Respiração edáfica e nutrientes na Amazônia (Região de Manaus): floresta arenícola, campinarana e campina ()

португальский. Resumo Medições da respiração edáfica (método de Walter & Haber) em floresta arenícola, campinarana e campina, na Reserva INPA-SUFRAMA e arredores (02°38'S, 60°01'W). em Manaus, Amazonas, forneceram médias (mg CO2/m2.h) de 60,18; 52,85 e 44,99 e valores de decomposição no solo (ton M.O./ha.ano) de 2,50; 2.20 e 1.87 respectivamente, estatisticamente diferentes. Incluindo a decomposição aérea, a produtividade primária da floresta arenícola é de 5,0 ton M.O./ha.ano, o valor mais baixo encontrado em florestas amazônicas, provavelmente devido à pobreza do solo em nutrientes minerais e à reduzida biomassa da floresta arenícola. Parece ocorrer aporte e/ou lavagem de nutrientes da fitomassa e seu acúmulo na serapilheira e, talvez, sua transferência direta para a biomassa, bem como grande perda de nutrientes do solo por percolação. Complexação, quelação e insolubilização podem reter certos nutrientes na serapilheira, provavelmente com ação de microrganismos, para os quais o ferro e o alumínio parecem ser importantes. Afora o ferro, os nutrientes retidos na serapilheira parecem depender do tipo de cobertura vegetal Exceto a 40 cm sob campina, todas as demais amostras de solo apresentaram concentrações de alumínio consideradas tóxicas a muitas plantas. Os maiores valores de pH foram encontrados no solo da campina e os menores, na campinarana. Diferenças de comportamento das frações granulométricas com o aumento da profundidade sob cada tipo de vegetação parecem indicar ocorrência de processos diferentes em cada solo. Os autores sugerem outros estudos sobre respiração edáfica durante o ano; sobre ciclagem de nutrientes; sobre alumínio e ferro e sua ação na vegetação e nos decompositores; sobre o solo em diferentes profundidades.

Английский. Summary Soil respiration measurements (Walter & Haber method) were taken in sand forest, campinarana and campina, in the INPA-SUFRAMA reserve and vicinities (02°38'S,60°01'W), near Manaus, Amazonas, Brazil. Carbon dioxide evolution from soil was measured during 7 periods (6 for campina) of 24 hours duration. Its conversion Into primary productivity has furnished mean values which have shown to be statistically different for each habitat, highly significant through the Willis rank-test. The mean values for soil respiration were 60.18, 52.85 and 44.99 mg CO2/m2.h, and the mean values for decomposition were 2.50, 2.20 and 1.87 tons org. mat./ha.year, respectively for sand forest, campinarana and campina. Considering aerial decomposition, the sand forest primary productivity was estimated at 5,0 tons org.mat./ha.year, the lowest figure reported to date for forests of this region. These results are probably due to the soil nutrient deficiency and to the low biomass of this kind of vegetation. Chemical analyses of leaves, litter and soil at different depths seem to indicate that nutrients may be deposited on and/or washed out of the phytomass by rain water; that they may accumulate in the litter layer; that they may then be transferred to biomass via microrhizae and predation in addition to the normal method of nutrient uptake by plants; and that there is a great loss of nutrients in the soil by water (and solutes) percolation. The accumulation of nutrients in the litter layer seems to be due to their complexation. chelation and insolubilization, processes in which microorganisms should have an Important role. Iron and aluminium should also be important in these processes, as well as for these microorganisms. The accumulation of nutrients in the litter layer seems also to be a direct result of the vegetation cover. An exception is iron, which has been shown to be indifferent to the vegetation cover. Except at 40 cm depth under campina all other soil samples have aluminium concentration considered to be toxic to most plants. The highest pH values were found for campina soil, and the lowest ones for campinarana soil. The different behaviour of the granulomerc fractions with increasing depths seems to indicate occurrence of different soil processes. The authors indicate complementary studies which might help in understanding these vegetation types: on annual soil respiration, on nutrient cycling, on aluminum and iron and their influence upon the vegetation and the decomposers, on the soil at different depths.