The increasing concern for rising CO2 concentrations from agricultural
activities has prompted the need to better understand the flux of gre
enhouse gases to the atmosphere. This work determines the effect of fo
ur fall tillage methods on short-term CO2 flux from a Hemerly clay loa
m (fine loamy, frigid Aeric Calciaquoll) in the northern Corn Pelt. Mo
ldboard plow only, moldboard plow plus disk harrow twice, disk harrow
once, and chisel plow once using standard tillage equipment following
a wheat (Triticum aestivum L.) crop were compared with no-tillage. The
CO2 flux was measured with a large portable system commonly used to m
easure canopy gas exchange of field crops. Measurements of CO2 flux we
re initiated within 5 min after tillage completion for each tillage tr
eatment and continued intermittently for 19 d. Moldboard plow had the
roughest soil surface and the highest initial CO2 flux (29 g m(-2) h(-
1)) and maintained the highest flux throughout the study. Moldboard pl
ow plus disking twice and chisel plow had similar initial rates (7 and
6 g m(-2) h(-1), respectively) that were greater than disk harrow and
no-tillage. The high initial CO2 fluxes were more related to depth of
soil disturbance that resulted in a rougher surface and Larger voids
than to residue incorporation. The differences in CO2 flux between til
lage treatments were small but consistent 19 d after initial tillage a
nd 64 mm rain. Lower CO, flux rates caused by tillage were associated
with Low soil disturbance and/or small voids. Tillage methods affected
the initial CO2 flux differently and suggest improved soil management
can minimize agriculture's impact on global CO2 increase.