Preprints
https://doi.org/10.5194/soil-2021-5
https://doi.org/10.5194/soil-2021-5

  12 Feb 2021

12 Feb 2021

Review status: this preprint is currently under review for the journal SOIL.

Nonlinear turnover rates of soil carbon following cultivation of native grasslands and subsequent afforestation of croplands

Guillermo Hernandez-Ramirez1, Thomas J. Sauer2, Yury G. Chendev3, and Alexander N. Gennadiev4 Guillermo Hernandez-Ramirez et al.
  • 1Department of Renewable Resources, University of Alberta, Edmonton, AB, T6G2R3, Canada
  • 2USDA-ARS, National Laboratory for Agriculture and Environment, Ames, IA 50011, USA
  • 3Department of Natural Resources Management and Land Cadastre, Belgorod State University, 85 Pobeda Street, Belgorod 308015, Russia
  • 4Lomonosov Moscow State University, Faculty of Geography, 119991, Moscow, GSP-1, 1 Leninskiye Gory, Russia

Abstract. Land use conversions can strongly impact soil organic matter (SOM) storage, which creates paramount opportunities for sequestering atmospheric carbon into the soil. It is known that land uses such as annual cropping and afforestation can decrease and increase SOM, respectively; however, the rates of these changes over time remain elusive. This study focused on extracting the kinetics (k) of turnover rates that describe these long-term changes in soil C storage and also quantifying the sources of soil C. We used topsoil organic carbon density and δ13C isotopic composition data from multiple chronosequences and paired sites in Russia and United States. Reconstruction of soil C storage trajectory over 250 years following conversion from native grassland to continual annual cropland revealed a C depletion rate of 0.010 years−1 (first-order k rate constant), which translates into a mean residence time (MRT) of 100 years (R2 ≥ 0.90). Conversely, soil C accretion was observed over 70 years following afforestation of annual croplands at a much faster k rate of 0.055 years−1. The corresponding MRT was only 18 years (R2 = 0.997) after a lag phase of 5 years. Over these 23 years of afforestation, trees contributed 14 Mg C Ha−1 to soil C accrual in the 0 to 15 cm depth increment. This tree-C contribution reached 22 Mg C Ha−1 at 70 years after tree planting. Over these 70 years of afforestation, the proportion of tree-C to whole soil C increased to reach a sizeable 79 %. Furthermore, assuming steady state of soil C in the adjacent croplands, we also estimated that 45 % of the prairie-C existent at time of tree planting was still present in the afforested soils 70 years later. As intrinsic of k modelling, the derived turnover rates that represent soil C changes over time are nonlinear. Soil C changes were much more dynamic during the first decades following a land use conversion than afterwards when the new land use system approached equilibrium. Collectively, results substantiated that C sequestration in afforested lands is a suitable means to proactively mitigate escalating climate change within a typical person's lifetime, as indicated by MRTs of few decades.

Guillermo Hernandez-Ramirez et al.

Status: open (until 04 Apr 2021)

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Guillermo Hernandez-Ramirez et al.

Guillermo Hernandez-Ramirez et al.

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