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

• Main Authors: G. Hernandez-Ramirez, T. J. Sauer, Y. G. Chendev, A. N. Gennadiev
• Format: Article
• Language: English
• Published: Copernicus Publications 2021-07-01
• Series: SOIL
• Online Access: https://soil.copernicus.org/articles/7/415/2021/soil-7-415-2021.pdf
• ISSN: 2199-3971; 2199-398X

<p>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 (<span class="inline-formula"><i>k</i></span>) 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 <span class="inline-formula"><i>δ</i>¹³</span>C 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 yr<span class="inline-formula">⁻¹</span> (first-order <span class="inline-formula"><i>k</i></span> rate constant), which translates into a mean residence time (MRT) of 100 years (<span class="inline-formula"><i>R</i>²≥0.90</span>). Conversely, soil C accretion was observed over 70 years following afforestation of annual croplands at a much faster <span class="inline-formula"><i>k</i></span> rate of 0.055 yr<span class="inline-formula">⁻¹</span>. The corresponding MRT was only 18 years (<span class="inline-formula"><i>R</i>²=0.997</span>) after a lag phase of 5 years. Over these 23 years of afforestation, trees contributed 14 Mg C ha<span class="inline-formula">⁻¹</span> to soil C accrual in the 0 to 15 cm depth increment. This tree-C contribution reached 22 Mg C ha<span class="inline-formula">⁻¹</span> 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 sizable 79 %. Furthermore, assuming steady state of soil C in the adjacent croplands, we also estimated that 45 % of the prairie C existent at the time of tree planting was still present in the afforested soils 70 years later. As an intrinsic property of <span class="inline-formula"><i>k</i></span> modeling, 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 a few decades.</p>