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Long-term effects of continuous direct seeding mulch-based cropping systems on soil nitrogen supply in the Cerrado region of Brazil
Authors:Alexandra Maltas  Marc Corbeels  Eric Scopel  Robert Oliver  Jean-Marie Douzet  Fernando Antonio Macena da Silva  Jacques Wery
Institution:(1) UMR System, Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD), SupAgro, Batiment 27, 2 place Viala, 34060 Montpellier Cedex 2, France;(2) Empresa Brasileira de Pesquisa Agropecuària EMBRAPA-Cerrados, P.O. Box 8223, 73301-970 Planaltina, DF, Brazil;(3) UPR Risques et Environnement, CIRAD, Avenue Agropolis, 34398 Montpellier Cedex 5, France;(4) EMBRAPA-CNPAF, P.O. Box 179, 74001-970 Goiania, GO, Brazil;(5) Present address: Tropical Soil Biology and Fertility Institute of the International Centre for Tropical Agriculture (TSBF-CIAT), P.O. Box MP 228, Mt. Pleasant, Harare, Zimbabwe
Abstract:In the Cerrado region of Brazil conventional soybean monoculture is since the 1980s being replaced by direct seeding mulch-based cropping (DMC) with two crops per year and absence of tillage practices. The objective of this study was to assess the long-term impact of DMC on soil organic matter accumulation and nitrogen (N) mineralization. Measurements of soil organic carbon (C) content, soil total N content and soil N mineralization, both under laboratory conditions using disturbed soil samples and under field conditions using intact soil cores were conducted on a chronosequence of 2-, 6-, 9- and 14-year-old DMC fields (DMC-2, DMC-6, DMC-9 and DMC-14, respectively). The average increase of organic C in the 0–30 cm topsoil layer under DMC was 1.91 Mg C ha−1 year−1. Soil total N increased with 103 kg N ha−1 year−1 (0–30 cm). The potential N mineralization rate under laboratory conditions (28°C, 75% of soil moisture at field capacity) was 0.27, 0.28, 0.39 and 0.36 mg N kg soil−1 day−1 for, respectively, the DMC-2, DMC-6, DMC-9 and DMC-14 soils. The corresponding specific N mineralization rates were 0.16, 0.15, 0.22 and 0.17 mg N g N−1 day−1. There was no obvious explanation for the higher specific N mineralization rate of soils under DMC-9, given the similar soil conditions and land-use history before DMC was introduced. Results from the in situ N incubation experiments were in good agreement with those from the laboratory incubations. We estimated that soil N mineralization increases with about 2.0 kg N ha−1 year−1 under DMC. The increase was mainly attributed to the larger soil total N content. These results indicate that even in the medium term (10 years), continuous DMC cropping has limited implications for N fertilization recommendations, since the extra soil N supply represents less than 20% of the common N fertilization dose for maize in the region.
Keywords:Cerrados  Chronosequence  No-tillage systems  Soil N mineralization  Soil organic carbon  Soil total nitrogen
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