Some T 2 Terrace Soils of Peninsular Malaysia: II. Mineralogy and Physico-chemical Characteristics*
The amount of gibbsite in the clay fraction of T 2 terrace so£ls appears to increase with the increase of sand content and with the improvement of drainage conditions. Kaolinite is the main mineral £n the clay fraction of so£ls. The imperfectly and poorly drained ones may also contain some mica,...
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1985
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my.upm.eprints.25402013-05-27T07:01:47Z http://psasir.upm.edu.my/id/eprint/2540/ Some T 2 Terrace Soils of Peninsular Malaysia: II. Mineralogy and Physico-chemical Characteristics* Jusop, Shamsuddin Tessens, Eddy The amount of gibbsite in the clay fraction of T 2 terrace so£ls appears to increase with the increase of sand content and with the improvement of drainage conditions. Kaolinite is the main mineral £n the clay fraction of so£ls. The imperfectly and poorly drained ones may also contain some mica, chlorite, mixed layers and feldspar. Anatase accumulates in the silt fraction of the well rjrained soils. The dominance of 1:1 clay minerals and/or sesquioxides is reflected £n the£r physico-chemical properties. Apparent CEC decreases with a decrease £n silt/clay ration. WDC/clay % appears to decrease with an increase in A l and/or organic matter. The ratio also decreases as the pH approaches pHo' 1985 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/2540/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia_II..pdf Jusop, Shamsuddin and Tessens, Eddy (1985) Some T 2 Terrace Soils of Peninsular Malaysia: II. Mineralogy and Physico-chemical Characteristics*. Pertanika, 8 (2). pp. 159-158. English |
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| description |
The amount of gibbsite in the clay fraction of T 2 terrace so£ls appears to increase with the
increase of sand content and with the improvement of drainage conditions. Kaolinite is the main
mineral £n the clay fraction of so£ls. The imperfectly and poorly drained ones may also contain some
mica, chlorite, mixed layers and feldspar. Anatase accumulates in the silt fraction of the well rjrained
soils. The dominance of 1:1 clay minerals and/or sesquioxides is reflected £n the£r physico-chemical
properties. Apparent CEC decreases with a decrease £n silt/clay ration. WDC/clay % appears to
decrease with an increase in A l and/or organic matter. The ratio also decreases as the pH approaches
pHo' |
| format |
Article |
| author |
Jusop, Shamsuddin Tessens, Eddy |
| spellingShingle |
Jusop, Shamsuddin Tessens, Eddy Some T 2 Terrace Soils of Peninsular Malaysia: II. Mineralogy and Physico-chemical Characteristics* |
| author_facet |
Jusop, Shamsuddin Tessens, Eddy |
| author_sort |
Jusop, Shamsuddin |
| title |
Some T 2 Terrace Soils of Peninsular Malaysia: II.
Mineralogy and Physico-chemical Characteristics* |
| title_short |
Some T 2 Terrace Soils of Peninsular Malaysia: II.
Mineralogy and Physico-chemical Characteristics* |
| title_full |
Some T 2 Terrace Soils of Peninsular Malaysia: II.
Mineralogy and Physico-chemical Characteristics* |
| title_fullStr |
Some T 2 Terrace Soils of Peninsular Malaysia: II.
Mineralogy and Physico-chemical Characteristics* |
| title_full_unstemmed |
Some T 2 Terrace Soils of Peninsular Malaysia: II.
Mineralogy and Physico-chemical Characteristics* |
| title_sort |
some t 2 terrace soils of peninsular malaysia: ii.
mineralogy and physico-chemical characteristics* |
| publishDate |
1985 |
| url |
http://psasir.upm.edu.my/id/eprint/2540/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia_II..pdf http://psasir.upm.edu.my/id/eprint/2540/ |
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