Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*

The charge properties of 8 sod series were studied. The study shows that gibbsite is related to the pH0 of these soils. Negative charges exceed positive charges at the pH range of 3 to 6, thus the PZNC of these soils cannot be obtained. The sum of A l and bases is a better estimate of ECEC than of...

Full description

Bibliographic Details
Main Authors: Jusop, Shamsuddin, Tessens, Eddy
Format: Article
Language:English
English
Published: 1985
Online Access:http://psasir.upm.edu.my/id/eprint/2545/
http://psasir.upm.edu.my/id/eprint/2545/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia.pdf
_version_ 1848839277017825280
author Jusop, Shamsuddin
Tessens, Eddy
author_facet Jusop, Shamsuddin
Tessens, Eddy
author_sort Jusop, Shamsuddin
building UPM Institutional Repository
collection Online Access
description The charge properties of 8 sod series were studied. The study shows that gibbsite is related to the pH0 of these soils. Negative charges exceed positive charges at the pH range of 3 to 6, thus the PZNC of these soils cannot be obtained. The sum of A l and bases is a better estimate of ECEC than of the PC of the soils. These soils are either in the recent or intermediate stage of weathering, shown by the low pH0 and high weathering index.
first_indexed 2025-11-15T07:08:53Z
format Article
id upm-2545
institution Universiti Putra Malaysia
institution_category Local University
language English
English
last_indexed 2025-11-15T07:08:53Z
publishDate 1985
recordtype eprints
repository_type Digital Repository
spelling upm-25452013-05-27T07:01:49Z http://psasir.upm.edu.my/id/eprint/2545/ Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties* Jusop, Shamsuddin Tessens, Eddy The charge properties of 8 sod series were studied. The study shows that gibbsite is related to the pH0 of these soils. Negative charges exceed positive charges at the pH range of 3 to 6, thus the PZNC of these soils cannot be obtained. The sum of A l and bases is a better estimate of ECEC than of the PC of the soils. These soils are either in the recent or intermediate stage of weathering, shown by the low pH0 and high weathering index. 1985 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/2545/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia.pdf Jusop, Shamsuddin and Tessens, Eddy (1985) Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*. Pertanika, 8 (2). pp. 169-179. English
spellingShingle Jusop, Shamsuddin
Tessens, Eddy
Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title_full Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title_fullStr Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title_full_unstemmed Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title_short Some T 2 Terrace Soils of Peninsular Malaysia: III. Surface Charge Properties*
title_sort some t 2 terrace soils of peninsular malaysia: iii. surface charge properties*
url http://psasir.upm.edu.my/id/eprint/2545/
http://psasir.upm.edu.my/id/eprint/2545/1/Some_T_2_Terrace_Soils_of_Peninsular_Malaysia.pdf