Characteristics of regolith developed on basalt in Pahang, Malaysia

The characteristics and degree of weathering in a deep regolith developed on basalt were investigated. A representative 15 m deep regolith of soil-saprolite-rock sequence, located in Pahang state, Malaysia, was selected. The intensity of weathering in this deep regolith was assessed by various weath...

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Main Authors: Hamdan, J., Ruhana, B., McRae, S.G.
Format: Article
Published: Marcel Dekker Inc. 2000
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author Hamdan, J.
Ruhana, B.
McRae, S.G.
author_facet Hamdan, J.
Ruhana, B.
McRae, S.G.
author_sort Hamdan, J.
collection UPM
description The characteristics and degree of weathering in a deep regolith developed on basalt were investigated. A representative 15 m deep regolith of soil-saprolite-rock sequence, located in Pahang state, Malaysia, was selected. The intensity of weathering in this deep regolith was assessed by various weathering indices as well as changes in the physicochemical properties and clay mineralogy of the regolith. The values of all weathering indices and other assessments gave strong evidences of intense weathering during saprolite formation. The low CEC and base cation values even in the saprolite layers were accounted by the extreme depletion of major elements such as potassium (K), sodium (Na), calcium (Ca), and magnesium (Mg), and significant enrichment of aluminum (Al), iron (Fe), titanium (Ti), copper (Cu), and niobium (Nb) occurred during saprolitization. The extreme weathering pattern of basalt differed from those described in granite and metamorphic rocks found in Peninsular Malaysia.
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spelling upm.eprints-1152602025-02-27T02:34:02Z http://psasir.upm.edu.my/id/eprint/115260/ Characteristics of regolith developed on basalt in Pahang, Malaysia Hamdan, J. Ruhana, B. McRae, S.G. The characteristics and degree of weathering in a deep regolith developed on basalt were investigated. A representative 15 m deep regolith of soil-saprolite-rock sequence, located in Pahang state, Malaysia, was selected. The intensity of weathering in this deep regolith was assessed by various weathering indices as well as changes in the physicochemical properties and clay mineralogy of the regolith. The values of all weathering indices and other assessments gave strong evidences of intense weathering during saprolite formation. The low CEC and base cation values even in the saprolite layers were accounted by the extreme depletion of major elements such as potassium (K), sodium (Na), calcium (Ca), and magnesium (Mg), and significant enrichment of aluminum (Al), iron (Fe), titanium (Ti), copper (Cu), and niobium (Nb) occurred during saprolitization. The extreme weathering pattern of basalt differed from those described in granite and metamorphic rocks found in Peninsular Malaysia. Marcel Dekker Inc. 2000 Article PeerReviewed Hamdan, J. and Ruhana, B. and McRae, S.G. (2000) Characteristics of regolith developed on basalt in Pahang, Malaysia. Communications in Soil Science and Plant Analysis, 31 (7-8). pp. 981-993. ISSN 0010-3624; eISSN: 0010-3624 https://www.tandfonline.com/doi/full/10.1080/00103620009370492 10.1080/00103620009370492
spellingShingle Hamdan, J.
Ruhana, B.
McRae, S.G.
Characteristics of regolith developed on basalt in Pahang, Malaysia
title Characteristics of regolith developed on basalt in Pahang, Malaysia
title_full Characteristics of regolith developed on basalt in Pahang, Malaysia
title_fullStr Characteristics of regolith developed on basalt in Pahang, Malaysia
title_full_unstemmed Characteristics of regolith developed on basalt in Pahang, Malaysia
title_short Characteristics of regolith developed on basalt in Pahang, Malaysia
title_sort characteristics of regolith developed on basalt in pahang malaysia
work_keys_str_mv AT hamdanj characteristicsofregolithdevelopedonbasaltinpahangmalaysia
AT ruhanab characteristicsofregolithdevelopedonbasaltinpahangmalaysia
AT mcraesg characteristicsofregolithdevelopedonbasaltinpahangmalaysia