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,...
| Main Authors: | , |
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| Format: | Article |
| Language: | English English |
| Published: |
1985
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| Online Access: | http://psasir.upm.edu.my/id/eprint/2540/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia_II..pdf |
| _version_ | 1825921476792942592 |
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| author | Jusop, Shamsuddin Tessens, Eddy |
| author_facet | Jusop, Shamsuddin Tessens, Eddy |
| author_sort | Jusop, Shamsuddin |
| collection | UPM |
| 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' |
| first_indexed | 2024-03-06T06:58:28Z |
| format | Article |
| id | upm.eprints-2540 |
| institution | Universiti Putra Malaysia |
| language | English English |
| last_indexed | 2024-03-06T06:58:28Z |
| publishDate | 1985 |
| record_format | dspace |
| spelling | 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 |
| spellingShingle | Jusop, Shamsuddin Tessens, Eddy Some T 2 Terrace Soils of Peninsular Malaysia: II. Mineralogy and Physico-chemical Characteristics* |
| title | 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_short | 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 |
| url | http://psasir.upm.edu.my/id/eprint/2540/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia_II..pdf |
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