Nz. Lupwayi et al., Soil microbial biomass and carbon dioxide flux under wheat as influenced by tillage and crop rotation, CAN J SOIL, 79(2), 1999, pp. 273-280
Soil organic matter is important both from an agronomic and an environmenta
l perspective because it affects the capacity of the soil to sustain crop g
rowth, and it is a source and sink of atmospheric CO2-C. Soil microbial bio
mass comprises a small proportion of total soil organic matter, but it is m
ore dynamic than total soil organic matter. Therefore, measurements of soil
microbial biomass may show the effects of soil management on potential cha
nges in soil organic matter before such effects can be detected by measurin
g total soil organic matter. The effects of tillage and crop rotation on so
il microbial biomass and activity were studied in 1995-1997 in the wheat ph
ase of different cropping rotations that had been established in 1992 under
zero tillage or conventional tillage in northern Alberta. Soil microbial b
iomass was often significantly (P < 0.05) higher, but never significantly l
ower, under zero tillage than under conventional tillage. However, CO2 evol
ution (basal respiration) was usually higher under conventional tillage tha
n under zero tillage, resulting in higher specific respiration (qCO(2)) und
er conventional tillage than under zero tillage. The higher additions but l
ower losses of labile C under zero tillage mean that more C is sequestered
in the soil in the zero-tillage system. Thus, this system contributes less
to atmospheric CO2 than conventional tillage, and that soil organic matter
accumulates more under zero tillage. Plots preceded by summerfallow, especi
ally under conventional tillage, usually had the lowest microbial biomass a
nd CO2 evolution, and plots preceded by legume crops had higher microbial b
iomass and lower qCO(2) than other treatments. Tillage and rotation had lit
tle effect on total soil organic matter 5 yr after the treatments had been
imposed, probably because of the cold climate of northern Alberta, but the
results confirm that the labile forms of soil C are more sensitive indicato
rs of soil organic C trends than total soil organic C. These effects of til
lage and rotation on soil microbial biomass were similar to those on microb
ial diversity reported previously. These results confirm that zero tillage
and legume-based crop rotations are more sustainable crop management system
s than conventional tillage and fallowing in the Gray Luvisolic soils of no
rthern Alberta.