2008 Joint Annual Meeting (5-9 Oct. 2008): Soil Organic C and Fertilizer N: What Relationship When Not Confounded?.

785-5 Soil Organic C and Fertilizer N: What Relationship When Not Confounded?.



Thursday, 9 October 2008: 9:30 AM
George R. Brown Convention Center, 371F
J. H. Grove, Plant and Soil Sciences, University of Kentucky, N-122L ASCN, Lexington, KY 40546-0091, E. M. Pena-Yewtukhiw, Divison of Plant and Soil Sciences, 1104 Agricultural Sciences Building, West Virginia University, Morgantown, WV 26506-6108, M. Diaz-Zorita, University of Buenos Aires, Faculty of Agronomy, M. T. de Alvear 1665 14 B, Capital Federal, 1060, Argentina and R.L. Blevins, Plant and Soil Sciences, 105 Plant Science Building, University of Kentucky, Lexington, KY 40546-0312
A recent report on the relationship of soil organic C to fertilizer N addition was confounded by the combined impacts of land use change, tillage, N fertilization and time. A long-term (37 yr) monoculture corn (Zea mays L.) tillage (moldboard plow, no-tillage) by N rate (0, 84, 168, 334 kg N per hectare) trial was sampled to a depth of 90 cm, as was the surrounding native grass sod (age greater than 80 yr), to determine the impact of N fertilization, without confounding, on soil organic C. Corn yield in both tillage systems rose with increasing fertilizer N rate, as did organic C, especially in the upper solum. Organic C depletion was most associated with tillage, though land use change (from sod to continuous corn) was also important. As expected, unfertilized sod exhibited greater organic C than unfertilized no-tillage or moldboard plowed soils. There was little tillage by N interaction, indicating that fertilizer N is positively related to soil organic matter levels and associated improvements in cropland soil productivity (grain yield), when considered without confounding.