Tuesday, 7 October 2008
George R. Brown Convention Center, Exhibit Hall E
Alassane Sissoko and Kokoasse Kpomblekou-A, Department of Agricultural and Environmental Sciences, Tuskegee University, Tuskegee, AL
Organic carbon
is generally low in Alabama
soils and varies considerably with cropping systems. Decomposition rates of
organic C in ten Alabama soils treated with two broiler litter (BL) samples were
investigated under laboratory conditions at room temperature. A 20-g surface
(0-15 cm) soil (<2-mm) was mixed with appropriate amounts of BL to give 9 g
organic C kg-1 soil. The soil-BL mixture was transferred into a French
square bottle and moistened to 60% water holding capacity. The incubation
bottle was connected to a continuous aerobic incubation apparatus. Air from a
laboratory outlet was connected to a scrubber consisting of 4 M NaOH,
concentrated H2SO4, a nanometer to regulate air flow, and
a manifold of tygon tubes passing the CO2-free
air through the incubation bottles, and test tubes containing 25 mL of NaOH solution of known molarity (0.2 M)
to trap the CO2 evolved from the incubation bottles. Controls were
also included to estimate the CO2 evolved from untreated soils. The
trapping solution was replaced with fresh solution on a regular basis. The CO2
trapped was determined potentiometrically by
titrating 20 mL aliquot of the NaOH
solution in the test tube with a standard HCl
solution (0.2 M). Before titration, an
excess 0.375 M BaCl2 solution
was added to precipitate carbonate. Soil samples obtained from organic farming
plots were similarly incubated for 30 days. Generally, the rate constant (k)
varied with soils and treatments. The k values of BL-amended soils ranged from
0.022 in Dothan
soil to 0.103 in Appling soil, while those of none amended soils varied from
0.00014 in Sucarnoochee soil to 0.031 in Troup soil. The
k values of the soils obtained from the organic farming plots were similar to
those of none amended soils suggesting that only recalcitrant organic C
remained in the soils.