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Climate and vegetation determine soil organic matter status in an alpine inner-tropical soil catena in the Fan Si Pan Mountain,Vietnam
Authors:P. Podwojewski  J. Poulenard  Minh Luu Nguyet  A. de Rouw  Van Thiet Nguyen  Quang Ha Pham  Duc Toan Tran
Affiliation:1. IRD, UMR BIOEMCO (Institut de Recherche pour le Développement) c/o School of Bioresources Engineering and Environmental Hydrology, University of KwaZulu-Natal, Box X01, Scottsville, 3209, South Africa;2. EDYTEM, Université de Savoie/CNRS, 73376 Le Bourget du Lac, France;3. IRD, IWMI (International Water Management Institute), MSEC program c/o Soils and Fertilizers Institute (SFI) Dong Ngac, Tu Liem District-Hanoi, Hanoi, Viet Nam;4. IRD, UMR BIOEMCO, University Pierre & Marie Curie, 4 place Jussieu, 75252, Paris Cedex, France;5. SFI (Soils and Fertilizers Institute, VAAS, MARD), Dong Ngac, Tu Liem District-Hanoi, Hanoi, Viet Nam
Abstract:High mountain ecosystems are generally considered to be particularly sensitive to global climate change. Studies of pedogenesis associated with altitudinal variation, vegetation type and soil carbon content on the same type of parent rock are very limited in inter-tropical mountain areas. Therefore the altitudinal variation of soil pedogenesis through 9 selected profiles from the altitude of 1340 m to 3143 m asl, the summit of the Fan Si Pan Mountain, in the north of Vietnam was examined. Fan Si Pan Mountain is composed of a homogenous alkaline granite rock and is the highest point of the Inter-tropical Continental Asia. The Soil Organic Matter properties (C, N, δ13C and δ15N contents) of the different grain-size fractions of the topsoil of 4 selected profiles corresponding to different ecosystems were also examined.
Keywords:Altitudinal gradient   Soil Organic Matter   Mountain soil   Soil genesis   Podzol
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