Abstract
No-till (NT) and reduced tillage (RT) treatments can potentially enhance soil organic carbon (SOC) stabilization and soil aggregation. The turnover rate of SOC is affected by soil aggregate stability and the distribution of SOC across different aggregate-associated soil fractions. Carbon turnover rate slows down when soil aggregation increases and C is protected within stable microaggregates (53–250 μm). We studied the long-term (~10 yrs) effect of NT and RT practice on SOC stabilization in four soils typical for the boreal region. Distribution of SOC in different soil fractions was analyzed by wet sieving and further isolating microaggregates (mM) from large (>2000 μm, LM) and small (250–2000 μm, sM) macroaggregates. Aggregate stability decreased in the order of NT > RT > CT at all study sites. A general trend of redistribution of SOC was found at all study sites, i.e., the LM fraction gained SOC whereas the sM fraction lost SOC under NT compared to CT, while three out of the four sites did not show any significant changes in total SOC content under NT compared to CT. Our results show no increase in the amount of mM fraction in NT practice. On the other hand, our hypothesis that there would be more SOC incorporated in mM fraction in NT and RT treatments compared to CT practice was corroborated at three of the four study sites. Overall, our results indicate that the potential to accumulate SOC under NT or RT compared to CT is limited in boreal agroecosystems.
Highlights
The increasing amount of CO concentration in the 2 atmosphere has led to an increased interest in mitigating greenhouse gas emissions while maintaining sustainable agricultural production
The amount of macroaggregates (M) was higher in NT compared to CT treatment at all study sites but a statistically significant difference was only found at site 4 (p=0.000)
Small macroaggregates were the dominant physical fractions at sites 2 and 3 where small macroaggregates (sM) fraction was more than half of the sample size (53% and 55%, respectively), whereas free microaggregates dominated at sites 1 and 4 occupying 47% and 65% of the soils, respectively
Summary
The increasing amount of CO concentration in the 2 atmosphere has led to an increased interest in mitigating greenhouse gas emissions while maintaining sustainable agricultural production. The amount of CO released to the atmosphere from agricultural soils is mainly dependent on the rate of soil organic carbon (SOC) formation versus decomposition [1] This key role in the soil-atmosphere carbon cycling makes preservation of SOC an essential component of sustainable cropping systems. Minimum tillage practices, including no-till (NT) and reduced tillage (RT) practices, have received attention due to their ability to increase C sequestration in agricultural soils by increasing aggregate stability [2]. This has been found especially in the tropics [3, 4] and temperate regions of the world [5]. The objectives of this study are to gain better understanding about the changes in the soil C dynamics
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