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Spatial variability of soil inorganic N in a mature oil palm plantation in Sabah, Malaysia


Citation

Abdul Rahim, Anuar and Kah, Joh Goh and Tee, Bee Heoh and Ahmed, Osumanu Haruna (2008) Spatial variability of soil inorganic N in a mature oil palm plantation in Sabah, Malaysia. American Journal of Applied Sciences, 5 (9). pp. 1239-1246. ISSN 1546-9239; ESSN: 1554-3641

Abstract

The identification and understanding of soil factors influencing yield variability of oil palm enable their efficient management. Soil samples were therefore collected from a fertilizer response trial on oil palm to study the spatial inorganic N distribution and some selected soil chemical properties as affected by long-term N fertilizer applications. The experiment was conducted on mature oil palms grown on Kumansi family (Typic Paleudults) soil in Tawau, Sabah, Malaysia. The soil samples were taken from 2 areas; with and without N treatments for 8 years. They were analyzed for total N, NH4+-N, NO3--N, exchangeable K, and pH. Semivariance analysis was used to characterize the spatial variance of soil NH4+-N and NO3--N while point kriging method was used to illustrate their spatial distributions. Results showed that application of N in the palm circle increased soil NH4+-N above 150 mg kg-1 at 0 to 15 cm depth. In unmanured plot, the NH4+-N contents were similar in the different sites within a palm area although the frond heap area tended to have higher NH4+-N probably due to the N return from the decaying cut fronds. The coefficient of variations for both soil NH4+-N and NO3--N exceeded 30% even within each microsite of palm circle, interrow, frond heaps, and harvesting path. Semivariance analysis showed that the maximum range of soil NH4+-N could be reached at 10 m and 90 m in areas with and without N respectively, indicating that the application of N fertilizer reduced its spatial variability in mature oil palm agroecosystem. The kriged soil map showed localized spots of high NH4+-N content, which corresponded to the palm circles where N fertilizer was applied. Gradual changes in soil fertility were observed in area without N, moving from northern to southern portion of the field. Long-term applications of N caused significant downward movement of NH4+-N and NO3--N to the lower soil depth. They also decreased the soil pH from 4.2 to 3.7, and caused leaching of K to the lower depth. Fertilizer should be broadcast in the interrow in mature oil palm agroecosystem to reduce spatial N variation and other detrimental effects.


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Additional Metadata

Item Type: Article
Divisions: Faculty of Agriculture
Faculty of Agriculture and Food Sciences
DOI Number: https://doi.org/10.3844/ajassp.2008.1239.1246
Publisher: Science Publications
Keywords: Spatial variability; Soil exchangeable ammonium; Soil available nitrate; Soil inorganic nitrogen; Oil palm; Malaysia
Depositing User: Norhazura Hamzah
Date Deposited: 14 Nov 2012 03:54
Last Modified: 23 Nov 2017 05:52
Altmetrics: http://www.altmetric.com/details.php?domain=psasir.upm.edu.my&doi=10.3844/ajassp.2008.1239.1246
URI: http://psasir.upm.edu.my/id/eprint/16799
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