2022
DOI: 10.3390/agriculture12081204
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No-Till Mitigates SOC Losses after Grassland Renovation and Conversion to Silage Maize

Abstract: Many studies recommend no-till (NT) to increase soil organic carbon (SOC) in the topsoil (<30 cm) of arable land to counterbalance greenhouse gas emissions. Its potential use to mitigate SOC losses during conversion and renovation of grassland ecosystems in the top meter soil is yet to be determined. The SOC dynamics of a 10-year-old grassland converted to silage maize (CM) and renovated and seeded (GR) using either conventional tillage (CT) or NT were compared to an undisturbed grassland control (GC) for 7… Show more

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Cited by 6 publications
(6 citation statements)
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“…Digestate fertilization might also potentially increased the decomposition of SOC (positive priming effect), counteracting most of the additional carbon inputs [ 43 ]. Very low carbon retention from organic fertilizers (liquid dairy manure) was reported in other studies in mono-cropped cereals [ 44 ] and silage maize [ 30 ]. The fertilizer-induced carbon retention was at least 20% in cropping systems including perennials in these studies.…”
Section: Discussionmentioning
confidence: 77%
See 1 more Smart Citation
“…Digestate fertilization might also potentially increased the decomposition of SOC (positive priming effect), counteracting most of the additional carbon inputs [ 43 ]. Very low carbon retention from organic fertilizers (liquid dairy manure) was reported in other studies in mono-cropped cereals [ 44 ] and silage maize [ 30 ]. The fertilizer-induced carbon retention was at least 20% in cropping systems including perennials in these studies.…”
Section: Discussionmentioning
confidence: 77%
“…The increase in SOC content between 2009 and 2017 was 500–600 kg ha −1 yr −1 higher in CR10 (0% maize, 75% leys) compared to CR6 (50% maize, 25% leys), providing strong evidence in support of hypothesis i. In a comparable field experiment on a sandy loam soil in northern Germany [ 30 ], stable SOC contents were found for crop rotations including both grass-clover leys and silage maize in one out of three years and with cattle slurry application. Since SOC content decreased under continuous maize and increased under permanent grassland, the authors concluded that the ley proportion needed to be higher than 33% to significantly enhance SOC stocks, as was the case in our study.…”
Section: Discussionmentioning
confidence: 81%
“…This finding is consistent with previous research showing low retention of digestate carbon and its negligible influence on isotopic composition in crop rotations (Poyda et al, 2022). Likewise, studies have reported low carbon retention from organic fertilizers like liquid dairy manure in monocropped cereals and silage maize (Maillard et al, 2016;De Los Rios et al, 2022b). Legume-grass mixtures and silage maize showed low sensitivity to fertilization, likely due to high biological nitrogen fixation in unfertilized treatments and limited impact of fertilization on root carbon inputs in crop rotations (Poyda et al, 2022).…”
Section: Conversely Judicious Nutrient Management Via Fertilizationmentioning
confidence: 99%
“…Previous research has determined that increasing the time of photosynthetic activity or plant cover throughout the year to increase net primary productivity (NPP), leaving crop residues on the field, as well as reducing the use of tillage can all have a positive impact on SOC, either by promoting its accumulation or by reducing its losses (Weil, 2000;De Los Rios et al, 2022a;2022b). A comprehensive review (King and Blesh, 2018) reported the benefits of using perennial crops and cover crops to increase the SCS of arable lands over cereal and grain-only rotations.…”
Section: Introductionmentioning
confidence: 99%
“…While similar to the distribution patterns of soil organic carbon (SOC), the changes in MBC and DOC content are more influenced by different treatments, resulting in two distinct profile distribution patterns with changes in tillage methods (NPT and RT). Under the NPT mode, the straw cover and no-tillage methods contribute to the accumulation of soil organic carbon [40]. After three years of deep loosening, the organic matter accumulated during the previous two years of no-tillage is incorporated into the 10-30 cm soil layer.…”
Section: Characteristics Of Soil Organic Carbon Profile Distributionmentioning
confidence: 99%