Abstract

The suitability of the fumigation-incubation (FI), fumigation-extraction (FE) (with specific k-factor determined by 14C-labelling) and substrate induced respiration (SIR) methods to obtain measures of the microbial biomass in forest soils from the Amazonian basin was examined. Several representitive topsoil (0–10 cm) samples were studied. A reasonable estimate of microbial biomass C in two acid Oxisols (pH <4.5) with a high clay content was obtained by the FI method, provided no correction was applied for basal CO 2 respiration. However, on two Ultisols and one Alfisol more consistent estimates of microbial C were obtained by the FI method, where correction for basal respiration was obtained using the respiration of non-fumigated (NF) soils between 0–10 d, or fumigated (F) soils between 10–20 d. Estimates of microbial C by the FE method did not differ significantly from those obtained by the FI method when calculated using a specifically-determined k-factor of 0.26 to convert the extractable-C flush to microbial biomass C. In the Ultisols and the Alfisol, the SIR method gave similar estimates of microbial C to those obtained by the FI and FE methods, but in both Oxisols microbial C was underestimated when a standard conversion factor was applied. Possibly the SIR assay was adversely affected by a high proportion of dormant organisms and a slow gaseous release of respired CO 2 from these heavy clay soils. When estimated using the FE method, microbial C was in the range 890–1100 μg C g −1 soil in the Oxisols, 340–470 μg C g −1 soil in the Ultisols and around 580 μg C g −1 soil in the Alfisol. Microbial C comprised 3–4% of the total soil organic C and microbial N 4–7% of total N. Microbial C-to-N ratios averaged 6.9 ± 0.8. Although the FI method can be used on these Amazonian soils, the FE method is more convenient and generally appears suitable for estimating both microbial C and N in the same extract. The SIR method is not recommened for use with Oxisols.

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