337-4 Nitrogen Mineralization In Cover Crop Above- and below-Ground Biomass Added to Soils.

See more from this Division: S08 Nutrient Management & Soil & Plant Analysis
See more from this Session: Nitrogen Management
Wednesday, November 3, 2010
Long Beach Convention Center, Exhibit Hall BC, Lower Level

Andrae K. Genus, Department of Agricultural and Environmental Sciences, Tuskegee University, Tuskegee, AL and Kokoasse Kpomblekou-A., Tuskegee University, Tuskegee, AL
Cover crops are grown to protect soil against wind and water erosion and/or to increase nitrogen (N) input into soil following incorporation of the biomass into soil. However, contributions of the above- and below-ground biomass to the total N mineralized pool are not well understood. A study was initiated to examine N mineralization in three soils amended with above or below-ground biomass of crimson clover, black oat, Sudan grass, or hairy vetch. The objectives of the study were to determine N mineralization rates in three Alabama soils and to establish relationships between soil properties and N mineralization kinetic parameters. Surface soils (0-15 cm) were selected to represent a range of chemical properties. The soil sample (< 2-mm) was mixed with silica sand and treated with above or below ground cover crop biomass to give a concentration of 300 mg N kg-1 soil. The mixture was packed into a leaching tube incubated at 25�1�C and leached every two weeks with 5 mM CaCl2 for 20 weeks. The inorganic N contents of the leachate were analyzed by steam distillation. A non-linear regression approach for N mineralization was used to estimate the readily mineralizable organic N pools (No) and the first-order rate constant (k). Cumulative ammonium (NH4+)-N and nirate (NO3-)-N were plotted against incubation time (weeks). Results showed that incubation of the soils without cover crop biomass increased NH4+-N and NO3- -N released only until four weeks but then stabilized at < 10 mg-N kg-1 soil. Addition of the cover crop biomass increased the amount of NH4+ and NO3- released significantly by (P < 0.05) as compared with the non-amended soils. On average, the cumulative NH4+-N released in the soils were 60, 30, and 20 mg kg-1 soil for Sucarnoochee, Maytag, and Colbert soils, respectively.