Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia

A study was conducted along the Kelantan–Terengganu Coastal Plains, Peninsular Malaysia to explain the occurrence of sandy beach ridges and to determine the physico-chemical properties of the soils formed on them. Two or occasionally three series of sandy ridges running parallel to the shoreline occ...

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Main Authors: Roslan, I., Jusop, Shamsuddin, Ishak, Che Fauziah, Abdul Rahim, Anuar
Format: Article
Language:English
Published: 2010
Subjects:
Online Access:http://psasir.upm.edu.my/id/eprint/15881/
http://psasir.upm.edu.my/id/eprint/15881/1/Occurrence%20and%20properties%20of%20soils%20on%20sandy%20beach%20ridges%20in%20the%20Kelantan.pdf
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author Roslan, I.
Jusop, Shamsuddin
Ishak, Che Fauziah
Abdul Rahim, Anuar
author_facet Roslan, I.
Jusop, Shamsuddin
Ishak, Che Fauziah
Abdul Rahim, Anuar
author_sort Roslan, I.
building UPM Institutional Repository
collection Online Access
description A study was conducted along the Kelantan–Terengganu Coastal Plains, Peninsular Malaysia to explain the occurrence of sandy beach ridges and to determine the physico-chemical properties of the soils formed on them. Two or occasionally three series of sandy ridges running parallel to the shoreline occur in the area. These ridges are believed to have been formed by the continuous action of the sea waves following changes in the sea level during the Holocene, the oldest ridge being the one farthest away from the shoreline. In between these ridges occurs a slight depression, usually occupied by soils under submerged condition. The soils on the ridges are subjected to the processes of soil formation, mainly podzolization. There is no horizon differentiation in the soils on the ridge nearest to the shoreline. However, soils on the older ridges contain spodic horizon, occurring at varying depths. Drainage and the depth below which this spodic horizon occurs are the deciding factors for determining soil type (series). Physically, the soils are sandy containing > 95% sand, with the drainage varying from moderately well to excessively-drained for the soils on the ridges. Under this condition, the mineralogy of the clay and silt fractions is dominated by quartz; some feldspars, mica, kaolinite, gibbsite and anatase are also present. Sandy nature of the soils on beach ridges, extreme leaching, low cation exchange capacity and low exchangeable bases leads to their low productivity.
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spelling upm-158812015-11-02T06:47:00Z http://psasir.upm.edu.my/id/eprint/15881/ Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia Roslan, I. Jusop, Shamsuddin Ishak, Che Fauziah Abdul Rahim, Anuar A study was conducted along the Kelantan–Terengganu Coastal Plains, Peninsular Malaysia to explain the occurrence of sandy beach ridges and to determine the physico-chemical properties of the soils formed on them. Two or occasionally three series of sandy ridges running parallel to the shoreline occur in the area. These ridges are believed to have been formed by the continuous action of the sea waves following changes in the sea level during the Holocene, the oldest ridge being the one farthest away from the shoreline. In between these ridges occurs a slight depression, usually occupied by soils under submerged condition. The soils on the ridges are subjected to the processes of soil formation, mainly podzolization. There is no horizon differentiation in the soils on the ridge nearest to the shoreline. However, soils on the older ridges contain spodic horizon, occurring at varying depths. Drainage and the depth below which this spodic horizon occurs are the deciding factors for determining soil type (series). Physically, the soils are sandy containing > 95% sand, with the drainage varying from moderately well to excessively-drained for the soils on the ridges. Under this condition, the mineralogy of the clay and silt fractions is dominated by quartz; some feldspars, mica, kaolinite, gibbsite and anatase are also present. Sandy nature of the soils on beach ridges, extreme leaching, low cation exchange capacity and low exchangeable bases leads to their low productivity. 2010 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/15881/1/Occurrence%20and%20properties%20of%20soils%20on%20sandy%20beach%20ridges%20in%20the%20Kelantan.pdf Roslan, I. and Jusop, Shamsuddin and Ishak, Che Fauziah and Abdul Rahim, Anuar (2010) Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia. Catena, 83 (1). pp. 55-63. ISSN 0341-8162 Beach ridges - Malaysia Coast changes - Malaysia Sandy soils - Testing
spellingShingle Beach ridges - Malaysia
Coast changes - Malaysia
Sandy soils - Testing
Roslan, I.
Jusop, Shamsuddin
Ishak, Che Fauziah
Abdul Rahim, Anuar
Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title_full Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title_fullStr Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title_full_unstemmed Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title_short Occurrence and properties of soils on sandy beach ridges in the Kelantan-Terengganu Plains, Peninsular Malaysia
title_sort occurrence and properties of soils on sandy beach ridges in the kelantan-terengganu plains, peninsular malaysia
topic Beach ridges - Malaysia
Coast changes - Malaysia
Sandy soils - Testing
url http://psasir.upm.edu.my/id/eprint/15881/
http://psasir.upm.edu.my/id/eprint/15881/1/Occurrence%20and%20properties%20of%20soils%20on%20sandy%20beach%20ridges%20in%20the%20Kelantan.pdf