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RESEARCH ARTICLE
Contents Vol 43(2)

Total soil organic matter and its labile pools following mulga (Acacia aneura) clearing for pasture development and cropping. 2. Total and labile nitrogen

R. C. Dalal A B D , B. P. Harms A B , E. Krull A C , W. J. Wang A B and N. J. Mathers A B
+ Author Affiliations
- Author Affiliations

A CRC for Greenhouse Accounting.

B Department of Natural Resources and Mines, Indooroopilly, Qld 4068, Australia.

C CSIRO Land and Water, Glen Osmond, SA 5064, Australia.

D Corresponding author. Email: Ram.Dalal@nrm.qld.gov.au

Australian Journal of Soil Research 43(2) 179-187 https://doi.org/10.1071/SR04076
Submitted: 16 June 2004  Accepted: 10 November 2004   Published: 1 April 2005

Abstract

Mulga (Acacia aneura) woodlands and open forests occupy about 150 Mha in Australia, and originally occupied 11.2 Mha in Queensland. Substantial areas (1.3 Mha) of the mulga vegetation have been cleared in Queensland, mostly for pasture production, but some areas are also used for cereal cropping. Twenty years after mulga clearing we found a significant loss of total soil organic C (28–35% from the 0–0.05 m depth) and light fraction C (>50% from the 0–1 m depth) from soil under pasture and cropping at a site in southern Queensland. We report here the changes in soil N and labile N pools in a paired-site study following conversion of mulga to buffel pasture (Cenchrus ciliaris) and cereal (mostly wheat) cropping for more than 20 years.

Conversion from mulga forest to pasture and cultivation resulted in greater losses of soil N than organic C in the top 0.1 m depths. As a result, C/N ratios in soil under both pasture and cropping were higher than soil under mulga, indicating a decline in soil organic matter quality after mulga clearing. Although land-use change had no significant effect on 15N natural abundance (δ15N) values of total soil N down to a depth of 1 m, δ15N values of wheat tops and roots indicated that the primary source of N under cropping was soil organic N, while that of buffel pasture was a mixed source of soil N and decomposed litter and root N. Light fraction N (<1.6 Mg/m3) declined by 60–70% throughout the 1 m soil profile under pasture and cropping, but it was 15N-enriched in these 2 land-use systems. The δ15N values of mulga phyllodes, twigs, and fine roots, indicated an input of atmospheric fixed N2 that was estimated to be about 25 kg N/ha.year. However, the source and magnitude of this N resource needs to be confirmed.

Soil N losses were estimated to be 12 kg N/ha.year under pasture and 17 kg N/ha.year under cropping over a 20-year period. These findings raise the issue of the long-term sustainable use of cleared mulga areas for pasture and/or cropping. The labile C and N pools and N mineralised also declined, which would have an immediate adverse effect on soil fertility and plant productivity of cleared Mulga Lands, as well as reducing their potential as a soil sink for greenhouse gases.

Additional keywords: soil N loss, δ15N, labile N, mineralisable N, N2 fixation.


Acknowledgments

We thank Ian Hill of ‘Mulga View’, St George, for his permission to access the site, Bruce Scriven for providing the past history of the site, and Rory Whitehead, Christine McCallum and Analytical Services staff for their technical assistance, Kamal Sangha for statistical analysis, Rene Diocares for δ15N analysis of ironbark leaves, and John Raison, Roger Gifford, and Jeff Baldock for their suggestions.


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