Titlebook: Soils, Ecosystem Processes, and Agricultural Development; Tropical Asia and Su Shinya Funakawa Book 2017 Springer Japan KK 2017 Environment

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Introduction,m-loss” agriculture, respectively, in tropical Asia and Africa. Firstly, shifting cultivation and/or slash-and-burn agriculture in different regions, i.e., in the forest–savanna boundary of Cameroon, monsoonal forests in Thailand, and the miombo woodland of Zambia, are analyzed. These agricultural s

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Influence of Climatic Factor on Clay Mineralogy in Humid Asia: Significance of Vermiculitization of s, are unstable and dissolve to form kaolinite and gibbsite. Under the lower pH conditions of the udic moisture regime in Japan and Indonesia, mica weathers to form 1.4-nm minerals. Differentiated in this way, the soil mineralogical properties are considered to affect the chemical properties of soil

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Significance of Active Aluminum and Iron on Organic Carbon Preservation and Phosphate Sorption/Releassed. The phosphate sorption capacity was strongly correlated with Al. + Fe.. The proportion of labile phosphate relative to added phosphate and the rate of phosphate released in sequential extractions were negatively correlated with Al. + Fe. and porosity of the soils (0.7–4-nm pore specific surfac

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Savannazation of African Tropical Forest Critically Changed the Soil Nutrient Dynamics in East CamerN) ratio is substantially smaller in forest than in savanna, indicating N-rich conditions in forest. There is also lower soil K stock in forest, indicating that K deficiency could be one of the limiting factors for afforestation. Second, I describe the difference in soil nutrient flow between forest

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