2015
DOI: 10.1016/j.still.2015.01.015
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Impact of no-till and reduced tillage on aggregation and aggregate-associated carbon in Northern European agroecosystems

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Cited by 156 publications
(109 citation statements)
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“…Contrary to the lower stability of microaggregates associated to coarse soils observed by Sheehy et al (2015), there was a very strong correlation between the WSA and the Sand proportion (r = 0.97). Thence a stability reduction occurred in samples RF4 and RF5 when the percentage of finer particles rose (Table 2).…”
Section: Physicochemical Characterizationcontrasting
confidence: 80%
“…Contrary to the lower stability of microaggregates associated to coarse soils observed by Sheehy et al (2015), there was a very strong correlation between the WSA and the Sand proportion (r = 0.97). Thence a stability reduction occurred in samples RF4 and RF5 when the percentage of finer particles rose (Table 2).…”
Section: Physicochemical Characterizationcontrasting
confidence: 80%
“…Despite the variability in OC fixation due to heterogeneity of soil matrices, and site conditions, and inherent randomness of representative samplings, the carbon sequestered in bulk soil by the photo‐activity of the iron‐porphyrin catalyst for three consecutive years reached an average of 3.54, 3.90, and 2.24 Mg ha −1 y −1 for the Torino, Piacenza, and Napoli experimental sites, respectively (Table ). These significant yearly amounts of fixed SOC were achieved under conventional tillage management, whereas the current highly experimented NT or RT practices are far from reaching such a large OC increase in cropped bulk soils even after several years, whether under boreal North European (Sheehy, Regina, Alakukku, & Six, ) or Mediterranean (Garcia‐Franco, Albaladejo, Almagro, & Martínez‐Mena, ) agroecosystems.…”
Section: Resultsmentioning
confidence: 99%
“…The results for the BD, TP and Mi are ascribed to: (i) the increase in the crop residue and soil organic carbon at the surface layer (NT) (Hickmann & Costa, 2012) and (ii) the formation and stabilization of biopores as a consequence of the absence of the soil disturbance in NT compared with CT (Kautz, 2014). In the absence of soil tillage, the increase in the soil organic carbon and the biopores improved the soil aggregation (Fernández-Ugalde et al, 2009;Sheehy et al, 2015), making the soil less dense and more porous (Cássaro et al, 2011).…”
Section: Resultsmentioning
confidence: 99%