Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system

The sediments in the Setiu Lagoon-estuary system on the east coast of Malaysia consist mostly of coarse to very fine panicles. The major portions of the sediment are negatively skewed. The estuary area is under the influence of transportative and erosive forces. The lack of silt and clay in the es...

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Main Authors: Yaacob, Rosnan, Husain, Mohd Lokman, Mohd Shazili, Noor Azhar
Format: Article
Language:English
Published: Universiti Putra Malaysia Press 1995
Online Access:http://psasir.upm.edu.my/id/eprint/3323/1/Grain-size_Distribution_of_Sediment_in_the_Vicinity.pdf
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author Yaacob, Rosnan
Husain, Mohd Lokman
Mohd Shazili, Noor Azhar
author_facet Yaacob, Rosnan
Husain, Mohd Lokman
Mohd Shazili, Noor Azhar
author_sort Yaacob, Rosnan
collection UPM
description The sediments in the Setiu Lagoon-estuary system on the east coast of Malaysia consist mostly of coarse to very fine panicles. The major portions of the sediment are negatively skewed. The estuary area is under the influence of transportative and erosive forces. The lack of silt and clay in the estuary is attributable to less depositional factor under the influence of stronger current than in the lagoon area. The beach sediment ranges from coarse to fine sand. Generally, the mean grain-size decreases towards the north-west sector. The skewness value of the beach sand area is mostly negative, indicating that the study area is under the influence of rather strong wave and current action.
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spelling upm.eprints-33232015-09-02T04:10:31Z http://psasir.upm.edu.my/id/eprint/3323/ Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system Yaacob, Rosnan Husain, Mohd Lokman Mohd Shazili, Noor Azhar The sediments in the Setiu Lagoon-estuary system on the east coast of Malaysia consist mostly of coarse to very fine panicles. The major portions of the sediment are negatively skewed. The estuary area is under the influence of transportative and erosive forces. The lack of silt and clay in the estuary is attributable to less depositional factor under the influence of stronger current than in the lagoon area. The beach sediment ranges from coarse to fine sand. Generally, the mean grain-size decreases towards the north-west sector. The skewness value of the beach sand area is mostly negative, indicating that the study area is under the influence of rather strong wave and current action. Universiti Putra Malaysia Press 1995 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/3323/1/Grain-size_Distribution_of_Sediment_in_the_Vicinity.pdf Yaacob, Rosnan and Husain, Mohd Lokman and Mohd Shazili, Noor Azhar (1995) Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system. Pertanika Journal of Tropical Agricultural Science, 18 (1). pp. 71-76. ISSN 0126-6128 http://www.pertanika.upm.edu.my/Pertanika%20PAPERS/JTAS%20Vol.%2018%20(1)%20Apr.%201995/JTAS%20Vol.18%20(1)%201995%20(Pg%2071-76).pdf
spellingShingle Yaacob, Rosnan
Husain, Mohd Lokman
Mohd Shazili, Noor Azhar
Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title_full Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title_fullStr Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title_full_unstemmed Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title_short Grain-size distribution of sediment in the vicinity of Setiu Lagoon-estuary system
title_sort grain size distribution of sediment in the vicinity of setiu lagoon estuary system
url http://psasir.upm.edu.my/id/eprint/3323/1/Grain-size_Distribution_of_Sediment_in_the_Vicinity.pdf
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