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Nitrogen and phosphorus as limiting factors for growth and primary production in a flooded savanna in the Venezuelan Llanos

Published online by Cambridge University Press:  01 February 2006

Guillermo Sarmiento
Affiliation:
Instituto de Ciencias Ambientales y Ecológicas, Universidad de los Andes, Mérida, Venezuela
Marta Pereira da Silva
Affiliation:
Instituto de Ciencias Ambientales y Ecológicas, Universidad de los Andes, Mérida, Venezuela Present address: Centro Nacional de Pesquisa do Gado de Corte, CNPGC-EMBRAPA, Campo Grande, MS, Brazil.
Maria Elena Naranjo
Affiliation:
Instituto de Ciencias Ambientales y Ecológicas, Universidad de los Andes, Mérida, Venezuela
Marcela Pinillos
Affiliation:
Instituto de Ciencias Ambientales y Ecológicas, Universidad de los Andes, Mérida, Venezuela Present address: Programa de Postgradação em Ecología, Universidade Federal de Río Grande do Sul, Porto Alegre, RS, Brazil.

Abstract

The effects of N, P, NP and NPKS application on plant growth, above-ground primary production and N and P accumulation in the above-ground biomass of a flooded savanna were assessed over two growth cycles. Application of N or P did not improve plant growth and primary production, addition of NP had a noticeable effect, whereas NPKS fertilization led to a three-fold increase in plant production. The four most important grasses in the analysed ecosystem responded to nutrient application with increasing growth, indicating that they all are constrained by nutrient availability, but each species exhibited a different seasonal growth pattern suggesting a temporal division of nutrient resources. N accumulated in the harvested biomass during the growth season was 50% above that of control plants when NP was applied and showed a four-fold increase when NPKS was added. With NP addition, in 2 mo plants accumulated three times more P in the harvested biomass than the control plants. The maximum N accumulated during the growth season in the NPKS treatment represented half the fertilizer N, and probably all the N added (15 g m−2) may have been used if the whole biomass had been considered. With the rather small amounts of P added to the soil in the P treatment (2 g m−2), the maximum amount of P accumulated after 2 mo scarcely represented 13% of the added P, suggesting that most of the fertilizer P became rapidly immobilized or sorbed, not being available to plants in the short term. However, the increasing growth rates of grasses during the following 7 mo indicate that some P fluxed from these pools to the soil solution and to plants.

Type
Research Article
Copyright
2006 Cambridge University Press

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