RELATIONSHIP BETWEEN THE AMOUNT AND THE ACTIVITY OF THE MICROBIAL BIOMASS IN DUTCH GRASSLAND SOILS - COMPARISON OF THE FUMIGATION INCUBATION METHOD AND THE SUBSTRATE-INDUCED RESPIRATION METHOD
J. Hassink, RELATIONSHIP BETWEEN THE AMOUNT AND THE ACTIVITY OF THE MICROBIAL BIOMASS IN DUTCH GRASSLAND SOILS - COMPARISON OF THE FUMIGATION INCUBATION METHOD AND THE SUBSTRATE-INDUCED RESPIRATION METHOD, Soil biology & biochemistry, 25(5), 1993, pp. 533-538
The aim of this study was to test whether soil texture and amount of a
vailable carbon affect microbial activity and the percentage of the so
il microbial biomass that is active. Total and active microbial biomas
s were determined by the fumigation-incubation method (FI) and the sub
strate-induced respiration method (SIR), respectively. The ratio bioma
ss-SIR: biomass-FI, indicating the percentage of active microbial biom
ass, and the ratio C mineralization:biomass-FI, indicating the activit
y of the microbial biomass, were both higher in soils with a coarse te
xture than in soils with a fine texture. The ratio C mineralization:bi
omass-SIR was not affected by soil texture. The ratios biomass-SIR: bi
omass-FI and C mineralization: biomass-FI were higher in the upper 10-
cm soil layer than in the 10-25 cm layer, while the ratio C mineraliza
tion: biomass-SIR was not affected by soil depth. During 25 weeks incu
bation, the amount of biomass-SIR as well as the C mineralization rate
decreased significantly. The amount of biomass-FI, however, did not c
hange significantly during incubation. Assuming that the amount of ava
ilable C decreases both with soil depth and during incubation, the obs
ervations indicate that smaller amounts of available carbon coincide w
ith a reduced activity of the biomass and a lower percentage of active
biomass. The close similarity between C mineralization rate and amoun
t of biomass-SIR shows that biomass-SIR is a good indicator of microbi
al activity, whereas the FI method is not suitable for this purpose.