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Objectives
Background
Earthworms are an integral part of sustainable farming systems. They have considerable impact on soil through their feeding, burrowing and casting activities. To effectively manage farming systems, it is essential that the role of earthworms in carbon dynamics is established and quantified.
Research
Earthworms were confined in containers filled with soil moistened to -10 kPa, compared to field bulk density and amended with 14 C-labelled plant materials. They were incubated within 1 L sealed glass jars at 16°C and the 14 CO 2 and 12 CO 2 released monitored. At the beginning and end of the incubation microbial biomass and distribution of microaggregates were measured .
Outcome
Under the experimental conditions, earthworms did
not increase the rate of decomposition of high C/N ratio, wheat
residues or low C/N ratio legume residues on the soil surface
or incorporated into the soil. Earthworms did, however, significantly
increase the decomposition of 'native' soil organic matter, with
A. rosea being more effective than A. trapezoides.
This was accompanied by a decrease in silt-sized aggregates in many soils. Some soils were more susceptible to aggregate breakdown than others but no correlation could be found between soil properties and susceptibility to microaggregate breakdown.
Implications
Although this was only a laboratory experiment, implications
are that earthworms have little overall effect on residue decomposition
under optimal moisture conditions but may have a negative effect
on soil microstructure in certain soil types.
RIRDC Project No: CSO-1A
RESEARCHERS: Morris Amato and Jan O Skjemstad
ORGANISATION: CSIRO Division of Soils
Private Bag No. 2 GLEN OSMOND SA 5064PHONE: 08 303 8531 or 08 303 8427
FAX: 08 303 8550
Last updated: 10 October 1996
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