Tillage practices and water erosion are the most important anthropogenic and naturalprocesses, respectively, driving soil organic C turnover in agricultural land. The aimof this study was to explore the responses of soil organic C (SOC) turnover to tillageand runoff by comparing the variation of soil aggregate-associated organic C (AOC)and intra-aggregate particulate organic C (iPOC) under simulated tillage and runoffconditions. Soil samples were collected from a native vegetation land with no culti-vation history in the Mollisol region of Northeast China. After a series of simulatedtillage (ST) and simulated runoff (SR) treatments, the samples were incubated for30 d and then separated through 2-, 1-, 0.25-, and 0.053-mm sieves by wet-sieving toobtain different aggregate size fractions. Each aggregate fraction was subsequentlyshaken for 18 h in 0.5% hexametaphosphate to get different intra-aggregate particlesize fractions. The proportion of the fractions and their AOC and iPOC were deter-mined. The ST treatment promoted the reaggregation of macroaggregates (>2 mm)by accelerating the turnover of their coarse iPOC (0.25–2 mm), leading to a lowerconcentration of AOC. Runoff transformed larger aggregates (>0.25 mm) to smallerparticles (<0.25 mm) without catalyzing C turnover. Fine iPOC (0.053–0.25 mm)could serve as an indicator for AOC (>1 mm) dynamics, especially associated withtillage operations. Our findings highlight the different influences of tillage and runoff,and the negative effect of tillage on SOC dynamics.
Affiliations
Northeast Forestry University
Citations
APA
Chicago
FWB
Li, L., Wang, E., Cao, W., Zhao, P., Lin, L., Zhai, G., & Cruse, R. M. (2022). Dynamics of soil aggregate‐associated carbon as influenced by simulated tillage and runoff. Soil Science Society of America Journal, 86(6), 1457-1469. https://doi.org/10.1002/saj2.20460 (Original work published 2022)