4.7 Article

Protection of soil carbon by microaggregates within earthworm casts

Journal

SOIL BIOLOGY & BIOCHEMISTRY
Volume 37, Issue 2, Pages 251-258

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2004.07.035

Keywords

aggregation; microaggregates; carbon; earthworms; carbon protection

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Earthworms are known to play a role in aggregate formation and soil organic matter (SOM) protection. However, it is Still unclear at what scale and how quickly earthworms manage to protect SOM. We investigated the effects of Aporrectodea caliginosa on aggregation and aggregate-associated C pools using C-13-labeled sorghum (Sorghum bicolor (L.) Moench) leaf residue. Two incubations were set up. The first incubation consisted of soil samples crushed <250 mum to break up all macroaggregates with three treatments: (i) control Soil; (ii) Soil + C-13- labeled residue and (iii) soil + C-13-labeled residue + earthworms. Earthworms were added after 8 d and 12 d (days) later, aggregate size distribution was measured together with total C and C-13 in each aggregate fraction. A second incubation was made to assay protected versus unprotected total C and 13C from 21-d laboratory incubations of intact and crushed large (>2000 pm) and small (250-2000 mum) macroaggregates and microaggregates (53-250 mum). Eight different pools of aggregate-associated C were quantified: (1) and (2) unprotected C pools in large and small macroaggregates, (3) unprotected C pools in microaggregates, (4) and (5) protected C pools in large and small macroaggregates, (6) protected C pool in microaggregates, and (7) and (8) protected C pools in microaggregates within large and small macroaggregates. In the presence of earthworms, a higher proportion of large macroaggregates was newly formed and these aggregates contained more C and C-13 compared to bulk soil. There were no significant differences between the samples with or without earthworms in the C pool-sizes protected by macroaggregates, microaggregates or microaggregates within small macroaggregates. However, in the presence of earthworms, the C protected by microaggregates within large macroaggregates was a significant pool and 22% of this C pool was newly added C. In conclusion, these results clearly indicate the direct involvement of earthworms in providing protection of soil C in microaggregates within large macroaggregates leading to a possible long-term stabilization of soil C. (C) 2004, Elsevier Ltd. All rights reserved.

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