Zinc fractionation of tropical paddy soils and their relationships with selected soil properties

Knowledge of zinc (Zn) distribution among various fractions will help to predict the potential of the soil to supply sufficient Zn for crop production. The present study was done to investigate Zn fractions, Zn availability factor (AF) and their relationship with soil properties of Zn-deficient trop...

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Main Authors: Soltani, Shahram Mahmoud, Musa, Mohamed Hanafi, Abd. Wahid, Samsuri, Syed Muhammad, Sharifah Kharidah
Format: Article
Published: Taylor & Francis 2015
Online Access:http://psasir.upm.edu.my/id/eprint/36046/
http://www.tandfonline.com/doi/full/10.1080/09542299.2015.1023091
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spelling my.upm.eprints.360462016-02-15T03:37:17Z http://psasir.upm.edu.my/id/eprint/36046/ Zinc fractionation of tropical paddy soils and their relationships with selected soil properties Soltani, Shahram Mahmoud Musa, Mohamed Hanafi Abd. Wahid, Samsuri Syed Muhammad, Sharifah Kharidah Knowledge of zinc (Zn) distribution among various fractions will help to predict the potential of the soil to supply sufficient Zn for crop production. The present study was done to investigate Zn fractions, Zn availability factor (AF) and their relationship with soil properties of Zn-deficient tropical paddy soils. The samples of two soil orders (six soil series) were sequentially extracted with chemical extractants in two different growth stages of rice (maximum tillering and flowering stages). The proportion of Zn fractions extracted at the maximum tillering stage followed the order, water soluble plus exchangeable (WE) < crystalline sesquioxide (Cry) < manganese oxide (MN) < organically bound (Org) < amorphous sesquioxide (Amor) < residual Zn (Res), whereas the order at the flowering stage was as follows: WE < Mn < Cry < Org < Amor < Res. Cation exchange capacity (CEC), clay content and organic carbon (OC) were the most important factors controlling the distribution of Zn in soils. The AF was low in Tok Young (1.79%), high in Telemong (17%) and medium in the rest of soil series (around 8%). A stepwise multiple linear regression and principal component analyses showed that OC, clay content and CEC were the main variables that explained the predictability of Zn fractions. The result of the length of submerging showed that the WE, Org and Cry concentrations decreased, while Amor, MN, and the sum of all Zn fractions increased with increase in the flooding period. The extractability and solid-phase fractionation of Zn in two different times of soil sampling showed the importance of timing of Zn fertilizer application and flooding or pre-flooding in Zn availability. Taylor & Francis 2015 Article PeerReviewed Soltani, Shahram Mahmoud and Musa, Mohamed Hanafi and Abd. Wahid, Samsuri and Syed Muhammad, Sharifah Kharidah (2015) Zinc fractionation of tropical paddy soils and their relationships with selected soil properties. Chemical Speciation and Bioavailability, 27 (2). pp. 53-61. ISSN 0954-2299 http://www.tandfonline.com/doi/full/10.1080/09542299.2015.1023091 10.1080/09542299.2015.1023091
institution Universiti Putra Malaysia
building UPM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Putra Malaysia
content_source UPM Institutional Repository
url_provider http://psasir.upm.edu.my/
description Knowledge of zinc (Zn) distribution among various fractions will help to predict the potential of the soil to supply sufficient Zn for crop production. The present study was done to investigate Zn fractions, Zn availability factor (AF) and their relationship with soil properties of Zn-deficient tropical paddy soils. The samples of two soil orders (six soil series) were sequentially extracted with chemical extractants in two different growth stages of rice (maximum tillering and flowering stages). The proportion of Zn fractions extracted at the maximum tillering stage followed the order, water soluble plus exchangeable (WE) < crystalline sesquioxide (Cry) < manganese oxide (MN) < organically bound (Org) < amorphous sesquioxide (Amor) < residual Zn (Res), whereas the order at the flowering stage was as follows: WE < Mn < Cry < Org < Amor < Res. Cation exchange capacity (CEC), clay content and organic carbon (OC) were the most important factors controlling the distribution of Zn in soils. The AF was low in Tok Young (1.79%), high in Telemong (17%) and medium in the rest of soil series (around 8%). A stepwise multiple linear regression and principal component analyses showed that OC, clay content and CEC were the main variables that explained the predictability of Zn fractions. The result of the length of submerging showed that the WE, Org and Cry concentrations decreased, while Amor, MN, and the sum of all Zn fractions increased with increase in the flooding period. The extractability and solid-phase fractionation of Zn in two different times of soil sampling showed the importance of timing of Zn fertilizer application and flooding or pre-flooding in Zn availability.
format Article
author Soltani, Shahram Mahmoud
Musa, Mohamed Hanafi
Abd. Wahid, Samsuri
Syed Muhammad, Sharifah Kharidah
spellingShingle Soltani, Shahram Mahmoud
Musa, Mohamed Hanafi
Abd. Wahid, Samsuri
Syed Muhammad, Sharifah Kharidah
Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
author_facet Soltani, Shahram Mahmoud
Musa, Mohamed Hanafi
Abd. Wahid, Samsuri
Syed Muhammad, Sharifah Kharidah
author_sort Soltani, Shahram Mahmoud
title Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
title_short Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
title_full Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
title_fullStr Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
title_full_unstemmed Zinc fractionation of tropical paddy soils and their relationships with selected soil properties
title_sort zinc fractionation of tropical paddy soils and their relationships with selected soil properties
publisher Taylor & Francis
publishDate 2015
url http://psasir.upm.edu.my/id/eprint/36046/
http://www.tandfonline.com/doi/full/10.1080/09542299.2015.1023091
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