Soil fertility status under shifting cultivation in East Kalimantan with special reference to mineralization patterns of labile organic matter

• Published in: Plant and soil 2009-06, Vol.319 (1-2), p.57-66
• Main Authors: Funakawa, Shinya, Makhrawie, M, Pulunggono, Heru Bagus
• Format: Article
• Language: English
• Subjects: Acid soils; Acidity; Agricultural soils; Agronomy. Soil science and plant productions; Animal, plant and microbial ecology; Biological and medical sciences; Biomedical and Life Sciences; Chemical, physicochemical, biochemical and biological properties; Cropping systems; Cultivation; East Kalimantan; Ecology; Fallowing; Forest soils; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Geochemistry; Life Sciences; Mineralization; Mineralogy; Nitrification; Nitrogen; Nitrogen mineralization; Orchard soils; Organic matter; Organic soils; Physicochemical properties; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Plant Physiology; Plant Sciences; Principal components analysis; Readily mineralizable soil organic matter; Regular Article; Shifting cultivation; Soil ecology; Soil fertility; Soil organic matter; soil pH; Soil properties; Soil science; Soil Science & Conservation; Soil-plant relationships. Soil fertility; Soil-plant relationships. Soil fertility. Fertilization. Amendments
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1007/s11104-008-9849-0

We investigated soil fertility status under shifting cultivation in East Kalimantan with special reference to mineralization patterns of labile soil organic matter (SOM). The soils in this region were generally strongly acidic with high Al, low bases and low pH values. A 133-day incubation experiment using fresh soils revealed that NH₄ ⁺ often accumulated during the course of N mineralization, indicating a delay of nitrification relative to N mineralization in these soils. Principal component analysis followed by stepwise multiple linear regression showed the contribution of soil physicochemical properties to mineralization patterns of SOM. Those results indicated that the overall SOM level positively contributed to the amount of readily mineralizable C and N, NH₄ at day 133, and NO₃ at day 133. The results also showed that the factors relating to soil acidity and P and K depletion, as well as accumulation of readily mineralizable C, contributed to suppress nitrification and accelerate NH₄ ⁺ accumulation and possibly subsequent N immobilization. Our results suggest that it will be difficult to establish a cropping system without a long period of fallow unless very high amounts of fertilizer as well as liming are applied in these regions.