Microcalorimetric method was applied to study some Amazonian soils in order
to establish the way by which the microbial soil activity is affected by t
he actual deforestation and burning suffered by the Amazonian rain forest.
Different soil samples were collected in the Amazonian State of Brazil. Pla
ces with autochthonal vegetation and places that which had been deforested
or burnt were elected due to its use in agriculture and cattle raising in a
n attempt to explore the difference in microbial growth behaviour. An LKB 2
277 heat-how microcalorimeter was used for all measurements at 298.15+/-0.0
2 K. The microcalorimetric data are presented together with some other meas
urements such as the physicochemical parameters and the number of microorga
nisms in soil samples. Power-time curves recorded from soil samples amended
with the same quantity of glucose showed significant differences among soi
ls used in the study. Results obtained were systematically studied in a mor
e quantitative way and the values of the microbial growth rate constant, mu
, total thermal effect, Q(T), and duration of the peak-time, PT, were calcu
lated from power-time curves. The collected data showed again important dif
ferences in the microbial activity among the soil samples suggesting that t
he native microbial activity of soils in tropical rain forests are dramatic
ally affected by the deforestation and burning. (C) 1999 Elsevier Science B
.V. All rights reserved.