Jp. Winter et al., MEASUREMENT OF MICROBIAL BIOMASS BY FUMIGATION-EXTRACTION IN SOIL STORED FROZEN, Soil Science Society of America journal, 58(6), 1994, pp. 1645-1651
This research examined the effect of freezing on soil microbial C and
N measured by CHCl3 fumigation-extraction (CFE). A soil was stored fro
zen (-15 degrees C) and sampled after 1, 7, and 170 d. Compared with a
nonfrozen soil, freezing had no effect on microbial C or N, except af
ter 7 d when C increased by 24% and N increased by 34%. The soil was a
lso subjected to freeze-thaw cycles (18/6 h). Microbial C and N were u
naffected by one cycle, increased with two, and decreased with three c
ycles. In a second experiment, soil was amended with C-14-glucose and
incubated for 1, 7, or 35 d (25 degrees C), then stored frozen for eit
her 1, 7, 21, or 35 d. Soil incubated for 1 d showed a decline in micr
obial C-14 (measured by CFE) after freezing for 7 to 35 d. Soil incuba
ted for 7 and 35 d contained a C-14 microbial population that was unaf
fected by freezing. At first glance, these observations indicated that
the CFE assay was not greatly affected by freezing soils; however, cl
oser examination indicated that microbial mortality had been masked by
a freezing-induced improvement in CFE efficiency. Increased efficienc
y may have resulted from improved aggregate dispersal following freezi
ng. Homogenization of soil samples improved extraction of microbial C
by 40%. In conclusion, we don't recommend that soils be frozen prior t
o CFE. Also, the physical disruption of soil during CFE must be severe
to remove any interference of aggregate stability on the results of t
his assay.