Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification
18 profiles belonging to 14 soil series of the Tz terrace soils of Peninsular Malaysia were studied. The soils are derived from alluvial materials of mixed origin of Holocene age. They are mainly Inceptisols. Others are classified as Entisols, Ultisols and Alfisols. The study indicates that the so...
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my.upm.eprints.22292013-05-27T06:59:42Z http://psasir.upm.edu.my/id/eprint/2229/ Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification Jusop, Shamsuddin Tessens, Eddy 18 profiles belonging to 14 soil series of the Tz terrace soils of Peninsular Malaysia were studied. The soils are derived from alluvial materials of mixed origin of Holocene age. They are mainly Inceptisols. Others are classified as Entisols, Ultisols and Alfisols. The study indicates that the soils are either in the recent or intermediate stage of weathering. The c/f related distribution is gefuric in the sandy families, gefuric and/or chitonic in the coarse loamy families, and porphyric in the fine loamy and the clayey families. It is found that phytoliths are more common in the east than in the west coast of the peninsula- 1983 Article NonPeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/2229/1/Some_T2_Terrace_Soils_of_Peninsular_Malaysia_I._Micromorphology.pdf Jusop, Shamsuddin and Tessens, Eddy (1983) Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification. Pertanika, 6 (3). pp. 61-89. English |
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18 profiles belonging to 14 soil series of the Tz terrace soils of Peninsular Malaysia were studied.
The soils are derived from alluvial materials of mixed origin of Holocene age. They are mainly Inceptisols.
Others are classified as Entisols, Ultisols and Alfisols. The study indicates that the soils are either in the
recent or intermediate stage of weathering. The c/f related distribution is gefuric in the sandy families,
gefuric and/or chitonic in the coarse loamy families, and porphyric in the fine loamy and the clayey
families. It is found that phytoliths are more common in the east than in the west coast of the peninsula- |
format |
Article |
author |
Jusop, Shamsuddin Tessens, Eddy |
spellingShingle |
Jusop, Shamsuddin Tessens, Eddy Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
author_facet |
Jusop, Shamsuddin Tessens, Eddy |
author_sort |
Jusop, Shamsuddin |
title |
Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
title_short |
Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
title_full |
Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
title_fullStr |
Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
title_full_unstemmed |
Some T2 Terrace Soils of Peninsular Malaysia: I. Micromorphology, Genesis and Classification |
title_sort |
some t2 terrace soils of peninsular malaysia: i. micromorphology, genesis and classification |
publishDate |
1983 |
url |
http://psasir.upm.edu.my/id/eprint/2229/1/Some_T2_Terrace_Soils_of_Peninsular_Malaysia_I._Micromorphology.pdf http://psasir.upm.edu.my/id/eprint/2229/ |
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