Soil Science Society of America Journal
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Soil Sci. Soc. Am. J. 77:1659–1666
doi:10.2136/sssaj2012.0423
Received 17 Dec. 2012.
*Corresponding author (lisamfultz@gmail.com).
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Aggregate Carbon Pools after 13 Years of Integrated
Crop-Livestock Management in Semiarid Soils
Soil Biology & Biochemistry
I
n the semiarid Texas High Plains, depletion of irrigation sources, frequent and
intense drought, high winds, and intensive agricultural practices have contrib-
uted to soil degradation resulting in poorly structured soils with low organic
matter (Bronson et al., 2004). Integrated crop-livestock systems are an alternative
to monoculture cropping, which can help alleviate or reverse soil degradation while
meeting the food and iber needs of the growing population (Franzluebbers, 2007;
Allen et al., 2012). Compared to CTN, the dominant crop system in this region,
ICL systems employ reduced or no-till management and high residue-returning
forages (i.e., low disturbance, high input systems). By increasing the amount of res-
idue inputs at the surface while minimizing soil disturbance with conservation till-
age practices, ICLs should build soil organic matter and, thus, enhance aggregate
Lisa M. Fultz*
Jennifer Moore-Kucera
Dep. of Plant and Soil Science
Box 42122
Texas Tech Univ.
Lubbock, TX 79409-2122
Ted M. Zobeck
Veronica Acosta-Martínez
USDA-ARS
Cropping Systems Research Lab.
3810 4th St.
Lubbock, TX 79415
Vivien G. Allen
Dep. of Plant and Soil Science
Box 42122
Texas Tech Univ.
Lubbock, TX 79409-2122
Integrated crop-livestock (ICL) systems that utilize perennial or high-residue
no-till annual forages may build soil organic matter and, thus, enhance aggre-
gate stability, water retention, nutrient cycling, and C storage. We examined
long-term effects of ICL management on soil organic C (SOC) pools com-
pared with continuous cotton [CTN; (Gossypium hirsutum L.)] at the system
and individual vegetation levels, both using limited irrigation (65 and 77%
replacement of evapotranspiration, respectively). Soil samples collected in
1997 (baseline) and 2010 were fractionated into four water stable aggre-
gate-size classes: macroaggregate (>250 μm), microaggregate (53–250 μm),
and silt + clay (<53 μm), and three intra-aggregate size classes: particulate
organic matter (>250 μm), microaggregates (53–250 μm), and silt + clay (<53
μm). Reduced tillage and increased vegetation inputs under WW-B. Dahl Old
World bluestem [Bothriochloa bladhii (Retz) S.T. Blake; bluestem], a com-
ponent of the ICL, resulted in increased mean weight diameter (1.5 mm in
bluestem vs. 0.40 mm in CTN) and higher proportions of macroaggregates
(59%) than under CTN. A continued increase in SOC was measured in the
ICL following 13 yr with 22% more SOC relative to CTN. The results from
the detailed soil aggregate C fractionation revealed that an ICL under limit-
ed irrigation enhanced SOC stored in protected, recalcitrant aggregate pools
(intra-aggregate microaggregate SOC of 8.2 and 5.4 mg g
-1
macroaggregate
in the ICL and CTN, respectively). These beneits impart important ecosys-
tem services such as potential C sequestration and reduced erosion potential,
which are especially important in these semiarid soils.
Abbreviations: CTN, continuous cotton; ICL, integrated crop-livestock; POM, particulate
organic matter; RCWF, rye-cotton-wheat-fallow; SOC, soil organic C; WFRC, wheat-
fallow-rye-cotton.