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SOIL & WATER MANAGEMENT & CONSERVATION

Rebuilding Organic Carbon Contents in Coastal Plain Soils Using Conservation Tillage Systems

^a USDA-ARS, Coastal Plains Soil, Water, and Plant Res. Center, 2611 West Lucas St., Florence, SC 29501
^b Clemson Univ., Pee Dee Research and Education Ctr., 2200 Pocket Rd., Florence, SC 29506

^* Corresponding author (jeff.novak{at}ars.usda.gov).

Long-term disk tillage (DT) for cotton (Gossypium hirsutum L.) production in the southeastern U.S. Coastal Plain has resulted in soil organic C (SOC) content reductions. Conservation tillage (CT) management in some studies can rebuild SOC levels. A field study, with two adjacent 3.5-ha fields, both containing soil series formed in upland and depressional areas, was conducted using a 6-yr rotation of corn (Zea mays L.) and cotton to determine the CT and DT effects on SOC contents and residue characteristics returned to the soil. Annual soil samples were collected from 50 locations per field at 0- to 3- and 3- to 15-cm. After 6 yr under CT, residue accumulation promoted a significant SOC increase in the 0- to 3-cm depth in the upland soil series (about 0.7 Mg SOC ha^–1). The lack of residue mixing in the 3- to 15-cm depth in upland soils under CT, however, resulted in a significant SOC content decline at this depth (1.25–2.51 Mg SOC ha^–1). There was no significant SOC content change in soils under CT formed in depressional areas or in all soils under DT. During 6 yr, 14.8 Mg ha^–1 of organic C from both corn and cotton residues was returned to soils under CT, but <4% was incorporated into the SOC pool. Levels of SOC in sandy upland soils can be increased at the surface after 6 yr of CT under a corn and cotton rotation, with the increase coming at the expense of an SOC decline at a deeper topsoil depth.

Abbreviations: CT, conservation tillage • DT, disk tillage • OC, organic carbon • SOC, soil organic carbon