401-39 Quantity and Quality of C, N and P in Oxisols Under Different Vegetations in Forest-Savanna Transitional Area At Eastern Cameroon.

Poster Number 1906

See more from this Division: S06 Soil & Water Management & Conservation
See more from this Session: General Soil and Water Management and Conservation: II
Wednesday, October 24, 2012
Duke Energy Convention Center, Exhibit Hall AB, Level 1
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So Sugihara1, Makoto Shibata1, Antonie Mvond Ze2, Shigeru Araki3 and Shinya Funakawa1, (1)Graduate school of Agriculture, Soil Science Laboratory, Kyoto University, Kyoto, Japan
(2)Faculty of Agriculture, Dschang University, Dschang, Cameroon
(3)Graduate school of Asian and African Area Studies, Kyoto University, Kyoto, Japan
Poster Presentation
  • SSSA|X^[2012.pdf (322.2 kB)
  • Forest-Savanna transitional area is widely distributed in the central Africa and deforestation has been occurred seriously, due to various human activities. To conserve the biodiversity by proper land management in this area, it is necessary to understand the characteristics of soil nutrients (C, N and P) with its physicochemical property. In the present study, we conducted the field survey around the Eastern Cameroon and make 10 soil profiles (80 cm depth) from five forest and five savanna profiles. Soil samples were collected from each layer and analyzed for pH(H2O), pH(KCl), soil texture, bulk density, exchangeable and total bases (K, Na, Ca, Mg), CEC, oxalate extractable Al and Fe, DCB extractable Al and Fe, total C, N and P contents, and Hedley fractionated P. All soils were classified as Oxisols. The most soil physicochemical properties were not different between the vegetations, while the clay content is clearly larger in forest than that in savanna, and bulk density was clearly smaller in forest than that in savanna at surface layers (0-5 and 5-10 cm; p<0.05). Accumulated C, N and P at the soil profile (0-80 cm) was 87.9, 7.7 and 3.7 t C N P ha-1 in forest, respectively, and was 98.6, 7.1 and 3.7 t C N P ha-1 in savanna, respectively, and there is no clear difference for the vegetation. On the other hand, quality of soil organic matter, i.e., C/N ratio, was clearly higher in savanna (13.0~15.7) than in forest (11.0~12.0) in the upper layer (0-40 cm; p<0.05). In addition, the rate of NaOH-extractable inorganic P, fixed by Al and Fe oxide, to the total P was also clearly higher in savanna (13.1~15.3%) than in forest (9.6~10.4%) for same soil depth (0-40 cm; p<0.05). These results indicate that accumulated C, N and P quality of upper layer should be different between the forest and savanna, indicating the different pattern of nutrient mineralization and hence degradation after cultivation.
    See more from this Division: S06 Soil & Water Management & Conservation
    See more from this Session: General Soil and Water Management and Conservation: II