Da. Wardle et A. Ghani, WHY IS THE STRENGTH OF RELATIONSHIPS BETWEEN PAIRS OF METHODS FOR ESTIMATING SOIL MICROBIAL BIOMASS OFTEN SO VARIABLE, Soil biology & biochemistry, 27(6), 1995, pp. 821-828
Physiological and biochemical methods for estimating soil microbial bi
omass are usually calibrated against other methods and parameters. How
ever, while calibrations are usually made over soils with a very wide
range of microbial biomass values (across a wide geographical range) t
hey are often used to assess relatively small differences in microbial
biomass across a narrower range of microbial biomass values (across a
smaller geographical area, e.g. within a single field), where their r
eliability may be considerably less. We investigated the abilities of
three methods of quantifying microbial biomass, i.e. substrate-induced
respiration (SIR), fumigation-incubation (FI) and fumigation-extracti
on (FE) to serve as predictors of each other across two geographical s
cales, i.e. across 12 sites over an area of approximate to 100 x 100 k
m; and within each of these sites (12 samples per site) over an area o
f 0.3 ha each. Over the larger scale, relationships between pairs of m
ethods were strong, with R(2) values always > 0.90. However, over the
smaller scale, correlations between pairs of methods were variable and
only significant for those sites in which spatial variability in soil
organic matter was relatively high. Uncertain relationships between S
IR and the fumigation-based methods may be expected because they apply
to different subsets of the soil biomass (i.e. glucose-responsive vs
chloroform-sensitive). However, we suggest that FI and FE are sometime
s weakly correlated because the FI decomposition constant k(C) and the
FE constant k(EC) vary differently relative to each other across unde
rlying gradients. Calibration equations for estimating microbial bioma
ss are most accurate when restricted to situations where the range of
biomass values is comparable to that from which the calibration was fi
rst derived, and to similar soil types. In our study, it appears that
calibration equations for predicting microbial biomass are only likely
to provide reliable relative estimates in situations where the coeffi
cient of variation (standard deviation/mean) of soil organic C is > 15
%.