amounts of sediment. In addition, time is a factor whereby the longer the sediment deposition process, the higher the sediment loads.Over a period of time, the high amount of sediment will settle down and the accumulated sediment will eat up the river bed thus causing the river to overflow or flooding. Thus, knowledge of the quantity, quality and dynamics of sediments is essential for managing our water resources systems and to against negative effects from happen.A study on sediment load was conducted at the Galing River in three different days which are 28/02/13, 13/03/13 and 27/03/13. Three sampling point representing the length of Galing River which is about 7.7km has been selected: Station 1 (S1) upstream Galing River, Station 2 (S2) mid-streams Galing River and Station 3 (S3) downstream Galing River (Figure 1). Sediment samples were collected using grab sampler. Three sample replications were collected from each station and the finding was presented by the average of the replicated samples. The samples collected were analysed in the laboratory.
format Conference or Workshop Item
author Nadiatul Adilah, Ahmad Abdul Ghani
Fatin Adnin, Mohamad Prim Nasir
author_facet Nadiatul Adilah, Ahmad Abdul Ghani
Fatin Adnin, Mohamad Prim Nasir
author_sort Nadiatul Adilah, Ahmad Abdul Ghani
title Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
title_short Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
title_full Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
title_fullStr Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
title_full_unstemmed Preliminary Study on Sediment Load at Sungai Galing, Kuantan, Pahang
title_sort preliminary study on sediment load at sungai galing, kuantan, pahang
publishDate 2013
url http://umpir.ump.edu.my/id/eprint/5719/1/CV-007.pdf
http://umpir.ump.edu.my/id/eprint/5719/
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