Journal
SOIL RESEARCH
Volume 56, Issue 2, Pages 182-191Publisher
CSIRO PUBLISHING
DOI: 10.1071/SR17039
Keywords
carbon storage in soil; deep ploughing; silt loam soil; soil inversion; soil tillage
Categories
Funding
- New Zealand Ministry of Primary Industries ('Soil carbon sink enhancement') [MAF: CONT-21681-SLMACC-MAU]
- New Zealand Agricultural Greenhouse Gas Research Centre (NZAGRC)
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Permanent pastures require periodic renewal (cultivation and resowing) to maintain their productive potential, which involves a short-term carbon (C) loss. Normal cultivation (ploughing or discing) often involves only the top 10-15 cm, or less, of pasture soils. A regrassing field trial with ryegrass plus white clover swards was established in 2011 to assess the effect of deeper ploughing (25 cm) on C storage in an imperfectly drained soil (Tokomaru silt loam). The site was core sampled (0-30 cm depth) 2 and 4 years (i.e. in 2013 and 2015 respectively) after cultivation and regrassing (soil inversion treatment) to assess changes in soil C content at different depths. At both times, an adjacent uncultivated ryegrass paddock (undisturbed pasture treatment) under similar grazing intensity was also sampled and C stocks were compared. Profiles of cultivated soils (soil inversion) showed higher (P < 0.01) C stocks than the adjacent permanent pasture at the nominal 15-25 and 25-30 cm depths and significantly lower (P < 0.01) C stocks in the topsoil (nominal 0-5 cm depth) for both years sampled (2013, 2015). These findings imply that the differences (inversion - pasture) were consistent 4 years after cultivation and deep ploughing at pasture renewal had resulted in an overall increase in soil C mass to approximately 30 cm of similar to 18% (13.9MgC ha(-1); equivalent soil mass 3701Mg soil ha(-1)) compared with not undertaking the regrassing. This gain in soil C may be temporary, but in a period of 4 years it has significantly increased the net residence time of C in soil related to soil inversion.
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