The minerology and chemical properties of soils on granite gneiss in three climatic zones in Sri Lanka

Shamshuddin Jusoh, . and Ruziah Salleh, . and Ahmad Husni M.H., . and Kamis Awang, . The minerology and chemical properties of soils on granite gneiss in three climatic zones in Sri Lanka. pp. 57-61. ISSN 0126-6128

Granite gneiss occurs sporadically throughout Sri Lanka. Depending on the climatic conditions and topography of the area the rock undergoes different degrees of chemical weathering. The mineralogy and chemical properties of four common granite gneiss soils occuring in three agro-ecological zones in Sri Lanka were studied. The soil in the wet zone is low in pH and basic exchangeable cations while the soils in the wet zone are high in pH and basic exchangeable cations. The colour of the soils changes from yellowish-brown to red as the soils get drier presumably due to the presence of haematite and/or goethite. Kaolinite halloysite and smectite are present in all the soils irrespective of the climatic conditions; the amount of halloysite decreases towards the surface. Biotite is abundant in the soil of the intermediate and dry zones but is absent in the soil of the wet zone. Gibbsite is present in the highly weathered soil of the wet zone. The concentration of Ca in soil solution is dependent on the amount in the soils existing in the form of exchangeable Ca. Additionally the solution Ca concentration is significantly correlated with the soil ECEC and te ECEC/CEC ratio.

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Abstract

Granite gneiss occurs sporadically throughout Sri Lanka. Depending on the climatic conditions and topography of the area the rock undergoes different degrees of chemical weathering. The mineralogy and chemical properties of four common granite gneiss soils occuring in three agro-ecological zones in Sri Lanka were studied. The soil in the wet zone is low in pH and basic exchangeable cations while the soils in the wet zone are high in pH and basic exchangeable cations. The colour of the soils changes from yellowish-brown to red as the soils get drier presumably due to the presence of haematite and/or goethite. Kaolinite halloysite and smectite are present in all the soils irrespective of the climatic conditions; the amount of halloysite decreases towards the surface. Biotite is abundant in the soil of the intermediate and dry zones but is absent in the soil of the wet zone. Gibbsite is present in the highly weathered soil of the wet zone. The concentration of Ca in soil solution is dependent on the amount in the soils existing in the form of exchangeable Ca. Additionally the solution Ca concentration is significantly correlated with the soil ECEC and te ECEC/CEC ratio.

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Item Type:	Article
Additional Information:	Summaries (En Ms)
AGROVOC Term:	SUELO DE GRANITO
AGROVOC Term:	SOLUCIONES DEL SUELO
AGROVOC Term:	PH DEL SUELO
AGROVOC Term:	PROPIEDADES FISICO-QUIMICAS SUELO
AGROVOC Term:	MINERALOGIA
AGROVOC Term:	ZONAS CLIMATICAS
AGROVOC Term:	TIPOS CLIMATICOS DE SUELOS
AGROVOC Term:	SRI LANKA
Depositing User:	Ms. Norfaezah Khomsan
Last Modified:	24 Apr 2025 05:52
URI:	http://webagris.upm.edu.my/id/eprint/17329

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