Soil Carbon Accumulation and Nutrient Availability in Managed and Unmanaged Eco-Systems of East Tennessee.

In the last two decades, urban and suburban lands grew by 34% in the United States with 16-20 million hectares maintained under turfgrass systems. Side by side comparison of turfgrass systems with other managed and unmanaged ecosystems have not been comprehensively conducted in the climate transition zone of the United States, despite the environmental significance of land use changes. Our objective was to determine the relative effects of C₃ and C₄ turfgrasses on soil organic carbon (SOC) accumulation and nutrient availability, in comparison with managed row crop and unmanaged woodlot and grassland systems. Soil samples from 0-5, 5-15, and 15-30 cm depths were collected during March 2017 at the University of Tennessee’s East Tennessee Research and Education Center from seven ecosystems: (i) corn (Zea mays L.)-soybean (Glycine max L.) rotation, (ii) continuous soybean, (iii) tall fescue (Festuca arundinacea L.), (iv) Kentucky bluegrass (Poa pratensis L.), (v) bermudagrass (Cynodon dactylon L.), (vi) unmanaged grassland, and (vii) unmanaged woodlot. All turfgrass species were established in 2012 and managed like low-input residential lawns. Within the 30 cm soil profile, turfgrass systems contained 4.2 kg m^-2 SOC at the time of sampling, which was 33% more than croplands and 34% less than unmanaged systems, and C₄ turfgrass systems contained 2.3 kg m^-2 SOC and 0.4 mg kg^-1 inorganic N, which were 56% and 57% lower than C₃ systems, respectively. Results from this study highlight that low-input lawns with suitable grass species can offer higher SOC stock and nutrient availability than conventional cropland systems.