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Soil Carbon pp 197–207Cite as

Storage of Total and Labile Soil Carbon Fractions Under Different Land-Use Types: A Laboratory Incubation Study

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Part of the book series: Progress in Soil Science ((PROSOIL))

Abstract

We studied the effect of different land uses (woodland, grassland and arable land) in two depths of a temperate silt-rich Typic Hapludalf on the storage of total organic C (TOC), readily oxidizable C (ROC), hot water-Extractable C (HWC), and cold water-Extractable C (CWC) fractions in bulk soil (<2 mm) and macroaggregates fractionated into small (1–2 mm), medium (2–4 mm) and large (5–8 mm) classes. A 120-day incubation was conducted to measure depletion of all C fractions. The highest C concentrations were associated with the macroaggregate-size classes but stored within the 1–2 mm aggregates for each of the soils. TOC and ROC concentrations depletion ranged from 1 to 14 % across the land uses throughout the incubation period. However, the concentrations of labile fractions (HWC; CWC) declined significantly during the incubation by 40–59 % and 3–35 % for the topsoil and subsoil respectively. This suggests that C fluxes are largely controlled by the highly bio-reactive labile fractions. Consequently, labile C is a promising measure for detecting changes in TOC following land use change. Woodland contained three to four times more TOC than grassland and arable land soils. Cultivation reduced C storage of this soil by >70 %.

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Correspondence to Shade J. Akinsete .

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Akinsete, S.J., Nortcliff, S. (2014). Storage of Total and Labile Soil Carbon Fractions Under Different Land-Use Types: A Laboratory Incubation Study. In: Hartemink, A., McSweeney, K. (eds) Soil Carbon. Progress in Soil Science. Springer, Cham. https://doi.org/10.1007/978-3-319-04084-4_21

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