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자료유형
학술대회자료
저자정보
Padmanabhan, E. (Curtin University of Technology) Eswaran, H. (USDA) Mermut, A.R. (University of Saskatchewan)
저널정보
한국토양비료학회 한국토양비료학회 학술발표회 초록집 The 9th International Conference of The East and Southeast Asis Federation of Soil Science Societies
발행연도
2009.10
수록면
144 - 148 (5page)

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Oxisols cover approximately 23% of the land surface in the tropics and are utilized extensively for agricultural purposes in the tropical countries. Under the variable input types of agricultural systems practiced locally, mapping of some of these soils still appears to be problematic. This hinders attempts to implement sustainable agro-management protocols. Since the introduction of Soil Taxonomy in 1975, several changes hve been made to the definition of Oxisols. The kandi concept, for instance, was introduced to improve the classification of transitional soils. However, the definition for Oxisols in Soil Taxonomy (1999) indicates that additional input is still required to refine the definition in order to resolve some of the outstanding classification problems. Therefore, the objective of this study is to examine the properties of some Oxisols and closely related soils in order to utilize this to enhance mapping strategies. Soils from Malaysia were used in this study. Field observations on these soils provided the first indication that some of the presently classified kandi-Alfisols and kandi-Ultisols were closer to Oxisols in terms of their properties. Water retention differences and apparent CEC of the subsurface horizons also supproted this idea. The types of extractable Fe-oxides and external specific surface areas of the clay fractions showed that many kandic horizons have surface properties that are similar to the oxic horizons. Micromorphology indicated that the gentic transition from the argillic to the oxic involves a diminishing expression of the argillic. The kandic horizon is therefore inferred as a transition to the oxic horizon.
It is proposed that the Oxisols be keyed out based only on the presece of an oxic horizon. The impact of this proposal on the definition of Oxisols is that, soils with kandic horizons that meet the properties of the proposed oxic subsurface horizon, will be grouped under this soil order. There will still be some kandi-Ultisols or kandi-Alfisols; however, these are soils that have much higher apparent CEC. Tesing of the proposed classification on some Malaysian soils showed that the new definition for Oxisols provides a better basis for the classification and mapping of the local soils and the development of meaningful soil management groups for plantations.

목차

Abstract
INTRODUCTION
MATERIALS AND METHODS
GENERAL PROPERTIES
MINERALO-CHEMISTRY
MICROMORPHOLOGY
PROPOSED CHANGES TO CLASSIFICATION AND MAPPING CRITERIA
IMPLICATIONS ON THE MAPPING AND DISTRIBUTION OF MALAYSIAN SOILS
CONCLUSION
REFERENCES

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UCI(KEPA) : I410-ECN-0101-2014-521-000652692