Division Soil and Water Management, Dep. of Land
Management and Economics,
Katholieke Univ. Leuven, Kasteelpark Arenberg 20 3001
Heverlee, Belgium.
Abstract
Although irrigation is considered
a benefi ciary management for increasing soil organic
C (SOC) stocks in (semi)arid environments, our understanding
of the impact of irrigation
on soil organic matter (SOM) dynamics in the fi eld
remains limited. We investigated the
effect of irrigation on soil C storage in relation
to soil aggregation by measuring C stocks of
bulk soil and different aggreagate fractions in the
top 20-cm layer of center-pivot irrigated
vs. dryland farming systems in semiarid southwestern
Nebraska. The irrigated fi elds (IRR)
showed increased C inputs and larger SOC stocks than
the dryland cultivated fi elds (DRY).
Fractionation of bulk soil samples into non-microaggregate-associated
particulate organic
matter (free POM) and microaggregate-associated POM,
silt, and clay fractions indicated
that the larger bulk SOC stock under IRR was explained
solely by an increase in microaggregate-
associated C storage Wet sieving of bulk soil showed
that microaggregation was remarkably
low under DRY and did not increase under IRR, suggesting
that the protection of
microaggregates inside macroaggregates was no prerequisite
for C sequestration under IRR.
The results of this study confi rm the potential of
irrigation to increase soil C stocks through
preferential sequestration of C inside microaggregates,
but question our understanding of the
mechanisms underlying this preferential sequestration.
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