Abstract
Optimizing a
three-way pact comprising crop yields, fertility inputs and greenhouse
gases may minimize the contribution of croplands to global warming.
Fluxes of N2O, CO2 and CH4 from soil were measured under maize (Zea mays L.) grown using 0, 60 and 120 kg N hm-2 as NH4NO3-N
and composted manure-N in three seasons on clay (Chromic luvisol) and
sandy loam (Haplic lixisol) soils in Zimbabwe. The fluxes were measured
using the static chamber methodology involving gas chromatography for
ample air analysis. Over an average of 122 days we estimated emissions
of 0.1 to 0.5 kg N2O-N hm−2, 711 to 1574 kg CO2-C hm−2 and−2.6 to 5.8 kg CH4-C hm−2
from six treatments during season II with the highest fluxes. The posed
hypothesis that composted manure-N may be better placed as a mitigation
option against soil emissions of GHG than mineral fertilizer-N was
largely supported by N2O fluxes during
the wet period of the year, but with high level of uncertainty. Nitrogen
addition might have stimulated both emissions and consumption of CH4
but the sink or source strength depended highly on soil water content.
We concluded that the application of mineral-N and manure input may play
an important role with reference to global warming provided the season
can support substantial crop productivity that may reduce the amount of N2O
loss per unit yield. Confidence in fluxes response to agricultural
management is still low due to sporadic measurements and limited
observations from the southern African region.
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