Fukumasu J., Poeplau C., Coucheney E., Jarvis N., Klöffel T., Köstel J. K., Kätterer T., Svensson D. N., Wetterlind J., Larsbo M.
Oxalate-extractable aluminum alongside carbon inputs may be a major determinant for organic carbon content in agricultural topsoils in humid continental climate.
The relative importance of various soil mineral constituents (e.g. clay-sized particles, aluminum- and ironbearing
mineral reactive phases) in protecting soil organic carbon (SOC) from decomposition is not yet fully
understood in arable soils formed from quaternary deposits in humid continental climates. In this study, we
investigated the relationships between soil physico-chemical properties (i.e. contents of oxalate-extractable
aluminum (Alox) and iron (Feox) and clay size particle < 2 μm), grain yield (as a proxy for carbon input) and
total SOC as well as SOC in different soil fractions for samples taken from the topsoil of an arable field at Bjertorp
in south-west Sweden. We found a positive correlation between Alox and total SOC content, where Alox
explained ca. 48% of the spatial variation in SOC. We also found that ca. 80% of SOC was stored in silt- and claysized
(SC) fractions, where Al-bearing reactive mineral phases (estimated by Alox) may be important for organicmineral
associations and clay aggregation. Our results were supported by data collated from the literature for
arable topsoil in similar climates, which also showed positive correlations between SOC and Alox contents (R2 =
23.1 – 74.5%). Multiple linear regression showed that including spatially-variable crop yields as a proxy for
carbon inputs improved the prediction of SOC variation across the Bjertorp field. Other unquantified soil
properties such as exchangeable calcium may account for the remaining unexplained variation in topsoil SOC.
We conclude that Al-bearing reactive mineral phases are more important than clay content and Fe-bearing
reactive mineral phases for SOC stabilization in arable topsoil in humid continental climates.