T he soil C sequestration potential of reduced tillage or CT has been extensively studied in other parts of the country, but there has been very little CT research under arid, irrigated agriculture systems, like those in California. California cropping systems are intensively managed and require tillage operations to address furrow irrigation needs. Diverse crop rotations and crops untested for reduced tillage regimes have complicated the development of CT approaches in this highly productive agricultural region. Reducing tillage of agricultural soils may improve agricultural sustainability by reducing fossil fuel consumption, labor needs, equipment maintenance, and soil erosion, and increase soil water conservation and soil C sequestration (Unger et al., 1997; Lal, 2001). Soil C sequestration potential is dependent on a number of factors including climate and parent material. California agricultural soils often have high clay content (loam to loamy clay) because of the depositional environment of the San Joaquin Valley. As a result, these soils may have a greater potential to promote organo-mineral interactions and stabilize C through aggregation; however, irrigation combined with California's warm climate (near-surface soil temperatures often averaging between 25 and 35°C) may enhance decomposer activity and limit the potential for soil C sequestration.