2014
DOI: 10.4141/cjss2013-094
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Soil organic carbon and land use: Processes and potential in Ontario’s long-term agro-ecosystem research sites

Abstract: Congreves, K. A., Smith, J. M., Németh, D. D., Hooker, D. C. and Van Eerd, L. L. 2014. Soil organic carbon and land use: Processes and potential in Ontario’s long-term agro-ecosystem research sites. Can. J. Soil Sci. 94: 317–336. Soil organic carbon (SOC) is crucial for maintaining a productive agro-ecosystem. Long-term research must be synthesized to understand the effects of land management on SOC storage and to develop best practices to prevent soil degradation. Therefore, this review compiled an inventory … Show more

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Cited by 26 publications
(7 citation statements)
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“…Correspondingly, a global meta-analysis showed NT had 48 g C m (2 yr (1 greater C than CT (West and Post 2002). Likewise, a recent meta-analysis of Ontario long-term tillage trials, which included both 1991 and 1995 long-term Ridgetown sites showed at all depths evaluated (0Á10, 0Á20, and 0Á45 cm) greater SOC storage with NT than CT systems by 6.9 g C m (2 yr (1 in the 0-to 45-cm depth (Congreves et al 2014).…”
Section: Tillage Systemsmentioning
confidence: 92%
“…Correspondingly, a global meta-analysis showed NT had 48 g C m (2 yr (1 greater C than CT (West and Post 2002). Likewise, a recent meta-analysis of Ontario long-term tillage trials, which included both 1991 and 1995 long-term Ridgetown sites showed at all depths evaluated (0Á10, 0Á20, and 0Á45 cm) greater SOC storage with NT than CT systems by 6.9 g C m (2 yr (1 in the 0-to 45-cm depth (Congreves et al 2014).…”
Section: Tillage Systemsmentioning
confidence: 92%
“…The soil organic matter concentration was not significantly affected by soil tillage or rotation system even after 6 yr of study (data not shown). The duration of the experiment might have been too short to see any effect on the soil organic matter concentration (Congreves et al, 2014). In the cold climate of Finland, Sheehy et al (2015) reported no effect after 9 to 11 yr of RT on soil organic matter concentration in the 0-to 20-cm depth in small cereals but a general redistribution of the C pool into macro-aggregate fractions.…”
Section: Soil Aggregation and Organic Mattermentioning
confidence: 97%
“…Exceptions to this tillage regime were in 1) CCSW and CCSWrc, which were disced rather than ploughed in advance of winter wheat, 2) CCAA, which was not tilled following the establishment of first-year alfalfa, and 3) AA, which was ploughed every four years. Alfalfa-based rotations received slightly less frequent tillage than corn-based rotations, however, in a review of this site tillage did not decrease SOC stocks in the top 20 cm (Congreves et al 2014). We therefore expect effects of slightly reduced tillage frequency to be moderate at most, but nevertheless interpret differences in soil health indices between the rotations in light of multiple possible drivers, focusing on the four main drivers outlined in the introduction.…”
Section: Field Site and Soil Samplingmentioning
confidence: 83%
“…Similarly, reducing tillage frequency from twice to once yearly had no statistically significant effect on SOC stocks in dryland Mollisols (Sainju et al 2007). Soils at the research site were Luvisols, and while assessments of tillage frequency effects on this soil type are infrequent, a review of tillage effects show that tillage slightly increased SOC stocks in the top 20 cm (Congreves et al 2014). Thus, given available comparisons, we consider that reductions in tillage frequency under AA and CCAA may explain a portion of the increase in SOC and MWD relative to, e.g., CCSS, but we find it unlikely that increases in soil characteristics documented here from AA to CCSS in terms of aggregate MWD (38% higher in AA) and SOC (37% higher in AA) were attributable only to tillage frequency rather than to C input quantity or quality.…”
Section: Carbon Input Quantity and Quality As Mediators Of Soc Levelsmentioning
confidence: 99%