Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia

Limited information is available about factors of soil organic carbon (SOC) preservation in soils along a climo-biosequence. The objective of this study was to evaluate the role of soil texture and mineralogy on preservation of SOC in the topsoil and subsoil along a climo-biosequence in the Main Ran...

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Main Authors: Haghighi, Amir Hossein Jafarzadeh, Jusop, Shamsuddin, Jol, Hamdan, Zainuddin, Norhazlin
Format: Article
Language:English
Published: Science Press, Institute of Mountain Hazards and Environment, CAS and Springer 2017
Online Access:http://psasir.upm.edu.my/id/eprint/15030/
http://psasir.upm.edu.my/id/eprint/15030/1/15030.pdf
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author Haghighi, Amir Hossein Jafarzadeh
Jusop, Shamsuddin
Jol, Hamdan
Zainuddin, Norhazlin
author_facet Haghighi, Amir Hossein Jafarzadeh
Jusop, Shamsuddin
Jol, Hamdan
Zainuddin, Norhazlin
author_sort Haghighi, Amir Hossein Jafarzadeh
building UPM Institutional Repository
collection Online Access
description Limited information is available about factors of soil organic carbon (SOC) preservation in soils along a climo-biosequence. The objective of this study was to evaluate the role of soil texture and mineralogy on preservation of SOC in the topsoil and subsoil along a climo-biosequence in the Main Range of Peninsular Malaysia. Soil samples from the A and B-horizons of four representative soil profiles were subjected to particle-size fractionation and mineralogical analyses including X-ray diffraction and selective dissolution. The proportion of SOC in the 250-2000 μm fraction (SOC associated with coarse sand) decreased while the proportion of SOC in the <53 μm fraction (SOC associated with clay and silt) increased with depth. This reflected the importance of the fine mineral fractions of the soil matrix for SOC storage in the subsoil. Close relationships between the content of SOC in the <53 μm fraction and the content of poorly crystalline Fe oxides [oxalate-extractable Fe (Feo) – pyrophosphate-extractable Fe (Fep)] and poorly crystalline inorganic forms of Al [oxalate-extractable Al (Alo) – pyrophosphate-extractable Al (Alp)] in the B-horizon indicated the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the B-horizon. The increasing trend of Feo — Fep and Alo — Alp over elevation suggest that the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the B-horizon increased with increasing elevation. This study demonstrates that regardless of differences in climate and vegetation along the studied climo-biosequence, preservation of SOC in the subsoil depends on clay mineralogy.
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spelling upm-150302019-05-08T07:49:58Z http://psasir.upm.edu.my/id/eprint/15030/ Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia Haghighi, Amir Hossein Jafarzadeh Jusop, Shamsuddin Jol, Hamdan Zainuddin, Norhazlin Limited information is available about factors of soil organic carbon (SOC) preservation in soils along a climo-biosequence. The objective of this study was to evaluate the role of soil texture and mineralogy on preservation of SOC in the topsoil and subsoil along a climo-biosequence in the Main Range of Peninsular Malaysia. Soil samples from the A and B-horizons of four representative soil profiles were subjected to particle-size fractionation and mineralogical analyses including X-ray diffraction and selective dissolution. The proportion of SOC in the 250-2000 μm fraction (SOC associated with coarse sand) decreased while the proportion of SOC in the <53 μm fraction (SOC associated with clay and silt) increased with depth. This reflected the importance of the fine mineral fractions of the soil matrix for SOC storage in the subsoil. Close relationships between the content of SOC in the <53 μm fraction and the content of poorly crystalline Fe oxides [oxalate-extractable Fe (Feo) – pyrophosphate-extractable Fe (Fep)] and poorly crystalline inorganic forms of Al [oxalate-extractable Al (Alo) – pyrophosphate-extractable Al (Alp)] in the B-horizon indicated the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the B-horizon. The increasing trend of Feo — Fep and Alo — Alp over elevation suggest that the importance of poorly crystalline Fe oxides and poorly crystalline aluminosilicates for the preservation of SOC in the B-horizon increased with increasing elevation. This study demonstrates that regardless of differences in climate and vegetation along the studied climo-biosequence, preservation of SOC in the subsoil depends on clay mineralogy. Science Press, Institute of Mountain Hazards and Environment, CAS and Springer 2017 Article PeerReviewed text en http://psasir.upm.edu.my/id/eprint/15030/1/15030.pdf Haghighi, Amir Hossein Jafarzadeh and Jusop, Shamsuddin and Jol, Hamdan and Zainuddin, Norhazlin (2017) Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia. Journal of Mountain Science, 14 (9). pp. 1763-1775. ISSN 1672-6316; ESSN: 1993-0321 https://link.springer.com/article/10.1007/s11629-015-3720-6 10.1007/s11629-015-3720-6
spellingShingle Haghighi, Amir Hossein Jafarzadeh
Jusop, Shamsuddin
Jol, Hamdan
Zainuddin, Norhazlin
Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title_full Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title_fullStr Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title_full_unstemmed Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title_short Preservation of organic matter in soils of a climo-biosequence in the main range of Peninsular Malaysia
title_sort preservation of organic matter in soils of a climo-biosequence in the main range of peninsular malaysia
url http://psasir.upm.edu.my/id/eprint/15030/
http://psasir.upm.edu.my/id/eprint/15030/
http://psasir.upm.edu.my/id/eprint/15030/
http://psasir.upm.edu.my/id/eprint/15030/1/15030.pdf