A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
Effect of Soil Texture on Carbon Dynamics and Storage Potential in TropicalForest Soils of Amazonia.Everaldo de C. C. Telles, Plinio B. de Camargo e Luis A. Martinelli 1 ; Susan E.Trumbore e Enir S. Costa 2 ; Joaquim dos Santos e Niro Higuchi 3 , Raimundo CosmeOliveira Junior e Elder Campos 4 .ectelles@cena.usp.br,pcamargo@cena.usp.br,zebu@cena.usp.br,setrumbo@uci.edu,salazar@essgrad.ps.uci.edu,joca@inpa.gov.br,niro@inpa.gov.br,cosme@cpatu.embrapa.br, elcmpr@hotmail.com1 CENA, Universidade de São Paulo, Av. Centenário 303, Piracicaba, SP 13416-000– Brazil; 2 University of California, Irvine, CA, 92697-3100 USA ; 3 Instituto Nacionalde Pesquisas da Amazônia /Brasil; 4 Embrapa Amazônia Oriental/Brazil.We investigated the role of soil clay content in the storage and dynamics of soil carbonat primary tropical forest sites spanning a range of soil texture by combining stable andradiocarbon isotope measurements of bulk and fractionated soil organic matter. Claycontent is a major control of the amount of refractory carbon in soils and thereforestrongly influences the storage and dynamics of carbon in tropical forest soils. Soils inprimary tropical forest have been proposed as a potentially large sink for carbon at a sitenear Manaus, in the central Amazon. Comparison of carbon contents of Oxisolssampled near Manaus, Brazil, over the past 20 years shows no measurable change inorganic carbon stocks with time. Simple models estimating the response of soil carbonpools to a 25% increase in productivity indicate that storage rates in soils averaging 0.4to 0.7 MgC ha -1 yr -1 in soil organic matter and 0.3 to 0.4 MgC ha -1 yr -1 in litter and rootsare possible in the first decade following the increase. Export of carbon in dissolvedform from terra firme soils can account for
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Effect of Soil Texture on Carbon <strong>Dynamics</strong> and Storage Potential in TropicalForest Soils of <strong>Amazon</strong>ia.Everaldo de C. C. Telles, Plinio B. de Camargo e Luis A. Martinelli 1 ; Susan E.Trumbore e Enir S. Costa 2 ; Joaquim dos Santos e Niro Higuchi 3 , Raimundo CosmeOliveira Junior e Elder Campos 4 .ectelles@cena.usp.br,pcamargo@cena.usp.br,zebu@cena.usp.br,setrumbo@uci.edu,salazar@essgrad.ps.uci.edu,joca@inpa.gov.br,niro@inpa.gov.br,cosme@cp<strong>at</strong>u.embrapa.br, elcmpr@hotmail.com1 CENA, Universidade de São Paulo, Av. Centenário 303, Piracicaba, SP 13416-000– Brazil; 2 University of California, Irvine, CA, 92697-3100 USA ; 3 Instituto Nacionalde Pesquisas da Amazônia /Brasil; 4 Embrapa Amazônia Oriental/Brazil.We investig<strong>at</strong>ed <strong>the</strong> role of soil clay content in <strong>the</strong> storage and dynamics of soil carbon<strong>at</strong> primary tropical forest sites spanning a range of soil texture by combining stable andradiocarbon isotope measurements of bulk and fraction<strong>at</strong>ed soil organic m<strong>at</strong>ter. Claycontent is a major control of <strong>the</strong> amount of refractory carbon in soils and <strong>the</strong>reforestrongly influences <strong>the</strong> storage and dynamics of carbon in tropical forest soils. Soils inprimary tropical forest have been proposed as a potentially large sink for carbon <strong>at</strong> a sitenear Manaus, in <strong>the</strong> central <strong>Amazon</strong>. Comparison of carbon contents of Oxisolssampled near Manaus, Brazil, over <strong>the</strong> past 20 years shows no measurable change inorganic carbon stocks <strong>with</strong> time. Simple models estim<strong>at</strong>ing <strong>the</strong> response of soil carbonpools to a 25% increase in productivity indic<strong>at</strong>e th<strong>at</strong> storage r<strong>at</strong>es in soils averaging 0.4to 0.7 MgC ha -1 yr -1 in soil organic m<strong>at</strong>ter and 0.3 to 0.4 MgC ha -1 yr -1 in litter and rootsare possible in <strong>the</strong> first decade following <strong>the</strong> increase. Export of carbon in dissolvedform from terra firme soils can account for