4.6 Article

Subsoiling during summer fallow in rainfed winter-wheat fields enhances soil organic carbon sequestration on the Loess Plateau in China

Journal

PLOS ONE
Volume 16, Issue 1, Pages -

Publisher

PUBLIC LIBRARY SCIENCE
DOI: 10.1371/journal.pone.0245484

Keywords

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Funding

  1. National Natural Science Fund of China [31801305, 31771727]
  2. China Postdoctoral Science Foundation [2015M581322, 2017T100169]
  3. Scientific and Technological Innovation Fund of Shanxi Agricultural University [2017YJ25]
  4. National Modern Agricultural Industry Technology System [CARS 03-01-24]
  5. Postgraduate Innovation Project of Shanxi Province [2019BY068]

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The study examined the effects of different tillage practices on soil organic carbon sequestration in rainfed winter-wheat fields in China's Loess Plateau region. Results showed that subsoiling during the summer fallow period significantly increased concentrations of different organic carbon forms at various soil depths compared to plow tillage and no tillage. Subsoiling was found to be more effective in increasing soil organic carbon stocks and concentrations, indicating its potential for managing the soil organic carbon pool in the study area.
Scientific management of the soil organic carbon (SOC) pool, e.g., through a reasonable tillage system, is a potential way to mitigate global climate change. There is scarce information about the effect of tillage during the summer fallow period on the SOC pool in rainfed winter-wheat fields. The present study was designed to evaluate the effects of tillage practices, i.e., plow tillage (PTF), subsoiling (STF) and no tillage (NTF), during the summer fallow period on SOC sequestration in winter-wheat fields in the rainfed area of the eastern Loess Plateau of China. The SOC, mineral-associated organic carbon (MOC), permanganate-oxidizable organic carbon (POxC) and particulate organic carbon (POC) concentrations were determined after four years of tillage implementation during the summer fallow period. Our results showed that in comparison to the adoption of NTF, the adoption of STF significantly increased POxC, POC and MOC concentrations by 56.6-111.2%, 45.7-118.7% and 26.2-29.4%, respectively, at the 10-20 and 30-40 cm soil depths before sowing (P < 0.05). The POxC and MOC concentrations under STF at depths of 0-10, 10-20, 20-30 and 30-50 cm were significantly greater than those under PTF and NTF after harvesting (P < 0.05). In addition, the SOC concentration and SOC stock under STF were significantly greater than those under NTF at the 0-10, 10-20, 20-30 and 30-40 cm soil depths before sowing and after harvesting (P < 0.05). Furthermore, in comparison to PTF and NTF, STF resulted in significantly higher SOC stocks by 12.0-25.3% and 7.1-19.2% than PTF and NTF, respectively, in the 0-10, 0-20, 0-30, 0-40 and 0-50 cm soil profiles at harvesting (P < 0.05). In summary, the adoption of STF could be beneficial to the management of the SOC pool in the 0-50 cm soil profile in the rainfed area of winter-wheat on the Loess Plateau of China.

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