Soil factors affecting the sustainability and productivity of perennial and annual pastures in the high rainfall zone of south-eastern Australia

Citation
Re. White et al., Soil factors affecting the sustainability and productivity of perennial and annual pastures in the high rainfall zone of south-eastern Australia, AUST J EX A, 40(2), 2000, pp. 267-283
Citations number
50
Categorie Soggetti
Agriculture/Agronomy
Journal title
AUSTRALIAN JOURNAL OF EXPERIMENTAL AGRICULTURE
ISSN journal
08161089 → ACNP
Volume
40
Issue
2
Year of publication
2000
Pages
267 - 283
Database
ISI
SICI code
0816-1089(2000)40:2<267:SFATSA>2.0.ZU;2-B
Abstract
A field study was carried out in the high rainfall zone (HRZ, >600 mm p.a.) of southern Australia from March 1994 to August 1997 to test the hypothesi s that sown perennial grasses and liming could make the existing pastures m ore sustainable through better use of water and nitrogen. The site, on an a cid duplex soil at Book Book near Wagga Wagga in southern New South Wales, was typical of much of the HRZ grazing country in southern New South Wales and north-east Victoria. The experiment consisted of 4 replicate paddocks ( each 0.135 ha) of 4 treatments: annual pasture (mainly ryegrass Lolium rigi dum, silver grass Vulpia spp., subterranean clover Trifolium subterraneum a nd broadleaf weeds) without lime, annual pasture with lime, perennial pastu re (phalaris Phalaris aquatica, cocksfoot Dactylis glomerata and subterrane an clover T. subterraneum) without lime, and perennial pasture with lime. S oil pH (0-10 cm) in the limed treatments was maintained at 5.5 (0.01 mol/L CaCl2), compared to 4.1 in the unlimed treatments. The pastures were rotati onally grazed with Merino ewe or wether hoggets at a stocking rate which va ried with the season, but was 10-25% higher on the limed pastures [14.8-17. 3 dry sheep equivalent (dse)/ha] than the unlimed pastures. One replicate s et of pasture treatments was intensively monitored for surface runoff, subs urface flow (at the top of the B horizon), water potential gradients and am monium volatilisation. Other measurements of nitrogen inputs, transformatio ns and losses were made on all paddocks. In a normal to wet year, surface runoff, subsurface flow and deep drainage (>180 cm depth) were about 40 mm less from the perennial than the annual pa stures. The reduction in deep drainage under the perennials was about one-t hird to one-half (20-29 mm/year). The smaller loss of solution NO3- from th e perennial pastures (up to 12 kg N/ha.year) suggested soil acidification u nder perennials was reduced by about 1 kmol H+/ha.year. Denitrification and volatilisation losses of N were small (1-12 kg N/ha.year). Nitrogen fixed by subterranean clover (above ground parts) ranged from 2-8 kg N/ha in the drought of 1994-95 to 128 kg N/ha in a normal year (1996). The soil-pasture nitrogen balance was positive for all treatments and averaged 76 kg N/ha.y ear over 2 years. The abundance of introduced and native earthworms increased from 85 to 250/ m(2) in the limed pastures between 1994 and 1997. Introduced species, such as Aporrectodea trapezoides, were especially responsive to lime. Animal pro duction per hectare was 10-25% higher on pastures with lime. Critical gross margins per dse were lowest ($16/ha) for a long-lived perennial pasture (> 15 years), and highest ($20/ha) for a short-lived perennial (5 years). Over all, there were substantial benefits in animal production, improved soil qu ality and water use from establishing perennial grass pastures with lime on these strongly acid soils.