Significant structural evolution of a long-term fallow soil in response to agricultural management practices requires at least 10 years after conversion

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Abstract

Agricultural practices can have significant effects on the physical and biological properties of soil. The aim of this study was to understand how the physical structure of a compromised soil, arising from long-term bare-fallow management, was modified by adopting different field management practices. We hypothesized that changing agricultural practices from bare-fallow to arable or grassland would influence the modification of pore structure via an increase in porosity and pore connectivity, and a more homogenous distribution of pore sizes, and that this change exerts a rapid evolution of soil structure following conversion. Soil aggregates (<2 mm) collected in successive years from field plots subjected to three contrasting managements were studied: bare-fallow, bare-fallow converted to arable, and bare-fallow converted to grassland. Soil structure was assessed by X-ray computed tomography on the aggregates at 1.5 μm resolution, capturing detail relevant to soil biophysical processes. The grassland system increased porosity, diversity of pore sizes, pore connectivity and pore-surface density significantly over the decade following conversion. However, measured at this resolution, the evolution of most of these metrics of soil structure required approximately 10 years post-conversion to show a significant effect. The arable system did not influence soil structural evolution significantly. Only pore size distribution was modified in grassland in a shorter time frame (2 years post-conversion). Hence, evolution of soil structural characteristics appears to require at least a decadal timescale following conversion to grassland. Highlights: The physical structure of a compromised soil was modified by adopting plant-based field management practices. Conversion to grassland increased pore size diversity after 2 years. Porosity, pore connectivity and pore surface density showed a significant modification between 7 and 10 years after conversion.

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Bacq-Labreuil, A., Neal, A. L., Crawford, J., Mooney, S. J., Akkari, E., Zhang, X., … Ritz, K. (2021). Significant structural evolution of a long-term fallow soil in response to agricultural management practices requires at least 10 years after conversion. European Journal of Soil Science, 72(2), 829–841. https://doi.org/10.1111/ejss.13037

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