4.7 Article

Does the duration of no-till implementation influence depth distribution of soil organic carbon, hydro-physical properties, and computed tomography-derived macropore characteristics?

Journal

SOIL & TILLAGE RESEARCH
Volume 222, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.still.2022.105426

Keywords

Tillage; Saturated hydraulic conductivity; Pore-size distribution; Plant available water content; X-ray computed tomography

Categories

Funding

  1. USDA Natural Resources Conservation Service, USA [G17AC00337]
  2. South Dakota Agricultural Experiment Station, USA [H351-09, H543-15, RWO 116]

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This study evaluated the effects of no-till (NT) practice on soil hydro-physical properties and found that long-term NT practice (LTNT) increased soil organic carbon (SOC) content, total nitrogen (TN) content, soil water retention (SWR), plant available water (PAW) content, and saturated hydraulic conductivity (Ksat). Short-term NT practice (STNT) had a more pronounced effect on the surface soil (0-10 cm). The study concluded that the conversion of tilled soil to NT practice has beneficial effects on SOC and hydro-physical conditions, but a longer implementation time is required to improve deeper soil profiles.
No-till (NT) is a sustainable alternative to conventional-till (CT), however, the impacts of NT and its duration on the depth distribution of soil organic carbon (SOC), physical and hydrological parameters are less studied. Therefore, the objective of this study was to evaluate the changes in soil hydro-physical properties and X-ray computed tomography (XCT)-derived macropore characteristics to a depth of 40 cm as influenced by the duration [short-(5-yr) and long-(30 yr) term] of NT practice on a previously conventionally-tilled (CT) soil. The treatments included: CT, initiated in 1991; long-term NT (LTNT),1991; and short-term NT (STNT), 2016 established on silty clay loam soil (Udic Haplustolls). Four replicated intact soil cores were collected from each treatment at 0-10, 10-20, 20-30, and 30-40 cm depths. Data showed that the LTNT stored 23% more SOC stock in the 0-40 cm depth as compared to the CT. The LTNT also increased the total nitrogen (TN) stock, soil water retention (SWR), plant available water (PAW) content, and saturated hydraulic conductivity (Ksat) to the depth of 40 cm as compared to the CT. The LTNT increased the XCT-derived soil macroporosity [pores with > 500 mu m equivalent cylindrical diameter (ECD)] and pore connectivity up to 20 cm than the CT. However, the STNT implementation increased the SWR at - 0.6, - 5, and - 30 kPa, pore connectivity, and Ksat only for the 0-10 cm depth than the CT. In addition, PAW showed a high correlation with SOC content [Pearson correlation coefficient (8) = 0.71], and Ksat was highly correlated with the modulus of XCT-derived Euler-Poincare ' characteristic (a measure of local connectivity; 8 = 0.61). The study highlighted that pore connectivity and Ksat in surface soil (0-10 cm) were most responsive to the implementation of NT on a previously tilled soil. Data suggest that a longer duration of NT implementation was required to improve the SOC and soil hydro-physical parameters to a deeper soil profile (0-40 cm). Therefore, we conclude that the conversion of tilled soil to NT practice has beneficial effects, depending upon the duration of NT implementation, in enhancing the SOC and hydro-physical conditions, which may help in storing more water in deeper soil for enhanced production.

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