2008 Joint Annual Meeting (5-9 Oct. 2008): Soil Physical C Sequestration in Response to Tillage and Crop Rotation.

528-5 Soil Physical C Sequestration in Response to Tillage and Crop Rotation.



Monday, 6 October 2008
George R. Brown Convention Center, 360AB
Irfan Aziz, Dept. of Agronomy, University of Arid Agriculture, Rawalpindi, Pakistan, T. Mahmood, Dept. of Environmental Sciences, University of Arid Agriculture, Rawalpindi, Pakistan, Y. Raut, The Ohio State University South Centers, 1864 Shyville Road, Piketon, OH 45661 and Khandakar Islam, Ohio State University - OARDC, OSU South Centers, 1864 Shyville Rd, Piketon, OH 45661-9749
Particulate organic matter (POM) is an important source of labile C and N protected by soil aggregates. A randomized block design in 2 (tillage system) x 3 (crop rotation) factorial arrangement was laid-out to evaluate the impact of tillage and crop rotation (1990 to 2007) on POM and POM associated C and N fractions. Tillage treatments (conventional tillage, CT and no-till, NT) were factored into continuous corn, corn-soybean, and corn–soybean-wheat-cowpeas rotation. Ten soil cores were collected at 0-7.5, 7.5-15, 15-22.5 and 22.5-30 cm), 2-mm sieved, and analyzed for POM, POM associated C and N, total C, pH, and bulk density (rb). Results showed that POM and POM associated C and N varied significantly by tillage and soil depth interaction. The POM, POM-C and POM-N increased significantly by NT compared to CT. However, crop rotation only influenced the POM-C. The CC had higher POM-C than CS and CSW. The POC significantly decreased with increasing soil depth under both tillage and crop rotation. NT x crop rotation had higher POM, POM-C ad POM-N fractions than CT x crop rotation. Continuous corn under NT significantly increased the POM-C in soil.